Content:

ST – Solar-Terrestrial Sciences

ST1.1 – Open Session on the Sun and Heliosphere

EGU2020-1654 | Displays | ST1.1

Electric-current Neutralization and Eruptive Activity of Solar Active Regions

Tibor Torok, Yang Liu, James E. Leake, Xudong Sun, and Viacheslav S. Titov

The physical conditions that determine the eruptive activity of solar active regions (ARs) are still not well understood. Various proxies for predicting eruptive activity have been suggested, with relatively limited success. Moreover, it is presently unclear under which conditions an eruption will remain confined to the low corona or produce a coronal mass ejection (CME).

Using vector magnetogram data from SDO/HMI, we investigate the association between electric-current neutralization and eruptive activity for a sample of ARs. We find that the vast majority of CME-producing ARs are characterized by a strongly non-neutralized total current, while the total current in ARs that do not produce CMEs is almost perfectly neutralized, even if those ARs produce strong (X-class) confined flares. This suggests that the degree of current neutralization can serve as a good proxy for assessing the ability of ARs to produce CMEs. 

 

How to cite: Torok, T., Liu, Y., Leake, J. E., Sun, X., and Titov, V. S.: Electric-current Neutralization and Eruptive Activity of Solar Active Regions, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1654, https://doi.org/10.5194/egusphere-egu2020-1654, 2020.

EGU2020-1777 | Displays | ST1.1

Observation-based modelling of magnetised CMEs in the inner heliosphere with EUHFORIA

Camilla Scolini, Jens Pomoell, Emmanuel Chané, Stefaan Poedts, Luciano Rodriguez, Emilia Kilpua, Manuela Temmer, Christine Verbeke, Karin Dissauer, Astrid Veronig, Erika Palmerio, and Mateja Dumbović

Coronal Mass Ejections (CMEs) are the primary source of strong space weather disturbances at Earth and other locations in the heliosphere. Understanding the physical processes involved in their formation at the Sun, propagation in the heliosphere, and impact on planetary bodies is therefore critical to improve current space weather predictions throughout the heliosphere. The capability of CMEs to drive strong space weather disturbances at Earth and other planetary and spacecraft locations primarily depends on their dynamic pressure, internal magnetic field strength, and magnetic field orientation at the impact location. In addition, phenomena such as the interaction with the solar wind and other solar transients along the way, or the pre-conditioning of interplanetary space due to the passage of previous CMEs, can significantly modify the properties of individual CMEs and alter their ultimate space weather impact. Investigating and modeling such phenomena via advanced physics-based heliospheric models is therefore crucial to improve the space weather prediction capabilities in relation to both single and complex CME events. 

In this talk, we present our progress in developing novel methods to model CMEs in the inner heliosphere using the EUHFORIA MHD model in combination with remote-sensing solar observations. We discuss the various observational techniques that can be used to constrain the initial CME parameters for EUHFORIA simulations. We present current efforts in developing more realistic magnetised CME models aimed at describing their internal magnetic structure in a more realistic fashion. We show how the combination of these two approaches allows the investigation of CME propagation and evolution throughout the heliosphere to a higher level of detail, and results in significantly improved predictions of CME impact at Earth and other locations in the heliosphere. Finally, we discuss current limitations and future improvements in the context of studying space weather events throughout the heliosphere.

How to cite: Scolini, C., Pomoell, J., Chané, E., Poedts, S., Rodriguez, L., Kilpua, E., Temmer, M., Verbeke, C., Dissauer, K., Veronig, A., Palmerio, E., and Dumbović, M.: Observation-based modelling of magnetised CMEs in the inner heliosphere with EUHFORIA, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1777, https://doi.org/10.5194/egusphere-egu2020-1777, 2020.

The Interstellar Boundary Explorer (IBEX) was launched in 2008 and has now returned observations over a full 11-year solar cycle (Solar Cycle 24). IBEX remotely images global ion distributions via charge exchange Energetic Neutral Atoms (ENAs) propagating inward from the heliosheath – the region between the termination shock and heliopause – and beyond. These observations have led to numerous discoveries about the outer heliosphere and its interaction with the surrounding interstellar medium. Heliospheric ENAs arise largely from two sources: the IBEX Ribbon, which is likely generated beyond the heliopause, in the very local interstellar medium, and the globally distributed flux (GDF), which is primarily produced in the heliosheath. In this talk we summarize some of the critical advances driven by IBEX observations. We also examine how the heliosphere and its interstellar interaction have evolved over the past solar cycle. For most of IBEX’s 11 years of observations, there was an overall reduction and then flattening of the ENA fluxes at all energies, consistent with a generally deflating, or shrinking, heliosphere. Over the past few years, IBEX has been observing the progressive response of the heliosphere to a large persistent increase in the solar wind output that passed 1 AU in the second half of 2014. This enhancement arrived at the outer heliosphere as indicated by an increase in the ENAs returning from the closest region of the inner heliosheath, south of the upwind direction, starting in the second half of 2016. Since then, the region of enhanced ENA emissions has expanded progressively outward from there, exposing increasingly further away regions of the heliosheath. IBEX observations over the past 11-years have led to a true scientific revolution in our understanding of the outer heliosphere and its interstellar interaction.

How to cite: McComas, D.: A Solar Cycle of Observations with the Interstellar Boundary Explorer (IBEX), EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5536, https://doi.org/10.5194/egusphere-egu2020-5536, 2020.

EGU2020-2069 | Displays | ST1.1 | Hannes Alfvén Medal Lecture

Magnetospheric Response to Solar Wind Forcing -ULF Wave - Particle interaction Perspective

Qiugang Zong

Sudden changes in solar wind forcing, e.g., those associated with interplanetary shocks and/or solar wind dynamic pressure pulses, can cause many fundamentally important phenomena in the Earth’s magnetosphere including electromagnetic wave generation, plasma heating and energetic particle acceleration. This presentation summarizes our present understanding of the magnetospheric response to solar wind forcing in the aspects of radiation belt electrons, ring current ions and plasmaspheric plasma based on in situ spacecraft measurements, ground-based magnetometer data, MHD and kinetic simulations. 

Magnetosphere response to sudden changes in solar wind forcing, is not a “one-kick” scenario. It is found that after the impact of solar wind structures on the Earth’s magnetosphere, plasma heating and energetic particle acceleration started nearly immediately and could last for a few hours. Even a small dynamic pressure change associated with an interplanetary shock or a solar wind pressure pulse can play a non-negligible role in magnetospheric physics. The impact leads to different kinds of waves including poloidal mode ULF waves. The fast acceleration of energetic electrons in the radiation belt and energetic ions in the ring current region usually contains two steps: (1) the initial adiabatic acceleration due to the magnetospheric compression; (2) followed by the wave-particle resonant acceleration dominated by global or localized poloidal ULF waves excited at various L-shells. 

Generalized theory of drift and drift-bounce resonance with growing or decaying ULF waves  (globally distributed or localized)  has been developed to explain in situ spacecraft observations. The new wave-related observational features like distorted energy spectrum, boomerang and fishbone pitch angle distributions of radiation belt electrons, ring current ions and plasmaspheric plasma can be explained in the frame work of this generalized theory. The results showed in this presentation can be widely used in the interaction of the solar wind with other planets such as Mercury, Jupiter, Saturn, Uranus and Neptune, and other astrophysical objects with magnetic fields.

How to cite: Zong, Q.: Magnetospheric Response to Solar Wind Forcing -ULF Wave - Particle interaction Perspective , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2069, https://doi.org/10.5194/egusphere-egu2020-2069, 2020.

EGU2020-17703 | Displays | ST1.1

The Solaris Solar Polar Mission

Donald M. Hassler, Jeff Newmark, Sarah Gibson, Louise Harra, Thierry Appourchaux, Frederic Auchere, David Berghmans, Robin Colaninno, Silvano Fineschi, Laurent Gizon, Sanjay Gosain, Todd Hoeksema, Christian Kintziger, John Linker, Pierre Rochus, Jesper Schou, Nicholeen Viall, Matt West, Tom Woods, and Jean-Pierre Wuelser and the Solaris Team

The solar poles are one of the last unexplored regions of the solar system. Although Ulysses flew over the poles in the 1990s, it did not have remote sensing instruments onboard to probe the Sun’s polar magnetic field or surface/sub-surface flows.

We will discuss Solaris, a proposed Solar Polar MIDEX mission to revolutionize our understanding of the Sun by addressing fundamental questions that can only be answered from a polar vantage point. Solaris uses a Jupiter gravity assist to escape the ecliptic plane and fly over both poles of the Sun to >75 deg. inclination, obtaining the first high-latitude, multi-month-long, continuous remote-sensing solar observations. Solaris will address key outstanding, breakthrough problems in solar physics and fill holes in our scientific understanding that will not be addressed by current missions.

With focused science and a simple, elegant mission design, Solaris will also provide enabling observations for space weather research (e.g. polar view of CMEs), and stimulate future research through new unanticipated discoveries.

How to cite: Hassler, D. M., Newmark, J., Gibson, S., Harra, L., Appourchaux, T., Auchere, F., Berghmans, D., Colaninno, R., Fineschi, S., Gizon, L., Gosain, S., Hoeksema, T., Kintziger, C., Linker, J., Rochus, P., Schou, J., Viall, N., West, M., Woods, T., and Wuelser, J.-P. and the Solaris Team: The Solaris Solar Polar Mission, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-17703, https://doi.org/10.5194/egusphere-egu2020-17703, 2020.

EGU2020-22 | Displays | ST1.1

On the magnetic characteristics of magnetic holes in the solar wind between Mercury and Earth

Martin Volwerk, Charlotte Goetz, Ferdinand Plaschke, Tomas Karlsson, and Daniel Heyner

The occurrence rate of linear and pseudo magnetic holes has been determined during MESSENGER’s cruise phase starting from Earth (2005) and arriving at Mercury (2011). It is shown that the occurrence rate of linear magnetic holes, defined as a maximum of 10â—¦ rotation of the magnetic field over the hole, slowly decreases from Mercury to Earth. The pseudo magnetic holes, defined as a rotation between 10â—¦ and 45â—¦ over the hole, have mostly a constant occurrence rate, with a slight increas in front of the Earth and a decrease around the Earth. The width and depth of these structures seem to strongly differ depending on whether they are inside
or outside of Venus’s orbit.

How to cite: Volwerk, M., Goetz, C., Plaschke, F., Karlsson, T., and Heyner, D.: On the magnetic characteristics of magnetic holes in the solar wind between Mercury and Earth, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-22, https://doi.org/10.5194/egusphere-egu2020-22, 2020.

EGU2020-5379 | Displays | ST1.1

The nature and origin of moving solar radio bursts associated with coronal mass ejections

Diana Morosan, Emilia Kilpua, Erika Palmerio, Benjamin Lynch, Jens Pomoell, Rami Vainio, Minna Palmroth, and Juska Räsänen

Flares and coronal mass ejections (CMEs) from the Sun are the most powerful and spectacular explosions in the solar system, capable of releasing vast amounts of magnetic energy over relatively short periods of time. These phenomena are often associated with particle acceleration processes that are often observed directly by spacecraft here at Earth. At the Sun, there are no direct methods of measuring these particles, which is necessary to predict their origin and propagation direction through the heliosphere. However, accelerated particles, in particular fast electrons, can generate emission at radio wavelengths through various mechanisms. Here, we exploit radio observations of Type II and Type IV radio bursts that accompany CME eruptions, in particular those radio bursts that show movement with the CME expansion in the low solar corona. Using multi-wavelength analysis, reconstruction of the radio emission and CME in three dimensions, we aim to determine the sources and locations of electron acceleration responsible for the Type II and Type IV emission in relation to the CME location and propagation. Such studies are important to understand CMEs and the sources of electron acceleration to ultimately improve the lead time to these impacts here at Earth.

How to cite: Morosan, D., Kilpua, E., Palmerio, E., Lynch, B., Pomoell, J., Vainio, R., Palmroth, M., and Räsänen, J.: The nature and origin of moving solar radio bursts associated with coronal mass ejections, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5379, https://doi.org/10.5194/egusphere-egu2020-5379, 2020.

One of the mysteries of solar energetic particle (SEP) events is the compositional variability in those events that are clearly shock-related and may be called gradual events.  In particular, the reason for the enhancement of Fe with respect to O or C at high energies has been debated over the past two decades, and yet it is still unsettled.  One hypothesis relates the compositional variability with whether the CME-driven shock is quasi-parallel or quad-perpendicular near the Sun, but this may not be easily tested using remote-sensing data alone. In recent years, however, CME-driven shock waves have been modelled by fitting shock-like features in EUV and white-light images with relatively simple shapes, and in combination with magnetic field models, ir is possible to compute shock parameters at the shock surface. In this presentation, we simulate a few CMEs whose associated SEP events show widely different Fe/O, using the Alfven wave Solar Model (AWSoM) that is part of the Space Weather Modeling Framework (SWMF). We constrain the input parameters of the simulations so that the observed pre-eruption corona, eruption and CME are well-reproduced. The shock surface, across which the shock parameters are highly non-uniform, is carefully traced, and the time-dependent connectivity of the shock surface with the observer at multiple spacecraft is compared with the SEP properties including composition. We discuss how much about the compositional variability of SEP events can be learned with this technique.

How to cite: Nitta, N., Jin, M., and Cohen, C.: Understanding the Origin of Variable Compositions of Gradual Solar Energetic Particle Events by Combining Observations and Numerical Simulations, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21333, https://doi.org/10.5194/egusphere-egu2020-21333, 2020.

EGU2020-18133 | Displays | ST1.1

Comparing different types of solar flares with radio bursts detected by SMOS

Manuel Flores Soriano and Consuelo Cid

SMOS is an Earth observing satellite that is been adapted to provide full polarization observations of the Sun at 1.4 GHz 24 hours a day. Its solar radio observations from the last decade will be released to the community by the middle of this year. In this presentation we show the capabilities of SMOS as a solar radio observatory and compare some of the most relevant radio bursts with data from GOES, LASCO, SDO and RSTN. We show how SMOS responds to different kinds of solar flares depending on their x-ray flux, and the kind of mass ejection or solar dimming that they have produced, if any. In addition to this we also show the potential of SMOS as a space weather tool to monitor GNSS satellites signal fades and to provide an early warning of Earth-directed coronal mass ejections.

How to cite: Flores Soriano, M. and Cid, C.: Comparing different types of solar flares with radio bursts detected by SMOS, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18133, https://doi.org/10.5194/egusphere-egu2020-18133, 2020.

EGU2020-18173 | Displays | ST1.1

Imaging the Solar Corona during the 2015 March 20 Eclipse using LOFAR

Aoife Maria Ryan, Peter T. Gallagher, Eoin P. Carley, Diana E. Morosan, Michiel A. Brentjens, Pietro Zucca, Richard Fallows, Christian Vocks, Gottfried Mann, Frank Breitling, Jasmina Magdalenic, Alain Kerdraon, and Hamish Reid

The solar corona is a highly-structured plasma which reaches temperatures of more than ~2MK. At low radio frequencies (≤ 400 MHz), scattering and refraction of electromagnetic waves are thought to broaden sources to several arcminutes. However, exactly how source size relates to scattering due to turbulence is still subject to investigation. This is mainly due to the lack of high spatial resolution observations of the solar corona at low frequencies. Here, we use the LOw Frequency ARray (LOFAR) to observe the solar corona at 120-180 MHz using baselines of up to ~3.5 km (~1--2’) during a partial solar eclipse of 2015 March 20. We use a lunar de-occultation technique to achieve higher spatial resolution than that attainable via traditional interferometric imaging. This provides a means of studying source sizes in the corona that are smaller than the angular width of the interferometric point spread function. 

How to cite: Ryan, A. M., Gallagher, P. T., Carley, E. P., Morosan, D. E., Brentjens, M. A., Zucca, P., Fallows, R., Vocks, C., Mann, G., Breitling, F., Magdalenic, J., Kerdraon, A., and Reid, H.: Imaging the Solar Corona during the 2015 March 20 Eclipse using LOFAR, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18173, https://doi.org/10.5194/egusphere-egu2020-18173, 2020.

EGU2020-21334 | Displays | ST1.1

Interplanetary shocks as a source of sustained gamma-ray emission from the Sun

Nat Gopalswamy and Pertti Mäkelä

It has recently been shown that the sustained gamma-ray emission (SGRE) from the Sun that lasts for hours beyond the impulsive phase of the associated flare is closely related to radio emission from interplanetary shocks (Gopalswamy et al. 2019, JPhCS, 1332, 012004, 2019). This relationship supports the idea that >300 MeV protons accelerated by CME-driven shocks propagate toward the Sun, collide with chromospheric protons and produce neutral pions that promptly decay into >80 MeV gamma-rays. There have been two challenges to this idea. (i) Since the location of the shock can be halfway between the Sun and Earth at the SGRE end time, it has been suggested that magnetic mirroring will not allow the high energy protons to precipitate. (ii) Lack of correlation between the number protons involved in the production of >100 MeV gamma-rays (Ng) and the number of protons (Nsep) in the associated solar energetic particle (SEP) event has been reported. In this paper, we show that the mirror ratio problem is no different from that in flare loops where electrons and protons precipitate to produce impulsive phase emissions. We also suggest that the lack of Ng – Nsep correlation is due to two reasons: (1) Nsep is underestimated in the case of eruptions happening at large ecliptic latitudes because the high-energy protons accelerated near the nose do not reach the observer. (2) In the case of limb events, the Ng is underestimated because gamma-rays from some part of the extended gamma-ray source do not reach the observer.

How to cite: Gopalswamy, N. and Mäkelä, P.: Interplanetary shocks as a source of sustained gamma-ray emission from the Sun, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21334, https://doi.org/10.5194/egusphere-egu2020-21334, 2020.

EGU2020-3711 | Displays | ST1.1

Effects of local particle acceleration in the solar wind

Olga Khabarova, Valentina Zharkova, Qian Xia, and Olga Malandraki

Recent observational and theoretical studies have shown that there is an unaccounted population of electrons and protons accelerated locally to suprathermal energies at reconnecting current sheets (RCSs) and 3-D dynamical plasmoids or 2-D magnetic islands (MIs) in the solar wind. The findings can be summarized as following: (i) RCSs are often subject to instabilities breaking those into 3D small-scale plasmoids/blobs or 2D magnetic islands (MIs) with multiple X- and O-nullpoints; (ii) RCSs and dynamical MIs can accelerate particles up to the MeV/nuc energies; (iii) accelerated particles may form clouds expanding far from a reconnecting region; and (iv) bi-directional(or counterstreaming) strahls observed in pitch-angle distributions (PADs) of suprathermal electrons may simply represent a signature of magnetic reconnection occurring at closed IMF structures (e.g., MIs), not necessarily connected to the Sun (Zharkova & Khabarova, 2012, 2015; Zank et al. 2014, 2015; Khabarova et al. 2015, 2016, 2017; 2018; le Roux 2016, 2017, 2018, 2019; Khabarova & Zank, 2017; Adhikari et al. 2019; Xia & Zharkova, 2018, 2020; Malandraki et al. 2019; Mingalev et al. 2019). We will briefly present an overview of the effects of local ion acceleration as observed at different heliocentric distances and focus on the impact of the locally-borne population of suprathermal electrons on typical patterns of PADs. 

Suprathermal electrons with energies of ~70eV and above are observed at 1 AU as dispersionless halo and magnetic field-aligned beams of strahls. For a long time, it has been thought that both populations originate only from the solar corona. This view has consequently impacted interpretation of typical patterns of suprathermal electron PADs observed in the solar wind. We present multi-spacecraft observations of counterstreaming strahls and dropouts in PADs within a previously reported region filled with plasmoids and RCSs, comparing observed PAD features with those predicted by PIC simulations extended to heliospheric conditions. We show typical features of PADs determined by acceleration of the ambient thermal electrons up to suprathermal energies in single RCSs and dynamical plasmoids. Our study suggests that locally-accelerated suprathermal electrons co-exist with those of solar origin. Therefore, some heat flux dropout and bi-directional strahl events observed in the heliosphere can be explained by local dynamical processes involving magnetic reconnection. Possible implications of the results for the interpretation of the strahl/halo relative density change with heliocentric distance and puzzling features of suprathermal electrons observed at crossings of the heliospheric current sheet and cometary comas are also discussed.

How to cite: Khabarova, O., Zharkova, V., Xia, Q., and Malandraki, O.: Effects of local particle acceleration in the solar wind, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3711, https://doi.org/10.5194/egusphere-egu2020-3711, 2020.

EGU2020-11505 | Displays | ST1.1

MMS Observations of Ion Cyclotron Waves in the Solar Wind

Hanying Wei, Lan Jian, Daniel Gershman, and Christopher Russell

Although electromagnetic ion cyclotron waves (ICWs) have been observed in the solar wind by multiple missions at heliocentric distances from 0.3 to 1 AU, there are still open questions on the generation mechanisms for these waves. Detailed analysis of the plasma distribution is needed to examine whether these waves are possibly generated locally.

In the solar wind, there are mainly three types of ion-driven instabilities responsible for parallel-propagating ICWs: ion cyclotron instabilities driven by ion component with temperature anisotropies greater than 1, parallel firehose instabilities driven by ion temperature anisotropies smaller than 1, and ion/ion magnetosonic instabilities driven by the relative drift between two ion components. In the solar wind frame, the waves due to ion cyclotron instability have left-handed polarization, while the waves due to firehose and ion/ion magnetosonic instabilities have right-handed polarization. Depending on the wave propagation parallel or anti-parallel to the magnetic field, the wave frequencies in the spacecraft frame are Doppler shifted higher or lower even with reversed handness. With the plasma data from Magnetospheric Multiscale (MMS) mission, we can examine the possible unstable mode with dispersion analysis and check if the prediction agrees with the observed wave mode. If the plasma measurements of the local solar wind do not support the wave growth, the waves could be possibly generated remotely close to the Sun and propagate away from the source region and are also carried outward by the solar wind flow. If these waves are generated remotely closer to the Sun, the wave properties at different heliocentric distances would help us better understand their sources.

The MMS spacecraft spends long periods of its orbit in the “pristine” solar wind starting end of 2017. From the 2017 December data we find over a hundred events and 42 of them last longer than 10 minutes which are called ICW storm events, and the longest event captured lasted over 2 hours. Although only about 17 of them have the plasma data available, we can perform case studies on these events first to investigate the wave properties and possible plasma instabilities, which will help us investigate the wave generation mechanisms due to local or remote sources.

How to cite: Wei, H., Jian, L., Gershman, D., and Russell, C.: MMS Observations of Ion Cyclotron Waves in the Solar Wind, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11505, https://doi.org/10.5194/egusphere-egu2020-11505, 2020.

Magnetic helicity is a quantity describing the twist, writhe, and torsion of magnetic field lines and magnetic configurations . The concept of magnetic helicity has successfully been applied to characterize solar coronal processes. A conjecture about one approximation relation between free magnetic free energy and relative magnetic helicity in the MHD extreme state of solar corona has been proposed by using the concept of magnetic helicity conservation and Lie-Poisson mechanical structure of MHD. We use constant α force-free filed extrapolation to check out this relation. We also apply this relation to analyze the results from the simulations and observations. Such relation may be helpful to predict the solar activity like the solar flares and CMEs

How to cite: Yang, S., Buechner, J., and Zhang, H.: Relation between the magnetic free energy and relative magnetic helicity in the MHD extreme state of solar corona, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-19255, https://doi.org/10.5194/egusphere-egu2020-19255, 2020.

We study the Solar Active Region (AR) 12673 in September 2017, which is the most flare productive AR in the solar cycle 24.  Observations from Goode Solar Telescope (GST) show the strong photospheric magnetic fields (nearly 6000 G) in polarity  inversion line (PIL) and apparent photospheric twist on September 6,  the day of X9.3 flare. Corresponding to the strong twist,   upflows are observed to last one day  at the center part of that section of PIL;  down flows are observed in two ends.  Transverse velocity fields are derived from flow tracking.   Both Non-Linear Force-Free Field (NLFFF) and Non-Force-Free Field (NFFF) extrapolations are carried out and compared to trace 3-D magnetic fields in corona. Combining with EOVSA, coronal magnetic fields between 1000 and 2000 gauss are found above the flaring PIL at the height range between 8 and 4Mm, outlining the structure of a fluxrope with sheared arcade.  The above magnetic and velocity fields, as well as thermal structure of corona, provide initial condition for further data-driven MHD simulation.

How to cite: Wang, H.: Three-Dimensional Magnetic and Velocity Structures of Active Region 12673, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2234, https://doi.org/10.5194/egusphere-egu2020-2234, 2020.

EGU2020-22028 | Displays | ST1.1

Analysis of Local Regimes of Turbulence generated by 3D Magnetic Reconnection

lucia sanna and Giovanni lapenta

The process of magnetic reconnection when studied in nature or when modeled in 3D simulations differs in one key way from the standard 2D paradigmatic cartoon: it is accompanied by many fluctuations in the electromagnetic fields and plasma properties. We developed a diagnostics to study the spectrum of fluctuations in the various regions around a reconnection site. We define the regions in terms of the local value of the flux function that determines the distance from the reconnection site, with positive values in the outflow and negative values in the inflow. We find that fluctuations belong to two very different regimes depending on the local plasma beta (defined as the ratio of plasma and magnetic pressures). The first regime develops in the reconnection outflows where beta is high and it is characterized by a strong link between plasma and electromagnetic fluctuations, leading to momentum and energy exchanges via anomalous viscosity and resistivity. But there is a second, low-beta regime: it develops in the inflow and in the region around the separatrix surfaces, including the reconnection electron diffusion region itself. It is remarkable that this low-beta plasma, where the magnetic pressure dominates, remains laminar even though the electromagnetic fields are turbulent.

[1] G. Lapenta et al 2020 ApJ 888 104,

How to cite: sanna, L. and lapenta, G.: Analysis of Local Regimes of Turbulence generated by 3D Magnetic Reconnection, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-22028, https://doi.org/10.5194/egusphere-egu2020-22028, 2020.

EGU2020-18577 | Displays | ST1.1

Solar cycle variation of simple and complex active regions

Shabnam Nikbakhsh, Eija Tanskanen, Maarit Käpylä, and Thomas Hackman

Solar active regions (ARs) emerge on the Sun’s photosphere and they frequently produce flares and coronal mass ejections which are among major space weather drivers. Therefore, studying ARs can improve space weather forecast.

The Mount Wilson Classification has been used since 1919 in order to group groups ARs according to their magnetic structures. In this study, we investigated the magnetic classification of 4797 ARs and their cyclic variation, using our daily approach for the period of January 1996 to December 2018.

We show that the monthly number of the simple ARs (SARs) attained their maximum during first peak of the solar cycle, whereas more complex ARs (CARs) reached their maximum roughly two years later, during the second peak of the cycle. We also demonstrate that the total abundance of CARs is very similar during a period of four years around their maximum number. We also studied the latitudinal distributions of SARs and CAR in northern and southern solar hemispheres and show that the independent of the complexity type, the distributions are the same in both hemispheres.

Furthermore, we investigated the earlier claim of increase in number of CARs due to the decrease in ARs latitudinal band. Here we show that, contrary to this claim, CARs attained their maximum number before the latitudinal band started to decrease in both northern and southern hemispheres.

How to cite: Nikbakhsh, S., Tanskanen, E., Käpylä, M., and Hackman, T.: Solar cycle variation of simple and complex active regions, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18577, https://doi.org/10.5194/egusphere-egu2020-18577, 2020.

EGU2020-2360 | Displays | ST1.1

Continuous components of solar activity oscillation spectrum and forecasting of solar activity

Dmitry Sokoloff, Peter Frick, Rodion Stepanov, and Frank Stefani

Spectrum of solar activity oscillations contains apart from the well-known 11-year activity cycle a continuous component, which includes, in particular, quasy-biennual oscillations as well as long-term oscillations including so-called Gleisberg cycle.  We suggest to consider the mid-term solar variability in terms of statistical dynamic of fully turbulent systems, where solid arguments are required to accept an isolated dominant frequency in a continuous (smooth) spectrum. What about the timescales longer than the Schwabe cycle, we consider them as a presence of long-term memory in solar dynamo and discuss statistical test for veryication of this interpretation. Sequences for statistical long-term forecast of solar activity are discussed.

How to cite: Sokoloff, D., Frick, P., Stepanov, R., and Stefani, F.: Continuous components of solar activity oscillation spectrum and forecasting of solar activity, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2360, https://doi.org/10.5194/egusphere-egu2020-2360, 2020.

EGU2020-10225 | Displays | ST1.1

Detailed Calibration of the Off-Axis Optical Characteristics for the X-Ray Telescope onboard Hinode

Junho Shin, Takashi Sakurai, Ryouhei Kano, Yong-Jae Moon, and Yeon-Han Kim

The X-Ray Telescope (XRT) onboard the Hinode satellite has a specially designed Wolter type grazing-incidence (GI) optics with a paraboloid-hyperboloid mirror assembly to measure the solar coronal plasma of temperatures up to 10 MK with a resolution of about one arcsec. One of the main purposes of this scientific mission is to investigate the detailed mechanism of energy transfer processes from the photosphere to the upper coronal region leading to its heating and the solar wind acceleration. To theoretically model the three-dimensional coronal structures is sensitive to the values of plasma properties at the base of solar corona and thus requires beforehand accurate empirical description of those properties. Though the telescope has provided unprecedented observations of solar corona for more than a decade, due to a wide field of view of 34 x 34 arcmin covering the full Sun, the optical performance of the instrument gradually deteriorates as it goes away from the optical center. For this reason, the off-axis characteristics of Hinode/XRT should be examined with care in order to precisely interpret the coronal plasma properties near the solar limb area.

This presentation will explain the importance of accurate calibration of the optical characteristics, especially for the data taken in the off-axis region. Our previous study has shown that the scattered light caused by the XRT mirror surface roughness has a power-law distribution and also shows an energy dependence, with which the PSF profile from the core to the scattering wing has been completed. We will introduce in this study how the level of scattering wing can be determined quantitatively for each focal plane filter from in-flight data analysis. We have also evaluated the vignetting effect in Hinode/XRT by analyzing the 2D distribution of effective area in the field of view taken from MSFC/XRCF pre-launch experiment. It is revealed that, unlike the case of Yohkoh/SXT, the degree of offset of an optical center is not serious and thus shows little deviation from rotational symmetry. Also important is that the vignetting pattern in XRT shows an energy dependence, which has never been considered before for the analyses of XRT data. More interesting results on the calibration of Hinode/XRT scattered light and the correction of vignetting effect will be introduced and discussed thoroughly. 

How to cite: Shin, J., Sakurai, T., Kano, R., Moon, Y.-J., and Kim, Y.-H.: Detailed Calibration of the Off-Axis Optical Characteristics for the X-Ray Telescope onboard Hinode, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-10225, https://doi.org/10.5194/egusphere-egu2020-10225, 2020.

EGU2020-8298 | Displays | ST1.1

Solar Particle Radiation Storms Forecasting and Analysis - The HESPERIA tools

Olga Malandraki, Bernd Heber, Patrick Kuehl, Marlon Núñez, Arik Posner, Michalis Karavolos, and Nikos Milas

Solar Energetic Particles (SEPs), ranging in energy from tens of keV to a few GeV, constitute an important con-tributor to the characterization of the space environment. SEP radiation storms may have durations from a period of hours to days or even weeks and have a large range of energy spectrum profiles. They pose a threat to mod-ern technology strongly relying on spacecraft and are a serious radiation hazard to humans in space, and are additionally of concern for avionics and commercial aviation in extreme cases. The High Energy Solar Particle Events forecasting and Analysis (HESPERIA) project, supported by the HORIZON 2020 programme of the Eu-ropean Union, has furthered our prediction capability of high-energy SEP events by developing new European capabilities for SEP forecasting and warning, while exploiting novel as well as already existing datasets. The HESPERIA UMASEP-500 tool makes real-time predictions of the occurrence of >500 MeV and Ground Level Enhancement (GLE) events from the analysis of soft X-ray flux and high-energy differential proton flux measured by the GOES satellite network. Regarding the prediction of GLE events for the period 2000-2016, this tool had a Probability of Detection (POD) of 53.8% and a False Alarm Ratio (FAR) of 30.0%. For this period, the tool obtained an Advanced Warning Time (AWT) of 8 min taking as reference the alert time from the first NMstation; using the time of the warning issued by the GLE Alert Plus tool for the aforementioned period as reference, the tool obtained an AWT of 15 min (Núñez et al. 2017). Based on the Relativistic Electron Alert System for Exploration (REleASE) forecasting scheme (Posner, 2007), the HESPERIA REleASE tools generate real-time predictions of the proton flux (30-50 MeV) at the Lagrangian point L1, making use of relativistic electrons (v>0.9c) and near-relativistic (v<0.8c) electron measurements provided by the SOHO/EPHIN and ACE/EPAM experiments, respectively. Analysis of historic data from 2009 to 2016 has shown the HESPERIA REleASE tools have a low FAR (∼30%) and a high POD (63%). Both HESPERIA tools are operational through the project’s website (http://www.hesperia.astro.noa.gr) at the National Observatory of Athens and presented in the recently published book on 'Solar Particle Radiation Storms Forecasting and Analysis, The HESPERIA HORIZON 2020 Project and Beyond', edited by Malandraki and Crosby, Springer, Astrophysics and Space Sciences Library, 2018, freely available at https://www.springer.com/de/book/9783319600505. The HESPERIA tools have been selected as a top priority internationally by NASA/CCMC to be included in the simulations of the manned-mission to Mars by Johnson Space Center (ISEP project). The National Observatory of Athens participates in the ISEP project with a relevant contract.

How to cite: Malandraki, O., Heber, B., Kuehl, P., Núñez, M., Posner, A., Karavolos, M., and Milas, N.: Solar Particle Radiation Storms Forecasting and Analysis - The HESPERIA tools , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-8298, https://doi.org/10.5194/egusphere-egu2020-8298, 2020.

EGU2020-5259 | Displays | ST1.1

EUHFORIA in the ESA Virtual Space Weather Modelling Centre

Stefaan Poedts

The goal of the ESA project "Virtual Space Weather Modelling Centre - Part 3" (2019-2021) is to further develop the Virtual Space Weather Modelling Centre (VSWMC), building on the Part 2 prototype system and focusing on the interaction with the ESA SSA SWE system. A first, limited version went operational in May 2019 under the H-ESC umbrella on the ESA SSA SWE Portal. The objective and scopes of this new project include: the efficient integration of new models and new model couplings, including daily automated end-to-end (Sun to Earth) simulations, the further development and wider use of the coupling toolkit  and front-end GUI, making the operational system more robust and user-friendly. The VSWMC-Part 3 project started on 1 October 2019.

EUHFORIA (‘European heliospheric forecasting information asset’) is integrated in the VSWMC and will be upgraded with alternative coronal models (Multi-VP and Wind-Predict) and flux-rope CME models, and new couplings will be made available, e.g. to more advanced magnetospheric models and radiation belt models, geo-effects models, and even SEP models. The first results will be discussed and put into perspective.

How to cite: Poedts, S.: EUHFORIA in the ESA Virtual Space Weather Modelling Centre, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5259, https://doi.org/10.5194/egusphere-egu2020-5259, 2020.

So far, most studies on the structure of coronal mass ejections (CMEs) are conducted through white-light coronagraphs, which demonstrate about one third of CMEs exhibit the typical three-part structure in the high corona (e.g., beyond 2 Rs), i.e., the bright front, the dark cavity and the bright core. In this presentation, we address the CME structure in the low corona (e.g., below 1.3 Rs) through extreme-ultraviolet (EUV) passbands and find that the three-part CMEs in the white-light images can possess a similar three-part appearance in the EUV images, i.e., a leading edge, a low-density zone, and a filament or hot channel. The analyses identify that the leading edge and the filament or hot channel in the EUV passbands evolve into the front and the core later within several solar radii in the white-light passbands, respectively. What's more, we find that the CMEs without obvious cavity in the white-light images can also exhibit the clear three-part appearance in the EUV images, which means that the low-density zone in the EUV images (observed as the cavity in white-light images) can be compressed and/or transformed gradually by the expansion of the bright core and/or the reconnection of magnetic field surrounding the core during the CME propagation outward. Our study suggests that more CMEs can possess the clear three-part structure in their early eruption stage. The nature of the low-density zone between the leading edge and the filament or hot channel is discussed.

How to cite: Song, H.: The Structure of Solar Coronal Mass Ejections in the Extreme-Ultraviolet Passbands, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4293, https://doi.org/10.5194/egusphere-egu2020-4293, 2020.

EGU2020-19496 | Displays | ST1.1

Segmentation of coronal features to understand the solar EIV and UV irradiance variability

Joe Zender, Rens van der Zwaart, Rangaiah Kariyappa, Luc Damé, and Gabriel Giono

The study of solar irradiance variability is of great importance in heliophysics, the Earth’s climate, and space weather applications. These studies require careful identifying, tracking and monitoring of features in the solar magnetosphere, chromosphere, and corona.  We studied the variability of solar irradiance for a period of 10 years (May 2010–January 2020) using the Large Yield Radiometer (LYRA), the Sun Watcher using APS and image Processing (SWAP) on board PROBA2, the Atmospheric Imaging Assembly (AIA), and the Helioseismic and Magnetic Imager (HMI) of on board the Solar Dynamics Observatory (SDO), and applied a linear model between the identified features and the measured solar irradiance by LYRA.

We used the spatial possibilistic clustering algorithm (SPoCA) to identify coronal holes, and a morphological feature detection algorithm to identify active regions (AR), coronal bright points (BPS), and the quite sun (QS) and segment coronal features from the EUV observations of AIA. The AIA segmentation maps were then applied on SWAP images, images of all AIA wavelengths, HMI line-of-sight (LOS) magnetograms, and parameters such as the intensity, fractional area, and contribution of ARs/CHs/BPs/QS features were computed and compared with LYRA irradiance measurements as a proxy for ultraviolet irradiation incident to the Earth atmosphere.

We modelled the relation between the solar disk features (ARs, CHs, BPs, and QS) applied to magnetrogram and EUV images against the solar irradiance as measured by LYRA and the F10.7 radio flux. To avoid correlation between different the segmented features, a principal component analysis (PCM) was done. Using the independent component, a straightforward linear model was used and corresponding coefficients computed using the Bayesian framework. The model selected is stable and coefficients converge well.

The application of the model to data from 2010 to 2020 indicates that both at solar cycle timeframes as well as shorter timeframes, the active region influence the EUV irradiance as measured at Earth. Our model replicates the LYRA measured irradiance well.

How to cite: Zender, J., van der Zwaart, R., Kariyappa, R., Damé, L., and Giono, G.: Segmentation of coronal features to understand the solar EIV and UV irradiance variability, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-19496, https://doi.org/10.5194/egusphere-egu2020-19496, 2020.

EGU2020-11425 | Displays | ST1.1

Evolution of the Alfvén Mach number associated with a coronal mass ejection shock

Ciara Maguire, Eoin Carley, Joseph McCauley, and Peter Gallagher

The Sun regularly produces large-scale eruptive events, such as coronal mass ejections (CMEs) that can drive shock waves through the solar corona. Such shocks can result in electron acceleration and subsequent radio emission in the form of a type II radio burst. However, the early-phase evolution of shock properties and its relationship to type II burst evolution is still subject to investigation. Here we study the evolution of a CME-driven shock by comparing three commonly used methods of calculating the Alfvén Mach number (MA), namely: shock geometry, a comparison of CME speed to a model of the coronal Alfvén speed, and the type II band-splitting method. We applied the three methods to the 2017 September 2 event, focusing on the shock wave observed in extreme ultraviolet (EUV) by the Solar Ultraviolet Imager (SUVI) on board GOES-16, in white-light by the Large Angle and Spectrometric Coronagraph (LASCO) on board SOHO, and the type II radio burst observed by the Irish Low Frequency Array (I-LOFAR). We show that the three different methods of estimating shock MA yield consistent results and provide a means of relating shock property evolution to the type II emission duration. The type II radio emission emerged from near the nose of the CME when MA was in the range 1.4-2.4 at a heliocentric distance of 1.6 R. The emission ceased when the CME nose reached 2.4 R, despite an increasing Alfvén Mach number (up to 4). We suggest the radio emission cessation is due to the lack of quasi-perpendicular geometry at this altitude, which inhibits efficient electron acceleration and subsequent radio emission.

How to cite: Maguire, C., Carley, E., McCauley, J., and Gallagher, P.: Evolution of the Alfvén Mach number associated with a coronal mass ejection shock, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11425, https://doi.org/10.5194/egusphere-egu2020-11425, 2020.

EGU2020-1501 | Displays | ST1.1

Examination of the EUV Intensity in the Open Magnetic Field Regions Associated with Coronal Holes

Guan-Han Huang, Chia-Hsien Lin, and Lou Chuang Lee

Coronal holes can be identified as the regions with magnetic field lines extending far away from the Sun, or the darkest regions in EUV/X-ray images with predominantly unipolar magnetic fields. A comparison between the locations of our determined regions with open magnetic field lines (OMF) and regions with low EUV intensity (LIR) reveals that only 12% of the OMF regions coincide with the LIRs. The aim of this study is to investigate the conditions leading to the different brightnesses of OMF regions, and to provide a means to predict whether an OMF region would be bright or dark. Examining the statistical distribution profiles of the magnetic field expansion factor (fs) and Atmospheric Imaging Assembly 193 Å intensity (I193) reveals that both profiles are approximately log-normal. The analysis of the spatial and temporal distributions of fs and I193 indicates that the bright OMF regions often are inside or next to regions with closed field lines, including quiet-Sun regions and regions with strong magnetic fields. Examining the relationship between I193 and fs reveals a weak positive correlation between log I193 and log fs , with a correlation coefficient ≈ 0.39. As a first-order approximation, the positive relationship is determined to be log I193 = 0.62 log fs + 1.51 based on the principle of the whitening/dewhitening transformation. This linear relationship is demonstrated to increase the consistency between the OMF regions and LIRs from 12% to 23%.

How to cite: Huang, G.-H., Lin, C.-H., and Lee, L. C.: Examination of the EUV Intensity in the Open Magnetic Field Regions Associated with Coronal Holes, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1501, https://doi.org/10.5194/egusphere-egu2020-1501, 2020.

EGU2020-4011 | Displays | ST1.1

On the Relation between Filament Chirality, Rotation Direction, and Morphology

Zhenjun Zhou, Rui Liu, Xing Cheng, Chaowei Jiang, Yuming Wang, Lijuan Liu, Guoqiang Wang, Tielong Zhang, and Jun Cui

Coronal mass ejections (CMEs) with enhanced south-component of the magnetic field are susceptible to producing geomagnetic storms. Filament chirality, rotation direction, and morphology are responsible for CMEs’ magnetic orientation and they are manifestations of magnetic helicity. However, different models predict different relations among them. In this paper, taking advantage of stereoscopic observations and a new method of determining the chirality of erupting filaments, we analyze 12 filaments that present a clear rotation during the eruption. The results based on the small sample support the argument that the filaments with for sinistral (dextral) chirality, they rotate clockwise (counterclock-wise), indicating the transformation of twist into writhe. Moreover, we also inspect soft X-ray and EUV hot temperature images and find that, the associated sigmoids are consistent with filaments prior to the eruption morphologically. However, once starting to rise up, the erupting filaments reverse their shapes from forward S-shaped to inversed S-shaped and vice versa.

How to cite: Zhou, Z., Liu, R., Cheng, X., Jiang, C., Wang, Y., Liu, L., Wang, G., Zhang, T., and Cui, J.: On the Relation between Filament Chirality, Rotation Direction, and Morphology, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4011, https://doi.org/10.5194/egusphere-egu2020-4011, 2020.

EGU2020-6928 | Displays | ST1.1

Magnetic flux transport in the photosphere of the Sun

Dmitrii Baranov, Elena Vernova, Marta Tyasto, and Olga Danilova

On the basis of the synoptic maps of the photospheric magnetic field obtained by the National Solar Observatory Kitt Peak for 1978-2016, a latitude-time diagram of the magnetic field was built. When averaging intensity values over the heliolongitude, the magnetic field sign was taken into account. In order to consider the characteristics of the distribution of weak magnetic fields an upper limit of 5 G was set.

The latitude-time diagram clearly shows inclined bands corresponding to positive and negative polarity magnetic flows drifting towards the poles of the Sun. Two groups of flows are observed: 1. Relatively narrow bands, with alternating polarity, beginning near the equator and reaching almost the poles of the Sun. Along the time axis, the flow length of one polarity is on the order of 1-2 years; 2. short powerful flows, 3-4.5 years wide, propagating from the spot zone to the poles. These flows reach the poles simultaneously with the begin of the polar field reversal, apparently representing  the so-called “Rush to the Poles” phenomenon.

The pattern of magnetic field transport is significantly different for the northern and southern hemispheres. Alternating flows of positive and negative polarities most clearly appear in the southern hemisphere during periods of positive polarity of the southern polar field. For the northern hemisphere the picture is much less clear but for individual time intervals alternating flows of opposite polarities can be traced. The slopes of magnetic flux bands allow us to estimate the rate of meridional drift of magnetic fields, which was slightly different for the two hemispheres: V = (16±2) m/s for the southern hemisphere and V = (21±4) m/s for the northern hemisphere. The results obtained indicate that the distribution of weak magnetic fields over the surface of the Sun has a complex structure that is different for the two hemispheres and varies from cycle to cycle.

How to cite: Baranov, D., Vernova, E., Tyasto, M., and Danilova, O.: Magnetic flux transport in the photosphere of the Sun, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6928, https://doi.org/10.5194/egusphere-egu2020-6928, 2020.

EGU2020-9247 | Displays | ST1.1

Data-driven modelling of erupting solar active regions

Daniel Price, Jens Pomoell, Erkka Lumme, and Emilia Kilpua

Fully understanding solar eruptions and their eventual consequences for the Earth requires a rigorous modelling approach due to the difficulty of directly measuring magnetic fields in the solar corona. Consequently, this study employs a time-dependent data-driven magnetofrictional model (TMFM) to simulate the coronal evolution of coronal mass ejections from multiple active regions. We processed HMI vector magnetograms with the Electric Field Inversion Toolkit to generate a time series of photospheric electric field maps which were used as the lower boundary to drive our TMFM simulations. Analysis was aided by computing maps of the squashing factor and twist, as well as by calculating coronal metrics such as the volume energy and helicity, and by comparison to AIA observations. Studying multiple events simultaneously permits comparative analysis and the evaluation of the model performance.

How to cite: Price, D., Pomoell, J., Lumme, E., and Kilpua, E.: Data-driven modelling of erupting solar active regions, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-9247, https://doi.org/10.5194/egusphere-egu2020-9247, 2020.

EGU2020-22351 | Displays | ST1.1

Quasi Periodic Oscillations in the Pre Phases of Recurrent Jets Highlighting Plasmoids in Current Sheet

Reetika Joshi, Ramesh Chandra, Brigitte Schmieder, Guillaume Aulanier, Pooja Devi, Fernando Moreno-Insertis, and Daniel Nóbrega-Siverio

Solar jets observed at the limb are important to determine the location of reconnection sites in the corona. In this study, we investigate six recurrent hot and cool jets occurring in the active region NOAA 12644 as it is crossing the west limb on April 04, 2017. These jets are observed in all the UV/EUV filters of SDO/AIA and in cooler temperature formation lines in IRIS slit jaw images. The jets are initiated at the top of a double chamber vault with cool loops on one side and hot loops on the other side. The existence of such double chamber vaults suggests the presence of emerging flux with cool loops, the hot loops being the reconnected loops similarly as in the models of Moreno-Insertiset al. 2008, 2013 and Nóbrega-Siverio et al. 2016. In the preliminary phase of the main jets, quasi periodic intensity oscillations accompanied by smaller jets are detected in the bright current sheet between the vault and the preexisting magnetic field. Individual kernels and plasmoids are ejected in open field lines along the jets. Plasmoids may launch torsional Alfven waves and the kernels would be the result of the untwist of the plasmoids in open magnetic field as proposed in the model of Wyper et al. 2016.

How to cite: Joshi, R., Chandra, R., Schmieder, B., Aulanier, G., Devi, P., Moreno-Insertis, F., and Nóbrega-Siverio, D.: Quasi Periodic Oscillations in the Pre Phases of Recurrent Jets Highlighting Plasmoids in Current Sheet, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-22351, https://doi.org/10.5194/egusphere-egu2020-22351, 2020.

EGU2020-20365 | Displays | ST1.1

Abrupt shrinking of solar corona in late 1990s and related changes in solar magnetic structure

Kalevi Mursula, Ilpo Virtanen, Jennimari Koskela, and Ismo Tähtinen

Several studies have noted on changes in the properties of sunspots, and in the mutual relations between various global parameters of solar magnetic activity (e.g. UV/EUV irradiance, radio and IR emissions, TSI/SSI), as well as between solar and ionospheric parameters since the onset of solar cycle 23. These changes have been suggested to be related to the overall reduction of solar activity at the aftermath of the decline of the Grand modern maximum of solar activity that prevailed during most of the 20th century. We have recently derived the longest record of coronal magnetic field intensities since 1968 using Mount Wilson Observatory and Wilcox Solar Observatory observations of the photospheric magnetic field and the PFSS model, and compared it with the heliospheric magnetic field observed at the Earth. We found that the time evolution of the coronal magnetic field during the last 50 years agrees with the heliospheric magnetic field only if the effective coronal size, the distance of the coronal source surface of the heliospheric magnetic field, is allowed to change in time. We calculated the optimum distance for each solar rotation and found that it experienced an abrupt decrease in the late 1990s. The effective volume of the solar corona shrunk to less than one half of its previous value during a short period of only a few years. This shrinking was related with a systematic change in the structure of the coronal magnetic field during the same time interval. We review these dramatic changes in the solar corona and discuss their possible connection to the changes in the different solar activity parameters and the reduction of the overall solar activity.

How to cite: Mursula, K., Virtanen, I., Koskela, J., and Tähtinen, I.: Abrupt shrinking of solar corona in late 1990s and related changes in solar magnetic structure, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-20365, https://doi.org/10.5194/egusphere-egu2020-20365, 2020.

EGU2020-21894 | Displays | ST1.1

Propagation of a Solar Moving Type IV Radio Burst Using LOFAR

Hongyu Liu, Pietro Zucca, Jasmina Magdalenic, Peijin Zhang, and Kyungsuk Cho

Type IV radio burst is the long-lasting broadband continuum emission in metric wave-length. In addition to the continuum emission Type IV radio bursts may show fine structure with high brightness temperature. The physical emission responsible for both continuum and fine structures is still under debate. In this study, we present a moving type IV radio burst observed by LOFAR. We performed a detailed comparison of NRH and LOFAR imaging. Using the full stokes parameterss from the LOFAR dynamic spectra, we have also calculated the degree of circular polarisation during the propagation of the moving type IV. Finally, we combined LOFAR interferometric data with SDO-AIA and LASCO-C2 to track the evolution of this type IV and relate it with the CME.

How to cite: Liu, H., Zucca, P., Magdalenic, J., Zhang, P., and Cho, K.: Propagation of a Solar Moving Type IV Radio Burst Using LOFAR, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21894, https://doi.org/10.5194/egusphere-egu2020-21894, 2020.

EGU2020-80 | Displays | ST1.1

Source size and Position of a Type IIIb-III Pair with LOFAR

Peijin Zhang, Pietro Zucca, Sarrvesh Sridhar, and Chuanbing Wang

Solar radio bursts originate mainly from high energy electrons accelerated by solar eruptions like solar flares, jets, and coronal mass ejections (CMEs).  A sub-category of solar radio bursts with a short time duration may be used as a proxy to understand the wave generation and propagation within the corona.  Complete case studies of the source size, position, and kinematics of short-term bursts are very limited due to instrumental limitations.
LOw-Frequency-ARray (LOFAR) is an advanced radio antenna array. It is capable of a variety of processing operations including correlation for standard interferometric imaging, the tied-array beam-forming, and the real-time triggering on incoming station data-streams. With recently upgraded LOFAR, we can achieve high spatial and temporal imaging for solar radio bursts.
Here we present a detailed analysis of the fine structures in the spectrum and of the radio source motion with imaging, the radio source of a type IIIb-III pair was imaged with the interferometric mode using the remote baselines of the (LOFAR). This study shows how the fundamental and harmonic components have a significant different source motion.  The apparent source of the fundamental emission at 26 MHz is about 4 times the speed of light, while the apparent source of the harmonic emission shows a speed of < 0.02 c.  We show that the apparent speed of the fundamental source is more affected by the scattering and refraction of the coronal medium.

How to cite: Zhang, P., Zucca, P., Sridhar, S., and Wang, C.: Source size and Position of a Type IIIb-III Pair with LOFAR, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-80, https://doi.org/10.5194/egusphere-egu2020-80, 2020.

EGU2020-7374 | Displays | ST1.1

Interferometric Observations of the Active Regions in Radio Domain Before and After the Total Solar Eclipse on 21 August 2017

Bartosz Dabrowski, Paweł Flisek, Christian Vocks, Diana Morosan, Peijin Zhang, Pietro Zucca, Jasmina Magdalenic, Richard Fallows, Andrzej Krankowski, Gottfried Mann, Leszek Blaszkiewicz, Pawel Rudawy, Marcin Hajduk, Adam Fron, Peter Gallagher, Aoife Maria Ryan, Kacper Kotulak, and Barbara Matyjasiak

We hereby present the interferometric LOFAR observations made before and after the total solar eclipse on 21 August 2017, during which the type III radio bursts have been detected.

The LOw-Frequency ARray (LOFAR) is a large radio interferometer operating in the frequency range of 10–240 MHz, designed and constructed by ASTRON (the Netherlands Institute for Radio Astronomy). The LOFAR telescope is an array of stations distributed throughout the Netherlands and other parts of Europe. Currently the system consist of 52 LOFAR stations located in Europe. Apart from the high time and frequency resolution of the dynamic spectra, LOFAR allows also a 2D imaging of the radio sources and tracking of their positions through the solar corona.

In this work we present a preliminary analysis of the dynamic spectra of type III radio bursts with radio images.

How to cite: Dabrowski, B., Flisek, P., Vocks, C., Morosan, D., Zhang, P., Zucca, P., Magdalenic, J., Fallows, R., Krankowski, A., Mann, G., Blaszkiewicz, L., Rudawy, P., Hajduk, M., Fron, A., Gallagher, P., Ryan, A. M., Kotulak, K., and Matyjasiak, B.: Interferometric Observations of the Active Regions in Radio Domain Before and After the Total Solar Eclipse on 21 August 2017, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7374, https://doi.org/10.5194/egusphere-egu2020-7374, 2020.

EGU2020-13366 | Displays | ST1.1

Near real time plasma irregularity monitoring by FORMOSAT-7/COSMIC-2

ShihPing Chen, Charles C. Lin, Rajesh Panthalingal Krishnanunni, Richard Eastes, and Jong-Min Choi

The near real-time global plasma bubble map is constructed by utilizing the FORMOSAT-7/COSMIC-2(F7/C2) radio occultation(RO) scintillation observations in low latitudes. Several tools investigating plasma bubbles like the rate of TEC index(ROTI), Range-Time-Intensity(RTI) diagrams of the Jicamarca Unattended Long-term Investigations of the Ionosphere and Atmosphere(JULIA), and the Global-scale Observations of the Limb and Disk(GOLD) 135.6nm airglow observations are provided validating the RO scintillations. Result shows that the F7/C2 scintillation is sensitive detecting plasma irregularities, especially for the bottom side of these bubbles, which can be used to investigating nighttime vertical plasma drifts in low latitudinal F-region. The hourly quick look of the low latitude plasma bubble occurrence and vertical ion drift around the globe is significant to the space weather monitoring.

How to cite: Chen, S., Lin, C. C., Panthalingal Krishnanunni, R., Eastes, R., and Choi, J.-M.: Near real time plasma irregularity monitoring by FORMOSAT-7/COSMIC-2, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-13366, https://doi.org/10.5194/egusphere-egu2020-13366, 2020.

EGU2020-4747 | Displays | ST1.1

Bimodal distribution of the solar wind using data from ACE spacecraft.

Carlos Larrodera and Consuelo Cid

The main goal of this work is to separate the behavior of the two types of quiet solar wind at 1 AU: fast and slow.
Our approach is a bi-Gaussian distribution function, formed by the addition of two Gaussian distribution functions, where each one represents one type of wind. We check our approach by fitting the bi-Gaussian to data from ACE spacecraft. We use level 2 data measured during solar cycles 23 and 24 of different solar wind parameters, including proton speed, proton temperature, density and magnetic field. Our results show that the approach is fine and only transient events departs from the proposed function. Moreover, we can show bi modal behavior of the solar wind at 1 AU, not only for the proton speed, but also for the other analyzed parameters. We also check the solar cycle dependence of the different fitting parameters.

How to cite: Larrodera, C. and Cid, C.: Bimodal distribution of the solar wind using data from ACE spacecraft., EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4747, https://doi.org/10.5194/egusphere-egu2020-4747, 2020.

EGU2020-19262 | Displays | ST1.1

Comparing the boundaries of interplanetary coronal mass ejections

Consuelo Cid, Carlos Larrodera, and Elena Saiz

The boundaries of interplanetary coronal mass ejections (ICMEs) are commonly established based on the magnetic field smoothness and/or the low temperature, when compared to normal solar wind. Based on the analysis of the ICME on 2015 January 6-7, observed by Wind and ACE spacecraft, Cid et al. (2016) proposed compositional signatures as the most precise diagnostic tool for the boundaries of ICMEs. Having as a starting point the ICMEs catalogues from Jian et al. (2006) and Richardson and Cane (2010), and the Wind spacecraft ICME catalogue on the NASA web site, we have compared the boundaries of all ICMEs observed by the ACE spacecraft attending to different signatures. This contribution shows the results of the study.

How to cite: Cid, C., Larrodera, C., and Saiz, E.: Comparing the boundaries of interplanetary coronal mass ejections, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-19262, https://doi.org/10.5194/egusphere-egu2020-19262, 2020.

EGU2020-21663 | Displays | ST1.1

Axial dipole moments of solar active regions in cycles 21-24

Iiro Virtanen, Ilpo Virtanen, Alexei Pevtsov, and Kalevi Mursula

The axial dipole moments of emerging active regions control the evolution of the axial dipole moment of the whole photospheric magnetic field and the strength of polar fields. Hale's and Joy's laws of polarity and tilt orientation affect the sign of the axial dipole moment of an active region, determining the normal sign for each solar cycle. If both laws are valid (or both violated), the sign of the axial moment is normal. However, for some active regions, only one of the two laws is violated, and the signs of these axial dipole moments are the opposite of normal. The opposite-sign axial dipole moments can potentially have a significant effect on the evolution of the photospheric magnetic field, including the polar fields.

We determine the axial dipole moments of active regions identified from magnetographic observations and study how the axial dipole moments of normal and opposite signs are distributed in time and latitude in solar cycles 21-24.We use active regions identified from the synoptic maps of the photospheric magnetic field measured at the National Solar Observatory (NSO) Kitt Peak (KP) observatory, the Synoptic Optical Long term Investigations of the Sun (SOLIS) vector spectromagnetograph (VSM), and the Helioseismic and Magnetic Imager (HMI) aboard the Solar Dynamics Observatory (SDO).

We find that, typically, some 30% of active regions have opposite-sign axial dipole moments in every cycle, often making more than 20% of the total axial dipole moment. Most opposite-signed moments are small, but occasional large moments, which can affect the evolution of polar fields on their own, are observed. Active regions with such a large opposite-sign moment may include only a moderate amount of total magnetic flux. We find that in cycles 21-23 the northern hemisphere activates first and shows emergence of magnetic flux over a wider latitude range, while the southern hemisphere activates later, and emergence is concentrated to lower latitudes. We also note that cycle 24 differs from cycles 21-23 in many ways. Cycle 24 is the only cycle where the northern butterfly wing includes more active regions than the southern wing, and where axial dipole moment of normal sign emerges on average later than opposite-signed axial dipole moment. The total axial dipole moment and even the average axial moment of active regions is smaller in cycle 24 than in previous cycles.

How to cite: Virtanen, I., Virtanen, I., Pevtsov, A., and Mursula, K.: Axial dipole moments of solar active regions in cycles 21-24, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21663, https://doi.org/10.5194/egusphere-egu2020-21663, 2020.

EGU2020-15185 | Displays | ST1.1

Stochastic Resonance could explain Recurrence of Grand Minima

Carlo Albert and Simone Ulzega

Proxies of solar activity have revealed repeated Grand Minima that occur with a certain regularity associated with the well-known Gleissberg and Süss/deVries cycles. These and other prominent cycles in the spectrum of solar activity are also seen in the spectrum of the planetary torque exerted on the solar tachocline, which has revived the hypothesis of a planetary influence on solar activity. It is not clear, however, how the extremely weak planetary forcing could influence the solar magnetic activity. Here, we suggest that stochastic resonance could explain the necessary amplification of the forcing and provide numerical evidence from stochastic time-delayed dynamo models. If the intrinsic noise of the solar dynamo allows for a frequent switching between active and quiescent stable states, tiny periodic forcings can be greatly amplified, provided the dynamo is poised close to a critical point. Such a forcing could be caused by a tidal modulation of the minimal magnetic field required for flux-tube buoyancy.

How to cite: Albert, C. and Ulzega, S.: Stochastic Resonance could explain Recurrence of Grand Minima, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-15185, https://doi.org/10.5194/egusphere-egu2020-15185, 2020.

ST1.2 – Multi-spacecraft Measurements in the Inner Heliosphere on Various Scales

EGU2020-13664 | Displays | ST1.2

Radial evolution of magnetic field fluctuations in an ICME sheath

Simon Good, Matti Ala-Lahti, Erika Palmerio, Emilia Kilpua, and Adnane Osmane

The sheaths of compressed solar wind that precede interplanetary coronal mass ejections (ICMEs) commonly display large-amplitude magnetic field fluctuations. As ICMEs propagate radially from the Sun, the properties of these fluctuations may evolve significantly. We present a case study of an ICME sheath observed by a pair of radially aligned spacecraft at around 0.5 and 1 AU from the Sun. Radial changes in fluctuation amplitude, compressibility, inertial-range spectral slope, permutation entropy, Jensen-Shannon complexity, and planar structuring are characterised.  We discuss the extent to which the observed evolution in the fluctuations is similar to that of solar wind emanating from steady sources at quiet times, how the evolution may be influenced by evolving local factors such as leading-edge shock orientation, and how the perturbed heliospheric environment associated with ICME propagation may impact the evolution more generally.

How to cite: Good, S., Ala-Lahti, M., Palmerio, E., Kilpua, E., and Osmane, A.: Radial evolution of magnetic field fluctuations in an ICME sheath, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-13664, https://doi.org/10.5194/egusphere-egu2020-13664, 2020.

EGU2020-6043 | Displays | ST1.2

Multi-spacecraft Observations of interacting CME flux ropes

Emilia Kilpua, Simon Good, Erika Palmerio, Eleanna Asvestari, Jens Pomoell, Erkka Lumme, Matti Ala-Lahti, Milla Kalliokoski, Diana Morosan, Daniel Price, Jasmina Magdalenic, Stefaan Poedts, and Yoshimi Futaana

Interactions between coronal mass ejections (CMEs) in interplanetary space are a highly important aspect for understanding their physical dynamics and evolution as well as their space weather consequences. Here we present an analysis of three CMEs that erupted from the Sun on June 12-14, 2012 using almost radially aligned spacecraft at Venus and Earth, complemented by heliospheric imaging and modelling with EUHFORIA. These multi-spacecraft observations were critical for interpreting the event correctly, in particular regarding the last two CMEs in the series (June 13 and June 14). At the orbit of Venus these CMEs were mostly separate with the June 14 CME just about to reach the previous CME. A significant interaction occurred before the CMEs reached the Earth. The shock of the June 14 CME had propagated through the June 13 CME and the two CMEs had coalesced into a single large flux rope structure before they reached the Earth. This merged flux rope had one of the largest magnetic field magnitudes observed in the near-Earth solar wind during Solar Cycle 24. We discuss also the general importance of multi-spacecraft observations and modelling using them in analyzing solar eruptions.

How to cite: Kilpua, E., Good, S., Palmerio, E., Asvestari, E., Pomoell, J., Lumme, E., Ala-Lahti, M., Kalliokoski, M., Morosan, D., Price, D., Magdalenic, J., Poedts, S., and Futaana, Y.: Multi-spacecraft Observations of interacting CME flux ropes, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6043, https://doi.org/10.5194/egusphere-egu2020-6043, 2020.

EGU2020-2736 | Displays | ST1.2

(Non)-radial propagation of the solar wind flow

Zdeněk Němeček, Tereza Ďurovcová, Jana Šafránková, Jiří Šimůnek, John D. Richardson, and Jaroslav Urbář

The solar wind aberration due to non-radial velocity components and the Earth orbital motion is important for the overall magnetosphere geometry because the magnetospheric tail is aligned with the solar wind flow. This paper investigates an evolution of non-radial components of the solar wind flow along the path from the Sun to 6 AU. A comparison of observations at 1 AU and closer to or further from the Sun based on measurements of many spacecraft at different locations in the heliosphere (Wind, ACE, Spektr-R, THEMIS B and C, Helios 1 and 2, Mars-Express, Voyager 1 and 2) shows that (i) the average values of non-radial components vary with the distance from the Sun and (ii) they differ according to solar wind streams.

How to cite: Němeček, Z., Ďurovcová, T., Šafránková, J., Šimůnek, J., Richardson, J. D., and Urbář, J.: (Non)-radial propagation of the solar wind flow , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2736, https://doi.org/10.5194/egusphere-egu2020-2736, 2020.

EGU2020-8621 | Displays | ST1.2

Multi-point observations of a reconnection outflow associated with interacting flux ropes in the solar wind

Zoltan Vörös, Emiliya Yordanova, Owen Roberts, and Yasuhito Narita

Twisted magnetic flux ropes embedded in an interplanetary coronal mass ejection (ICME) often contain oppositely oriented magnetic fields and potentially reconnecting current sheets. Reconnection outflows in the solar wind can be identified through magnetic field and plasma signatures, for example, through decreasing magnetic field magnitude, enhanced bulk velocity, temperature and (anti)correlated rotations of the magnetic field and plasma velocity. We investigate a reconnection outflow observed by ACE, WIND and Geotail spacecraft within the interaction region of two flux ropes embedded into an ICME. The SOHO spacecraft, located 15 RE upstream, 120 RE in GSE Y and 5 RE in GSE Z direction from the ACE spacecraft, does not see any plasma signatures of the reconnection outflow. At the same time the other spacecraft, also separated by more than 200 RE in X and Y GSE directions, observe strong plasma and magnetic field fluctuations at the border of the exhaust.  The fluctuations could be associated with Kelvin-Helmholtz (KH) instability at the border of the reconnection outflow with strong flow shear.  It is speculated that the KH instability driven fluctuations and dissipation is responsible for stopping the reconnection outflow which is therefore not seen by SOHO.

How to cite: Vörös, Z., Yordanova, E., Roberts, O., and Narita, Y.: Multi-point observations of a reconnection outflow associated with interacting flux ropes in the solar wind, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-8621, https://doi.org/10.5194/egusphere-egu2020-8621, 2020.

EGU2020-18966 | Displays | ST1.2

Kinetic models of current sheets in the solar wind

Thomas Neukirch, Ivan Vasko, Anton Artemyev, and Oliver Allanson

Current sheets in the collisionless solar wind usually have kinetic spatial scales. In-situ measurements (e.g. by Artemis) show that these current sheets are often approximately force-free, i.e. the directions of their current density and magnetic field are aligned, despite the fact that the plasma β is found to be of the order of one. The measurements also often show systematic asymmetric spatial variations of the plasma density and temperature across the current sheets, whilst the plasma pressure is approximately uniform. We present analytical equilibrium distribution functions of self-consistent force-free collisionless current sheets which allow for asymmetric plasma density and temperature gradients.

How to cite: Neukirch, T., Vasko, I., Artemyev, A., and Allanson, O.: Kinetic models of current sheets in the solar wind, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18966, https://doi.org/10.5194/egusphere-egu2020-18966, 2020.

STEREO has provided over 10 yr of continuous monitoring of CMEs and CME-driven shock waves from the Sun to Earth-like distances, as well as multipoint measurements of SEPs in the keV to 100 MeV energy range. These observations have revealed a number of puzzling properties of SEPs. For instance, gradual and impulsive SEP events have been measured over extended ranges of longitudes by STEREO, sometimes extending over 360 degrees around the Sun. Multi-spacecraft remote-sensing observations have allowed us to perform shock wave modeling in 3D, and to derive and examine consistently critical shock parameters during their evolution. I will present a connection of the shocks/CMEs to SEP properties from multi-spacecraft in-situ measurements by alleviating projection effects, accounting for both the complexities of coronal shocks and how they are likely to connect magnetically with in-situ spacecraft. A comparison between the shock wave parameters derived from 3D modeling and observations, and SEP characteristics confirm predictions of diffusive shock acceleration, that efficient acceleration of SEPs should naturally occur at shock regions where the shock Mach number is high. I will also discuss how modeling shock waves and estimating their magnetic connectivity can be useful in future studies to determine the solar origin of particle events measured by Parker Solar Probe.

How to cite: Kouloumvakos, A. and Rouillard, A. P.: Shock wave properties in the solar corona and their associations with multi-spacecraft solar energetic particle events measured near 1AU., EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11889, https://doi.org/10.5194/egusphere-egu2020-11889, 2020.

EGU2020-21246 | Displays | ST1.2

Energetic particles measurements on the lunar far-side by Lunar Lander Neutron and Dosimetry(LND) experiment

Zigong Xu, Robert F Wimmer-Schweingruber, Jingnan Guo, Jia Yu, Shenyi Zhang, Thomas Berger, Daniel Matthiae, Soenke Burmeister, Stephan Boettcher, and Bernd Heber

After Chang’E 4 successfully landed on the far side of the moon on Jan 3rd, 2019, the Lunar Lander Neutron and Dosimetry experiment has been working for 13 lunar days from January, 2019 to January, 2020, sending back the measurements of dose, linear energy transfer (LET) spectrum, neutrons, and charged particles. Here, we show observations of charged particles especially protons and Helium ions during quiet time. We also present two solar energetic particle events registered by LND in May 2019, which are also the first such measurements on the far-side surface of the moon. The temporal variations of particle fluxes on the far side of the moon detected by LND provide a new observation site in space and can be helpful to improve our understanding of particle propagation and transport in the heliosphere.

 

How to cite: Xu, Z., Wimmer-Schweingruber, R. F., Guo, J., Yu, J., Zhang, S., Berger, T., Matthiae, D., Burmeister, S., Boettcher, S., and Heber, B.: Energetic particles measurements on the lunar far-side by Lunar Lander Neutron and Dosimetry(LND) experiment, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21246, https://doi.org/10.5194/egusphere-egu2020-21246, 2020.

EGU2020-3690 | Displays | ST1.2

Long-term properties of the solar wind and their relation to solar cycles

Anna Salohub, Jana Šafránkova, Zdeněk Němeček, Lubomír Přech, and Tereza Ďurovcová

The solar wind variations during particular solar cycles have been described in many previous studies including the solar cycle 23 that was characterized by a long, deep, and very complex solar minimum with very low values of many solar wind parameters.

Using statistical methods, we analyzed 25 years of Wind spacecraft measurements with motivation to reveal differences and similarities in magnetic field components and solar wind plasma parameters in individual solar cycles. We tracked the changes of the solar magnetic field strength, and components, solar wind speed, density, dynamic pressure, temperature, and composition). Except quiet solar wind conditions during solar minima and maxima, we also selected significant discontinuities (ICME and CIRs) and investigated their influence on profiles of average parameters. For this, we followed other quantities connected with their presence as their average front normals, regions of transitions between high and slow wind streams, special interplanetary magnetic field orientations, etc.). We discuss a behavior of investigated parameters over solar cycles as well as on shorter time scales (in the order of days and hours).

How to cite: Salohub, A., Šafránkova, J., Němeček, Z., Přech, L., and Ďurovcová, T.: Long-term properties of the solar wind and their relation to solar cycles, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3690, https://doi.org/10.5194/egusphere-egu2020-3690, 2020.

EGU2020-7451 | Displays | ST1.2

Solar wind radial evolution via future multi-spacecraft in-situ observations

Štěpán Štverák, Milan Maksimovic, Petr Hellinger, and Pavel M. Trávníček

Our understanding of the solar wind evolution, its energy budget, and role of the key mechanisms providing the energy exchange between the plasma particles and electromagnetic fluctuations along the expansion, is highly limited by the single point nature of most in situ spacecraft measurements. Obviously it is difficult to observe and track the individual processes in space and time from this narrow perspective. One way to improve our knowledge of these large-scale variations is to employ multi-spacecraft observations, namely rather rare so called line-up events where one can potentially observe the true evolution of individual solar wind plasma parcels. A pioneering work in this field was done using Helios I&II missions. Here we present an analyses of using such tool for future events predicted to be available from the very recent missions Parker Solar Probe and Solar Orbiter (and optionally BepiColombo).

How to cite: Štverák, Š., Maksimovic, M., Hellinger, P., and Trávníček, P. M.: Solar wind radial evolution via future multi-spacecraft in-situ observations, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7451, https://doi.org/10.5194/egusphere-egu2020-7451, 2020.

EGU2020-4009 | Displays | ST1.2

Radial Evolution of Coronal Mass Ejections in the Inner Heliosphere: Catalog and Analysis

Tarik Salman, Reka Winslow, and Noé Lugaz

Our knowledge of the properties of Coronal Mass Ejections (CMEs) in the inner heliosphere is constrained by the relative lack of plasma observations between the Sun and 1 AU. In this work, we present a comprehensive catalog of 47 CMEs measured in situ measurements by two or more radially aligned spacecraft (MESSENGER, Venus Express, STEREO, and Wind/ACE). We estimate the CME impact speeds at Mercury and Venus using a drag-based model and present an average propagation profile of CMEs (speed and deceleration/acceleration) in the inner heliosphere. We find that CME deceleration continues past Mercury's orbit but most of the deceleration occurs between the Sun and Mercury. We examine the exponential decrease of the maximum magnetic field strength in the CME with heliocentric distance using two approaches: a modified statistical method and analysis from individual conjunction events. Findings from both the approaches are on average consistent with previous studies but show significant event-to-event variability. We also find the expansion of the CME sheath to be well fit by a linear function. However, we observe the average sheath duration and its increase to be fairly independent of the initial CME speed, contradicting commonly held knowledge that slower CMEs drive larger sheaths. We also present an analysis of the 3 November 2011 CME observed in a longitudinal conjunction between MESSENGER, Venus Express, and STEREO-B focusing on the expansion of the CME and its correlation with the exponential fall-off of the maximum magnetic field strength in the ejecta.

How to cite: Salman, T., Winslow, R., and Lugaz, N.: Radial Evolution of Coronal Mass Ejections in the Inner Heliosphere: Catalog and Analysis, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4009, https://doi.org/10.5194/egusphere-egu2020-4009, 2020.

EGU2020-13474 | Displays | ST1.2

Spatial coherence of interplanetary coronal mass ejection-driven sheaths at 1 AU

Matti Ala-Lahti, Julia Ruohotie, Simon Good, Emilia Kilpua, and Noé Lugaz

We report on the longitudinal coherence of sheath regions driven by interplanetary coronal mass ejections (ICMEs). ICME sheaths are significant drivers of geomagnetic activity at the Earth, with a considerable fraction of ICME-driven storms being either entirely or primarily induced by the sheath. Similarly to Lugaz et al. (2018; doi:10.3847/2041-8213/aad9f4), we have analyzed two-point magnetic field measurements made by the ACE and Wind spacecraft in 29 ICME sheaths to estimate the coherence scale lengths, defined as the spatial scale at which correlation between measurements falls to zero, of the field magnitude and components. Scale lengths for the sheath are found to be mostly smaller than the corresponding values in the ICME driver, an expected result given that ICME sheaths are characterized by highly fluctuating, variable magnetic fields, in contrast to the often more coherent ejecta. A relatively large scale length for the magnetic field component in the GSE y-direction was found. We discuss how magnetic field line draping around the ejecta and the alignment of pre-existing magnetic structures by the preceding shock may explain the observed results. In addition, we consider the existence of longitudinally extended and possibly geoeffective magnetic field fluctuations within ICME sheaths, the full understanding of which requires further multi-spacecraft analysis.

How to cite: Ala-Lahti, M., Ruohotie, J., Good, S., Kilpua, E., and Lugaz, N.: Spatial coherence of interplanetary coronal mass ejection-driven sheaths at 1 AU, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-13474, https://doi.org/10.5194/egusphere-egu2020-13474, 2020.

EGU2020-10717 | Displays | ST1.2

Geomagnetic Response to a Chain of Interplanetary Coronal Mass Ejections

Mojtaba Akhavan-Tafti, Dominique Fontaine, Olivier Le Contel, and James Slavin

The most geoeffective storms in the Space Age have been driven solely by the sheath preceding an interplanetary coronal mass ejection (ICME) or by a combination of the sheath and an ICME magnetic cloud. In the present study, the magnetospheric response to a chain of three independent and well-spaced ICMEs (Pdyn > 15 nPa and Sym-H < -50 nT) spanning one month (December 12, 2015 – January 12, 2016) is investigated using WIND, Cluster, and MMS fields and plasma measurements. The first of the three ICMEs consists of a sheath preceding an ICME (ICME-SH). The latter two ICMEs are preceded by a combination of the sheath and an ICME magnetic cloud (ICME-SH-MC).

Following the passage of the first ICMEs (ICME-SH) the interplanetary environment was made up of moderate Alfvenic Mach number (MA ~ 10) and average magnetopause standoff distance (RMP ~ 11 RE). The arrival of the ICME-SH-MC then initiated a sudden storm commencement (SSC) phase. During the SSC, the storm index (Sym-H ~ +50 nT) remained positive through the ICME shock and sheath regions. The storm index and the Alfvenic Mach number sharply declined (Sym-H~ -200 nT and MA ~ 1.0, respectively) with the arrival of the leading edge of the magnetic cloud (BIMF, core ~ 20 nT) and the associated sharp IMF Bz reversal (Bz<0). The Alfvenic Mach number and IMF Bz are found to directly correlate with the Sym-H index. ICME-SH-MC compressed the magnetopause standoff distance (∂RMP/∂t ~ -1 RE/min), resulting in a sudden reduction in the total magnetospheric volume (∂VMP/∂t ~ -3×102 RE3/min), as determined by cross-scale observations. In particular, the sharp drops in the magnetospheric volume (relative change in volume >30%) with the arrival of each of the three independent ICMEs are shown to start with the SSC and remain low through the main phase, before slowly recovering (∂VMP/∂t ~ +1 RE3/min) to the pre-ICME conditions during the recovery phase.

How to cite: Akhavan-Tafti, M., Fontaine, D., Le Contel, O., and Slavin, J.: Geomagnetic Response to a Chain of Interplanetary Coronal Mass Ejections, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-10717, https://doi.org/10.5194/egusphere-egu2020-10717, 2020.

EGU2020-11070 | Displays | ST1.2

The Effect of Variable Solar Wind Conditions on the Bow Shock Structure and its Ability to Generate Energetic Ions

Harald Kucharek, Matthew Young, Noe Lugaz, Charles Farrugia, Steven Schwartz, and Karlheinz Trattner

Turbulent fluctuations in the magnetic field and in the bulk plasma parameters of the solar wind have important effects on the propagation and evolution of energetic particles throughout the heliosphere and on the coupling of the solar wind to the Earth's magnetosphere. At the shock the solar wind kinetic energy is converted into downstream plasma heating, ion reflection and acceleration. Changes in upstream plasma conditions can result in changes in the dynamics of the shock, its structure, and the suprathermal ion population it generates. These upstream variations can be due to transients, interplanetary shocks, and other discontinuities. They can also result from nonlinear interactions, causing an intermittent energy dissipation and leading to possible currents sheet structures. A number of these events can be found in observations from STEREO (for interplanetary traveling shocks) and CLUSTER/MMS (for the Earth’s bow shock) in the magnetosheath. 

We performed 3D-hybrid simulations to study the effects of spatially confined disturbances, such as density enhancements, depletions, and current layers/sheets and studied the shock dynamics, and the energetic particle release at various distances from the bow shock. The results of these simulations are then discussed in terms of multi-spacecraft observations in the magnetosheath at various scales.  The results show that shock reformation is highly impacted by density depressions/enhancements and so is the generation of waves and suprathermal ions. Also, upstream solar wind variations can alter the shock properties considerably at the various virtual spacecraft in the simulations.

How to cite: Kucharek, H., Young, M., Lugaz, N., Farrugia, C., Schwartz, S., and Trattner, K.: The Effect of Variable Solar Wind Conditions on the Bow Shock Structure and its Ability to Generate Energetic Ions, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11070, https://doi.org/10.5194/egusphere-egu2020-11070, 2020.

EGU2020-4064 | Displays | ST1.2

A critical look at studying the interplanetary drivers of the magnetospheric disturbances

Yuri Yermolaev, Irina Lodkina, Lidia Dremukhina, Michael Yermolaev, and Alexander Khokhlachev

Although the main types of solar wind (the so-called interplanetary drivers), which may contain the southward component of the interplanetary magnetic field (Bz <0) and cause disturbances in the magnetosphere, have long been known, it has only recently been discovered that different types of drivers cause a different reaction of the magnetosphere for identical field variations (Borovsky and Denton,2006, Yermolaev et al., 2013). This discovery led to a significant increase in the number of investigations studying the response of the magnetosphere-ionosphere system to various drivers. At the same time, the number of incorrect approaches in this direction of research has increased. These errors can be attributed to 4 large classes. (1) First class includes works whose authors uncritically reacted to previously published works and use incorrect results to identify types of drivers. (2) Some authors independently incorrectly identified driver types. (3) Very often, authors associate the perturbation of the magnetosphere-ionosphere system caused by a complex driver (a sequence of single drivers) with one of the drivers, ignoring the complex nature. For example, a magnetic storm is often caused by a compression region Sheath in front of an interplanetary CME (ICME), but the authors consider the ICME to be a cause of disturbance, not Sheath. (4) Finally, there is a “lost driver” of magnetospheric disturbances: some authors simply do not consider the Sheath compression region before ICME if there is no interplanetary shock (IS) before Sheath, although this type of driver, “Sheath without IS”, generates about 10% of moderate and strong geomagnetic storms (Yermolaev et al., 2017, 2020). These errors lead to numerous mistakes and incorrect conclusions.
The work is supported by the RFFI grant 19-02-00177а. 

References
Borovsky, J. E., and M. H. Denton (2006), Differences between CME‐driven storms and CIR‐driven storms, J. Geophys. Res., 111, A07S08, doi:10.1029/2005JA011447

Yermolaev, Y. I., N. S. Nikolaeva, I. G. Lodkina, and M. Y. Yermolaev (2012), Geoeffectiveness and efficiency of CIR, sheath, and ICME in generation of magnetic storms, J. Geophys. Res., 117, A00L07, doi:10.1029/2011JA017139


Yermolaev, Y.I., Lodkina, I.G., Nikolaeva, N.S. et al. (2017), Some problems of identifying types of large-scale solar wind and their role in the physics of the magnetosphere, Cosmic Res. 55: 178. https://doi.org/10.1134/S0010952517030029

Yermolaev, Y.I., Lodkina, I.G., et al. (2020), Some problems of identifying types of large-scale solar wind and their role in the physics of the magnetosphere. 4. Lost driver, Cosmic Res. 59, in press

 

How to cite: Yermolaev, Y., Lodkina, I., Dremukhina, L., Yermolaev, M., and Khokhlachev, A.: A critical look at studying the interplanetary drivers of the magnetospheric disturbances , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4064, https://doi.org/10.5194/egusphere-egu2020-4064, 2020.

Understanding the evolution of interplanetary coronal mass ejections (ICMEs) as they propagate through the heliosphere is essential in forecasting space weather severity. Much of our knowledge of ICMEs has been gained using in-situ measurements from single spacecraft, although the increasing number of missions in the inner heliosphere has led to an increase in multi-spacecraft studies improving our understanding of the global structure of ICMEs. Whilst most such recent studies have focused on the inner heliosphere within 1 AU, Juno cruise phase data provides a new opportunity to study ICME evolution over greater distances. We present analysis of ICMEs observed in-situ both by Juno and at least one other spacecraft within 1 AU to investigate their evolution as they propagate through the heliosphere. Investigation of the sheath region and timing considerations between spacecraft allows for the general shape of the shock front to be reconstructed. Combining in-situ observations and results of flux rope fitting techniques determines the global picture of the ICME as it propagates. However, effects on in-situ observations due to radial evolution and due to the longitudinal separation between multi-spacecraft remain hard to separate. We note the importance of the interplanetary environment in which the ICME propagates and the need for caution in radial alignment studies.  

How to cite: Davies, E., Forsyth, R., and Good, S.: Using In-Situ Juno Observations to Understand the Evolution of Interplanetary Coronal Mass Ejections Within 1 AU and Beyond , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-13767, https://doi.org/10.5194/egusphere-egu2020-13767, 2020.

EGU2020-17957 | Displays | ST1.2

BepiColombo and Solar Orbiter coordinated observations: scientific cases and measurements opportunities

Lina Hadid, Melinda Dosa, Madar Akos, Tommaso Alberti, Johannes Benkhoff, Zsofia Bebesi, Lea Griton, George C. Ho, Kazumasa Iwai, Miho Janvier, Anna Milillo, Yoshizumi Miyoshi, Daniel Mueller, Go Murukami, Jim M. Raines, Daikou Shiota, Andrew Walsh, Joe Zender, and Yannis Zouganelis

BepiColombo and Solar Orbiter are two spacecraft that will be both travelling in the inner heliosphere for 5 years, between the launch of Solar Orbiter (planned in February 2020) and the end of the cruise phase of BepiColombo (2018 - 2025). Both BepiColombo (ESA/JAXA) and Solar Orbiter (ESA/NASA) are carrying exceptional and complementary plasma instrumental payloads and magnetometers. Besides, the remote-sensing instruments on board of Solar Orbiter will provide invaluable information on the state of the Sun, and therefore some contextual information for BepiColombo observations. During the five years to come, BepiColombo will evolve between the Earth and the orbit of Mercury, while Solar Orbiter’s highly elliptical orbit will cover distances from 1.02 AU to 0.28 AU.  We present here the scientific cases, modelling tools, measurement opportunities and related instruments operations that have been identified in the frame of potential coordinated observations campaign between the spacecraft.

How to cite: Hadid, L., Dosa, M., Akos, M., Alberti, T., Benkhoff, J., Bebesi, Z., Griton, L., C. Ho, G., Iwai, K., Janvier, M., Milillo, A., Miyoshi, Y., Mueller, D., Murukami, G., M. Raines, J., Shiota, D., Walsh, A., Zender, J., and Zouganelis, Y.: BepiColombo and Solar Orbiter coordinated observations: scientific cases and measurements opportunities, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-17957, https://doi.org/10.5194/egusphere-egu2020-17957, 2020.

EGU2020-7892 | Displays | ST1.2

Forecasting the Dst index from L5 in-situ data using PREDSTORM: accuracy and applicability

Rachel Bailey, Christian Moestl, Martin Reiss, Andreas Weiss, Ute Amerstorfer, Tanja Amerstorfer, Juergen Hinterreiter, and Maike Bauer

STEREO-B and STEREO-A are both important proxies for potential solar wind monitors at the Sun-Earth L5 point. In this study, measurements from STEREO-B are used to determine how well the Dst index in particular can be predicted using data measured near the L5 point. This is useful for determining the geoeffectivity of storms resulting from high-speed solar wind streams. Observed solar wind speeds are first mapped to the near-Earth environment as if they had been measured at L1, and the Dst is predicted from the data using a solar wind-to-Dst model. We find that Dst predicted from L5 data performs better than a recurrence model assuming the solar wind conditions repeat every 27 days, although not as well as when predicted from L1 data. The newly developed approach is currently implemented in the PREDSTORM software package to provide a real-time Dst forecast using STEREO-A data.

How to cite: Bailey, R., Moestl, C., Reiss, M., Weiss, A., Amerstorfer, U., Amerstorfer, T., Hinterreiter, J., and Bauer, M.: Forecasting the Dst index from L5 in-situ data using PREDSTORM: accuracy and applicability, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7892, https://doi.org/10.5194/egusphere-egu2020-7892, 2020.

EGU2020-2446 | Displays | ST1.2

Using Ghost Fronts to Predict the Arrival Time of CMEs during 13-17 June 2012

Yutian Chi, Chris Scott, Chenglong Shen, and Yuming Wang
Coronal mass ejections (CME) are large-scale eruptions of magnetized plasma and huge energy through the corona and out into interplanetary space.
A mount of CMEs observed by HI-1 cameras present two fronts that are similar in shape but separated by a few degrees in elongation. Scott et al. (2019) interpret the ghost fronts as projections of separate discrete sections of the physical boundary of the  CME. Ghost fronts could provide information about the longitudinal shape of CME in the field of view of Hi- 1, which can be used to improve the forecast of the arrival time of ICME. During 13-15 June 2012, STEREO/SECCHI recorded two successive launched Earth-directed CMEs. Both of the two CMEs show clearly two fronts in HI-1 images. We use the ghost fronts to predict the arrival time of the two CMEs and utility the in-situ measurements from VEX and Wind to verify the accuracy of the prediction of ghost fronts model. 

How to cite: Chi, Y., Scott, C., Shen, C., and Wang, Y.: Using Ghost Fronts to Predict the Arrival Time of CMEs during 13-17 June 2012, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2446, https://doi.org/10.5194/egusphere-egu2020-2446, 2020.

EGU2020-6750 | Displays | ST1.2

Observations and results from the High-Energy Particle Detector (HEPD) on-board CSES-01 satellite

Matteo Martucci and the CSES-Limadou Collaboration

The China Seismo-Electromagnetic Satellite (CSES-01) is a mission developed by

the Chinese National Space Administration (CNSA) together with the Italian Space Agency (ASI), to investigate the near-Earth electromagnetic, plasma and particle environment. In addition, it has been designed to detect a wide number of disturbances of the ionosphere/magnetosphere transition region.

One of the main instruments on-board CSES-01 is the High Energy Particle Detector (HEPD); it is an advanced detector, completely designed and built in Italy, based on a tower of 16 scintillators and a silicon tracker that provides good energy resolution and a wide angular acceptance for electrons/positrons (3–100 MeV), protons (30–200 MeV) and light nuclei up to Oxygen.

The very good capabilities in particle detection and separation make the detector extremely well suited for Space Weather purposes;  being also able to continuously monitor the magnetospheric environment with high stability in time, HEPD can detect small variations related to transient phenomena taking place on the Sun and propagating through the solar wind.
After two years of data-taking, HEPD showed impressive capabilities in measuring the various particle distributions along its orbit, starting from sub-cutoff protons/electrons, up to galactic cosmic ray particles at higher latitudes. The former class includes both stably-trapped particles in the Radiation Belts and particles bounced back from the top of the atmosphere without being able to escape the magnetic trap (re-entrant albedo). For cosmic ray particles, precise measurements of their spectra are needed to understand the acceleration and subsequent propagation of low-energy particles in the inner sector of the heliosphere and, more general, in our Galaxy.

We report precision measurements of the protons in the >30 MeV energy region and electrons in the >5 MeV energy range, performed by HEPD in a un-disturbed heliosphere during a low solar activity period (2018/2020).

How to cite: Martucci, M. and the CSES-Limadou Collaboration: Observations and results from the High-Energy Particle Detector (HEPD) on-board CSES-01 satellite, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6750, https://doi.org/10.5194/egusphere-egu2020-6750, 2020.

ST1.3 – Exploring the near-Sun environment – Results from the first orbits of Parker Solar Probe and preparation for Solar Orbiter

EGU2020-22164 * | Displays | ST1.3 | Highlight

Solar Orbiter: Europe's mission to the Sun

Yannis Zouganelis, Daniel Mueller, Chris St Cyr, Holly Gilbert, and Teresa Nieves-Chinchilla

ESA’s Solar Orbiter mission is scheduled for launch in February 2020, and will focus on exploring the linkage between the Sun and the heliosphere. It is a collaborative mission with NASA that will collect unique data that will allow us to study, e.g., the coupling between macroscopic physical processes to those on kinetic scales, the generation of solar energetic particles and their propagation into the heliosphere, and the origin and acceleration of solar wind plasma. By approaching as close as 0.28 AU, Solar Orbiter will view the Sun with high spatial resolution and combine this with in-situ measurements of the surrounding heliosphere. Over the course of the mission, the highly elliptical orbit will get progressively more inclined to the ecliptic plane. Thanks to this new perspective, Solar Orbiter will deliver images and comprehensive data of the unexplored Sun’s polar regions and the side of the Sun not visible from Earth. This talk will provide a mission overview, highlight synergies with NASA’s Parker Solar Probe and summarise current status.

How to cite: Zouganelis, Y., Mueller, D., St Cyr, C., Gilbert, H., and Nieves-Chinchilla, T.: Solar Orbiter: Europe's mission to the Sun, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-22164, https://doi.org/10.5194/egusphere-egu2020-22164, 2020.

EGU2020-17904 | Displays | ST1.3 | Highlight

The SO/PHI instrument on Solar Orbiter and its data products

Sami K. Solanki, Johann Hirzberger, Thomas Wiegelmann, Achim Gandorfer, Joachim Woch, and José Carlos del Toro Iniesta

A central instrument of Solar Orbiter is the Polarimetric and Helioseismic Imager, SO/PHI. It is a vector magnetograph that also provides data for helioseismology. SO/PHI is composed of two telescopes, a full-disk telescope (FDT) and a high-resolution telescope (HRT). The HRT will observe at a resolution as high as 200 km on the solar surface, while the FDT will obtain the magnetic field and velocity of the full solar disc whenever it observes. SO/PHI will be the first solar spectro-polarimeter to leave the Sun-Earth line, opening up some unique perspectives, such as the first detailed view of the solar poles. This will allow not just a more precise and exact mapping of the polar magnetic field than possible so far, but will also enable us to follow the dynamics of individual magnetic features at high latitudes and to determine solar surface and sub-surface flows right up to the poles. In addition to its standard data products (vector magnetograms, continuum images and maps of the line-of-sight velocity), SO/PHI will also provide higher-level data products. These will include synoptic charts, local magnetic field extrapolations starting from HRT data and global magnetic field extrapolations (from FDT data) with potential field source-surface (PFSS) models and possibly also non-potential models such as NLFFF (non-linear force-free fields), magnetostatics and MHD. The SO/PHI data products will usefully complement the data taken by other instruments on Solar Orbiter and on Solar Probe, as well as instruments on the ground or in Earth orbit. Combining with observations by Earth-based and near-Earth telescopes will enable new types of investigations, such as stereoscopic polarimetry and stereoscopic helioseismology.

How to cite: Solanki, S. K., Hirzberger, J., Wiegelmann, T., Gandorfer, A., Woch, J., and del Toro Iniesta, J. C.: The SO/PHI instrument on Solar Orbiter and its data products , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-17904, https://doi.org/10.5194/egusphere-egu2020-17904, 2020.

EGU2020-5800 | Displays | ST1.3 | Highlight

The Radio and Plasma Waves (RPW) Instrument on Solar Orbiter : Capabilities, Performance and First results.

Milan Maksimovic, Jan Souček, Stuart D. Bale, Xavier Bonnin, Thomas Chust, Yuri Khotyaintsev, Matthieu Kretzschmar, Dirk Plettemeier, Manfred Steller, and Štěpán Štverák

We will review the instrumental capabilities of the Radio and Plasma Waves (RPW) Instrument on Solar Orbiter which at the time of writing this abstract is planned for a launch on February 5th 2020. This instrument is designed to measure in-situ magnetic and electric fields and waves from 'DC' to a few hundreds of kHz. RPW will also observe solar radio emissions up to 16 MHz. The RPW instrument is of primary importance to the Solar Orbiter mission and science requirements, since it is essential to answer three of the four mission overarching science objectives. In addition, RPW will exchange on-board data with the other in-situ instruments, in order to process algorithms for interplanetary shocks and type III Langmuir waves detections. If everything goes well after the launch, we will hopefully be able to present the first RPW data and results gathered during the commissioning.

How to cite: Maksimovic, M., Souček, J., Bale, S. D., Bonnin, X., Chust, T., Khotyaintsev, Y., Kretzschmar, M., Plettemeier, D., Steller, M., and Štverák, Š.: The Radio and Plasma Waves (RPW) Instrument on Solar Orbiter : Capabilities, Performance and First results., EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5800, https://doi.org/10.5194/egusphere-egu2020-5800, 2020.

EGU2020-22044 | Displays | ST1.3

Energetic Particles in the Inner Heliosphere: Solar Orbiter

Robert F. Wimmer-Schweingruber, Javier Rodriguez-Pacheco, Stephan Böttcher, Ignacio Cernuda, Nina Dresing, Wolfgang Dröge, Sandra Eldrum, Francisco Espinose Lara, Raul Gomez-Herrero, Bernd Heber, George Ho, Andreas Klassen, Alexander Kollhoff, Shrinivasrao Kulkarni, Gottfried Mann, César Martin, Glenn Mason, Daniel Pacheco, Manuel Prieto, and Sebastian Sanchez and the Robert F. Wimmer-Schweingruber

To be measured as energetic particles in the heliosphere ions and electrons must undergo three processes: injection, acceleration, and transport. Suprathermal seed particles have speeds well above the fast magnetosonic speed in the solar wind frame of reference and can vary from location to location and within the solar activity cycle. Acceleration sites include reconnecting current sheets in solar flares or magnetospheric boundaries, shocks in the solar corona, heliosphere and a planetary obstacles, as well as planetary magnetospheres. Once accelerated, particles are transported from the acceleration site into and throughout the heliosphere. Thus, by investigating properties of energetic particles such as their composition, energy spectra, pitch-angle distribution, etc. one can attempt to distinguish their origin or injection and acceleration site. This in turn allows us to better understand transport effects whose underlying microphysics is also a key ingredient in the acceleration of particles.

In this presentation we will present some clear examples which link energetic particles from their observing site to their source locations. These include Jupiter electrons, singly-charged He ions from CIRs, and 3He from solar flares. We will compare these examples with the measurement capabilities of the Energetic Particle Detector (EPD) on Solar Orbiter and consider implications for the key science goal of Solar Orbiter and Solar Proble Plus – How the Sun creates and controls the heliosphere.

How to cite: Wimmer-Schweingruber, R. F., Rodriguez-Pacheco, J., Böttcher, S., Cernuda, I., Dresing, N., Dröge, W., Eldrum, S., Espinose Lara, F., Gomez-Herrero, R., Heber, B., Ho, G., Klassen, A., Kollhoff, A., Kulkarni, S., Mann, G., Martin, C., Mason, G., Pacheco, D., Prieto, M., and Sanchez, S. and the Robert F. Wimmer-Schweingruber: Energetic Particles in the Inner Heliosphere: Solar Orbiter, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-22044, https://doi.org/10.5194/egusphere-egu2020-22044, 2020.

EGU2020-19143 | Displays | ST1.3

First observations of the Search Coil Magnetometer on Solar Orbiter / RPW: results and performances

Matthieu Kretschmar, Volodya Krasnoselskikh, Jean-Yves Brochot, Guillaume Jannet, Thierry Dudok de Wit, Clara Froment, Milan Maksimovic, Thomas Chust, Olivier Le Contel, Jan Soucek, and David Pisa

The Search Coil Magnetometer (SCM) onboard Solar Orbiter is part of the Radio and Plasma Waves (RPW) experiment and measures the variations of the magnetic field between 10 Hz and 50 kHz on three axes and between 1 kHz and 1MHz in one axis. The SCM is located on the boom of the spacecraft and its signal is processed by the LFR, TDS, and HFR analyzers of the RPW experiment. These measurements are essential for the characterization of waves and turbulence in the solar wind. We will describe the first observations made by the instrument with an emphasis on its performances. 

How to cite: Kretschmar, M., Krasnoselskikh, V., Brochot, J.-Y., Jannet, G., Dudok de Wit, T., Froment, C., Maksimovic, M., Chust, T., Le Contel, O., Soucek, J., and Pisa, D.: First observations of the Search Coil Magnetometer on Solar Orbiter / RPW: results and performances, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-19143, https://doi.org/10.5194/egusphere-egu2020-19143, 2020.

EGU2020-20154 | Displays | ST1.3

Relative abundance diagnostics with SPICE, the EUV spectrometer on-board Solar Orbiter

Natalia Zambrana Prado, Eric Buchlin, and Hardi Peter

With the launches of Parker Solar Probe and Solar Orbiter, we are closer than ever to linking solar activity on the surface and in the corona to the inner heliosphere. In this quest, relative abundance measurements will be key as different structures on the Sun have different abundances as a consequence of the FIP (First Ionization Potential) effect.

Comparing in-situ and remote sensing composition data, coupled with modeling, will allow us to trace back the source of heliospheric plasma. Solar Orbiter has a unique combination of in-situ and remote sensing instruments that will hopefully allow us to make such comparisons.

High telemetry will not always be available with SPICE (SPectral Imaging of the Coronal Environment), the EUV spectrometer on board Solar Orbiter. We have therefore developed a method for measuring relative abundances that is both telemetry efficient and reliable. Unlike methods based on Differential Emission Measure (DEM) inversion, the Linear Combination Ratio (LCR) method does not require a large number of spectral lines. This new method is based on optimized linear combinations of only a few UV spectral lines. We present some abundance diagnostics applied to synthesized radiances of spectral lines observable by SPICE.

How to cite: Zambrana Prado, N., Buchlin, E., and Peter, H.: Relative abundance diagnostics with SPICE, the EUV spectrometer on-board Solar Orbiter, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-20154, https://doi.org/10.5194/egusphere-egu2020-20154, 2020.

EGU2020-4720 | Displays | ST1.3

The Proton and Alpha Sensor (PAS) of Solar Orbiter Mission: design, operation, scientific return simulation, and first flight results

Philippe Louarn, andrei fedorov, and Christopher Owen and the SWA/PAS team

Solar Orbiter is an ESA/NASA mission that will provide an unprecedented opportunity to discover the fundamental connections between the rapidly varying solar atmosphere and the solar wind. The Solar Wind Analyzer (SWA) plasma package shall provide comprehensive in-situ measurements of the solar wind. In particular, the Proton-Alpha Sensor (PAS) will determine the properties of the dominant solar wind ion population through the measurement of the 3D distribution function, density, bulk velocity, temperature, and heat fluxes, at temporal cadences ranging form 4 s to ~0.1 s. The closest approach of Solar Orbiter to the Sun is 0.28 AU. At this distance the solar wind Vow, solar UV, and solar infrared fluxes increase by a factor 13 compared to near-Earth space. The PAS instrument will provide high cadence 3D distribution function measurements (up to 13 per second) all the way from closest approach to 1 AU. This paper give a basic information about PAS design, and describes the PAS measurement scheme adopted for varying solar wind conditions and our approach to the fast sampling of 3D distribution functions. We also provide a simulations of the expected scientific return. If possible, a first glance of PAS commissioning results will be presented.

How to cite: Louarn, P., fedorov, A., and Owen, C. and the SWA/PAS team: The Proton and Alpha Sensor (PAS) of Solar Orbiter Mission: design, operation, scientific return simulation, and first flight results, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4720, https://doi.org/10.5194/egusphere-egu2020-4720, 2020.

EGU2020-19314 | Displays | ST1.3 | Highlight

Plasma and magnetic field dynamics in the young solar wind

Justin Kasper and the On behalf of the SWEAP Investigation science team

Parker Solar Probe (PSP) has completed four encounters with the Sun since launch, three with a perihelion of 35.7 solar radii and one at 27.9 solar radii in January of this year.  More than a factor of two closer to the Sun than any previous mission, observations by the spacecraft are already revealing a surprisingly dynamic and non-thermal solar wind plasma near the Sun.  An overview of initial findings related to the solar wind and coronal plasmas will be presented, including the discovery of large-amplitude velocity spikes, highly non-thermal distribution functions, and large non-radial flows of plasma near the Sun observed by the Solar Wind Electrons Alphas and Protons (SWEAP) Investigation plasma instruments and the FIELDS Investigation electromagnetic field instruments.  Once PSP dropped below a quarter of the distance from the Sun to the Earth, SWEAP began to detect a persistent and growing rotational circulation of the plasma around the Sun peaking at 40-50 km/s at perihelion as the Alfvén mach number fell to 3.  This finding may support theories for enhanced stellar angular momentum loss due to rigid coronal rotation, but the circulation is large, and angular momentum does not appear to be conserved, suggesting that torques still act on the young wind at these distances.  PSP also measured numerous intense and organized Alfvénic velocity spikes with strong propagating field reversals and large jumps in speed.  These field reversals and jets call for an overhaul in our understanding of the turbulent fluctuations that may, by energizing the solar wind, hold the key to its origin.

How to cite: Kasper, J. and the On behalf of the SWEAP Investigation science team: Plasma and magnetic field dynamics in the young solar wind, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-19314, https://doi.org/10.5194/egusphere-egu2020-19314, 2020.

EGU2020-19398 | Displays | ST1.3 | Highlight

The Dust Environment in the Inner Heliosphere

Russell Howard, Guillermo Stenborg, David Malaspina, Jamey Szalay, and Petr Pokorny

The Parker Solar Probe (PSP) mission has completed 4 encounters through the solar corona significantly closer to the Sun than previous measurements. While PSP does not have a dedicated dust detector, measurements by the various instruments can provide insights into the dust environment in the inner heliosphere.  Throughout the PSP orbit, interplanetary dust is impacting the spacecraft.  Three-dimensional reconstructions of FIELDS observations show that the rate and direction of the dust impacts varies throughout the PSP orbit.  During the encounter WISPR also finds the rate of impacts changes through the encounter period, but also a decrease in the intensity of the light scattered by the dust particles.  The smooth decrease in the WISPR intensity beginning at about 0.1 AU is consistent with the production of Beta-meteroids seen by FIELDS. In this presentation, we will discuss the observations from the FIELDS and WISPR instruments and discuss initial models of the dust environment.  The authors acknowledge support from the NASA Parker Solar Probe program.

How to cite: Howard, R., Stenborg, G., Malaspina, D., Szalay, J., and Pokorny, P.: The Dust Environment in the Inner Heliosphere, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-19398, https://doi.org/10.5194/egusphere-egu2020-19398, 2020.

EGU2020-6063 * | Displays | ST1.3 | Highlight

Energetic Particle Environment near the Sun from Parker Solar Probe

Nathan Schwadron and the PSP-ISʘIS Group

NASA’s Parker Solar Probe (PSP) mission recently plunged through the inner heliosphere to perihelia at ~24 million km (~35 solar radii), much closer to the Sun than any prior human made object. Onboard PSP, the Integrated Science Investigation of the Sun (ISʘIS) instrument suite made groundbreaking measurements of solar energetic particles (SEPs). Here we discuss the near-Sun energetic particle radiation environment over PSP’s first two orbits, which reveal where and how energetic particles are energized and transported. We find a great variety of energetic particle events accelerated both locally and remotely. These include co-rotating interaction regions (CIRs), “impulsive” SEP events driven by acceleration near the Sun, and events related to Coronal Mass Ejections (CMEs). These ISʘIS observations made so close to the Sun provide critical information for investigating the near-Sun transport and energization of solar energetic particles that was difficult to resolve from prior observations. We discuss the physics of particle acceleration and transport in the context of various theories and models that have been developed over the past decades. This study marks a major milestone with humanity’s reconnaissance of the near-Sun environment and provides the first direct observations of the energetic particle radiation environment in the region just above the corona.

How to cite: Schwadron, N. and the PSP-ISʘIS Group: Energetic Particle Environment near the Sun from Parker Solar Probe, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6063, https://doi.org/10.5194/egusphere-egu2020-6063, 2020.

EGU2020-1901 | Displays | ST1.3 | Highlight

Properties of Suprathermal-through-Energetic He Ions Associated with Stream Interaction Regions Observed over Parker Solar Probe’s First Two Orb¬¬its

Mihir Desai and the Parker Solar Probe ISOIS, FIELDS & SWEAP Team

The Integrated Science Investigation of the Sun (IS☉IS) suite on board NASA’s Parker Solar Probe (PSP) observed six distinct enhancements in the intensities of suprathermal-through-energetic (~0.03-3 MeV nucleon-1) He ions associated with corotating or stream interaction regions during its first two orbits. Our results from a survey of the time-histories of the He intensities, spectral slopes, and anisotropies, and the event-averaged energy spectra during these events show: 1) In the two strongest enhancements, seen at 0.35 au and 0.85 au, the higher energy ions arrive and maximize later than those at lower energies. In the event seen at 0.35 au, the He ions arrive when PSP was away from the SIR trailing edge and entered the rarefaction region in the high-speed stream; 2) The He intensities are either isotropic or show sunward anisotropies in the spacecraft frame; and 3) In all events, the energy spectra between ~0.2–1 MeV nucleon-1are power-laws of the form ∝E-2. In the two strongest events, the energy spectra are well represented by flat power-laws between ~0.03–0.4 MeV nucleon-1modulated by exponential roll-overs between ~0.4–3 MeV nucleon-1. We conclude that the SIR-associated He ions originate from sources or shocks beyond PSP’s location rather than from acceleration processes occurring atnearby portions of local compression regions. Our results also suggest that rarefaction regions that typically follow the SIRs facilitate easier particle transport throughout the inner heliosphere such that low energy ions do not undergo significant energy loss due to adiabatic deceleration, contrary to predictions of existing models.

How to cite: Desai, M. and the Parker Solar Probe ISOIS, FIELDS & SWEAP Team: Properties of Suprathermal-through-Energetic He Ions Associated with Stream Interaction Regions Observed over Parker Solar Probe’s First Two Orb¬¬its, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1901, https://doi.org/10.5194/egusphere-egu2020-1901, 2020.

EGU2020-11550 | Displays | ST1.3

The Evolution and Role of Solar Wind Turbulence in the Inner Heliosphere

Christopher Chen and the PSP FIELDS and SWEAP Teams

The first two orbits of the Parker Solar Probe (PSP) spacecraft have enabled the first in situ measurements of the solar wind down to a heliocentric distance of 0.17 au (or 36 Rs). Here, we present an analysis of this data to study solar wind turbulence at 0.17 au and its evolution out to 1 au. While many features remain similar, key differences at 0.17 au include: increased turbulence energy levels by more than an order of magnitude, a magnetic field spectral index of -3/2 matching that of the velocity and both Elsasser fields, a lower magnetic compressibility consistent with a smaller slow-mode kinetic energy fraction, and a much smaller outer scale that has had time for substantial nonlinear processing. There is also an overall increase in the dominance of outward-propagating Alfvenic fluctuations compared to inward-propagating ones, and the radial variation of the inward component is consistent with its generation by reflection from the large-scale gradient in Alfven speed. The energy flux in this turbulence at 0.17 au was found to be ~10% of that in the bulk solar wind kinetic energy, becoming ~40% when extrapolated to the Alfven point, and both the fraction and rate of increase of this flux towards the Sun is consistent with turbulence-driven models in which the solar wind is powered by this flux.

How to cite: Chen, C. and the PSP FIELDS and SWEAP Teams: The Evolution and Role of Solar Wind Turbulence in the Inner Heliosphere, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11550, https://doi.org/10.5194/egusphere-egu2020-11550, 2020.

EGU2020-22182 | Displays | ST1.3

Analysis of the Internal structure of the Streamer Blow Out Observed by the Parker Solar Probe during the First Solar Encounter

Teresa Nieves-Chinchilla, Adam Szabo, Kelly E. Korreck, Nathalia Alzate, Laura A. Balmaceda, Benoit Lavraud, Kristoff Paulson, Ayris A. Narock, Samantha Wallace, Lan K. Jian, Janet G. Luhman, Huw Morgan, Aleida Higginson, and Charles N. Arge and the PSP team

We present an analysis of the internal structure of a coronal mass ejection (CME) detected by in situ instruments onboard the Parker Solar Probe (PSP) spacecraft during its first solar encounter. On 2018 November 11 at 23:53 UT, the FIELDS magnetometer measured an increase in strength of the magnetic field as well as a coherent change in the field direction. The SWEAP instrument simultaneously detected the low proton temperature and signatures of bi-directionality in the electron pitch angle distribution (PAD). These signatures are indicative of a CME embedded in the slow solar wind. In conjunction with PSP was the STEREO A spacecraft, which enabled the remote observation of a streamer blow-out by the SECCHI suite of instruments. The source at the Sun of the slow and well-structured flux-rope was identified in an overlying streamer.

Our detailed inspection of the internal transient structure magnetic properties suggests high complexity in deviations from an ideal flux rope 3D topology. Reconstructions of the magnetic field conguration reveal a highly distorted structure consistent with the highly elongated `bubble' observed remotely. A double-ring substructure observed in the SECCHI-COR2 eld of view (FOV) is suggestive of a double internal flux rope. Furthermore, we describe a scenario in which mixed topology of a closed flux rope is combined with the magnetically open structure, which helps explain the flux dropout observed in the measurements of the electron PAD. Our justication for this is the plethora of structures observed by the EUV imager (SECCHI-EUVI) in the hours preceding the streamer blowout evacuation. Finally, taking advantage of the unique observations from PSP, we explore the first stages of the effects of coupling with the solar wind and the evolutionary processes in the magnetic structure. We found evidence of bifurcated current sheets in the structure boundaries suggestive of magnetic reconnection. Our analysis of the internal force imbalance indicates that internal Lorentz forces continue to dominate the evolution of the structure in the COR2 FOV and serves as the main driver of the internal flux rope distortion as detected in situ at PSP solar distance.

How to cite: Nieves-Chinchilla, T., Szabo, A., Korreck, K. E., Alzate, N., Balmaceda, L. A., Lavraud, B., Paulson, K., Narock, A. A., Wallace, S., Jian, L. K., Luhman, J. G., Morgan, H., Higginson, A., and Arge, C. N. and the PSP team: Analysis of the Internal structure of the Streamer Blow Out Observed by the Parker Solar Probe during the First Solar Encounter, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-22182, https://doi.org/10.5194/egusphere-egu2020-22182, 2020.

EGU2020-11552 | Displays | ST1.3

The forming slow solar wind imaged along streamer rays by the wide-angle imager on Parker Solar Probe

Nicolas Poirier, Athanasios Kouloumvakos, Alexis P. Rouillard, Rui Pinto, Angelos Vourlidas, Guillermo Stenborg, Emeline Valette, Russell A. Howard, Phillip Hess, Arnaud Thernisien, Nathan Rich, Léa Griton, Mikel Indurain, Nour-Edine Raouafi, Michael Lavarra, and Victor Réville

The Wide-field Imager for Solar PRobe (WISPR) obtained the first high-resolution images of coronal rays at heights below 15 Rsun when Parker Solar Probe (PSP) was located inside 0.25 AU during the first encounter. We exploit these remarkable images to reveal the structure of coronal rays at scales that are not easily discernible in images taken from near 1 AU. To analyze and interpret WISPR observations which evolve rapidly both radially and longitudinally, we construct a latitude versus time map using full WISPR dataset from the first encounter. From the exploitation of this map and also from sequential WISPR images we show the presence of multiple sub-structures inside streamers and pseudo-streamers. WISPR unveils the fine-scale structure of the densest part of streamer rays that we identify as the solar origin of the heliospheric plasma sheet typically measured in situ in the solar wind. We exploit 3-D magneto-hydrodynamic (MHD) models and we construct synthetic white-light images to study the origin of the coronal structures observed by WISPR. Overall, including the effect of the spacecraft relative motion towards the individual coronal structures we can interpret several observed features by WISPR. Moreover, we relate some coronal rays to folds in the heliospheric current sheet that are unresolved from 1 AU. Other rays appear to form as a result of the inherently inhomogeneous distribution of open magnetic flux tubes. This work was funded by the European Research Council through the project SLOW_SOURCE - DLV-819189.

How to cite: Poirier, N., Kouloumvakos, A., Rouillard, A. P., Pinto, R., Vourlidas, A., Stenborg, G., Valette, E., Howard, R. A., Hess, P., Thernisien, A., Rich, N., Griton, L., Indurain, M., Raouafi, N.-E., Lavarra, M., and Réville, V.: The forming slow solar wind imaged along streamer rays by the wide-angle imager on Parker Solar Probe, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11552, https://doi.org/10.5194/egusphere-egu2020-11552, 2020.

The relative helium abundance (AHe) and alpha-proton relative drift often serve as one of the solar wind source identifiers. However, observations at 1 AU suggest that these relative properties may be affected by the interaction of different solar wind streams. Since the influence of stream interaction is reduced near the Sun, a comparison of observations at 1 AU and close to the Sun could help to reveal the processes which lead to AHe variations. In-situ measurements near the Sun are provided by the SWEAP instrument onboard Parker Solar Probe. It consists of electrostatic analyzers (SPANs) and the Faraday cup (SPC). SPAN-Ai measures the 3-D ion distribution from the shadowed region behind the spacecraft thermal shield and is equipped with a mass-to-charge detection. SPC is directed to the Sun and provides fast measurements of the ion reduced distribution function (RDF) as a function of energy/charge. We develop a new data analysis technique for computations of the proton and helium parameters from the RDFs measured by SPC and compare it with SPAN observations. Then, we combine the PSP measurements with observations at 1 AU and focus on variations of the helium properties. Finally, we discuss the connection between AHe variations and changes of the solar wind source region.

How to cite: Durovcova, T. and the PSP: Comparison of properties of the solar wind helium component close to the Sun and at 1 AU, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2750, https://doi.org/10.5194/egusphere-egu2020-2750, 2020.

EGU2020-4911 | Displays | ST1.3

GEANT 4 Simulation of the Helios E6 - Proton Contamination of Relativistic Electron Measurements

Malte Hörlöck, Bernd Heber, and Johannes Marquardt

The Helios mission consisted of two almost identical spacecraft in highly elliptic orbits launched in 1974 (Helios A) and 1976 (Helios B). Until Parker Solar Probes first perihelion, Helios B was the first spacecraft to reach a distance of 0.29 AU to the Sun. One of its instruments is the Experiment 6 (E6) which was designed and built at the Christian-Albrechts-University Kiel in order to measure ions (protons up to iron) in the energy range of 1.3 MeV/nucleon up to several GeV/nucleon and electrons in the energy range from 0.3 to about 8 MeV. The instrument relies on the dE/dx-E and on the dE/dx-Cherenkov method for stopping and penetrating particles, respectively. Electrons are separated from ions by the signal in the first 100 µm thick solid state detector. Any particle that does not trigger this detector is identified as an electron. Since the solid state detectors are not working perfectly, a significant part of protons is identified as electrons. Here, we present a new method to correct the electron measurements for the cross talk based on detailed instrument simulations.

How to cite: Hörlöck, M., Heber, B., and Marquardt, J.: GEANT 4 Simulation of the Helios E6 - Proton Contamination of Relativistic Electron Measurements, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4911, https://doi.org/10.5194/egusphere-egu2020-4911, 2020.

EGU2020-14874 | Displays | ST1.3

Initial in-flight performance results from Solar Orbiter RPW/BIAS

Yuri V. Khotyaintsev, Andris Vaivads, Daniel B. Graham, Niklas J. T. Edberg, Erik P. G. Johansson, Milan Maksimovic, Stuart D. Bale, Thomas Chust, Matthieu Kretzschmar, and Jan Soucek

The BIAS subsystem is a part of the Radio and Plasma Waves (RPW) instrument on the ESA Solar Orbiter mission. It allows sending bias current to each of the three RPW antennas. By setting the appropriate bias current the antenna potential can be shifted closer to the local plasma potential. This allows us to measure the floating potential of the spacecraft, as well as the electric field in the DC/LF frequency range with higher accuracy and lower noise level. Here we present the very initial results on RPW/BIAS in-flight performance based on the operations during the instrument commissioning.

How to cite: Khotyaintsev, Y. V., Vaivads, A., Graham, D. B., Edberg, N. J. T., Johansson, E. P. G., Maksimovic, M., Bale, S. D., Chust, T., Kretzschmar, M., and Soucek, J.: Initial in-flight performance results from Solar Orbiter RPW/BIAS, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-14874, https://doi.org/10.5194/egusphere-egu2020-14874, 2020.

EGU2020-18183 | Displays | ST1.3

Electromagnetic radiation from upper-hybrid wave turbulence driven by electron beams in solar plasmas

Gaetan Gauthier, Catherine Krafft, and Philippe Savoini

Solar radio bursts of Type III are believed to result from a sequence of physical processes ultimately leading to electromagnetic wave emissions near the electron plasma frequency ωp and its harmonic 2ωp. The radiation bursts are due to energetic electron beams accelerated during solar flares. When propagating in the solar corona and the interplanetary wind, these fluxes excite Langmuir and upper-hybrid wave turbulence, which can be further transformed into electromagnetic radiation near the frequencies ωp and 2ωp.

It is believed that, in a homogeneous plasma, Langmuir turbulence evolves due to three-wave interaction processes, such as the fusion of Langmuir waves L with sound waves S leading to the formation of electromagnetic waves Tωp at ωp or the decay of L-waves into S-waves and Tωp-waves. On the other hand, the electromagnetic waves radiated at 2ωp should arise from the coalescence L + L’ --> Tp of Langmuir waves L generated by the beam with Langmuir waves L’ coming from the electrostatic decay L --> L’ +  S.

Large-scale 2D3V Particle-In-Cell simulations have been performed with the fully kinetic code Smilei [Derouillat et al., 2018], using parameters typical of Type III solar radio busts. The excitation of upper-hybrid wave turbulence by energetic electron beams propagating in magnetized plasmas leads ultimately to electromagnetic emissions near the fundamental and the harmonic plasma frequencies.

Derouillat et al. , Comput. Phys. Commun., 222, 351, 2017.

How to cite: Gauthier, G., Krafft, C., and Savoini, P.: Electromagnetic radiation from upper-hybrid wave turbulence driven by electron beams in solar plasmas, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18183, https://doi.org/10.5194/egusphere-egu2020-18183, 2020.

EGU2020-18573 | Displays | ST1.3

Large-scale electron solar wind parameters of the inner heliosphere with Parker Solar Probe/FIELDS

Karine Issautier, Mingzhe Liu, Michel Moncuquet, Nicole Meyer-Vernet, Milan Maksimovic, Stuart Bale, and Marc Pulupa

We present in situ properties of electron density and temperature in the inner heliosphere obtained during the three first solar encounters at 35 solar radii of the Parker Solar Probe mission. These preliminary results, recently shown by Moncuquet et al., ApJS, 2020, are obtained from the analysis of the plasma quasi-thermal noise (QTN) spectrum measured by the radio RFS/FIELDS instrument along the trajectories extending between 0.5 and 0.17 UA from the Sun, revealing different states of the emerging solar wind, five months apart. The temperature of the weakly collisional core population varies radially with a power law index of about -0.8, much slower than adiabatic, whereas the temperature of the supra-thermal population exhibits a much flatter radial variation, as expected from its nearly collisionless state. These measured temperatures are close to extrapolations towards the Sun of Helios measurements.

We also present a statistical study from these in situ electron solar wind parameters, deduced by QTN spectroscopy, and compare the data to other onboard measurements. In addition, we focus on the large-scale solar wind properties. In particular, from the invariance of the energy flux, a direct relation between the solar wind speed and its density can be deduced, as we have already obtained based on Wind continuous in situ measurements (Le Chat et al., Solar Phys., 2012). We study this anti-correlation during the three first solar encounters of PSP.

How to cite: Issautier, K., Liu, M., Moncuquet, M., Meyer-Vernet, N., Maksimovic, M., Bale, S., and Pulupa, M.: Large-scale electron solar wind parameters of the inner heliosphere with Parker Solar Probe/FIELDS, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18573, https://doi.org/10.5194/egusphere-egu2020-18573, 2020.

EGU2020-18888 | Displays | ST1.3

The RPW Time Domain Sampler (TDS) on Solar Orbiter: In-flight performance and first data

Jan Soucek, Ludek Uhlir, Radek Lan, David Pisa, Ivana Kolmasova, Ondrej Santolik, Vratislav Krupar, Oksana Kruparova, Milan Maksimovic, Matthieu Kretzschmar, Yuri Khotyaintsev, and Thomas Chust

The Radio and Plasma Wave instrument (RPW) for Solar Orbiter includes a Time Domain Sampler sub-unit (TDS) designed to capture electromagnetic waveform measurements of high-frequency plasma waves and antenna voltage spikes associated with dust impacts. TDS will digitize three components of the electric field and one magnetic component at 524 kHz sampling rate and scan the obtained signal for plasma waves and dust impact signatures. The main science target of TDS are Langmuir waves observed in the solar wind in association with Type II and Type III solar bursts, interplanetary shocks, magnetic holes, and other phenomena. In this poster, we present the scientific data products provided by the TDS instrument and discuss the first data obtained during the commissioning phase. The first data will be used to evaluate the actual performance of the RPW TDS instrument.

How to cite: Soucek, J., Uhlir, L., Lan, R., Pisa, D., Kolmasova, I., Santolik, O., Krupar, V., Kruparova, O., Maksimovic, M., Kretzschmar, M., Khotyaintsev, Y., and Chust, T.: The RPW Time Domain Sampler (TDS) on Solar Orbiter: In-flight performance and first data , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18888, https://doi.org/10.5194/egusphere-egu2020-18888, 2020.

EGU2020-21075 | Displays | ST1.3

Stream Interaction Regions in the Inner Heliosphere: Insights from the First Four Orbits of Parker Solar Probe

Robert Allen, George Ho, Lan Jian, David Lario, Dusan Odstrcil, Charles Arge, Sam Badman, Stuart Bale, Anthony Case, Eric Christian, Christina Cohen, Carl Henney, Matthew Hill, Shaela Jones, Justin Kasper, Kelly Korreck, David Malaspina, David McComas, Nour Raouafi, and Michael Stevens

The first four orbits of Parker Solar Probe (PSP) consists of many observations of stream interaction regions (SIRs), which form when fast solar wind streams overtake slower solar wind. While it is known that SIRs accelerate ions in the heliosphere and can trigger geomagnetic storms, the temporal and radial evolution of SIRs is still an active topic of research. During the first four orbits of PSP, SIRs were observed by PSP at small heliospheric distances, as well as at 1 au by the Advanced Composition Explorer (ACE), Wind, and Solar Terrestrial Relations Observatory (STEREO) missions. These SIRs are observed not only at different heliospheric distances, but also at different points in the temporal development of the stream interface. Through analyzing the various SIRs together, insight can be gained in regards to the spatial and temporal evolution of SIR characteristics, as well as to the mechanisms of particle acceleration and transport along the SIR interface. The general characteristics of SIRs observed by PSP during the first four orbits are presented, and an in-depth comparison of a few of the SIR events is conducted to further analyze the evolution of SIR streams in the inner heliosphere. These observations show examples of a fast solar wind stream steepening into an SIR, with evidence of locally accelerated particles via compressive mechanisms at the interface distinguishable from observations of particles likely accelerated at shocks formed at larger heliospheric distances.

How to cite: Allen, R., Ho, G., Jian, L., Lario, D., Odstrcil, D., Arge, C., Badman, S., Bale, S., Case, A., Christian, E., Cohen, C., Henney, C., Hill, M., Jones, S., Kasper, J., Korreck, K., Malaspina, D., McComas, D., Raouafi, N., and Stevens, M.: Stream Interaction Regions in the Inner Heliosphere: Insights from the First Four Orbits of Parker Solar Probe, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21075, https://doi.org/10.5194/egusphere-egu2020-21075, 2020.

EGU2020-21407 | Displays | ST1.3

Seeing Helios electron data through the eyes of Solar Orbiter: modelling the angular response of EPD/EPT and its application to the full inversion of Helios events

Daniel Pacheco, Angels Aran, Raul Gomez-Herrero, Neus Agueda, David Lario, Bernd Heber, Blai Sanahuja, Nicolas Wijsen, and Robert F. Wimmer-Schweingruber

The pitch-angle distribution of electron intensities is an essential piece of information in order to understand the transport processes undergone by the particles in their journey from their acceleration sites to the spacecraft and, to infer properties of the particle sources such as their intensity and duration.

In a previous work, we modelled fifteen solar relativistic electron events observed at different heliocentric radial distances by the Helios spacecraft (Pacheco et al. 2019). We used a Monte-Carlo transport model and an inversion procedure to fit the in-situ observations, and inferred both the electron mean free path in the interplanetary space and the injection histories of the electrons at two solar radii from the Sun. We applied a full inversion procedure, that is, we considered both the angular and the energetic responses of the Helios/E6 particle experiment in the modelling of the electron events.

By using the same methodology as previously employed for ACE/EPAM, STEREO/SEPT and Helios/E6 instruments, we have modelled the angular response of the Electron Proton Telescope (EPT) of the Energetic Particle Detector (EPD) on board Solar Orbiter. Here, we present the study of the modelled angular response and its application to several of the solar energetic particle (SEP) events previously modelled as if Solar Orbiter were located at the Helios position. We compare the pitch-angle distributions measured by Solar Orbiter and Helios at different phases of the intensity-time profile of the SEP events, that is, near the particle onset, peak and on the decay of the event, and for different interplanetary magnetic field orientations provided by the Helios measurements.

We found that despite Helios were spinning spacecraft which gathered electron information from eight angular sectors, the four Solar Orbiter/EPD/EPT fields of view will often offer similar angular coverage. We also found that, under specific circumstances, EPT can obtain better pitch angle distribution information than Helios, specifically when the interplanetary magnetic field points away from the ecliptic.

We expect, then, that Solar Orbiter will provide us with numerous and valuable observations that will permit us to untangle the transport effects that electrons, protons and ions suffer in their journey through interplanetary space.

How to cite: Pacheco, D., Aran, A., Gomez-Herrero, R., Agueda, N., Lario, D., Heber, B., Sanahuja, B., Wijsen, N., and Wimmer-Schweingruber, R. F.: Seeing Helios electron data through the eyes of Solar Orbiter: modelling the angular response of EPD/EPT and its application to the full inversion of Helios events, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21407, https://doi.org/10.5194/egusphere-egu2020-21407, 2020.

EGU2020-22532 | Displays | ST1.3

High resolution multi-viewpoint observations of CME kinematics and dynamics

Niclas Mrotzek and Volker Bothmer

Coronal mass ejections (CMEs) are impulsive outbursts of coronal plasma bound in magnetic structures. Their initiation and evolution into the heliosphere covers several orders of magnitude of temporal and spatial scales that can be observed with space-borne extreme ultraviolet imagers, coronagraphs and heliospheric imagers. In this work we present a systematic investigation of the early dynamics of CMEs including their kinematics, orientation and geometrical evolution. For this purpose, a dedicated set of 21 Earth-directed CMEs between July 2011 and November 2012 was selected and analyzed. The CME parametrization is obtained by applying a 3D modelling method, the Graduated Cylindrical Shell (GCS) model, to simultaneous multi-viewpoint observations taken with the SECCHI instrument suite onboard the twin STEREO spacecraft and with the LASCO coronagraphs onboard the SOHO satellite. By using these instruments, the CME dynamics including the kinematics and geometry, are covered in high detail over a wide spatial range. For the majority of events it started in the field of view of EUVI below 2 solar radii and extended into the field of view of HI1 up to 100 solar radii. The results reveal interactions of the CMEs with the ambient solar wind. CME deflections of up to 31° in longitude and 18° in latitude were measured within the first 30 solar radii. Furthermore, evidence of CME oscillations with periods between 29 and 93 minutes were found. The analysis provides important implications for more reliable space weather forecasts and further analysis through the new observations from Parker Solar Probe and Solar Orbiter.

 

How to cite: Mrotzek, N. and Bothmer, V.: High resolution multi-viewpoint observations of CME kinematics and dynamics, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-22532, https://doi.org/10.5194/egusphere-egu2020-22532, 2020.

EGU2020-8398 | Displays | ST1.3

Modelling coronal mass ejection flux ropes signatures using Approximate Bayesian Computation: applications to Parker Solar Probe

Andreas Weiss, Christian Möstl, Teresa Nieves-Chinchilla, Tanja Amerstorfer, Erika Palmerio, Martin Reiss, Rachel Bailey, Jürgen Hinterreiter, Ute Amerstorfer, and Maike Bauer

We present an updated three-dimensional coronal rope ejection (3DCORE) model and an associated pipeline that is capable of producing extremely large ensembles of synthetic in-situ magnetic field measurements from simulated coronal mass ejection flux ropes. The model assumes an empirically motivated torus-like flux rope structure that expands self-similarly and contains an embedded analytical magnetic field. Using an Approximate Bayesian computation (ABC) algorithm we validate the model by showing that it is capable of qualitatively reproducing measured flux rope signatures. The ABC algorithm also gives us uncertainty estimates in the form of probability distributions for all model parameters. We show the first results for applying our model and algorithms to coronal mass ejections observed in situ by Parker Solar Probe, specifically the event on 2018 November 12 at 0.26AU, where we attempt to reproduce the measured magnetic field signatures and furthermore reconstruct the global flux rope geometry.

How to cite: Weiss, A., Möstl, C., Nieves-Chinchilla, T., Amerstorfer, T., Palmerio, E., Reiss, M., Bailey, R., Hinterreiter, J., Amerstorfer, U., and Bauer, M.: Modelling coronal mass ejection flux ropes signatures using Approximate Bayesian Computation: applications to Parker Solar Probe, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-8398, https://doi.org/10.5194/egusphere-egu2020-8398, 2020.

EGU2020-11111 | Displays | ST1.3

Seed Population Pre-Conditioning and Acceleration Observed by Parker Solar Probe

Jonathan Niehof and Nathan Schwadron and the PSP/IS☉IS team

A series of solar energetic particle (SEP) events were observed at Parker Solar Probe (PSP) by the Integrated Science Investigation of the Sun (IS☉IS) during the period from April 18, 2019 through April 24, 2019. The PSP spacecraft was located near 0.48 au from the Sun on Parker spiral field lines that projected out to 1 au within ∼25° of near Earth spacecraft. These SEP events, though small compared to historically large SEP events, were amongst the largest observed thus far in the PSP mission and provide critical information about the space environment inside 1 au during SEP events. During this period the Sun released multiple coronal mass ejections (CMEs). One of these CMEs observed was initiated on April 20, 2019 at 01:25 UTC, and the interplanetary CME (ICME) propagated out and passed over the PSP spacecraft. Observations by the Electromagnetic Fields Investigation (FIELDS) show that the magnetic field structure was mostly radial throughout the passage of the compression region and the plasma that followed, indicating that PSP did not directly observe a flux rope internal to the ICME, consistent with the location of PSP on the flank of the ICME. Analysis using relativistic electrons observed near Earth by the Electron, Proton and Alpha Monitor (EPAM) on the Advanced Composition Explorer (ACE) demonstrates the presence of flare-accelerated seed populations during the events observed. The energy spectrum of the IS☉IS observed seed population below 1 MeV is consistent with the superposition of acceleration processes near the limit of plasma stability. IS☉IS observations reveal the compression and acceleration of seed populations during the passage of the ICME, which is likely a key part of the pre-acceleration process that occurs close to the Sun and pre-conditions the energetic particle acceleration process.

How to cite: Niehof, J. and Schwadron, N. and the PSP/IS☉IS team: Seed Population Pre-Conditioning and Acceleration Observed by Parker Solar Probe, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11111, https://doi.org/10.5194/egusphere-egu2020-11111, 2020.

EGU2020-17554 | Displays | ST1.3

Determination of Solar Energetic Particle anisotropies based on four-sector measurements - Study based on STEREO/SEPT in preperation of SolO/EPT

Maximilian Bruedern, Nina Dresing, Bernd Heber, Lars Berger, Alexander Kollhoff, and Patrick Kühl

With the launch of Solar Orbiter (SolO) Solar Energetic Particles (SEPs) can be observed at a radial distance of 0.284 to 0.9 AU and an inclination out of the ecliptic up to 34 degree. The properties of SEP observations carry information about their source at the Sun as well as their transport through the interplanetary medium. Their energy is mostly determined close to the Sun. As SEPs propagate outward along the Interplanetary Magnetic Field (IMF) the pitch-angle with respect to the local field is systematically focused due to the radially decreasing IMF. However, stochastic changes are induced by scattering at fluctuations of the IMF. Often the first order anisotropy of SEPs is calculated to disentangle imprints of source and transport. Strong anisotropies indicate periods of weak pitch-angle scattering. Although many modeling and observational studies are based on the anisotropy, its uncertainty is often neglected which could result in inaccurate conclusions. Therefore, we propose a new method based on a bootstrap approach where we consider (1) directional instrument responses, (2) the variation of the magnetic field, and (3) the stochastic nature of detection. Here, we present our procedure and final results for different SEP events using measured data of the IMF and particle fluxes by the Solar Electron and Proton Telescope (SEPT) on board of each STEREO spacecraft. The SEPT provides four viewing directions with a view cone of 0.66 sr each on a three axis stabilized spacecraft. In contrast the Electron and Proton Telescope (EPT) on board SolO also consists of four viewing directions but each telescope has a much smaller view cone of 0.21 sr. Due to the very similar instrument setup we can apply our method both to the SEPT and EPT.

How to cite: Bruedern, M., Dresing, N., Heber, B., Berger, L., Kollhoff, A., and Kühl, P.: Determination of Solar Energetic Particle anisotropies based on four-sector measurements - Study based on STEREO/SEPT in preperation of SolO/EPT, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-17554, https://doi.org/10.5194/egusphere-egu2020-17554, 2020.

EGU2020-18502 | Displays | ST1.3

Radial Evolution of Inverted Heliospheric Magnetic Field Between 0.3 and 1 AU

Allan Macneil, Mathew Owens, Robert Wicks, Mike Lockwood, Matthew Lang, and Sarah Bentley

Local inversions, or ‘switchbacks’, in the heliospheric magnetic field (HMF) have recently been identified as prominent features in the inner heliosphere through observations by Parker Solar Probe. These inversions coincide with spikes in radial velocity, and have been interpreted as possibly being the result of jets originating in the corona. While magnetic inversions with similar properties to these jets have also been observed by Helios around its perihelion of ~0.3 AU, inversions with a range of properties and scales have long been studied at distances of 1 AU and beyond. The processes which form the inversions seen outside of 0.3 AU, and whether they are a result of solar wind formation in the solar corona or the transport of solar wind through the heliosphere, are not clear. We present a statistical study on the occurrence of inverted heliospheric magnetic field using Helios 1 observations spanning heliocentric distances 0.3—1 AU. The evolution of inversion occurrence allows us to identify probable locations in the heliosphere where inversions may be produced. Based on these results, we make suggestions as to which processes are most likely responsible for inverted HMF observed between 0.3 and 1 AU.

How to cite: Macneil, A., Owens, M., Wicks, R., Lockwood, M., Lang, M., and Bentley, S.: Radial Evolution of Inverted Heliospheric Magnetic Field Between 0.3 and 1 AU, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18502, https://doi.org/10.5194/egusphere-egu2020-18502, 2020.

EGU2020-20181 | Displays | ST1.3

Acceleration of particles in different parts of erupting coronal mass ejections

Valentina Zharkova, Qian Xia, Joel Dahlin, and Spiro Antiochos

We examine particle energisation in CMEs generated via the breakout mechanism and explore both 2D and 3D MHD configurations. In the breakout scenario, reconnection at a breakout current sheet (CS) initiates the flux rope eruption by destabilizing the quasi-static force balance. Reconnection at the flare CS triggers the fast acceleration of the CME, which forms flare loops below and triggers particle acceleration in flares. We present test-particle studies that focus on two selected times during the impulsive and decay phases of the eruption and obtain particle energy gains and spatial distributions. We find that particles accelerated more efficiently in the flare CS than in the breakout CS even in the presence of large magnetic islands. The maximum particle energy gain is estimated from the energization terms based on the guiding-center approximation. Particles are first accelerated in the CSs (with or without magnetic islands) where Fermi-type acceleration dominates. Accelerated particles escape to the interplanetary space along open field lines rather than trapped in flux ropes, precipitate into the chromosphere along the flare loops, or become trapped in the flare loop top due to the magnetic mirror structure. Some trapped particles are re-accelerated, either via re-injection to the flare CS or through a local betatron-type acceleration associated with compression of the magnetic field. The energy gains of particles result in relatively hard energy spectra during the impulsive phase. During the gradual phase, the relaxation of the shear in magnetic field reduces the guiding magnetic field in the flare CS, which leads to a decrease in particle energization efficiency.

How to cite: Zharkova, V., Xia, Q., Dahlin, J., and Antiochos, S.: Acceleration of particles in different parts of erupting coronal mass ejections, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-20181, https://doi.org/10.5194/egusphere-egu2020-20181, 2020.

EGU2020-5027 | Displays | ST1.3

Energy spectra of carbon and oxygen - Predictions from HELIOS E6 for Solar Orbiter HET

Johannes Marquardt, Bernd Heber, Robert Elftmann, and Robert Wimmer-Schweingruber

Anomalous cosmic rays (ACRs) are well-suited to probe the transport conditions of energetic particles in the innermost heliosphere. We revisit the HELIOS Experiment 6 (E6) data in view of the upcoming Solar Orbiter Energetic Particle Detector (EPD) suite that will perform measurements during a comparable solar minimum within the same distance.

Adapting the HELIOS energy ranges for oxygen and carbon to the ones given by the High Energy Telescope (HET) allows us to determine predictions for the upcoming measurements but also to put constraints on particle transport models that provide new insight into the boundary conditions close to the Sun.

We present here the adapted energy spectra of galactic cosmic ray (GCR) carbon and oxygen, as well as of ACR oxygen during solar quiet time periods between 1975 to 1977. Due to the higher energy threshold of HET in comparison to E6 gradients of about 20% at 15 MeV/nucleon are expected. The largest ACR gradient measured by E6 was obtained to be about 75% between 9 and 13 MeV/nucleon and 0.4 AU and 1 AU.

How to cite: Marquardt, J., Heber, B., Elftmann, R., and Wimmer-Schweingruber, R.: Energy spectra of carbon and oxygen - Predictions from HELIOS E6 for Solar Orbiter HET , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5027, https://doi.org/10.5194/egusphere-egu2020-5027, 2020.

A new method to calculate semi-analytically the radiation efficiency of electromagnetic waves emitted at specific frequencies by electrostatic wave turbulence in solar plasmas with random density fluctuations is presented. It is applied to the case of electromagnetic emissions radiated at the fundamental plasma frequency ωp by beam-driven Langmuir wave turbulence during Type III solar bursts. It is supposed that the main radiation mechanism is the linear conversion of electrostatic to electromagnetic waves on the background plasma density fluctuations, at constant frequency. Due to the presence of such inhomogeneities, the rates of electromagnetic radiation are modified compared to the case of uniform plasmas. Results show that the radiation efficiency of Langmuir wave turbulence into electromagnetic emissions at ωp is nearly constant asymptotically, the electromagnetic energy density growing linearly with time, and is proportional to the average level of density fluctuations. Comparisons with another analytical method developed by the authors and with space observations are satisfactory.

How to cite: Krafft, C. and Volokitin, A.: Efficiency of electromagnetic emission by electrostatic turbulence in solar plasmas with density inhomogeneities, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21572, https://doi.org/10.5194/egusphere-egu2020-21572, 2020.

EGU2020-7595 | Displays | ST1.3

Type III Radio Bursts and Langmuir Wave Excitation

Gottfried Mann, Christian Vocks, Mario Bisi, Eoin Carley, Bartosz Dabrowski, Richard Fallows, Peter Gallagher, Andrzej Krankowski, Jasmina Magdalenic, Christophe Marque, Diana Morosan, Hanna Rothkaehl, and Pietro Zucca

Type III radio bursts are a common phenomenon the Sun’s nonthermal radio radiation. They appear as stripes of enhanced radio emission with a rapid drift from high to low frequencies in dynamic radio spectra. They are considered as the radio signatures of beams of energetic electrons travelling along magnetic field lines from the solar corona into the interplanetary space. With the ground based radio interferometer LOFAR and the instrument FIELDS onboard NASA’s “Parker Solar Probe” (PSP) , type III radio bursts can be observed simultaneously from high (10-240 MHz) to low frequencies (0.01-20 MHz) with LOFAR and PSP’s FIELDs, respectively. That allows to track these electron beams from the corona up to the interplanetary space. Assuming that a population of energetic electrons is initially injected, the velocity distribution function of these electrons evolves into a beam like one. Such distribution function leads to the excitation of Langmuir waves which convert into radio waves finally observed as type II radio bursts. Numerical calculations of the electron-beam-plasma interaction reveal that the Langmuir waves are excited by different parts of the energetic electrons at different distances in the corona and interplanetary space. This result is compared with special type III radio bursts observed with LOFAR and PSP’s FIELDS.

How to cite: Mann, G., Vocks, C., Bisi, M., Carley, E., Dabrowski, B., Fallows, R., Gallagher, P., Krankowski, A., Magdalenic, J., Marque, C., Morosan, D., Rothkaehl, H., and Zucca, P.: Type III Radio Bursts and Langmuir Wave Excitation, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7595, https://doi.org/10.5194/egusphere-egu2020-7595, 2020.

EGU2020-20919 | Displays | ST1.3

Energetic and Suprathermal Particle Composition Measurements from Solar Orbiter

George Ho, Glenn Mason, Robert Wimmer-Schweingruber, and Javier Rodríguez-Pacheco

Particles that have energies of a few times the solar wind plasma energy up to 100s of keV/q are called suprathermal particles. Recent studies have revealed that these particles play a significant role as seed particles for further acceleration to higher energies.  This may occur either close to the Sun in solar energetic particle (SEP) events, but also locally at 1 AU in energetic storm particle events, or even outside 1 AU as ions accelerated in Corotating Interaction Regions. The constituents of this suprathermal ion reservoir are therefore expected to vary in time and space. The composition and spectra of these ions provide us the telltale of their origin and acceleration mechanism.  It is therefore important to make high time resolution measurements of the composition and spectra of this particle population in the inner heliosphere to better characterize its origins and role as a seed population in particle acceleration processes. Because of the vastly different mass-per-charge ratios of the various possible origins of suprathermal ions, we expect to see distinct difference and radial dependencies in their abundances in low-energy accelerated particles in the inner heliosphere.  Here we describe the measurements that we will be making on Solar Orbiter that will make significant contributions to the understanding of the particle population in this largely unexplored energy range.

How to cite: Ho, G., Mason, G., Wimmer-Schweingruber, R., and Rodríguez-Pacheco, J.: Energetic and Suprathermal Particle Composition Measurements from Solar Orbiter, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-20919, https://doi.org/10.5194/egusphere-egu2020-20919, 2020.

EGU2020-10050 | Displays | ST1.3

The RPW Low Frequency Receiver (LFR) on Solar Orbiter: in-situ LF electric and magnetic field measurements of the solar wind expansion

Thomas Chust, Olivier Le Contel, Matthieu Berthomier, Alessandro Retinò, Fouad Sahraoui, Alexis Jeandet, Paul Leroy, Jean-Christophe Pellion, Véronique Bouzid, Bruno Katra, Rodrigue Piberne, Yuri Khotyaintsev, Andris Vaivads, Volodya Krasnoselskikh, Matthieu Kretzschmar, Jan Souček, Ondrej Santolík, Milan Maksimovic, and Stuart D. Bale and the MMS team

Solar Orbiter (SO) is an ESA/NASA mission for exploring the Sun-Heliosphere connection which has been launched in February 2020. The Low Frequency Receiver (LFR) is one of the main subsystems of the Radio and Plasma Wave (RPW) experiment on SO. It is designed for characterizing the low frequency (~0.1Hz–10kHz) electromagnetic fields & waves which develop, propagate, interact, and dissipate in the solar wind plasma. In correlation with particle observations it will help to understand the heating and acceleration processes at work during its expansion. We will present the first LFR data gathered during the Near Earth Commissioning Phase, and will compare them with MMS data recorded in similar solar wind condition.

How to cite: Chust, T., Le Contel, O., Berthomier, M., Retinò, A., Sahraoui, F., Jeandet, A., Leroy, P., Pellion, J.-C., Bouzid, V., Katra, B., Piberne, R., Khotyaintsev, Y., Vaivads, A., Krasnoselskikh, V., Kretzschmar, M., Souček, J., Santolík, O., Maksimovic, M., and Bale, S. D. and the MMS team: The RPW Low Frequency Receiver (LFR) on Solar Orbiter: in-situ LF electric and magnetic field measurements of the solar wind expansion, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-10050, https://doi.org/10.5194/egusphere-egu2020-10050, 2020.

EGU2020-20293 | Displays | ST1.3

Localized magnetic field structures and their boundaries in the near-Sun solar wind from Parker Solar Probe measurements

Vladimir Krasnoselskikh and the PSP Magnetic Structures

One of the most striking discoveries made by Parker Solar Probe during its first three encounters with the Sun is the presence of a multitude of relatively small-scale structures that stand out as sudden deflections of the magnetic. They were named “switchbacks” since some of them show up the full reversal of the radial component of the magnetic field and return to “regular” solar wind conditions. We carried out an analysis of three typical switchback structures having slightly different characteristics: I. Alfv´enic structures, where the variations of the magnetic field components take place conserving the magnitude of the magnetic field constant; II. Compressional, where the magnetic field magnitude varies together with changes of the components of the magnetic field; III. Structures manifesting full reversal of the magnetic field, they may be presumably similar to Alfv´enic, but they are some extremal class of “switchback structures”. We analyzed the properties of the magnetic field of these structures and the characteristics of their boundaries. Our observations and analysis lead to the conclusion that the structures represent localized magnetic field tubes moving with respect to surrounding plasma. The very important characteristic of these tubes consists of the existence of a relatively narrow boundary layer on the surface of the tube that accommodates flowing currents. These currents supposedly closed on the surface of the structure, and typically they have comparable azimuthal and the tube axes aligned components. These currents are supported by the presence of the effective electric field ensured by quite strong gradients of the density, and ion plasma pressure. The ion beta is typically larger than one inside the structure, and less than one outside. Another important feature is an electromagnetic wave accommodated on the surface of the structure. Its role consists in assistance to particles in carrying currents, to electrons parallel to magnetic field, and perpendicular to field to ions.

How to cite: Krasnoselskikh, V. and the PSP Magnetic Structures: Localized magnetic field structures and their boundaries in the near-Sun solar wind from Parker Solar Probe measurements, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-20293, https://doi.org/10.5194/egusphere-egu2020-20293, 2020.

ST1.6 – Exploration of the Heliosphere and the Interstellar Medium with IMAP and Interstellar Probe

EGU2020-3981 | Displays | ST1.6 | Highlight

Interstellar Heliosphere Probes (IHPs)

Qiugang Zong

Supersonic solar wind streams away from the Sun in all directions, interaction with the local interstellar medium to form a giant plasma bubble, which is coined by A. J. Dessler as “heliosphere”. Voyager 1& 2 spacecraft have recently encountered the heliospheric boundaries of this plasma bubble, e.g. the termination shock, heliosheath and heliopause.

To explore further on the dynamics on the heliospheric boundaries, even the hydrogen wall, and the local interstellar medium,  an Interstellar Heliosphere Probes (IHPs)mission have been proposed to Chinese national space agency (two spacecraft, one towards the nose of the heliopause, one opposite). The plan is that the spacecraft is to reach 100AU when it is 100th anniversary of the PR China (2049). Thus, IHP will allow us to discover, explore, and understand fundamental astrophysical processes in the largest plasma laboratory-- the heliosphere.

How to cite: Zong, Q.: Interstellar Heliosphere Probes (IHPs), EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3981, https://doi.org/10.5194/egusphere-egu2020-3981, 2020.

EGU2020-6119 | Displays | ST1.6 | Highlight

Interstellar Probe: The Next Step

Ralph McNutt, Mike Gruntman, Stamatios Krimigis, Edmond Roelof, Pontus Brandt, Kathleen Mandt, Steven Vernon, Michael Paul, and Robert Stough

An “Interstellar Probe” to the nearby interstellar medium has been discussed in the scientific community for almost 60 years. The key concept has always been to depart from the Sun outward “as fast as possible.” Scientific goals have principally focused on heliospheric topics throughout multiple studies, with potential “bonus science” in both astrophysics and planetary science. The passages of Voyagers 1 and 2 into that medium have only raised multiple new questions, rather than “solving” the outstanding question of the interaction of the solar wind with the nearby interstellar medium. In particular, solar activity apparently continues to have an effect on nearby interstellar space, magnetic field changes in crossing from the heliosheath into the local medium are only in magnitude and not direction, and the three-dimensional structure of the energetic neutral atom (ENA) “ribbon” remains unknown. The power levels on the Voyagers continue to decrease toward the operational floor which is likely to be reached within the next five years, limiting the extent of our exploration, and ending heliophysics deep-space measurements beyond the asteroid belt for the indefinite future. The salient question for a dedicated mission is “What can the Interstellar Probe do that no other mission can do?” The answer requires an in-depth look at current capabilities for such a mission, e.g., solar system escape speed, data downlink bandwidth, and mission lifetime with science topics, technological readiness of mission and instrument concepts, and realistic mission costs. To provide technical input to the upcoming Solar and Space Physics Decadal Survey, NASA has contracted with the Johns Hopkins University Applied Physics Laboratory (APL) to execute a “First Pragmatic Interstellar Probe Mission Study.” The effort focuses on near-term engineering readiness (ready for launch by 2030) but also includes input regarding compelling science and associated required measurements and instrumentation, assuming that such a mission would commence during the next Decadal time period. This is not a Science Definition Team (SDT) exercise, but rather an assessment of possibilities. In that spirit, we continue to seek input from across the international space science community regarding potential science goals, measurements, instruments, and their implementation readiness in order to help inform the engineering team in support of a concept mission. We provide a status report on this ongoing effort.

How to cite: McNutt, R., Gruntman, M., Krimigis, S., Roelof, E., Brandt, P., Mandt, K., Vernon, S., Paul, M., and Stough, R.: Interstellar Probe: The Next Step, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6119, https://doi.org/10.5194/egusphere-egu2020-6119, 2020.

 We describe the very local interstellar medium (VLISM)
immediately outside of the outer heliosphere. The VLISM consists 
of four partially ionized clouds - the Local Interstellar Cloud (LIC), 
G cloud, Blue cloud, and Aql cloud that are in contact with the outer 
heliosphere, and ionized gas produced by extreme-UV radiation 
primarily from the star Epsilon CMa. We construct the 
three-dimensional shape of the LIC based on interstellar line 
absorption along 62 sightlines and show that in the direction of 
Epsilon CMa, Beta CMa, and Sirius B the neutral hydrogen column 
density from the center of the LIC looking outward is a minimum. 
We call this region the ``hydrogen hole''. In this direction, the 
presence of Blue cloud absorption and the absence of LIC absorption 
can be simply explained by the Blue cloud lying just outside of the 
heliosphere. We propose that the outer edge of the Blue cloud is a 
Str\"omgren shell driven toward the heliosphere by high pressures in 
the H II region. The outer edges of other clouds facing Epsilon CMa 
are likely also Stromgren shells. Unlike previous models, the LIC
surrounds less than half of the heliosphere.

We find that the vectors of neutral and ionized helium flowing
through the heliosphere are inconsistent with the mean LIC flow 
vector and describe several possible explanations. The ionization
of nearby intercloud gas is consistent with photo-ionization by 
Epsilon CMa and hot white dwarfs without requiring additional 
sources of ionization or million degree plasma. In the upwind 
direction, the heliosphere is passing through an environment of 
several LISM clouds, which may explain the recent influx of 
interstellar grains containing 60Fe from supernova ejecta measured 
in Antarctica snow. The Sun will leave the outer partof the LIC 
in less than 1900 years, perhaps this year, to either enter the 
partially ionized G cloud or a highly ionized intercloud layer. 
The heliosphere will change in either scenario. An instrumented 
deep space probe sending back in situ plasma and magnetic field 
measurements from 500-1,000 AU is needed to understand the 
heliosphere environment rather than integrated data along the 
sightlines to stars.  

How to cite: Linsky, J.: What lies immediately outside of the heliosphere in the very local interstellar medium (VLISM): morphology of the Local Interstellar Cloud, its hydrogen hole, Stromgren Shells, and 60Fe accretion, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1410, https://doi.org/10.5194/egusphere-egu2020-1410, 2020.

EGU2020-5547 * | Displays | ST1.6 | Highlight

Overview of the Instellar Mapping and Acceleration Probe (IMAP) Mission

David McComas

This talk provides an overview of the Interstellar Mapping and Acceleration Probe (IMAP) mission and what we hope and expect to learn from it. IMAP is currently in Phase B and is slated to launch in the fall of 2024. IMAP simultaneously investigates two of the most important, and intimately coupled, research areas in Heliophysics today: 1) the acceleration of energetic particles and 2) the interaction of the solar wind with the local interstellar medium. IMAP’s ten instruments provide a complete set of observations to simultaneously examine the particle injection and acceleration processes at 1 AU while remotely dissecting the global heliospheric interaction and its response to particle populations generated through these processes. For more information about IMAP, see: McComas, D.J., et al., Interstellar mapping and acceleration Probe (IMAP): A New NASA Mission, Space Science Review, 214:116, doi:10.1007/s11214-018-0550-1, 2018.

Open Access: https://link.springer.com/article/10.1007%2Fs11214-018-0550-1 

How to cite: McComas, D.: Overview of the Instellar Mapping and Acceleration Probe (IMAP) Mission, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5547, https://doi.org/10.5194/egusphere-egu2020-5547, 2020.

EGU2020-18777 | Displays | ST1.6

Heliospheric Energetic Neutral Atoms: Numerical Modelling and Comparison with IBEX-Hi data

Igor Baliukin, Vladislav Izmodenov, and Dmitry Alexashov

The Interstellar Boundary Explorer (IBEX) spacecraft has been measuring fluxes of the Energetic Neutral Atoms (ENAs) using the IBEX-Hi (0.3 – 6 keV) instrument since 2008. We have developed the numerical model to calculate ENA hydrogen fluxes employing reconstruction of the trajectories of the atoms (backward in time) from 1 au, where they are observed by IBEX, to the point of their origin in the inner heliosheath, i.e. the region of the perturbed solar wind between the termination shock and the heliopause, where the plasma is strongly heated (T ~ 106 K). Along the trajectory of the atom, differential fluxes of the newly originated ENAs with a given speed are integrated, and losses due to ionization processes (charge exchange with protons and photoionization) are also taken into account.

The key factor in the simulation is a detailed consideration of the supra-thermal component of pickup ions (PUIs) that originate in the region of the supersonic solar wind and picked by the heliospheric magnetic field since this component is «parental» to the ENA. We take into account the supra-thermal component by solving the kinetic equation under the assumption that PUI distribution function is isotropic everywhere in the heliosphere. This method compares favorably with other existing approaches since it is based on fundamental physical laws.

We have calculated model maps of the ENA fluxes based on the previously developed kinetic-MHD models of the SW/LISM interaction (Izmodenov & Alexashov, 2015, 2020), and performed the comparison with IBEX-Hi data. The IBEX-Hi data is one of the few sources of knowledge about the structure of the heliospheric boundary, imposing significant limitations on the parameters of the model of the heliosphere. As a result of the comparison, we concluded that 1) ENA fluxes from the region of the inner heliosheath are extremely sensitive to the form of PUI distribution function; 2) the model of the heliosphere Izmodenov & Alexashov (2020) that differs from the model Izmodenov & Alexashov (2015) in configuration of the interstellar magnetic field reproduces the IBEX-Hi data better; 3) despite a relatively good agreement, there are some qualitative differences between the model calculations and IBEX-Hi data in some energy channels of IBEX-Hi. The reasons for these differences are discussed.

How to cite: Baliukin, I., Izmodenov, V., and Alexashov, D.: Heliospheric Energetic Neutral Atoms: Numerical Modelling and Comparison with IBEX-Hi data, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18777, https://doi.org/10.5194/egusphere-egu2020-18777, 2020.

EGU2020-10815 | Displays | ST1.6

Scattering of Interstellar Neutral Atoms in the Outer Heliosheath

Pawel Swaczyna, David J. McComas, Eric J. Zirnstein, and Jacob Heerikhuisen

Interstellar neutral (ISN) atoms from the very local interstellar medium (VLISM) penetrate the heliosphere and are observed by detectors located near 1 au, e.g., on the Interstellar Boundary Explorer (IBEX), and in the future on the Interstellar Mapping and Acceleration Probe (IMAP). Interpretation of these observations provides insight into the physical conditions in the VLISM but requires modeling of the processes that change distributions of ISN atoms inside the heliosphere and beyond. Here, we focus on the consequences of collisional scattering in the outer heliosheath (OHS), beyond the heliopause. Charge exchange collisions create secondary atoms from the OHS ions, which have a different flow speed and temperature than pristine ISN atoms, especially close to the heliopause. It is widely assumed that these collisions do not change directions of interacting particle velocities. We show that this assumption is not justified for the typical collisions speed in the OHS, and therefore the distribution functions of secondary atoms are different than those calculated without this momentum exchange.  This angular scattering in charge exchange collisions results in secondary atom production terms that show elongated distributions aligned with the relative bulk speed of the parent populations, as well as higher temperatures (up to ~3000 K) and shifted bulk speeds (up to ~2 km s-1). Distributions of ISN atoms are also affected by elastic collisions that similarly show significant scattering for collision energies typical in the OHS. Eventually, these scattering processes modify distributions of ISN atom observed in the heliosphere directly and as pickup ions. These effects may help explain systematical discrepancies between the IBEX data and current models.

How to cite: Swaczyna, P., McComas, D. J., Zirnstein, E. J., and Heerikhuisen, J.: Scattering of Interstellar Neutral Atoms in the Outer Heliosheath, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-10815, https://doi.org/10.5194/egusphere-egu2020-10815, 2020.

EGU2020-2107 | Displays | ST1.6

Mirror instability driven by pickup ions in the outer heliosheath

Amenehsadat Mousavianzehaie, Kaijun Liu, and Kyungguk Min

Kinetic linear instability analysis and hybrid simulations are carried out to examine the role of mirror instability in scattering the pickup ions in the outer heliosheath. The dynamics of these pickup ions is essential to
the understanding of the energetic neutral atom (ENA) ribbon observed by the Interstellar Boundary EXplorer
(IBEX). While most previous studies have focused on the ion cyclotron instability driven by the pickup ions,
recent work based on a simple ring velocity distribution of the pickup ions suggested that the mirror mode can
also be unstable and contribute to the scattering of the pickup ions. The present study performs linear analysis
as well as hybrid simulations for a more realistic, multi-component pickup ion velocity distribution given by the
global modeling of neutral atoms in the heliosphere. The linear theory results indicate unstable mirror modes
with considerable growth rates. The corresponding hybrid simulations further confirm that the mirror modes can
grow and aid the pitch-angle broadening of the pickup ions. So the role of mirror mode should not be ignored in
the stability study of the outer heliosheath pickup ions.

How to cite: Mousavianzehaie, A., Liu, K., and Min, K.: Mirror instability driven by pickup ions in the outer heliosheath, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2107, https://doi.org/10.5194/egusphere-egu2020-2107, 2020.

Interaction between the solar wind and the local interstellar environment has been studied using several observation techniques, including in-situ sampling of the plasma, magnetic field,  energetic ions by the Voyager spacecraft; remote-sensing observations of energetic neutral atoms (IBEX, Cassini); and the primary and secondary populations of interstellar neutral gas (IBEX-Lo). Understanding the processes at the heliospheric boundary and of the conditions outside the heliosphere is typically  done by fitting parameters used in models of this interaction to various observables, including the Voyager crossing distances of the termination shock and the heliopause, the size of the IBEX ribbon and its center directions, the sky distribution of the Lyman-alpha helioglow, and the flux of interstellar gas at 1 au from direct-sampling observations. Typically, it is expected that all or most of these observables are successfully reproduced. Even though the interaction of interstellar neutral gas with the solar wind and solar EUV output is sometimes taken into account, the global heliosphere is usually simulated as a stationary structure, with the solar wind flux, density, and magnetic field variation ignored. However, solar wind is a dynamic phenomenon, which results in variations in the plasma flow both inside and outside the heliopause and in variations of the distance to the heliopause. Based on in-situ solar wind observations, dynamic pressure of the solar wind may change by a factor of 2, which may result in a heliopause distance change by 50%, counting from the lowest-pressure conditions.

Interstellar neutral atoms reaching detectors at 1 au or contributing to the helioglow observed from 1 au need very different times to travel from the interaction  region , typically located at ~1.75 of the heliopause distance to 1 au. While the primary ISN atoms take 3—4 solar cycles to travel from this region to 1 au, with a physical time spread (not an uncertainty!) of about one solar cycle, the atoms from secondary population take as much as 15 solar cycles, with a large spread of 7 solar cycles. This implies that ISN He atoms sampled by IBEX-Lo, as well as those observed as the helioglow, originate from two different and disparate epochs. While it may be expected that the interstellar conditions at a time scale of 200 years are little variable, solar wind is definitely varying, with secular changes superimposed on the solar cycle variation.

Direct-sampling observations provide information on the plasma flow in the OHS inside ~60° around the inflow direction, with well-defined regions of the OHS contributing atoms to individual pixels observed by IBEX and IMAP at different orbits. However, the information obtained is heavily averaged over time, and the epoch  imprinted on these population is very different to the epochs characteristic for in-situ observations from the Voyagers (by 50 to 170 years!)  and remote-sensing observations of the much faster-running energetic neutral atoms.

How to cite: Bzowski, M., Kubiak, M., and Heerikhuisen, J.: What epoch and space region at the heliospheric boundaries are probing IBEX and IMAP observations of interstellar neutral gas populations?, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-9610, https://doi.org/10.5194/egusphere-egu2020-9610, 2020.

In this presentation solar wind electrons and protons are studied which, after their passage over the solar wind termination shock, are convected downstream into the heliosheath. Due to the electric nature of this shock, downstream electrons appear highly energized with non-equilibrium,  kappa-like  distributions . When looking upon the moments of these downstream electrons and protons, it turns out as a surprise that the pressure of the electrons, compared to the protons, is larger by a factor of 2. Then it is taken into account that the pressure of kappa-distributed particles contains contributions from particles with super-luminal velocities which need to be removed from the pressure values . Even when these reductions are carried out, it is manifest that the heliosheath pressures of electrons and protons are of equal orders of magnitudes. In conclusion it is found that there is no pressure deficit in the heliosheath with respect to the ambient interstellar medium.

How to cite: Fahr, H.-J.: The pressure-relevance of suprathermal solar wind electrons for the heliosheath, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-63, https://doi.org/10.5194/egusphere-egu2020-63, 2020.

EGU2020-2187 | Displays | ST1.6

Temporal measurements of the interstellar helium focusing cone by the Magnetospheric Multiscale Mission(MMS)

Roman Gomez, Stephen Fuselier, James Burch, Joey Mukherjee, Carrie Gonzalez, Karlheinz Trattner, Michael Starkey, and Robert Strangeway

The Sun and its associated heliosphere travels through the local interstellar medium (LISM) at 26 km/s.  This results in a flow of neutral particles constantly entering the heliosphere at the same velocity.  Neutral atoms with trajectories close to the Sun, which survive its ionizing radiation environment, become gravitationally attracted to it resulting in a focusing cone, a region of enhanced neutral density, downwind of the Sun.  The increased neutral density in these regions leads to a higher density of pickup ions created by charge-exchange of the neutrals.  In near-Earth orbit, the Magnetospheric Multiscale spacecraft (4 in all) have orbital apogees on the dayside during Earth’s annual encounter with the helium focusing cone (from mid-November to mid-December).  Since launching in March of 2015, regular acquisitions with the Hot Plasma Composition Analyzers (HPCAs) have been conducted, with acquisitions from 2017 through 2019 occurring with a 29 RE apogee, ensuring long intervals in the pristine Solar Wind.   We provide measurements of the focusing cone during the declining phase of the previous solar cycle. These measurements are used to investigate the effect of solar radiation on the focusing cone.

How to cite: Gomez, R., Fuselier, S., Burch, J., Mukherjee, J., Gonzalez, C., Trattner, K., Starkey, M., and Strangeway, R.: Temporal measurements of the interstellar helium focusing cone by the Magnetospheric Multiscale Mission(MMS), EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2187, https://doi.org/10.5194/egusphere-egu2020-2187, 2020.

EGU2020-18647 | Displays | ST1.6

Low energetic Interstellar hydrogen atoms in the heliosphere: Decade of IBEX observations

Olga Katushkina, Vladislav Izmodenov, and André Galli

This work is devoted to the analysis of the interstellar hydrogen fluxes measured by IBEX spacecraft from 2009 to 2018. To calculate the fluxes we use our 3D time-dependent kinetic model of the hydrogen distribution in the heliosphere that takes into account non-maxwellian behavior of the velocity distribution function of hydrogen atoms due to charge exchange with protons at the heliospheric boundary. The temporal variations of the hydrogen fluxes during the entire solar cycle are considered and analyzed by comparison of the IBEX-Lo data and the model results. During solar maximum the measured fluxes are too low, therefore we choose several years 2009-2011 and 2017-2018 when the signal-to-noise ratio is appropriate. A parametric search is performed to determine the influence of different model parameters on the full sky maps of the fluxes. It is found that solar radiation pressure is the most crucial parameter for the position of the maximum fluxes, while the heliolatitudinal variations of the charge exchange ionization rate influence the shape of the maps during solar minimum conditions. The quantitative differences between the data and the model results are demonstrated, and several possible reasons for them are discussed.

How to cite: Katushkina, O., Izmodenov, V., and Galli, A.: Low energetic Interstellar hydrogen atoms in the heliosphere: Decade of IBEX observations, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18647, https://doi.org/10.5194/egusphere-egu2020-18647, 2020.

Solar wind and EUV flux are dominant ionization factors for the interstellar gas inside the heliosphere. They vary in time with the solar cycle and with heliographic latitude. The modulation of the solar ionizing factors affects the fluxes of interstellar neutral (ISN) gas and energetic neutral atoms (ENAs) on their way from heliospheric boundaries to IBEX in the Earth’s vicinity. IBEX has been measuring ISN gas of hydrogen, helium, neon, and oxygen, as well as hydrogen ENAs since the beginning of the solar cycle 24. Most of the ISN gas species observed by IBEX-Lo are prone to variations in time of the in-ecliptic ionization rates. In case of H ENAs, variations of the out-of-ecliptic solar wind are significant for data interpretation.

We present a model of ionization rates based on available observations of the solar wind and the solar EUV flux. We follow methodology discussed by Sokół et al. 2019 (ApJ 872:57), however with data selection revised according to recent data releases. We focus on ionization rates for various species in and out of the ecliptic during the decade of IBEX observations. We discuss similarities and differences in the dominant ionization processes, the latitudinal modulation, and the evolution in time.

How to cite: Sokol, J. M.: Observation-based Ionization Rates during the Decade of IBEX Observations, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6167, https://doi.org/10.5194/egusphere-egu2020-6167, 2020.

The Interstellar Mapping and Acceleration Probe (IMAP) mission by NASA, to be launched in 2024, aims at deepening the understanding of the solar heliosphere by verifying and extending the results obtained from the Interstellar Boundary Explorer (IBEX). IMAP-Lo is a neutral atom imaging and analysis instrument to be used to measure heliospheric Energetic Neutral Atoms (ENAs), mainly H, He, O, Ne in the energy range from 10 eV to 1 keV. One key point of improvement of IMAP-Lo compared to IBEX-Lo is having more accurate calibration methods for ENAs at hand. The IMAP-Lo calibration will be carried out in MEFISTO, a calibration facility for ion and neutral particle instruments at the University of Bern. MEFISTO consists of an ion beam source with energies 10 eV/q - 100 keV/q, a removeable beam neutralization stage for neutral atoms from 10 eV to 3 keV, and a large vacuum test chamber.

The beam neutralization process relies on a charge conversion surface and thus results in an energy loss of about 15%, and energy-dependent transmission. It is therefore essential to be able to measure the effective neutral particle flux and beam energies provided at the exit of the neutraliser to improve the calibration process for an ENA instrument, such as IMAP-Lo.

The Absolute Beam Monitor (ABM) is a new laboratory device dedicated to measure the absolute neutral particle flux and coarse energy distribution of a neutral atom beam. The present prototype consists of a tungsten start surface [GJ(1] and two electron multipliers contained in a box of about 1 dm3 volume. By counting the start, stop and coincidence signal rates we infer the effective number of neutral atoms. In addition, the particle energy is determined by a time-of flight measurement.

We present the measurement principle and demonstrate the validity of the concept with the ABM prototype. Neutral H, He, and O beams at different energies and fluxes have been evaluated in MEFISTO with the ABM prototype. The results are compared with IBEX-Lo calibration measurements.

How to cite: Gasser, J., Wurz, P., and Galli, A.: Absolute Beam Monitor: a device to measure the absolute particle flux of a neutral atom beam – prototype development and testing, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3302, https://doi.org/10.5194/egusphere-egu2020-3302, 2020.

EGU2020-19605 | Displays | ST1.6

Interstellar Probe: Pushing the Frontier of Space Science

Pontus Brandt, Kathleen Mandt, Elena Provoronikova, Casey Lisse, Kirby Runyon, Abigail Rymer, Ralph McNutt, and Michael Paul and the The Interstellar Probe Study Team

An Interstellar Probe beyond our heliosphere in to the largely unexplored interstellar medium (ISM) would be the furthest and boldest step in robotic space exploration ever taken. A dedicated payload of in-situ and remote sensing instruments would uncover the new regime of physics at work in the heliospheric boundary region and offer the first external view of the global heliosphere that is currently missing in the family portrait of all other types of astrospheres observed. Beyond about 400 AU the Probe would reach the ISM and for the first time begin its sampling of the properties of the local interstellar cloud (LIC) that our Sun and neighboring star systems are immersed in.

An Interstellar Probe has been discussed since around 1960 in several NASA and international studies. The compelling science objectives have remained almost unchanged and are focused on understanding the plasma physics in the interaction region between the heliosphere and the ISM. Their importance have been amplified by the recent unexpected findings by the Voyager 1 and 2 spacecraft that are nearing their end of life at less than 150 AU from the Sun. Remote observations in Energetic Neutral Atoms (ENAs) by the NASA IBEX and Cassini missions have made the remarkable discoveries of ENA emission morphologies that have come as a complete surprise and still lack a satisfactory explanation. Hubble Space Telescope observations have now also made it clearer that the Sun is about to exit the LIC and perhaps already has, which is a unique event of astronomical scales that an Interstellar Probe could explore in-situ for the first time. In addition to these top-priority objectives, contributions of unprecedented science value to planetary sciences and astrophysics are possible including flybys of at least one Kuiper Belt Object, in-situ and remote observations of the dust debris disk, and the extra-galactic background light.

Here we review the outstanding questions and current state of understanding of the global heliosphere, the ISM and what planetary and astrophysics augmentations can offer. We summarize the compelling science case for an Interstellar Probe, including a range of possible science payloads and the associated operation scenarios. The results stem from the study of a Pragmatic Interstellar Probe currently underway, funded by NASA, and led by The Johns Hopkins University Applied Physics Laboratory with active participation from a large, international team of scientists and engineers. The study focuses on finding realistic mission architectures among a trade space of propulsion options, trajectories, risks and reliability challenges. The study considers operation out to 1000 AU, a survival probability of 85% over 50 years and electrical power of no less than 400 W at the beginning of mission. Over twice the speed of Voyager 1 (the fastest spacecraft currently) has already been achieved in the design using conventional propulsion, with a direct inject to Jupiter followed by a Jupiter Gravity Assist. In order to provide input requirements to the mission study, several possible payloads with different mass allocations and associated mission requirements, trade-offs and risks have been identified.

How to cite: Brandt, P., Mandt, K., Provoronikova, E., Lisse, C., Runyon, K., Rymer, A., McNutt, R., and Paul, M. and the The Interstellar Probe Study Team: Interstellar Probe: Pushing the Frontier of Space Science, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-19605, https://doi.org/10.5194/egusphere-egu2020-19605, 2020.

EGU2020-17863 | Displays | ST1.6 | Highlight

KET 02: An electron and ion telescope for an interstellar mission

Bernd Heber, Robert Wimmer-Schweingruber, Marlon Köberle, Patrick Kühl, and Stephan Böttcher

The recent AMS 02 measurements show that the very local interstellar spectra (VLIS) for galactic cosmic rays cannot be directly measured at the Earth below rigidities of 40-60 GV because of solar modulation. With Voyager 1and Voyager II crossing the heliopause in 2012 and 2018, in situ experimental LIS data below 100 MeV/nuc constrain computed galactic CR spectra. However, the energy spectra in between can so far only be derived by models. This gap could be narrowed by flying an instrument like the The COsmic and Solar Particle INvestigation Kiel Electron Telescope (COSPIN/KET) that measured protons and alpha-particles in the energy range from about 4 to above 2000 MeV/n and electrons in the range up to 10 GeV in distinguished energy channels. Such a telescope would consist of two parts: 1) an entrance telescope of two semiconductors comprising a silica-aerogel Cherenkov detector with a refractive index of 1.066, selecting particles with speeds v/c = b > 0.938, and 2) a calorimeter, a lead-fluoride Cherenkov detector followed by a scintillation detector measuring escaping particles.

How to cite: Heber, B., Wimmer-Schweingruber, R., Köberle, M., Kühl, P., and Böttcher, S.: KET 02: An electron and ion telescope for an interstellar mission, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-17863, https://doi.org/10.5194/egusphere-egu2020-17863, 2020.

EGU2020-2043 | Displays | ST1.6

PKU Energetic Particle Instrument

Liu Yang, Linghua Wang, Qiugang Zong, Xiangqian Yu, Yongfu Wang, Weighing Shi, and Robert Wimmer-Schweingruber

The PKU energetic particle instrument (EPI) is designed to make measurements of the three-dimensional distribution of suprathermal electrons and ions with good time, energy and angular resolutions in the interplanetary space, respectively, at energies from 20 keV to 1 MeV and from 20 keV to 11 MeV.  The EPI consists of four dual-double-ended foil/magnet semi-conductor telescopes, which cleanly separate electrons in the energy range of 20–400 keV and ions from 20 keV–6 MeV. The output of front detectors is taken in anti-coincidence with center detectors, to achieve the low background. The magnet telescopes also employ the well-established dE/dx vs. total energy approach to determine the nuclear charge and mass of some ion species.

How to cite: Yang, L., Wang, L., Zong, Q., Yu, X., Wang, Y., Shi, W., and Wimmer-Schweingruber, R.: PKU Energetic Particle Instrument, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2043, https://doi.org/10.5194/egusphere-egu2020-2043, 2020.

EGU2020-6657 | Displays | ST1.6

The GEANT4 simulation of PKU Solar Electron and Ions Telescope

Xiangqian Yu, Xin Huang, Linghua Wang, Weihong Shi, Yongfu Wang, Haobo Fu, and Zixuan Liu

The Solar Electron and Ion Telescope (SEIT), proposed by Peking University for a L1 non-spinning spacecraft mission, is designed to provide Omni-directional investigation of Solar energetic electrons and Ions with good time, energy and angular resolution. SEIT consists of multi group two dual double-ended magnet/foil particle telescopes which cleanly separate and measure electrons in the energy range from 50–400 keV and Ions from 60–7000 keV expected to be including protons, C and O. The multi group particle telescopes can cover the Omni-directional space. Each two dual double-ended magnet/foil particle telescopes set-up refers to the detector stack with view cones in two opposite directions: one side (electron side) is consisted of a 300um and a 500um Silicon detector whose distance is only 100um to chive a high performance, the 300um Silicon is on the front and covered by a 5um thin parylene foil to leave the electron spectrum essentially unchanged but stops low energy Ions, the other side (Ions side) is consisted of a 100um and a 500um Silicon detector whose distance is only 100um to chive a high performance and the front of the telescope is surrounded by a magnet to sweep away electrons but lets ions pass. The dead layer of the detector is only 100 Å and each detector is divided into five pixels to chive a high angular resolution. The time resolution is 1s. Simulation shows that the maximum counts of the 20 pixels can reach to 2452, while the minimum energy deposition of the 20 pixels is 300 keV. We now describe the design and GEANT4 simulation of SEIT.

How to cite: Yu, X., Huang, X., Wang, L., Shi, W., Wang, Y., Fu, H., and Liu, Z.: The GEANT4 simulation of PKU Solar Electron and Ions Telescope, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6657, https://doi.org/10.5194/egusphere-egu2020-6657, 2020.

EGU2020-12082 | Displays | ST1.6

The Deflection Magnet Design for PKU Energetic Particle Instrument

Weihong Shi, Xiangqian Yu, Yongfu Wang, Linghua Wang, Xin Huang, and Zixuan Liu

The Energetic Particle Instrument (EPI), proposed by Peking University for a L1 mission, is designed to provide the three-dimensional distribution of suprathermal electrons and ions with good time, energy and angular resolutions in the interplanetary space, respectively, at energies from 20 keV to 1 MeV and from 20 keV to 11 MeV.  The EPI consists of four dual-double-ended foil/magnet semi-conductor telescopes, which cleanly separate electrons in the energy range from 20 to 400 keV and ions from 20 keV to 6 MeV.

The magnet of semi-conductor telescopes consists of four type 677H rare earth permanent magnets and a soft iron frame. Due to the high saturation polarization and high magnetic anisotropy of the Nd2Fe14B strongly magnetic matrix phase, this system can make the magnetic field strong enough to make the electrons deflected.

A frame made of iron-cobalt alloy VACOFLUX 50 will be able to combine two pairs of magnets and cause the magnetic field to decay rapidly in the far field. In this way, the two air gaps in the system can simultaneously provide a deflecting magnetic field for a pair of anti-parallel sensor systems.

How to cite: Shi, W., Yu, X., Wang, Y., Wang, L., Huang, X., and Liu, Z.: The Deflection Magnet Design for PKU Energetic Particle Instrument, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-12082, https://doi.org/10.5194/egusphere-egu2020-12082, 2020.

EGU2020-13050 | Displays | ST1.6

A High Temporal, Spatial and Energy Resolution Grid-based Energetic Neutral Atom (ENA) Imager: the Physical Design

Yongfu Wang, Qiugang Zong, Linghua Wang, Hongfei Chen, and Hong Zou

Substorm is the global disruptive activity in Earth’s magnetotail, including phenomena such as reconnection, plasmoid, flux rope, BBFs, energetic particle injection, and aurora etc. The ground based observations are often hard to determine the time sequences of substorm activities, while the satellite in-situ observations often cannot distinguish between temporal and spatial variations, therefore the global imaging observations are very useful in substorm studies. In this study we demonstrate the physical design of a grid-based energetic neutral atom (ENA) imager that can provide high temporal, spatial and energy resolution ENA imaging of Earth’s magnetotail. The ENA imager takes advantage of spatial Fourier modulation to the ENA fluxes to construct the ENA images, which is inspired by RHESSI. The physical design including imaging process, the charged particle reflector, and the ENA species discrimination etc. are described, along with the engineering progresses.

How to cite: Wang, Y., Zong, Q., Wang, L., Chen, H., and Zou, H.: A High Temporal, Spatial and Energy Resolution Grid-based Energetic Neutral Atom (ENA) Imager: the Physical Design, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-13050, https://doi.org/10.5194/egusphere-egu2020-13050, 2020.

EGU2020-21360 | Displays | ST1.6

The Influence of Space Radiation on the Relative Permittivity of Dielectrics

Siyu Song, Hongfei chen, Xiangqian Yu, and Qiugang Zong

In the study of internal charging of dielectrics inside the spacecraft, we mainly focus on the influence of conductivity of dielectrics induced by space radiation(Radiation Induced Conductivity), and regard the relative permittivity as constant. However, during the ground testing of dielectrics, we found that the relative permittivity of dielectrics decreased after being exposed to electron beams, thus affecting the electric field and the release of charge inside dielectrics. The relative permittivity can gradually returned to the initial state when the radiation stops. In the paper, we present the experiment result and try to give explanations on the mechanism behind this phenomenon.

How to cite: Song, S., chen, H., Yu, X., and Zong, Q.: The Influence of Space Radiation on the Relative Permittivity of Dielectrics, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21360, https://doi.org/10.5194/egusphere-egu2020-21360, 2020.

EGU2020-21672 | Displays | ST1.6

Ring current decay during storm recover phase: RBSP Observation

Ao Chen, Chao Yue, Hongfei Chen, and Qiugang Zong

Ring curent is an important current system in the Earth's magnetosphere. Many charged particles, especially protons and oxygen ions, move around the Earth due to due to electromagnetic drifts, which forms the ring current. During the main phase of a magnetic storm, ring current will grow stronger while it will decay slowly during recover phase. It is thought that charge exchange is the main mechanism of ring current decay [Daglis et al., 1999]. Hereby we use charge exchange theories to calculate charge exchange lifetimes of protons and oxygen ions during recover phase of many storms. Meanwhile, data of RBSP has been used for fitting in order to get real lifetimes of  protons and oxygen ions. We compared the observed lifetimes with the theory prediction and find that  a. the two are close at high L(>4) values and low energy(<55keV) for protons, b. the two are similar in a wide energy(1~600keV) range but a relatively narrow L(different at different energies) range, c. day or night make little difference on the comparison results.

How to cite: Chen, A., Yue, C., Chen, H., and Zong, Q.: Ring current decay during storm recover phase: RBSP Observation, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21672, https://doi.org/10.5194/egusphere-egu2020-21672, 2020.

ST1.7 – Dynamical processes and particle acceleration associated with current sheets, magnetic islands and turbulence-borne structures in different plasmas

EGU2020-1944 | Displays | ST1.7

The Energy Spectrum of Solar Energetic Electron Events

Linghua Wang, Zixuan Liu, Haobo Fu, and Sam Krucker

Solar energetic electron events (SEEs) are one of the most common particle acceleration phenomena occurring at the Sun, and their energy spectrum likely reflects the crucial information on the acceleration. Here we present a statistical survey of the energy spectrum of 160 SEEs measured by Wind/3DP with a clear velocity dispersion at energies of ~1-200 keV from January 1995 through December 2016, utilizing a general spectrum formula proposed by Liu et al. (2000). We find that among these 160 SEEs, 144 (90%) have a power-law (or power-law-like) spectrum bending down at high energies, including 108 (67.5%) double-power-law events, 24 (15%) Ellison-Ramaty-like events and 12 (7.5%) log-parabola events, while 16 (10%) have a power-law spectrum extending to high energies. The average power-law spectral index βis 2.1±0.4 for double-power-law events, 1.7±0.8 for Ellison-Ramaty-like events, and 2.8±0.11 for single-power-law events. For the 108 double-power-law events, the spectral break energy Eranges from 2 keV to 165 keV, with an average of 71±79 keV, while the average spectral index βat energies above E0is 4.4±2.3. Eshows a positive correlation with the electron peak flux at energies above ~40 keV, while βhas a negative correlation with the electron peak flux at energies above ~15 keV.  

How to cite: Wang, L., Liu, Z., Fu, H., and Krucker, S.: The Energy Spectrum of Solar Energetic Electron Events, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1944, https://doi.org/10.5194/egusphere-egu2020-1944, 2020.

EGU2020-1959 | Displays | ST1.7 | Highlight

Large-scale particle acceleration during magnetic reconnection in solar flares

Xiaocan Li and Fan Guo

Magnetic reconnection is a primary driver of magnetic energy release and particle acceleration processes in space and astrophysical plasmas. Solar flares are a great example where observations have suggested that a large fraction of magnetic energy is converted into nonthermal particles and radiation. One of the major unsolved problems in reconnection studies is nonthermal particle acceleration. In the past decade or two, 2D kinetic simulations have been widely used and have identified several acceleration mechanisms in reconnection. Recent 3D simulations have shown that the reconnection layer naturally generates magnetic turbulence. Here we report our recent progresses in building a macroscopic model that includes these physics for explaining particle acceleration during solar flares. We show that, for sufficient large systems, high-energy particle acceleration processes can be well described as flow compression and shear. By means of 3D kinetic simulations, we found that the self-generated turbulence is essential for the formation of power-law electron energy spectrum in non-relativistic reconnection. Based on these results, we then proceed to solve an energetic particle transport equation in a compressible reconnection layer provided by high-Lundquist-number MHD simulations. Due to the compression effect, particles are accelerated to high energies and develop power-law energy distributions. The power-law index and maximum energy are both comparable to solar flare observations. This study clarifies the nature of particle acceleration in large-scale reconnection sites and initializes a framework for studying large-scale particle acceleration during solar flares.

How to cite: Li, X. and Guo, F.: Large-scale particle acceleration during magnetic reconnection in solar flares, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1959, https://doi.org/10.5194/egusphere-egu2020-1959, 2020.

EGU2020-2099 | Displays | ST1.7 | Highlight

Characterization of turbulent magnetic reconnection in solar flares with microwave imaging spectroscopy

Gregory Fleishman, Dale Gary, Bin Chen, Sijie Yu, Natsuha Kuroda, and Gelu Nita

Magnetic reconnection plays a central role in highly magnetized plasma, for example, in solar corona. Release of magnetic energy due to reconnection is believed to drive such transient phenomena as solar flares, eruptions, and jets. This energy release should be associated with a decrease of the coronal magnetic field. Quantitative measurements of the evolving magnetic field strength in the corona are required to find out where exactly and with what rate this decrease takes place. The only available methodology capable of providing such measurements employs microwave imaging spectroscopy of gyrosynchrotron emission from nonthermal electrons accelerated in flares. Here, we report microwave observations of a solar flare, showing spatial and temporal changes in the coronal magnetic field at the cusp region; well below the nominal reconnection X point. The field decays at a rate of ~5 Gauss per second for 2 minutes. This fast rate of decay implies a highly enhanced, turbulent magnetic diffusivity and sufficiently strong electric field to account for the particle acceleration that produces the microwave emission. Moreover, spatially resolved maps of the nonthermal and thermal electron densities derived from the same microwave spectroscopy data set allow us to detect the very acceleration site located within the cusp region. The nonthermal number density is extremely high, while the thermal one is undetectably low in this region indicative of a bulk acceleration process exactly where the magnetic field displays the fast decay. The decrease in stored magnetic energy is sufficient to power the solar flare, including the associated eruption, particle acceleration, and plasma heating. We discuss implications of these findings for understanding particle acceleration in solar flares and in a broader space plasma context.

How to cite: Fleishman, G., Gary, D., Chen, B., Yu, S., Kuroda, N., and Nita, G.: Characterization of turbulent magnetic reconnection in solar flares with microwave imaging spectroscopy, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2099, https://doi.org/10.5194/egusphere-egu2020-2099, 2020.

EGU2020-7605 | Displays | ST1.7

Characteristics of turbulence in transition regions near large-scale boundaries in the solar wind.

Maria Riazantseva, Liudmila Rakhmanova, Georgy Zastenker, Yuri Yermolaev, Irina Lodkina, Jana Safrankova, Zdenek Nemecek, and Lubomir Prech

Fluctuations of solar wind parameters can be strongly affected by the presence of sharp boundaries between different large-scale structures. Turbulence cannot develop freely across such boundaries, just as it could in the undisturbed solar wind. It can lead the growing of fluctuation level and changes in shape and properties of turbulent cascade too. The compression regions, for example  Sheath regions before magnetic clouds, and CIR regions (the compression areas between fast solar wind from coronal holes and slow solar wind  from coronal streamers), are  typical examples of such transitions.  Here we present the analysis of turbulence spectrum changes during crossings of  Sheath and CIR regions. We use unique high time resolution plasma measurements by BMSW instrument at Spektr-R spacecraft in order to consider both MHD and kinetic scales of turbulent cascade.  We analyze the base properties of  turbulence spectra: spectral power and slopes at corresponding scales, break frequency between scales, and also shape of spectra. We began by examining of the case study crossings of the transition regions and then compared statistically the spectral properties in such regions with the same ones in the undisturbed solar wind. We have shown that spectra fall nonlinearly at kinetic scales and become steeper with growing of fluctuation level in transition regions, at the same time the slope of spectra at MHD scale remains almost Kolmogorov. Withal some interesting features can be observed in the vicinity of the break between characteristic scales during crossing of transition regions. The given results reveal the lack of energy balance between MHD and kinetic scales, and can indicate the intensification of dissipation processes and the additional plasma heating in the  transition regions. The work is supported by Russian Science Foundation grant 16-12-10062.

How to cite: Riazantseva, M., Rakhmanova, L., Zastenker, G., Yermolaev, Y., Lodkina, I., Safrankova, J., Nemecek, Z., and Prech, L.: Characteristics of turbulence in transition regions near large-scale boundaries in the solar wind., EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7605, https://doi.org/10.5194/egusphere-egu2020-7605, 2020.

We explore solar wind re-acceleration during their passage through reconnecting current sheets in the interplanetary space using the particle-in-cell approach. We investigate particle acceleration in 3D Harris-type reconnecting current sheets with a single or multiple X-nullpoints taking into account the ambient plasma feedback to the presence of accelerated particles. We also consider coalescent and squashed magnetic islands formed in the current sheets with different magnetic field topologies, thickness, ambient density, and mass ratios. With the PIC approach, we detected distinct populations of two groups of particles, transit and bounced ones, which have very different energy and asymmetric pitch-angle distributions associated with the magnetic field parameters. We present a few cross-sections of the simulated pitch-angle distributions of accelerated particles and compare them with the in-situ observations of solar wind particles. This comparison indicates that locally generated superthermal electrons can account for the counter-streaming ‘strahls’ often observed in pitch-angle distribution spectrograms of the satellites crossing heliospheric current sheets.

How to cite: Xia, Q. and Zharkova, V.: Solar wind re-acceleration in local current sheets and their diagnostics from observations, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-9446, https://doi.org/10.5194/egusphere-egu2020-9446, 2020.

EGU2020-3710 | Displays | ST1.7

Differential rotation of the solar corona and its importance for helioseismology

Vladimir Obridko and Olga Badalyan

It is shown that the solar corona rotates differentially at all heliocentric distances up to the source surface. As the distance increases, the differential rotation gradient decreases, and the rotation becomes more and more rigid. At small distances, the corona at latitudes above $\approx \pm 40^{\circ}$ rotates faster than the photosphere at the same latitudes. The type of the rotation depends also on the phase of the activity cycle. The differential rotation gradient is the largest in the vicinity of the cycle minimum. It is shown that time variations in the coronal rotation characteristics are associated with the tilt of the magnetic equator of the Sun. Based on the concept that the differential rotation of the corona reflects the rotation of deep subphotospheric layers, we compared the changes in the coronal rotation characteristics with distance with the helioseismic data and showed their satisfactory agreement. The results obtained allow us to suggest that the rotation of the solar corona can be used as indicator of the differential rotation of subphotospheric layers and calculate the nature of some current sheets in heliosphere/

How to cite: Obridko, V. and Badalyan, O.: Differential rotation of the solar corona and its importance for helioseismology, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3710, https://doi.org/10.5194/egusphere-egu2020-3710, 2020.

EGU2020-4289 | Displays | ST1.7

Solar and Interplanetary Turbulence: Lagrangian Coherent Structures

Abraham C.L. Chian, Luis R. Bellot Rubio, Heng Q. Feng, Tiago F. P. Gomes, Milan Gosic, Daniela Grasso, Qiang Hu, Kanya Kusano, Rodrigo A. Miranda, Pablo R. Munoz, Erico L. Rempel, David Ruffolo, Suzana S. A. Silva, and De J. Wu

The dynamics of solar and interplanetary plasmas is governed by coherent structures such as current sheets and magnetic flux ropes which are responsible for the genesis of intermittent turbulence via magnetic reconnections in solar supergranular junctions, solar coronal loops, the shock-sheath region of an interplanetary coronal mass ejection, and the interface region of two interplanetary magnetic flux ropes. Lagrangian coherent structures provide a new powerful technique to detect time- or space-dependent transport barriers, and objective (i.e., frame invariant) kinematic and magnetic vortices in space plasma turbulence. We discuss the basic concepts of Lagrangian coherent structures in plasmas based on the computation of the finite-time Lyapunov exponent, the Lagrangian averaged vorticity deviation and the integrated averaged current deviation, as well as their applications to numerical simulations of MHD turbulence and space and ground observations.

How to cite: Chian, A. C. L., Bellot Rubio, L. R., Feng, H. Q., Gomes, T. F. P., Gosic, M., Grasso, D., Hu, Q., Kusano, K., Miranda, R. A., Munoz, P. R., Rempel, E. L., Ruffolo, D., Silva, S. S. A., and Wu, D. J.: Solar and Interplanetary Turbulence: Lagrangian Coherent Structures , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4289, https://doi.org/10.5194/egusphere-egu2020-4289, 2020.

The solar magnetic field (SMF) has historically been considered as dipole in order to build models of the radially expanding corona, that is, the solar wind in the solar minimum. The simplified approach suggests the existence of only one quasi-stationary current sheet (QCS) of solar origin in the heliosphere, namely, the heliospheric current sheet (HCS). However, the SMF becomes more complicated over the solar cycle, comprising higher-order components. The overlapping of the dipole and multipole components of the SMF suggests a formation of more than one QCS in the corona, which may expand further to the heliosphere. We study the impact of the quadrupole and octupole harmonics of the SMF on the formation and spatial characteristics of QCSs, building a stationary axisymmetric MHD model of QCSs in the heliosphere. It is shown that if the dipole component dominates, a single QCS appears in the solar wind at low heliolatitudes as the classic HCS. In other cases, the number of QCSs varies from one to three, depending on the relative input of the quadrupole and octupole components. QCSs possess a conic form and may occur at a wide variety of heliolatitudes. The existence of QCSs opens wide opportunities for explanations of puzzling observations of cosmic rays and energetic particles in the heliosphere and, at the same time, raises a risk of misinterpretation of in situ crossings of QCSs because of mixing up the HCS and higherheliolatitude QCSs, which can be significantly disturbed in the dynamical solar wind.

How to cite: Kislov, R.: Quasi-stationary current sheets of the solar origin in the heliosphere, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-466, https://doi.org/10.5194/egusphere-egu2020-466, 2020.

So far, the problem of a short-term forecast of geomagnetic storms can be considered as solved. Meanwhile, mid-term prognoses of geomagnetic storms with an advance time from 3 hours to 3 days are still unsuccessful (see  https://www.swpc.noaa.gov/sites/default/files/images/u30/Max%20Kp%20and%20GPRA.pdf).

 This fact suggests a necessity of looking for specific processes in the solar wind preceding geomagnetic storms. Knowing that magnetic cavities filled with magnetic islands and current sheets are formed in front of high-speed streams of any type (Khabarova et al., 2015, 2016, 2018; Adhikari et al., 2019), we have performed an analysis of the corresponding ULF variations in the solar wind density observed at the Earth's orbit from hours to days before the arrival of a geoeffective stream or flow. The fact of the occurrence of ULF-precursors of geomagnetic storms was noticed a long time ago (Khabarova 2007; Khabarova & Yermolaev, 2007) and related prognostic methods were recently developed (Kogai et al. 2019), while the problem of automatization of the prognosis remained unsolved.

 A new geomagnetic storm forecast method, which employs a Recurrent Neural Network (RNN) for an automatic pattern search, is proposed. An ability of self-teaching and extracting deeply hidden non-linear patterns is the main advantage of Deep Neural Networks (DNNs) with multiple layers over traditional Machine Learning methods. We show a success of the RNN method, using either the unprocessed solar wind density data or Wavelet analysis coefficients as the input parameter for a DNN to perform an automatic mid-term prognosis of geomagnetic storms.  

Adhikari, L., et al. 2019, The Role of Magnetic Reconnection–associated Processes in Local Particle Acceleration in the Solar Wind, ApJ, 873, 1, 72, https://doi.org/10.3847/1538-4357/ab05c6
Kogai T.G. et al., Pre-storm ULF variations in the solar wind density and interplanetary magnetic field as key parameters to build a mid-term prognosis of geomagnetic storms. “GRINGAUZ 100: PLASMA IN THE SOLAR SYSTEM”, IKI RAS, Moscow, June 13–15, 2018, 140-143, ISBN 978-5-00015-043-6. https://www.researchgate.net/publication/327781146_Pre-storm_ULF_variations_in_the_solar_wind_density_and_interplanetary_magnetic_field_as_key_parameters_to_build_a_mid-term_prognosis_of_geomagnetic_storms
 Khabarova O. V., et al. 2018,  Re-acceleration of energetic particles in large-scale heliospheric magnetic cavities, Proceedings of the IAU, 76-82, https://doi.org/10.1017/S1743921318000285 
Khabarova O.V., et al. Small-scale magnetic islands in the solar wind and their role in particle acceleration. II. Particle energization inside magnetically confined cavities. 2016, ApJ, 827, 122, http://iopscience.iop.org/article/10.3847/0004-637X/827/2/122
Khabarova O., et al. Small-scale magnetic islands in the solar wind and their role in particle acceleration. 1. Dynamics of magnetic islands near the heliospheric current sheet. 2015, ApJ, 808, 181, https://doi.org/10.1088/0004-637X/808/2/181

Khabarova O.V., Current Problems of Magnetic Storm Prediction and Possible Ways of Their Solving. Sun&Geosphere,  http://sg.shao.az/v2n1/SG_v2_No1_2007-pp-33-38.pdf , 2(1), 33-38, 2007

Khabarova O.V. & Yu.I.Yermolaev, Solar wind parameters' behavior before and after magnetic storms, JASTP, 70, 2-4, 2008, 384-390, http://dx.doi.org/10.1016/j.jastp.2007.08.024

How to cite: Fridman, M.: Neural network applications in geomagnetic storm prognosis based on the pre-storm occurrence of magnetic islands in the solar wind, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1848, https://doi.org/10.5194/egusphere-egu2020-1848, 2020.

EGU2020-2102 | Displays | ST1.7

Formation of current sheets and plasmoids within corotating/stream interaction regions

Timofey Sagitov and Roman Kislov

High speed streams originating from coronal holes are long-lived plasma structures that form corotating interaction regions (CIRs) or stream interface regions (SIRs) in the solar wind. The term CIR is used for streams existing for at least one solar rotation period, and the SIR stands for streams with a shorter lifetime. Since the plasma flows from coronal holes quasi-continuously, CIRs/SIRs simultaneously expand and rotate around the Sun, approximately following the Parker spiral shape up to the Earth’s orbit.

Coronal hole streams rotate not only around the Sun but also around their own axis of simmetry, resembling a screw. This effect may occur because of the following mechanisms: (1) the existence of a difference between the solar wind speed at different sides of the stream, (2) twisting of the magnetic field frozen into the plasma, and  (3) a vortex-like motion of the edge of the mothering coronal hole at the Sun. The screw type of the rotation of a CIR/SIR can lead to centrifugal instability if CIR/SIR inner layers have a larger angular velocity than the outer. Furthermore, the rotational plasma movement and the stream distortion can twist magnetic field lines. The latter contributes to the pinch effect in accordance with a well-known criterion of Suydam instability (Newcomb, 1960, doi: 10.1016/0003-4916(60)90023-3). Owing to the presence of a cylindrical current sheet at the boundary of a coronal hole, conditions for tearing instability can also appear at the CIR/SIR boundary. Regardless of their geometry, large scale current sheets are subject to various instabilities generating plasmoids. Altogether, these effects can lead to the formation of a turbulent region within CIRs/SIRs, making them filled with current sheets and plasmoids. 

We study a substructure of CIRs/SIRs, characteristics of their rotation in the solar wind, and give qualitative estimations of possible mechanisms which lead to splitting of the leading edge a coronal hole flow and consequent formation of current sheets within CIRs/SIRs.

How to cite: Sagitov, T. and Kislov, R.: Formation of current sheets and plasmoids within corotating/stream interaction regions, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2102, https://doi.org/10.5194/egusphere-egu2020-2102, 2020.

EGU2020-2210 | Displays | ST1.7

Force balance in current sheets

Olеg Mingalev and Igor Mingalev

A new form of the proton force balance equation for the plasma consisting of collisionless protons and magnetized electrons is obtained. In the equation, the electric field is expressed through the magnetic field and the divergence of electron pressure tensor. The latter is reqiured for the correct determination of boundary conditions in models of current sheets to control the force balance in the models of that type. From this, a general form of the force balance equation in a one-dimensional current sheet is obtained, and effects of electron pressure anisotropy are considered. We reproduce realistic stationary configurations of current sheets using novel methods of numerical simulations and the Vlasov equation solving. 

How to cite: Mingalev, O. and Mingalev, I.: Force balance in current sheets, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2210, https://doi.org/10.5194/egusphere-egu2020-2210, 2020.

EGU2020-3145 | Displays | ST1.7

Evolution of Flare-accelerated Electrons in the Solar Corona and Chromosphere Revealed by Spatially Resolved Microwave and Hard X-Ray Analysis

Natsuha Kuroda, Gregory Fleishman, Dale Gary, Gelu Nita, Bin Chen, and Sijie Yu

Hard X-ray (HXR) and microwave (MW) observations are highly complementary for studying electron acceleration and transport processes in solar flares. In recent years, a new effort has been made in the MW domain using new high-resolution, multifrequency data from The Expanded Owens Valley Solar Array (EOVSA) and a breakthrough numerical modeling infrastructure that enables us to study properties of high-energy electrons in unprecedented cadence and quantitative detail. This study introduces the observation of an M1.2 flare that occurred on 2017 September 9 and analyzes the evolution of the nonthermal electrons in the corona based on EOVSA MW spectral imaging data. We find a significant spectral hardening of the MWemitting nonthermal electron population in the corona, using EOVSA lower-frequency (<7 GHz) observations over a selected 4-minute window of the flare's impulsive phase. We compare this spectral evolution with the evolution of the spectral index of nonthermal electrons emitting in the chromosphere, derived from HXR observations from the Reuven Ramaty High Energy Solar Spectroscopic Imager. We discuss the general picture of the evolution of the nonthermal electron population in this flare by incorporating observations at the two complementary wavelengths. We also make an estimate of the total energy of the nonthermal electrons contained in the observed coronal low-frequency MW source and discuss its temporal evolution.

How to cite: Kuroda, N., Fleishman, G., Gary, D., Nita, G., Chen, B., and Yu, S.: Evolution of Flare-accelerated Electrons in the Solar Corona and Chromosphere Revealed by Spatially Resolved Microwave and Hard X-Ray Analysis, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3145, https://doi.org/10.5194/egusphere-egu2020-3145, 2020.

EGU2020-3730 | Displays | ST1.7

Current sheets, magnetic islands and associated particle acceleration in the solar wind as observed by Ulysses near the ecliptic plane

Olga Malandraki, Olga Khabarova, Roberto Bruno, Gary Zank, and Gang Li and the ISSI-405 team

Recent studies of particle acceleration in the heliosphere have revealed a new mechanism that can locally energize particles up to several MeV/nuc. Stream-stream interactions as well as the heliospheric current sheet – stream interactions lead to formation of large magnetic cavities, bordered by strong current sheets (CSs), which in turn produce secondary CSs and dynamical small-scale magnetic islands (SMIs) of ~0.01AU or less owing to magnetic reconnection. It has been shown that particle acceleration or re-acceleration occurs via stochastic magnetic reconnection in dynamical SMIs confined inside magnetic cavities observed at 1 AU. The study links the occurrence of CSs and SMIs with characteristics of intermittent turbulence and observations of energetic particles of keV-MeV/nuc energies at ~5.3 AU. We analyze selected samples of different plasmas observed by Ulysses during a widely discussed event, which was characterized by a series of high-speed streams of various origins that interacted beyond the Earth’s orbit in January 2005. The interactions formed complex conglomerates of merged interplanetary coronal mass ejections, stream/corotating interaction regions and magnetic cavities. We study properties of turbulence and associated structures of various scales. We confirm the importance of intermittent turbulence and magnetic reconnection in modulating solar energetic particle flux and even local particle acceleration. Coherent structures, including CSs and SMIs, play a significant role in the development of secondary stochastic particle acceleration, which changes the observed energetic particle flux time-intensity profiles and increases the final energy level to which energetic particles can be accelerated in the solar wind.

How to cite: Malandraki, O., Khabarova, O., Bruno, R., Zank, G., and Li and the ISSI-405 team, G.: Current sheets, magnetic islands and associated particle acceleration in the solar wind as observed by Ulysses near the ecliptic plane, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3730, https://doi.org/10.5194/egusphere-egu2020-3730, 2020.

EGU2020-3945 | Displays | ST1.7

Mechanisms of formation of multiple current sheets in the heliospheric plasma sheet

Evgeniy Maiewski, Helmi Malova, Roman Kislov, Victor Popov, Anatoly Petrukovich, and Lev Zelenyi

When spacecraft cross the heliospheric plasma sheet (HPS) that separates large-scale magnetic sectors of the opposite direction in the solar wind, multiple rapid fluctuations of a sign of the radial magnetic field component are observed very often, indicating the presence of multiple current sheets occurring within the HPS. Possible mechanisms of formation of these structures in the solar wind are proposed. Taking into accout that the streamer belt in the solar corona is believed to be the main source of the slow solar wind in the heliosphere, we suggest that the effect of the multi-layered HPS is determined by the extension of many streamer-belt-borne thin current sheets oriented along the neutral line of the interplanetary magnetic field. Within the framework of a proposed MHD model, self-consistent distributions of the key solar wind characteristics which depend on streamer propreties are investigated. It is shown that both single and multiple streamers that are capable of reaching a remote boundary surface can form the observed multiple current sheets with azimuthal currents alternating in direction inside the HPS. The implications of these results for the interpretation of observations in the solar wind are discussed.

How to cite: Maiewski, E., Malova, H., Kislov, R., Popov, V., Petrukovich, A., and Zelenyi, L.: Mechanisms of formation of multiple current sheets in the heliospheric plasma sheet, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3945, https://doi.org/10.5194/egusphere-egu2020-3945, 2020.

EGU2020-5597 | Displays | ST1.7

Observations and Simulations of Reconnecting Current Sheets in the Solar Corona

Spiro Antiochos, Pankaj Kumar, Judy Jarpen, and Joel Dahlin

Jets and mass ejections are ubiquitous features of the Sun’s corona. These explosive dynamics are all believed to be driven by magnetic reconnection at two types of current sheets that form in the solar atmosphere: those that form at magnetic null points and separatrix surfaces, and those, such as the heliospheric current sheet, that form as a result of a large expansion of a bipolar magnetic field. In our breakout model, both types of current sheets are essential for the explosive release of magnetic energy. We report on the first direct observations of reconnection and island formation in a null-point current sheet associated with a large coronal jet. The topology and velocities of the islands are in excellent agreement with our numerical simulations of coronal jets. We discuss the implications of the observations and our models for understanding the energetic particles produced by these events and their release into interplanetary space, as well as the implications for observations by Solar Orbiter and the Parker Solar Probe.

This work was supported by the NASA Living With a Star Program.

 

How to cite: Antiochos, S., Kumar, P., Jarpen, J., and Dahlin, J.: Observations and Simulations of Reconnecting Current Sheets in the Solar Corona, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5597, https://doi.org/10.5194/egusphere-egu2020-5597, 2020.

EGU2020-8461 | Displays | ST1.7

Non-Extensive Statistical Analysis of Energetic Particle Flux Enhancements Caused by the Interplanetary Coronal Mass Ejection-Heliospheric Current Sheet Interaction

Evgenios Pavlos, Olga Malandraki, Olga Khabarova, Leonidas P. Karakatsanis, George P. Pavlos, and George Livadiotis

In this study we use theoretical concepts and computational-diagnostic tools of Tsallis non-extensive statistical theory (Tsallis q-triplet: qsen, qrel, qstat), complemented by other known tools of nonlinear dynamics such as Correlation Dimension and surrogate data, Hurst exponent, Flatness coefficient, and p-modeling of multifractality, in order to describe and understand Small-scale Magnetic Islands (SMIs) structures observed in Solar Wind (SW) with a typical size of ~0.01–0.001 AU at 1 AU. Specifically, we analyze ~0.5 MeV energetic ion time-intensity and magnetic field profiles observed by the STEREO A spacecraft during a rare, widely discussed event. Our analysis clearly reveals the non-extensive character of SW space plasmas during the periods of SMIs events, as well as significant physical complex phenomena in accordance with nonlinear dynamics and complexity theory. As our analysis also shows, a non-equilibrium phase transition parallel with self-organization processes, including the reduction of dimensionality and development of long-range correlations in connection with anomalous discussion and fractional acceleration processes can be observed during SMIs events.

How to cite: Pavlos, E., Malandraki, O., Khabarova, O., Karakatsanis, L. P., Pavlos, G. P., and Livadiotis, G.: Non-Extensive Statistical Analysis of Energetic Particle Flux Enhancements Caused by the Interplanetary Coronal Mass Ejection-Heliospheric Current Sheet Interaction, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-8461, https://doi.org/10.5194/egusphere-egu2020-8461, 2020.

EGU2020-8520 | Displays | ST1.7

Earth’s magnetotail as the reservoir of accelerated single- and multicharged oxygen ions replenishing radiation belts

Elena Parkhomenko, Vladimir Kalegaev, Helmi Malova, Mikhail Panasyuk, Victor Popov, Natalia Vlasova, and Lev Zelenyi

In this work we are studying multicharged oxygen ion acceleration during substorms in the Earth's magnetotail as the source of ring current replenishment by energetic ion population. We used measurements obtained by the CRRES spacecraft for the comparison of experimental spectra of oxygen charge state in the outer region of the ring current and proton radiation belt with model results. We present a numerical model that allows to evaluate acceleration of oxygen ions O+-O+8 in the course of two possible perturbation processes: A) passage of multiple dipolarization fronts in the magnetotail; B) passage of fronts followed by electromagnetic turbulence. It is shown that acceleration processes depend on particle charges and time scale of electric field variations. Oxygen ions O+8 with average initial energies 12 keV are accelerated efficiently during multiple dipolarization processes of type (A) and their energies increased up to 7.4 MeV, whereas ions O+1 with the same energies were energized up to 1.9 МeV. It is shown that oxygen ions O+-O+2 are able to penetrate into the ring/radiation belts region with L between L=4.5 and L=7.5 in the process of plasma transfer on dipolarization fronts. For oxygen O+-O+8 the additional acceleration mechanism is required, such as large-scale electromagnetic turbulence, when the ions can get energies comparable with experimentally observed ones in the indicated range of L shell values. It is shown that the taking into account electromagnetic fluctuations, accompanying magnetic dipolarization, may explain the appearance of oxygen ion flows with energies greater than 3MeV in the near- Earth’s space.

How to cite: Parkhomenko, E., Kalegaev, V., Malova, H., Panasyuk, M., Popov, V., Vlasova, N., and Zelenyi, L.: Earth’s magnetotail as the reservoir of accelerated single- and multicharged oxygen ions replenishing radiation belts, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-8520, https://doi.org/10.5194/egusphere-egu2020-8520, 2020.

EGU2020-9348 | Displays | ST1.7

Small-scale variations of helium abundance in different large-scale solar wind structures

Alexander Khokhlachev, Maria Riazantseva, Liudmila Rakhmanova, Yuri Yermolaev, Irina Lodkina, and Georgy Zastenker

The boundaries between large-scale solar wind streams are often accompanied by sharp changes in helium abundance.  Wherein the high value of relative helium abundance is known as a sign of some large-scale solar wind structures ( for example magnetic clouds). Unlike the steady slow solar wind where the helium abundance is rather stable and equals ~5%, in magnetic clouds its value can grow significantly up to 20% and more, and at the same time helium component becomes more variable.  In this paper we analyze the small-scale variations of solar wind plasma parameters, including the helium abundance variations in different large-scale solar wind streams, especially in magnetic clouds and Sheath regions before them. We use rather long intervals of simultaneous measurements at Spektr-R (spectrometer BMSW) and Wind (spectrometer 3DP) spacecrafts.  We choose the intervals with rather high correlation  level of plasma parameters as a whole to be sure that we are deal with the same plasma stream.  The intervals associated with different large scale-solar wind structures are selected by using of our catalog ftp://ftp.iki.rssi.ru/pub/omni/catalog/. For selected intervals we examine cross-correlation function for Spektr-R and Wind measurements  to reveal the local spatial inhomogeneities by helium abundance which can be observed only at one of spacecrafts, and we determine properties of ones. Such inhomogeneities can be generate by turbulence, which is typically getting more intense in the considered disturbed intervals in the solar wind. The work is supported by Russian Science Foundation grant 16-12-10062.

How to cite: Khokhlachev, A., Riazantseva, M., Rakhmanova, L., Yermolaev, Y., Lodkina, I., and Zastenker, G.: Small-scale variations of helium abundance in different large-scale solar wind structures, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-9348, https://doi.org/10.5194/egusphere-egu2020-9348, 2020.

EGU2020-10039 | Displays | ST1.7

High-Resolution Three-Dimensional MHD Simulations of Plasmoid Formation in Solar Flares

Joel Dahlin, Spiro Antiochos, and C. Richard DeVore

In highly conducting plasmas, reconnecting current sheets are often unstable to the generation of plasmoids, small-scale magnetic structures that play an important role in facilitating the rapid release of magnetic energy and channeling that energy into accelerated particles. There is ample evidence for plasmoids throughout the heliosphere, from in situ observations of flux ropes in the solar wind and planetary magnetospheres to remote-sensing imaging of plasma ‘blobs’ associated with explosive solar activity such as eruptive flares and coronal jets. Accurate models for plasmoid formation and dynamics must capture the large-scale self-organization responsible for forming the reconnecting current sheet. However, due to the computational difficulty inherent in the vast separation between the global and current sheet scales, previous numerical studies have typically explored configurations with either reduced dimensionality or pre-formed current sheets. We present new three-dimensional MHD studies of an eruptive flare in which the formation of the current sheet and subsequent reconnection and plasmoid formation are captured within a single simulation. We employ Adaptive Mesh Refinement (AMR) to selectively resolve fine-scale current sheet dynamics. Reconnection in the flare current sheet generates many plasmoids that exhibit highly complex, three-dimensional structure. We show how plasmoid formation and dynamics evolve through the course of the flare, especially in response to the weakening of the reconnection “guide field” linked to the global reduction of magnetic shear. We discuss implications of our results for particle acceleration and transport in eruptive flares as well as for observations by Parker Solar Probe and the forthcoming Solar Orbiter.

How to cite: Dahlin, J., Antiochos, S., and DeVore, C. R.: High-Resolution Three-Dimensional MHD Simulations of Plasmoid Formation in Solar Flares, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-10039, https://doi.org/10.5194/egusphere-egu2020-10039, 2020.

We present multi-spacecraft observations of pitch-angle distributions (PADs) of suprathermal electrons at ~1 AU which cannot be easily interpreted within the classical paradigm that all suprathermal electrons originate in the solar corona. We suggest that suprathermal electrons accelerated locally in the solar wind are mixed up with the well-known population of electrons of solar origin. Using PIC simulations, we show that key PAD features such as (i) heat flux dropouts and vertical PAD stripes encompassing reconnecting current sheets (RCSs), (ii) bi-directionality of strahls, and (iii) dramatically different PAD patterns observed in different energy channels can be explained by the behavior of electrons accelerated up to hundreds eV directly in the solar wind while thermal particles pass through local RCSs and/or dynamical 3D plasmoids (or 2D magnetic islands).

How to cite: Khabarova, O., Zharkova, V., Xia, Q., and Malandraki, O.: Counterstreaming strahls and dropouts observed in pitch angle distributions of suprathermal electrons as possible signatures of local particle acceleration in the solar wind, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-10819, https://doi.org/10.5194/egusphere-egu2020-10819, 2020.

Spacecraft observations show the radial dependence of the solar wind temperature to be slower than what is expected from the adiabatic cooling of the solar wind expanding radially outwards from the sun. The most viable process considered to explain the observed slower-than-adiabatic cooling is the heating of the solar wind plasma by dissipation of the turbulent fluctuations. In solar wind which is  a collisionless plasma in turbulent state, macroscopic energy is cascaded down to kinetic scales where kinetic plasma processes can finally dissipate the energy into heat. The kinetic scale plasma processes responsible  for the dissipation of energy are, however, not well understood. A number of observational and simulation studies have shown that the heating is concentrated in and around current sheets self-consistently formed at kinetic scales. The current sheets contain free energy sources for the growth of plasma instabilities which can serve as the mechanism of the collisionless dissipation. A detailed information on the free energy sources contained in these current sheets of plasma turbulence is lacking but essential to understand the role of  plasma instabilities in collisionless dissipation.

We carry out 2-D hybrid simulations of kinetic plasma turbulence to study in detail free energy sources available in the current sheets formed in the turbulence. We focus on three free energy sources, namely, plasma density gradient, velocity gradients for both ions and electrons and ion temperature anisotropy. Our simulations show formation of current sheets in which electric current parallel to the externally applied magnetic field flows in a thickness of the order of an ion inertial length. Inside a current sheet, electron flow velocity dominates ion flow velocity in the parallel direction resulting in a larger cross-gradient of the former. The perpendicular electron velocity inside a current sheet also has variations sharper than the corresponding ion velocity. Cross gradients in plasma density are weak (under 10 % variation inside current sheets). Ion temperature is anisotropic in current sheets. Thus the current in the sheets is primarily due to electron shear flow. A theoretical model to explain the difference between electron and ion velocities in current sheets is developed. Spacecraft observations of electron shear flow in space plasma turbulence will be pointed out.   

These results suggest that the current sheets formed in kinetic plasma turbulence are close to the force free equilibrium rather than the often assumed Harris equilibrium.  This demands investigations of the linear stability properties and nonlinear evolution of force free current sheets with temperature anisotropy. Such studies can provide effective dissipation coefficients to be included in macroscopic model of the solar wind evolution.   

How to cite: Jain, N. and Buechner, J.: Free energy sources in kinetic scale current sheets formed in collisionless plasma turbulence, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21518, https://doi.org/10.5194/egusphere-egu2020-21518, 2020.

EGU2020-19937 | Displays | ST1.7

Mapping magnetic field and relativistic electrons along a solar flare current sheet

Gregory Fleishman, Bin Chen, Gary Dale, and Gelu Nita et al.

In the standard model of solar flares, a large-scale reconnection current sheet (RCS) is postulated as the central engine for powering the flare energy release and accelerating particles. However, where and how the energy release and particle acceleration occur remain unclear due to the lack of measurements for the magnetic properties of the RCS. Here we report the first measurement of spatially-resolved magnetic field and flare-accelerated relativistic electrons along a large-scale RCS in a solar flare. The measured magnetic field profile shows a local maximum where the reconnecting field lines of opposite polarities closely approach each other, known as the reconnection X point. The measurements also reveal a local minimum near the bottom of the RCS above the flare loop-top, referred to as a "magnetic bottle". This spatial structure agrees with theoretical predictions and numerical modeling results. A strong reconnection electric field of over 4000 V/m is inferred near the X point. This location, however, shows a local depletion of microwave-emitting relativistic electrons. In contrast, the relativistic electrons concentrate at or near the magnetic bottle structure, where more than 99% of them reside at each instant. Our observations suggest crucial new input to the current picture of high energy electron acceleration.

How to cite: Fleishman, G., Chen, B., Dale, G., and Nita et al., G.: Mapping magnetic field and relativistic electrons along a solar flare current sheet, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-19937, https://doi.org/10.5194/egusphere-egu2020-19937, 2020.

EGU2020-8189 | Displays | ST1.7

General Spectrum Fitting for Energetic Particles

Zixuan Liu, Linghua Wang, Haobo Fu, Krucker Sam, and Wimmer-Schweingruber Robert

We propose a general fitting formula of energy spectrum of suprathermal particles, J=AE-β1[1+(E/E0)α](β1-β2)/α, where J is the particle flux (or intensity), E is the particle energy, A is the amplitude coefficient, E0 represents the spectral break energy, α (>0) describes the sharpness of energy spectral break around E0, and the power-law index β12) gives the spectral shape before (after) the break.  When α tends to infinity (zero), this spectral formula becomes a classical double-power-law (logarithmic-parabola) spectrum. When both β2 and E0 tend to infinity, this formula can be simplified to an Ellison-Ramaty-like equation. Under some other specific parameter conditions, this formula can be transformed to a Kappa or Maxwellian function. Considering  the uncertainties both in particle intensity and energy, we fit this general formula well to the representative energy spectra of various suprathermal particle phenomena including solar energetic particles (electrons, protons,  3He and heavier ions), shocked particles, anomalous cosmic rays, hard X-rays, solar wind suprathermal particles, etc. Therefore, this general spectrum fitting formula would help us to comparatively examine the energy spectrum of different suprathermal particle phenomena and understand their origin, acceleration and transportation.

How to cite: Liu, Z., Wang, L., Fu, H., Sam, K., and Robert, W.-S.: General Spectrum Fitting for Energetic Particles, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-8189, https://doi.org/10.5194/egusphere-egu2020-8189, 2020.

EGU2020-10694 | Displays | ST1.7

Current sheets and waves inside magnetosheath jets

Primoz Kajdic, Xochitl Blanco-Cano, Tomas Karlsson, and Savvas Raptis

Magnetosheath jets were first discovered by Nemeček et al., 1998 and were defined as events in the magnetosheath that exhibit ion fluxes at least 50 % higher than those in the surrounding plasma. Later authors used different physical quantities in order to study these phenomena, such as velocity, density and dynamic pressure. Magnetosheath jets are usually found in the parts of the magnetosheath that are magnetically connected to the quasi-parallel sections of the Earth's bow-shock, although jets in the so called quasi-perpendicular magnetosheath have also been observed. There are several proposed mechanisms for their formation, the most accepted ones being the formation due to the rippled surface of quasi-parallel shocks, and the transmission of upstream large-amplitude magnetic structures (SLAMS) across the bow-shock. Here we make use of the Magnetospheric Multiscale Mission burst mode data in order to present observations of waves and current sheets inside magnetosheath jets. We show that these phenomena occur commonly and provide additional mechanisms that dissipate the solar wind kinetic energy downstream of the bow-shock.

How to cite: Kajdic, P., Blanco-Cano, X., Karlsson, T., and Raptis, S.: Current sheets and waves inside magnetosheath jets, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-10694, https://doi.org/10.5194/egusphere-egu2020-10694, 2020.

EGU2020-10698 | Displays | ST1.7

Peculiarities of quasi-adiabatic dynamics of charged particles in current sheets with magnetic shear

Helmi Malova, Victor Popov, and Elena Grigorenko

The dynamics of quasi-adiabatic ions in the current sheet (CS) of the Earth's magnetotail during substorms is investigated, when CS is thinned, and the scale of the magnetic inhomogeneity is about proton gyroradius. Experimental data indicate sometimes that the shear magnetic component from the interplanetary magnetic field can penetrate within the magnetosphere and support self-consistent currents. The numerical model of CS is constructed, taking into account the normal magnetic component and shear component of three types: 1) constant profile within CS, 2) bell-shaped and 3) antisymmetric ones. Poincaré maps characterizing quasi-adiabatic dynamics of ions are studied. The jumps of quasi-adiabatic invariant of motion are calculated, and comparison is made with the case of the absent magnetic shear. It is shown that the presence of constant and bell-shaped magnetic components in the current sheet leads to the asymmetric scattering of particles in the North-South direction after their interaction with CS and corresponding differences in the structure of the phase space. It is demonstrated that the jumps of the approximate invariant Iz depend on the location of the plasma source in the Northern or Southern hemispheres.  At the same time, for configurations with anti-symmetric shear component, the particle scattering near the sheet plane is negligible, therefore in this case it is no scattering asymmetry, and the jumps of invariants of motion are smallest; they do not depend on the value of the magnetic field amplitude inside CS. Applications of these results to interpret experimental observations are discussed.

How to cite: Malova, H., Popov, V., and Grigorenko, E.: Peculiarities of quasi-adiabatic dynamics of charged particles in current sheets with magnetic shear, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-10698, https://doi.org/10.5194/egusphere-egu2020-10698, 2020.

EGU2020-11700 | Displays | ST1.7

Current sheets with multi-component plasma in planetary magnetospheres

Victor Popov, Vladimir Domrin, Helmi Malova, Elena Grigorenko, and Anatoly Petrukovich

The self-consistent hybrid model of a thin current sheet with a thickness about several proton gyroradii in a space plasma is proposed, taking into account multicomponent collisionless space plasma. Several plasma components are often presented in planetary magnetotails (Hermean, Martian, Terrestrial and other ones). Influence of heavy oxygen ions with different properties on current sheet structure is analyzed. It is shown that high relative concentrations of oxygen ions, as well as their relatively high temperatures and flow drift speeds lead to a significant thickening of the sheet and a formation of an additional embedding scale. For some real parameters the profiles of self-consistent current densities and magnetic field have symmetrical jumps of derivatives, i.e. sharp changes of gradients. The comparison is made with observations in the Martian magnetosphere. The qualitative agreement of simulation results with observational data is shown.

How to cite: Popov, V., Domrin, V., Malova, H., Grigorenko, E., and Petrukovich, A.: Current sheets with multi-component plasma in planetary magnetospheres , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11700, https://doi.org/10.5194/egusphere-egu2020-11700, 2020.

ST1.8 – Winds of change: New perspectives on the properties of solar transients throughout the heliosphere

Atmospheric science and forecasting, concerned with a volume ~1013 m3, is underpinned by an extensive observational network; point measurements at 10k land-based stations, 4k ships and buoys, and around 1k dedicated balloon launches and aircraft; remote sensing from hundreds of radars and 10 dedicated operational satellites providing independent “look directions” through the atmosphere. By comparison, the heliosphere is a vastly under-sampled system. In the ~1028 m3 volume contained within Earth orbit, there has been a maximum of 5 simultaneous point measurements and remote sensing from (at most) 3 simultaneous vantage points. This makes it difficult to reliably interpret observations in terms of the 3-dimensional structure and extent of solar wind transients. Solar Orbiter, Parker Solar Probe, STEREO-A and L1 monitors (and a possible future L5 monitor), as well as more limited solar wind measurements from planetary/cometary missions, will shortly provide unprecedented observational coverage and thus a unique opportunity to better understand solar wind transients. Nevertheless, sampling will remain sparse and connecting point observations and interpreting remote sensing observations will remain ambiguous. Global models of the solar wind can aid greatly in this regard. This talk will summarise how observations and models can be best combined to exploit the strengths of both, and what we can learn about solar wind transients.

How to cite: Owens, M.: Connecting the dots: Multi-point observations for solar wind science and forecasting, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2643, https://doi.org/10.5194/egusphere-egu2020-2643, 2020.

EGU2020-3172 | Displays | ST1.8

A New Model to Describe the Magnetic Structure of CMEs

Nada Al-Haddad and Noé Lugaz

The structure of coronal mass ejections (CMEs) has been the center of numerous studies over the past few decades. Defining the magnetic field orientation locally and globally has proven to be a challenging problem, due to the limited nature of observations that we have, as well as our reliance on the current paradigm of highly-twisted flux ropes. Studies suggest that not all CMEs measured in situ fit within the simple twisted and well-organized flux rope topology. Additionally, many of the events that can be well fitted by existing static flux rope models, do not have as simple a structure as that assumed by the models. This is clear from remote observations and multi-spacecraft measurements. With the wealth of data that we have today, as well as the affluence of research and analysis performed over the last 40 years, it is dues time to present an alternative paradigm, that better represents those data. In this work, we discuss this new paradigm and the literature leading to it. 

How to cite: Al-Haddad, N. and Lugaz, N.: A New Model to Describe the Magnetic Structure of CMEs, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3172, https://doi.org/10.5194/egusphere-egu2020-3172, 2020.

EGU2020-3341 | Displays | ST1.8

Relating CME density derived from remote sensing data to CME sheath solar wind plasma pile up as measured in-situ

Manuela Temmer, Lukas Holzknecht, Mateja Dumbovic, Bojan Vrsnak, Nishtha Sachdeva, Stephan Heinemann, Karin Dissauer, Camilla Scolini, Eleanna Asvestari, Astrid Veronig, and Stefan Hofmeister

For better estimating the drag force acting on coronal mass ejections (CMEs) in interplanetary space and ram-pressure at planets, improved knowledge of the evolution of CME density/mass is highly valuable. We investigate a sample of 29 well observed CME-ICME events, for which we determine the de-projected 3D mass (STEREO-A and -B data), and the CME volume using GCS modeling (STEREO, SoHO). Expanding the volume to 1AU distance, we derive the density and compare the results to in-situ proton density measurements separately for the ICME sheath and magnetic structure. A fair agreement between calculated and measured density is derived for the magnetic structure as well for the sheath if taking into account mass pile up of solar wind plasma. We give evidence and observational assessment that during the interplanetary propagation of a CME 1) the magnetic structure has rather constant mass and 2) the sheath region at the front of the driver is formed from piled-up mass that is rather depending on the solar wind density ahead of the CME, than on the CME speed. 

How to cite: Temmer, M., Holzknecht, L., Dumbovic, M., Vrsnak, B., Sachdeva, N., Heinemann, S., Dissauer, K., Scolini, C., Asvestari, E., Veronig, A., and Hofmeister, S.: Relating CME density derived from remote sensing data to CME sheath solar wind plasma pile up as measured in-situ , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3341, https://doi.org/10.5194/egusphere-egu2020-3341, 2020.

EGU2020-5543 | Displays | ST1.8

Can we explain the low geo-effectiveness of the fast halo CMEs in 2002 with EUHFORIA?

Brigitte Schmieder, Stefaan Poedts, and Christine Verbeke

In 2002 (Cycle 23), a weak impact on the magnetosphere of the Earth has been reported for six halo CMEs related to six X-class flares and with velocities higher than 1000 km/s. The registered Dst minima are all between -17 nT and -50 nT.  A study of the Sun-Earth chain of phenomena related to these CMEs reveals that four of them have a source at the limb and two have a source close to the solar disk center (Schmieder et al., 2020). All of CME magnetic clouds had a low z‑component of the magnetic field, oscillating between positive and negative values.

We performed a set of EUHFORIA simulations in an attempt to explain the low observed Dst and the observed magnetic fields. We study the degree of deviation of these halo CMEs from the Sun-Earth axis and as well as their deformation and erosion due to their interaction with the ambient solar wind (resulting in magnetic reconnections) according to the input of parameters and their chance to hit other planets. The inhomogeneous nature of the solar wind and encounters  are also important parameters influencing the impact of CMEs on planetary magnetospheres.

 

How to cite: Schmieder, B., Poedts, S., and Verbeke, C.: Can we explain the low geo-effectiveness of the fast halo CMEs in 2002 with EUHFORIA?, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5543, https://doi.org/10.5194/egusphere-egu2020-5543, 2020.

EGU2020-21455 | Displays | ST1.8

An Adaptive Prediction System for Specifying Solar Wind Conditions Near the Sun

Martin Reiss, Peter MacNeice, Karin Muglach, Nick Arge, Christian Möstl, Pete Riley, Jürgen Hinterreiter, Rachel Bailey, Andreas Weiss, Mathew Owens, Tanja Amerstorfer, and Ute Amerstorfer

The ambient solar wind flows and fields influence the complex propagation dynamics of coronal mass ejections in the interplanetary medium and play an essential role in shaping Earth's space weather environment. A critical scientific goal in the space weather research and prediction community is to develop, implement and optimize numerical models for specifying the large-scale properties of solar wind conditions at the inner boundary of the heliospheric model domain. Here we present an adaptive prediction system that fuses information from in situ measurements of the solar wind into numerical models to better match the global solar wind model solutions near the Sun with prevailing physical conditions in the vicinity of Earth. In this way, we attempt to advance the predictive capabilities of well-established solar wind models such as the Wang-Sheeley-Arge model. We perform a statistical analysis of the resulting solar wind predictions for the years 2006 to 2015. The proposed prediction scheme improves all the coronal/heliospheric model combinations investigated by approximately 15-20 percent in terms of various comprehensive prediction validation measures. We discuss why this is the case, and conclude that our findings have important implications for future practice in applied space weather research and prediction.

How to cite: Reiss, M., MacNeice, P., Muglach, K., Arge, N., Möstl, C., Riley, P., Hinterreiter, J., Bailey, R., Weiss, A., Owens, M., Amerstorfer, T., and Amerstorfer, U.: An Adaptive Prediction System for Specifying Solar Wind Conditions Near the Sun, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21455, https://doi.org/10.5194/egusphere-egu2020-21455, 2020.

EGU2020-5958 | Displays | ST1.8

A Survey of Interplanetary Small Flux Ropes at Mercury

Réka Winslow, Amy Murphy, Nathan Schwadron, Noé Lugaz, Wenyuan Yu, Charles Farrugia, and Jonathan Niehof

Small flux ropes (SFRs) are interplanetary magnetic flux ropes with durations from a few minutes to a few hours. We have built a comprehensive catalog of SFRs at Mercury using magnetometer data from the orbital phase of the MESSENGER mission (2011-2015). In the absence of solar wind plasma measurements, we developed strict identification criteria for SFRs in the magnetometer observations, including conducting force-free field fits for each flux rope. We identified a total of 48 events that met our strict criteria, with events ranging in duration from 2.5 minutes to 4 hours. Using superposed epoch analysis, we obtained the generic SFR magnetic field profile at Mercury. Due to the large variation in Mercury's heliocentric distance (0.31-0.47 AU), we split the data into two distance bins. We found that the average SFR profile is more symmetric "farther from the Sun", in line with the idea that SFRs form closer to the Sun and undergo a relaxation process in the solar wind. Based on this result, as well as the SFR durations and the magnetic field strength fall-off with heliocentric distance, we infer that the SFRs observed at Mercury are expanding as they propagate with the solar wind. We also determined that the SFR occurrence frequency is nearly four times as high at Mercury as for similarly detected events at 1 AU. Most interestingly, we found two SFR populations in our dataset, one likely generated in a quasi-periodic formation process near the heliospheric current sheet, and the other formed away from the current sheet in isolated events.

How to cite: Winslow, R., Murphy, A., Schwadron, N., Lugaz, N., Yu, W., Farrugia, C., and Niehof, J.: A Survey of Interplanetary Small Flux Ropes at Mercury, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5958, https://doi.org/10.5194/egusphere-egu2020-5958, 2020.

Recent advances in kinetic modeling reveal essential properties of the suprathermal populations opening perspectives for a realistic interpretation of their implications. Of particular importance are the suprathermal electron strahl (or beaming) populations, guided by the heliospheric magnetic field as kinetic-scale traces of the continuous solar outflows. We outline the main implications of the strahls by connecting their signatures in the velocity distributions with macroscopic properties of the solar wind, and processes conditioning their relaxation via coherent or non-coherent radiative emissions. The electron strahls may also help understanding major changes in the magnetic field topology in the outer corona, as shown by the most recent data from Solar Parker Probe, and during energetic (transient) events like coronal mass ejections, implying or not reconnection, but leading to strong interaction regions and shocks. 

How to cite: Lazar, M.: Suprathermal electron strahls. From small scale modeling to heliospheric implications, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5845, https://doi.org/10.5194/egusphere-egu2020-5845, 2020.

EGU2020-966 | Displays | ST1.8

Coupling the MULTI-VP model with EUHFORIA

Evangelia Samara, Jasmina Magdalenic, Rui F. Pinto, Veronika Jercic, Camilla Scolini, Luciano Rodriguez, and Stefaan Poedts

The EUropean Heliospheric FORecasting Information Asset (EUHFORIA) is a new 3D magnetohydrodynamic (MHD) space weather prediction tool (Pomoell and Poedts, 2018). EUHFORIA models solar wind and coronal mass ejections (CMEs) all the way from the Sun to 2 AU. It consists of two different domains; the coronal part, which extends from the solar surface to 0.1 AU and the heliospheric part, which covers the spatial domain from 0.1 AU onwards. For the reconstruction of the global solar corona, the empirical Wang-Sheeley-Arge (WSA, Arge, 2003) model is currently used, in combination with the potential field source surface (PFSS) model and the Schatten current sheet (SCS) model, in order to reconstruct the magnetic field up to 0.1 AU and produce the plasma boundary conditions required by the 3D MHD heliospheric part to initiate. In the framework of the ongoing validation of the solar wind modeling with EUHFORIA, we implemented and tested a different coronal model, the so-called MULTI-VP model (Pinto and Rouillard, 2017). First results and comparisons of EUHFORIA modeled output at Earth produced by employing the WSA and MULTI-VP coronal models, will be presented.

How to cite: Samara, E., Magdalenic, J., Pinto, R. F., Jercic, V., Scolini, C., Rodriguez, L., and Poedts, S.: Coupling the MULTI-VP model with EUHFORIA, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-966, https://doi.org/10.5194/egusphere-egu2020-966, 2020.

EGU2020-17669 | Displays | ST1.8

Modeling and forecasting the background solar wind with data-driven physics-based models

Michael Lavarra, Rui Pinto, Alexis Rouillard, Athanasios Kouloumvakos, Alessandro Bemporad, Charles Nickolos Arge, Matthieu Alexandre, and Vincent Genot

The quasi-steady solar wind flow is a key component of space weather, being the source of corotating density structures that perturb planetary atmospheres and affect the propagation of impulsive perturbations (such as CME). Fast and slow wind streams develop at different places in the solar atmosphere, reflecting the global distribution of the coronal magnetic field during solar cycle and its consequences for heat and mass transport across the corona. I will present recent advances on global solar wind simulations that provides robust and fully physics-based predictions of the structure and physical parameters of the solar wind based on a multi-1D approach (MULTI-VP, ISAM). Such advances relate to the driving the models with time-dependant magnetogram data, to the inclusion of transient heating phenomena, and to switching from a fluid to a multi-species description of the solar wind. The model was also driven by daily synchronic magnetograms (ADAPT) for a full solar rotation and the simulation results were compared to UVCS plane-of-sky data.The simulations produce a large range of synthetic observables (e.g multi-spacecraft in-situ measurements, white-light and EUV imagery) meant to be compared to data from current and future missions (e.g Solar Orbiter and Parker Solar Probe), and to establish physiccal connections between remote observation of the solar surface and corona and the interplanetary medium.

How to cite: Lavarra, M., Pinto, R., Rouillard, A., Kouloumvakos, A., Bemporad, A., Arge, C. N., Alexandre, M., and Genot, V.: Modeling and forecasting the background solar wind with data-driven physics-based models, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-17669, https://doi.org/10.5194/egusphere-egu2020-17669, 2020.

EGU2020-15568 | Displays | ST1.8

Unsupervised classification of the solar wind using Self-Organizing Maps

Jorge Amaya, Romain Dupuis, and Giovanni Lapenta

During the past decades different methods of classification of the solar wind have been proposed. These include simple models separating the “fast” from “slow” flows (Arya and Freeman, 1991, Yordanova et al., 2009, among others), complex empirical methods grouping its properties in multiple categories associated to its origin in the solar atmosphere (Xu et Borovsky, 2015), and more recently probabilistic classifications based on Gaussian processes (Camporeale et al., 2017).

Solar wind classification serves four main purposes: 1) statistical analysis of different wind types, 2) interpretation of observations in the magnetosphere, 3) diagnostics of physical processes in the Sun, and 4) identification of solar cycle effects on the Earth’s plasma environment. In this work, instead of using empirical methods, we use the machine learning technique known as Self-Organizing Maps (SOM) to automatically classify the solar wind at 1AU, without human intervention, using observations gathered by the ACE mission.

The ACE spacecraft has been continuously recording solar wind data for the past 22 years. We use hourly averaged solar wind parameters from the ACE Science Center in CalTech for this study. Each entry in this database can be considered as a single point in a multi-dimensional (ND) space. SOM techniques transform all the points in this space into a single 2D space with a small number of L x L nodes. The nodes are the 2D representation of the cloud of points in the ND space, grouping together around each node, points with similar properties. The nodes in this 2D map are interrelated, maintaining a structural topology that is useful for their interpretation. Each one of the nodes in the SOM map can viewed as one of the possible L x L classes. We go one step further, automatically grouping together nodes in the map that are close in the ND space, reducing the total number of classes to only a few. We compare the results obtained using SOM with the methods introduced above, showing the similarities and differences. We show that the SOM technique, which does not rely on human intervention, can be used to properly describe the different types of solar wind conditions observed in a full solar cycle.

How to cite: Amaya, J., Dupuis, R., and Lapenta, G.: Unsupervised classification of the solar wind using Self-Organizing Maps, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-15568, https://doi.org/10.5194/egusphere-egu2020-15568, 2020.

EGU2020-11003 | Displays | ST1.8

Modelling the evolution of CMEs and their shocks through different solar wind structures

Erika Palmerio, Christina Lee, Leila Mays, and Dusan Odstrcil

The evolution of coronal mass ejections (CMEs) as they travel away from the Sun is one of the major issues in heliophysics and space weather. After erupting, CMEs propagate outwards through the background solar wind flow, which in turn may significantly affect CME evolution by means of e.g. acceleration, deflection, and/or rotation. In order to determine to which extent the ambient wind can alter the speed, trajectory, and orientation of a CME, we run a series of 3D magnetohydrodynamics simulations (using the coupled solar–heliospheric WSA–Enlil model) to conduct a multi-vantage point study of the radial and longitudinal evolution of CME structures as they propagate up to Earth’s (1 AU) and Mars’ (1.5 AU) orbits. We explore a broad range of input CME parameters (initial radial speed, angular width) and ambient solar wind conditions (slow versus fast wind) to investigate the different evolutionary behaviours of CMEs and their driven shocks and sheath regions. To study the radial and longitudinal evolution for the modelled CME ejecta and shock events, we examine the resulting magnetic field and plasma time series at different heliocentric distances (0.5 AU, 1 AU, and 1.5 AU) and heliolongitudes (in 30° increments). This work will help establish a set of expected CME behaviours at Earth’s and Mars’ radial distances, which can be used for analysing real CME events.

How to cite: Palmerio, E., Lee, C., Mays, L., and Odstrcil, D.: Modelling the evolution of CMEs and their shocks through different solar wind structures, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11003, https://doi.org/10.5194/egusphere-egu2020-11003, 2020.

EGU2020-16546 | Displays | ST1.8

A Catalogue of Coronal Mass Ejections Observed by the Heliospheric Imagers throughout the STEREO Mission

David Barnes, Jackie Davies, and Richard Harrison

Understanding the evolution of the solar wind is fundamental to advancing our knowledge of energy and mass transport in the solar system, rendering it crucial to space weather and its prediction. The advent of truly wide-angle heliospheric imaging has revolutionised the study of Coronal Mass Ejections (CMEs) by enabling their direct and continuous observation out to 1 AU and beyond. A catalogue of CMEs has been compiled using data from the Heliospheric Imagers (HIs) on board the two STEREO spacecraft, which began as part of the FP7 HELCATS project. The mission was launched in 2006 and continues to provide data, therefore spanning 13 years, over which more than two-thousand CMEs have been observed using HI. To these CMEs, we apply geometric models that make use of both single-spacecraft and stereoscopic observations in order to determine their kinematic properties. These include CME speed, acceleration, propagation direction and launch time. The resulting kinematic properties and their statistics are discussed in the context of existing CME catalogues produced from coronagraph observations. This is done with emphasis on how the different models we apply influence our results and how these differences evolve over the solar cycle and as the angular separation of the STEREO spacecraft increases throughout the mission.

How to cite: Barnes, D., Davies, J., and Harrison, R.: A Catalogue of Coronal Mass Ejections Observed by the Heliospheric Imagers throughout the STEREO Mission, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-16546, https://doi.org/10.5194/egusphere-egu2020-16546, 2020.

EGU2020-18165 | Displays | ST1.8

Turbulent properties of CME-driven sheath regions

Dominique Fontaine, Emiliya Kilpua, Matti Alalathi, Erika Palmerio, Adnane Osmane, Clement Moissard, Emiliya Yoradanova, Lina Z. Hadid, and Miho Janvier

We have analysed magnetic field fluctuations in sheath regions ahead of interplanetary coronal mass ejections (CMEs). CME sheaths are one of the key drivers of space weather disturbances, but their detailed structure and formation are relatively poorly understood. The level of magnetic field fluctuations in sheaths is generally much higher than in the ambient solar wind. We compare fluctuation properties in different parts of a sheath observed at the orbit of Earth using by the Wind spacecraft. Our findings show that in general the transition from the preceding solar wind to the sheath generates new fluctuations that are mostly compressive and which increase intermittency.  Spectral indices are mostly steeper than the -5/3 Kolmogorov index. The standard p-model did not show a good fit (in either the Kraichnan or Kolmogorov form), but the extended p-model was in a very good agreement. This suggests that turbulence may not be fully developed in CME sheaths in general. Our study also reveals that turbulent properties can vary considerably between different sheaths and in different subregions of the sheath, and can be significantly modified by the presence of small coherent structures. The findings support the view that sheath formation is a complex process with multiple physical mechanisms playing a role in generating the turbulence. 

How to cite: Fontaine, D., Kilpua, E., Alalathi, M., Palmerio, E., Osmane, A., Moissard, C., Yoradanova, E., Hadid, L. Z., and Janvier, M.: Turbulent properties of CME-driven sheath regions, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18165, https://doi.org/10.5194/egusphere-egu2020-18165, 2020.

EGU2020-625 | Displays | ST1.8

How Reliable are CME speeds derived from single viewpoint observations?

Evangelos Paouris, Angelos Vourlidas, Athanasios Papaioannou, and Anastasios Anastasiadis

Images of Coronal Mass Ejections (CMEs) are primarily acquired by space-based coronagraphs. Such images capture the outward flow of density structures from the Sun by observing Thompson-scattered sunlight from the free electrons entrained in these structures. Because the emission is optically thin, CMEs images are projections of their real 3D structure on the field of view (FOV) of the coronagraph. As a result, the CME characteristics (e.g. linear speed, angular width) calculated from these images, suffer from projection effects and their reliability needs to be quantified. In this work we apply a geometrical method for the de-projection of the linear CME speeds of 4009 CMEs from the CDAW catalog, associated with solar flares (3225 C-class, 736 M-class and 48 X-class solar flares). Our aim is to provide a robust quantification of the reliability of the CME properties from L1 (SOHO/LASCO) single viewpoint measurements.

In addition, we compare the intensity and location of solar flares with the CME kinematic characteristics. In particular, 482 M-class solar flares associated with CMEs with an angular width 30°< w < 120°, show a dependence of the mean CME linear speed with the longitude of the parent solar flare, indicating that projection effects of CMEs should be reduced near the solar limb. However, such deprojections tend to overcorrect the CME speed for sources near the solar meridian. They result in speeds of the order of 5000-7000 km/s, which seem physically unreasonable. By considering the 3D extent of the CMEs, we provide a novel geometrical correction of the deprojected CME linear speed. The resulting speeds range from a few 100 km/s up to almost 2600 km/s, a much more physically acceptable correction. This study has important implications for Space Weather applications since the reliable estimation of the CME linear speed has a direct effect on the time of arrival of CMEs at Earth and the quantification of the expected peak flux of solar radiation storms.

Acknowledgement: This work was funded from the State Scholarships Foundation of Greece (I.K.Y.), in the framework of: "Funding Post-doctoral Researchers" of the b.p.: "Human Resources Development, Education and Lifelong Learning" from ESPA (2014-2020).

 

How to cite: Paouris, E., Vourlidas, A., Papaioannou, A., and Anastasiadis, A.: How Reliable are CME speeds derived from single viewpoint observations?, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-625, https://doi.org/10.5194/egusphere-egu2020-625, 2020.

EGU2020-7838 | Displays | ST1.8

Using Forbush decreases at Earth and Mars to measure the radial evolution of ICMEs

Johan von Forstner, Jingnan Guo, Robert F. Wimmer-Schweingruber, Mateja Dumbović, Miho Janvier, Pascal Démoulin, Astrid Veronig, Manuela Temmer, Athanasios Papaioannou, Sergio Dasso, Donald M. Hassler, and Cary J. Zeitlin

Interplanetary coronal mass ejections (ICMEs), large clouds of plasma and magnetic field regularly expelled from the Sun, are one of the main drivers of space weather effects in the solar system. While the prediction of their arrival time at Earth and other locations in the heliosphere is still a complex task, it is also necessary to further understand the time evolution of their geometric and magnetic structure, which is even more challenging considering the limited number of available observation points.

Forbush decreases (FDs), short-term drops in the flux of galactic cosmic rays (GCR), can be caused by the shielding from strong and/or turbulent magnetic structures in the solar wind, such as ICMEs and their associated shock/sheath regions. In the past, FD observations have often been used to determine the arrival times of ICMEs at different locations in the solar system, especially where sufficient solar wind plasma and magnetic field measurements are not (or not always) available. One of these locations is Mars, where the Radiation Assessment Detector (RAD) onboard the Mars Science Laboratory (MSL) mission's Curiosity rover has been continuously measuring GCRs and FDs on the surface for more than 7 years.

In this work, we investigate whether FD data can be used to derive additional information about the ICME properties than just the arrival time by performing a statistical study based on catalogs of FDs observed at Earth or Mars. In particular, we find that the linear correlation between the FD amplitude and the maximum steepness, which was already seen at Earth by previous authors (Belov et al., 2008, Abunin et al., 2012), is likewise present at Mars, but with a different proprtionality factor.

By consulting physics-based analytical models of FDs, we find that this quantity is not expected to be influenced by the different energy ranges of GCR particles observed by the instruments at Earth and Mars. Instead, we suggest that the difference in FD characteristics at the two planets is caused by the radial enlargement of the ICMEs, and particularly their sheath regions, as they propagate from Earth (1 AU) to Mars (~ 1.5 AU). This broadening factor derived from our analysis extends observations for the evolution closer to the Sun by Janvier et al. (2019, JGR Space Physics) to larger heliocentric distances and is consistent with these results.

How to cite: von Forstner, J., Guo, J., Wimmer-Schweingruber, R. F., Dumbović, M., Janvier, M., Démoulin, P., Veronig, A., Temmer, M., Papaioannou, A., Dasso, S., Hassler, D. M., and Zeitlin, C. J.: Using Forbush decreases at Earth and Mars to measure the radial evolution of ICMEs, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7838, https://doi.org/10.5194/egusphere-egu2020-7838, 2020.

EGU2020-20456 | Displays | ST1.8

Understanding our capabilities in observing and modelling Coronal Mass Ejections

Christine Verbeke, Marilena Mierla, M. Leila Mays, Christina Kay, Mateja Dumbovic, Manuela Temmer, Erika Palmerio, Evangelos Paouris, Hebe Cremades, Pete Riley, Camilla Scolini, and Juergen Hinterreiter

Coronal Mass Ejections (CMEs) are large-scale eruptions of plasma and magnetic fields from the Sun. They are considered to be the main drivers of strong space weather events at Earth. Multiple models have been developed over the past decades to be able to predict the propagation of CMEs and their arrival time at Earth. Such models require input from observations, which can be used to fit the CME to an appropriate structure.

When determining input parameters for CME propagation models, it is common procedure to derive kinematic parameters from remote-sensing data. The resulting parameters can be used as inputs for the CME propagation models to obtain an arrival prediction time of the CME f.e. at Earth. However, when fitting the CME structure to obtain the needed parameters for simulations, different geometric structures and also different parts of the CME structure can be fitted. These aspects, together with the fact that 3D reconstructions strongly depend on the subjectivity and judgement of the scientist performing them, may lead to uncertainties in the fitted parameters. Up to now, no large study has tried to map these uncertainties and to evaluate how they affect the modelling of CMEs.  

Fitting a large set of CMEs within a selected period of time, we aim to investigate the uncertainties in the CME fittings in detail. Each event is fitted multiple times by different scientists. We discuss statistics on uncertainties of the fittings. We also present some first results of the impact of these uncertainties on CME propagation modelling.

Acknowledgements: This work has been partly supported by the International Space Science Institute (ISSI) in the framework of International Team 480 entitled: Understanding Our Capabilities In Observing And Modelling Coronal Mass Ejections'.

How to cite: Verbeke, C., Mierla, M., Mays, M. L., Kay, C., Dumbovic, M., Temmer, M., Palmerio, E., Paouris, E., Cremades, H., Riley, P., Scolini, C., and Hinterreiter, J.: Understanding our capabilities in observing and modelling Coronal Mass Ejections, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-20456, https://doi.org/10.5194/egusphere-egu2020-20456, 2020.

EGU2020-6272 | Displays | ST1.8

CME Expansion as Revealed by Joint Measurements by STEREO, Wind, MESSENGER and Venus Express

Noé Lugaz, Tarik Salman, Réka Winslow, Nada Al-Haddad, Charles Farrugia, Bin Zhuang, and Antoinette Galvin

The radial expansion of magnetic ejecta (ME) has been investigated through the analysis of remote observations, the variation of their properties with radial distance and from local in situ plasma measurements showing a decreasing speed profile, as first discussed almost 40 years ago. However, little is known on how local measurements compare to global measurements of expansion and what causes the different expansion properties of different CMEs. In order to correctly forecast CME properties at Earth from measurements below 0.9 AU CME expansion must be considered, and first, understood.  Here, we take advantage of 42 CMEs being measured by two spacecraft in radial conjunction to determine how the magnetic field decrease with distance, as a measure of their global expansion. As all these CMEs are also measured near 1 AU by STEREO or Wind, we are able to determine their local expansion from the speed decrease. We find that these two measures have little relation with each other, even when looking only at the events with the closest conjunctions (in term of angular separation). We also determine the relation between measures of the CME expansion and the CME properties. Lastly, we also determine the evolution of the ME radial, azimuthal and north-south magnetic field with distance, which allow us to compare their evolution with the expectations from force-free field configurations.

How to cite: Lugaz, N., Salman, T., Winslow, R., Al-Haddad, N., Farrugia, C., Zhuang, B., and Galvin, A.: CME Expansion as Revealed by Joint Measurements by STEREO, Wind, MESSENGER and Venus Express , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6272, https://doi.org/10.5194/egusphere-egu2020-6272, 2020.

EGU2020-7829 | Displays | ST1.8

Prediction of CME arrivals; differences based on stereoscopic heliospheric imager data

Jürgen Hinterreiter, Tanja Amerstorfer, Martin A. Reiss, Manuela Temmer, Christian Möstl, Maike Bauer, Ute V. Amerstorfer, Rachel L. Bailey, and Andreas J. Weiss

Forecasting the arrival time and speed of CMEs is of high importance. However, uncertainties in the forecasts are high. We present the results of post-event prediction of CME arrivals using ELEvoHI (ELlipse Evolution model based on Heliospheric Imager observations) ensemble modeling. The model uses time-elongation profiles provided by HI (Heliospheric Imager) onboard STEREO (Solar TErrestrial RElations Observatory) and assumes an elliptical shape of the CME front. The drag force exerted by the ambient solar wind is an essential factor influencing the dynamic evolution of CMEs in the heliosphere. To account for this effect, ELEvoHI utilizes the modeled ambient solar wind provided by the Wang-Sheeley-Arge model. We carefully select 12 CMEs between February 2010 and July 2012, which show clear signatures in STEREO-A and STEREO-B HI images, have a corresponding in-situ signature, and propagate close to the ecliptic plane. As input to ELEvoHI, we make use of STEREO-A and STEREO-B time-elongation profiles for each CME and compare the predicted arrival times and speeds based on both vantage points with each other. We present our model results and discuss possible reasons for the differences in the arrival times of up to 15 hours.

How to cite: Hinterreiter, J., Amerstorfer, T., Reiss, M. A., Temmer, M., Möstl, C., Bauer, M., Amerstorfer, U. V., Bailey, R. L., and Weiss, A. J.: Prediction of CME arrivals; differences based on stereoscopic heliospheric imager data, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7829, https://doi.org/10.5194/egusphere-egu2020-7829, 2020.

ST1.9 – Theory and Simulation of Solar System Plasmas

EGU2020-5435 | Displays | ST1.9

How does dissipation work in the electron diffusion region of asymmetric magnetic reconnection

Michael Hesse, Cecilia Norgren, Paul Tenfjord, James Burch, Yi-Hsin Liu, Li-Jen Chen, Naoki Bessho, Susanne Spinnangr, and Håkon Kolstø

At some level, magnetic reconnection functions by means of a balance between current dissipation, and current maintenance due to the reconnection electric field. While this dissipation is well understood process in symmetric magnetic reconnection, the way nonideal electric fields interact with the current density in asymmetric reconnection is still unclear. In symmetric reconnection, the current density maximum, the X point location, and the nonideal electric field determined by the divergence of the electron pressure tensor usually coincide. In asymmetric reconnection, however, the electric field at the X point can be partly provided by bulk inertia terms, implying that the X point cannot be the dominant location of dissipation. On the other hand, we know that the nongyrotropic pressure-based electric field must dominate at the stagnation point of the in-plane electron flow, and that electron distributions here feature crescents. The further fact that the current density peak is shifted off the position of the X point indicates that there may be a relation between this current density enhancement, the location of the stagnation point, and the electron nongyrotropies. In this presentation we report on further progress investigating the physics of the electron diffusion region in asymmetric reconnection with a focus on how to explain the dissipation operating under these conditions. 

How to cite: Hesse, M., Norgren, C., Tenfjord, P., Burch, J., Liu, Y.-H., Chen, L.-J., Bessho, N., Spinnangr, S., and Kolstø, H.: How does dissipation work in the electron diffusion region of asymmetric magnetic reconnection, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5435, https://doi.org/10.5194/egusphere-egu2020-5435, 2020.

EGU2020-15156 | Displays | ST1.9 | Highlight

Automated characterization of magnetic reconnection using particle distributions

Romain Dupuis, Jorge Amaya, Giovanni Lapenta, Martin Goldman, and David Newman

Magnetic reconnection is a fundamental process for many plasma phenomena converting the stored magnetic energy into kinetic energy, thermal energy, and particle acceleration energy. Various missions have been launched, the latest being Magnetospheric Multiscale Mission (MMS), to improve the understanding of reconnection with in-situ measurements. In particular, particle distributions provide a rich insight on the local physics but a unique specific distribution cannot be used as a signature for reconnection as it does not reflect the phenomenon for all the possible external conditions. For instance, a strong anisotropy can be observed near the electron exhaust [1] while crescent-shaped distributions can be detected near the electron stagnation point for asymmetric reconnection [2].

From Particle-In-Cells (PIC) simulations, we developed a detection algorithm using a machine learning technique called Gaussian Mixture Model approximating the underlying density function by a sum of Gaussians [3]. The objective is twofold: finding a good approximation for the distribution while keeping a statistical meaning to the different components of the sum. The deviation from classical Maxwellians and the distributions with complex shapes provide a good measurement to identify reconnection. The algorithm was successfully applied to 2.5D simulations and large regions around the diffusion region and the separatrix were spotted. Different kinds of distributions have been efficiently identified.

The presented results tend to extend this method to other sources of data:

  1. 3D simulations: although reconnection in 2D is well understood, many unanswered questions persist for 3D systems. Usually, such simulations show regions of millions of kilometers while having a sufficient resolution to be able to observe the tiny regions in which the original reconnection events occur. A deep analysis and understanding of these very large simulations appear as very challenging. Therefore, we expect that our method supports the analysis by automatically identifying various regions of interest with potential reconnection.
  2. observational data: as the model has been validated on simulations, we are interested to apply the method on real data from the MMS mission. Will the observations made by scientists of the mission compare with the result of a fully automatic tool? In particular, the data pre-processing providing cleaned and readable data to the algorithm is very challenging.

In conclusion, the Gaussian Mixture Model approach is a first attempt to automatically characterize various kinetic behaviors encountered in both numerical simulations and space missions. In particular, it represents a very good potential to support data analysis of spacecraft observations but also fully three-dimensional simulations.

This contribution has received funding from the European Union’s Horizon 2020 research and innovation programme under grant agreement No 776262 (AIDA, ).

[1] Shuster et al. “Highly structured electron anisotropy in collisionless reconnection exhausts”, 2014, Geophysical Research Letters, 41, 5389

[2] Burch et al., “Electron-scale measurements of magnetic reconnection in space.”, 2016b, Science, vol. 352, no 6290, p. aaf2939

[3] Dupuis et al., “Characterizing magnetic reconnection regions using Gaussian mixture models on particle velocity distributions”, 2020, ApJ, accepted,

How to cite: Dupuis, R., Amaya, J., Lapenta, G., Goldman, M., and Newman, D.: Automated characterization of magnetic reconnection using particle distributions, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-15156, https://doi.org/10.5194/egusphere-egu2020-15156, 2020.

EGU2020-2165 | Displays | ST1.9 | Highlight

Kinetic theory and simulation of electron-strahl scattering in the solar wind

Daniel Verscharen, Seong-Yeop Jeong, Benjamin Chandran, Chadi Salem, Marc Pulupa, and Stuart Bale

We investigate the scattering of strahl electrons by microinstabilities as a mechanism for creating the electron halo in the solar wind. We develop a mathematical framework for the description of electron-driven microinstabilities and discuss the associated physical mechanisms. We find that an instability of the oblique fast-magnetosonic/whistler (FM/W) mode is the best candidate for a microinstability that scatters strahl electrons into the halo. We derive approximate analytic expressions for the FM/W instability threshold in two different βregimes, where βc is the ratio of the core electrons' thermal pressure to the magnetic pressure, and confirm the accuracy of these thresholds through comparison with numerical solutions to the hot-plasma dispersion relation. We find that the strahl-driven oblique FM/W instability creates copious FM/W waves under low-βc conditions when U0s>3wc, where U0s is the strahl speed and wis the thermal speed of the core electrons. These waves have a frequency of about half the local electron gyrofrequency. We also derive an analytic expression for the oblique FM/W instability for βc~1. The comparison of our theoretical results with data from the Wind spacecraft confirms the relevance of the oblique FM/W instability for the solar wind. In addition, we find a good agreement between our theoretical results and numerical solutions to the quasilinear diffusion equation. We make predictions for the electron strahl close to the Sun, which will be tested by measurements from Parker Solar Probe and Solar Orbiter.

How to cite: Verscharen, D., Jeong, S.-Y., Chandran, B., Salem, C., Pulupa, M., and Bale, S.: Kinetic theory and simulation of electron-strahl scattering in the solar wind, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2165, https://doi.org/10.5194/egusphere-egu2020-2165, 2020.

EGU2020-2532 | Displays | ST1.9 | Highlight

Coherent emission driven by energetic ring-beam electrons in the solar corona

Xiaowei Zhou, Patricio Munoz Sepulveda, Joerg Buechner, and Siming Liu

We analyzed properties of waves excited by mildly relativistic electron beams propagating along magnetic field with a ring-shape perpendicular momentum distribution in neutral and current-free solar coronal plasmas. These plasmas are subject to both the beam and the electron cyclotron maser (ECM) instabilities driven by the positive momentum gradient of the ring-beam electron distribution in the directions parallel and perpendicular to the ambient magnetic field, respectively. To explore the related kinetic processes self-consistently, 2.5-dimensional fully kinetic particle-in-cell (PIC) simulations were carried out.

To quantify excited wave properties in different coronal conditions, we investigated the dependence of their energy and polarization on the ring-beam electron density and magnetic field. In general, electrostatic waves dominate the energetics of waves and nonlinear waves are ubiquitous. In weakly magnetized plasmas, where the electron cyclotron frequency ωce is lower than the electron plasma frequency ωpe, it is difficult to produce escaping electromagnetic waves with frequency ω > ωpe and small refractive index ck/ω < 1 (k and c are the wavenumber and the light speed, respectively). Highly polarized and anisotropic escaping electromagnetic waves can, however, be effectively excited in strongly magnetized plasmas with ωcepe ≥ 1. The anisotropy of the energy, circular polarization degree (CPD), and spectrogram of these escaping electromagnetic waves strongly depend on the number density ratio of the ring-beam electrons to the background electrons. In particular, their CPDs can vary from left-handed to right-handed with the decrease of the ring-beam density, which may explain some observed properties of solar radio bursts (e.g., radio spikes) from the solar corona.

How to cite: Zhou, X., Munoz Sepulveda, P., Buechner, J., and Liu, S.: Coherent emission driven by energetic ring-beam electrons in the solar corona, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2532, https://doi.org/10.5194/egusphere-egu2020-2532, 2020.

The role of turbulence is one of key issues for understanding the magnetic and plasma energy conversion, plasma heating and high energy particles acceleration in large temporal-spatial scale turbulent magnetic reconnection (LTSTMR; observed current sheet thickness to characteristic electron length, Larmor radius for low-beta and electron inertial length for high-beta, ratios on the order of ten to the power of ten or higher; observed evolution time to electron cyclotron time ratios on the order of ten to the power of ten or higher) . Solar atmosphere activities (e.g., limbs, flares, coronal mass ejections, solar winds and so on), which are the most important phenomenon in the solar and Sun-Earth space systems, are typical LTSTMRs.

Here we used our newly developed RHPIC-LBM algorithm[*]  to perform the role of  turbulence in the magnetic fluctuation-induced self-generating-organization  (MF-ISGO), the turbulence in the plasma turbulence-induced self-feeding-sustaining (PT-ISFS), and the interaction of turbulence between MF-ISGO and PT-ISFS in the continuous kinetic-dynamic-hydro fully coupled LTSTMR. 

First, we find that the self-generated turbulence by magnetic field and plasma motion collective interaction include two fully coupled processes of 1) fluid vortex induced magnetic reconnection (MR) and 2) MR induced fluid vortex. The Biermann battery effect and  alpha-effect can not only generate magnetic fields, but can server them to trigger MR, the Spitzer resistance and turbulence resistance (beta-effect)  can not only generate magnetic eddies, but can server  them to trigger fluid turbulence.  

Then, we find that these interaction leads to vortex splitting and phase separating instabilities, and there are four species instabilities coexist in the evolution process. 1) Vortex separation interface instabilities. 2)Magnetic fluctuation-induced self-generating-organization instabilities. 3) Plasma turbulence-induced self-feeding-sustaining instabilities. 4) Vortex shedding instabilities.

Finally, the nuanced details of the magnetic topological structure and the topological characterization of flow structures in plasma of the simulated 3D LTSTMR are also presented.

The characterization of turbulence anisotropy and the turbulence acceleration of the LTSTMR are presented in Part II and Part III of this three-paper series study.

*Techniques and algorithms for RHPIC-LBM have been developed in previous studies (e.g.,Zhu2020a, Zhu2020b)

References

Zhu, B. J., Yan, H., Zhong, Y., et al. 2020a, Appl Math Model, 78, 932, doi: 10.1016/j.apm.2019.09.043

Zhu, B. J., Yan, H., Zhong, Y., et al. 2020b, Appl Math Model, 78, 968,doi: 10.1016/j.apm.2019.05.027

How to cite: Zhu, B., Yan, H., Cheng, H., Zhong, Y., Du, Y., and Yuen, D. A.: Self-generated turbulence by plasmas and magnetic field collective interaction in 3D large temporal-spatial turbulent magnetic reconnection: I. The Basic Feature, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7950, https://doi.org/10.5194/egusphere-egu2020-7950, 2020.

EGU2020-3573 | Displays | ST1.9

Identifying and Quantifying the Role of Magnetic Reconnection in Space Plasma Turbulence

Jeffersson Andres Agudelo Rueda, Daniel Verscharen, Robert Wicks, Christopher Owen, Georgios Nicolaou, Andrew Walsh, Yannis Zouganelis, and Santiago Vargas

One of the outstanding open questions in space plasma physics is the heating problem in the solar corona and the solar wind. In-situ measurements, as well as MHD and kinetic simulations, suggest a relation between the turbulent nature of plasma and the onset of magnetic reconnection as a channel of energy dissipation, particle acceleration and a heating mechanism. It has also been proven that non-linear interactions between counter propagating Alfvén waves drives plasma towards a turbulent state. On the other hand, the interactions between particles and waves becomes stronger at scales near the ion(electron) gyroradious ρi (ρe ), and so turbulence can enhance conditions for reconnection and increase the number of reconnection sites. Therefore, there is a close link between turbulence and reconnection. We use fully kinetic particle in cell (PIC) simulations, able to resolve the kinetic phenomena, to study the onset of reconnection in a 3D simulation box with parameters similar to the solar wind under Alfvénic turbulence. We identify in our simulations characteristic features of reconnection sites as steep gradients of the magnetic field strength alongside with the formation of strong current sheets and inflow-outflow patterns of plasma particles near the diffusion regions. These results will be used to quantify the role reconnection in plasma turbulence.

How to cite: Agudelo Rueda, J. A., Verscharen, D., Wicks, R., Owen, C., Nicolaou, G., Walsh, A., Zouganelis, Y., and Vargas, S.: Identifying and Quantifying the Role of Magnetic Reconnection in Space Plasma Turbulence, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3573, https://doi.org/10.5194/egusphere-egu2020-3573, 2020.

EGU2020-19295 | Displays | ST1.9 | Highlight

Multiscale analysis of Hall-MHD and Hybrid-PIC simulations of plasma turbulence: structures or waves?

Emanuele Papini, Antonio Cicone, Mirko Piersanti, Luca Franci, Simone Landi, and Petr Hellinger

Turbulence in space and astrophysical plasmas is an intrinsically chaotic and multiscale phenomenon that involves nonlinear coupling across different temporal and spatial scales. There is growing evidence that plasma instabilities, such as magnetic reconnection taking place in localized current sheets, enhance the energy dissipation toward small sub-ion scales. However, it is hotly debated whether the dominant contribution to the scale-to-scale energy transfer at kinetic scales is due to non-linear wave interactions or to coherent structures. Here we present the results from a multiscale study of 2D Hall-MHD and hybrid Particle-in-cell (PIC) numerical simulations of decaying turbulence, performed by means of Multidimensional Iterative Filters (MIF), a new technique developed for the spatio-temporal analysis of non-stationary non-linear multidimensional signals. Results show that, at the maximum of turbulent activity, the power spectrum of magnetic fluctuations at sub-ion scales is formed by localized structures and/or perturbations with temporal frequencies smaller than the ion-cyclotron frequency. Going toward smaller kinetic scales, the contribution of low-medium frequency perturbations to the magnetic spectrum becomes important. However, the dispersion relation and polarization properties of such perturbations are not consistent with those of Kinetic Alfvèn Waves (KAW). We conclude that the dynamics of turbulence at sub-ion scales is mainly shaped by localized intermittent structures, with no apparent contribution of KAW-like interactions at small scales.

How to cite: Papini, E., Cicone, A., Piersanti, M., Franci, L., Landi, S., and Hellinger, P.: Multiscale analysis of Hall-MHD and Hybrid-PIC simulations of plasma turbulence: structures or waves?, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-19295, https://doi.org/10.5194/egusphere-egu2020-19295, 2020.

EGU2020-4108 | Displays | ST1.9 | Highlight

Transport ratios of the kinetic Alfvén mode in space plasmas

Yasuhito Narita, Zoltan Vörös, Owen Wyn Roberts, and Masahiro Hoshino

Electric field properties of the kinetic Alfvén mode are analytically studied by constructing the dielectric tensor of the plasma using the linear Vlasov theory and reducing (and identifying) the tensor elements into that of the fluid picture such as the polarization drift, the Hall current, and the diamagnetic current. Off-diagonal dielectric responses do not primarly contribute to the dispersion relation of the kinetic Alfvén mode, but play an important role in the electric field polarization (field rotation sense around the mean magnetic field) and parallel component of the field. The polarization becomes more circular and the parallel component enhances at larger perpendicular wavenumbers. Analytic expression of fluctuation sense serves as a tool to identify the kinetic Alfvén mode in space plasma observations.

How to cite: Narita, Y., Vörös, Z., Roberts, O. W., and Hoshino, M.: Transport ratios of the kinetic Alfvén mode in space plasmas, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4108, https://doi.org/10.5194/egusphere-egu2020-4108, 2020.

Solar flares originate from the release of the energy stored in the magnetic field of solar active regions. Generally, the photospheric magnetograms of active regions are used as the input of the solar flare forecasting model. However, solar flares are considered to occur in the low corona. Therefore, the role of 3D magnetic field of active regions in the solar flare forecast should be explored. We extrapolate the 3D magnetic field using the potential model for all the active regions during 2010 to 2017, and then the deep learning method is applied to extract the precursors of solar flares in the 3D magnetic field data. We find that the 3D magnetic field of active regions is helpful to build a deep learning based forecasting model.

How to cite: Huang, X.: Solar flare forecasting model using 3D magnetic field data, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-13298, https://doi.org/10.5194/egusphere-egu2020-13298, 2020.

EGU2020-2695 | Displays | ST1.9

Magnetohydrostatic modelling of the solar atmosphere: Test and application

Xiaoshuai Zhu and Thomas Wiegelmann
Both magnetic field and plasma play important roles in activities in the solar atmosphere. Unfortunately only the magnetic fields in the photosphere are routinely measured precisely. We aim to extrapolate these photospheric vector magnetograms upwards into  the solar atmosphere. In this work we are mainly interested in reconstructing the upper solar photosphere and chromosphere. In these layers magnetic and non-magnetic forces are equally important. Consequently we have to compute an equilibrium of plasma and magnetic forces with a magnetohydrostatic model. A optimization approach which minimize a functional defined by the magnetohydrostatic equations is used in the model. In this talk/poster, I will present a strict test of the new code with a radiative MHD simulation and its first application to a high resolution vector magnetogram measured by SUNRISE/IMaX.

How to cite: Zhu, X. and Wiegelmann, T.: Magnetohydrostatic modelling of the solar atmosphere: Test and application, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2695, https://doi.org/10.5194/egusphere-egu2020-2695, 2020.

 It is well-known that there is a gradient, there will drive a flow inevitably. For example, a density-gradient may drive a diffusion flow, an electrical potential-gradient may drive an electric current in plasmas, etc. Then, what flows will be driven when a magnetic-gradient occurs in solar atmospheric plasmas?

Considering the ubiquitous distribution of magnetic-gradient in solar plasma loops, this work demonstrates that magnetic-gradient pumping (MGP) mechanism is valid even in the partial ionized solar photosphere, chromosphere as well as in the corona. MGP drives energetic particle flows which carry and convey kinetic energy from the underlying atmosphere to move upwards, accumulate around the looptop and increase there temperature and pressure, and finally lead to eruptions around the looptop by triggering ballooning instabilities. This mechanism may explain the evolution of solar plasma loops, the formation of the observing hot cusp-structures above flaring loops in most preflare phases, and the triggering of eruptions in solar plasma loops. Therefore, the magnetic-gradient may play as a natural driver of solar eruptions.

Furthermore, we may also apply MGP mechanism to understand many other astrophysical phenomena, such as the coronal heating, the temperature distribution above sunspots, the formation of solar plasma jets, type-II spicule, and fast solar wind above coronal holes, as well as the fast plasma jets related to white dwarfs, neutron stars and black holes.

Additionally, we also proposed to test the above MGP mechanism by using the new generation observations of the broadband spectral radioheliographs, such as MUSER, EVOSA, and SRH, etc.

How to cite: Tan, B.: Magnetic Gradient May Play as a Natural Driver of Solar Eruptions, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-22259, https://doi.org/10.5194/egusphere-egu2020-22259, 2020.

EGU2020-4982 | Displays | ST1.9

MHD simulation of solar flare by applying analytical energetic fast electron model

Wenzhi Ruan and Rony Keppens

In order to study the evaporation of chromospheric plasma and the formation of hard X-ray (HXR) sources in solar flare events, we coupled an analytic energetic electron model with the multi-dimensional MHD simulation code MPI-AMRVAC. The transport of fast electrons accelerated in the flare looptop is governed by the test particle beam approach reported in Emslie et al. (1978), now used along individual field lines. Anomalous resistivity, thermal conduction, radiative losses and gravity are included in the MHD model. The reconnection process self-consistently leads to formation of a flare loop system and the evaporation of chromospheric plasma is naturally recovered. The non-thermal HXR emission is synthesized from the local fast electron spectra and local plasma density, and thermal bremsstrahlung soft X-ray (SXR) emission is synthesized based on local plasma density and temperature. We found that thermal conduction is  an efficient way to trigger evaporation flows. We also found that the generation of a looptop HXR source is a result of fast electron trapping, as evidenced by the pitch angle evolution. By comparing the SXR flux and HXR flux, we found that a possible reason for the “Neupert effect” is that the increase of non-thermal and thermal energy follows the same tendency.

How to cite: Ruan, W. and Keppens, R.: MHD simulation of solar flare by applying analytical energetic fast electron model, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4982, https://doi.org/10.5194/egusphere-egu2020-4982, 2020.

EGU2020-3029 | Displays | ST1.9 | Highlight

An optimization principle for computing stationary MHD equilibria with solar wind flow

Thomas Wiegelmann, Thomas Neukirch, Dieter Nickeler, and Iulia Chifu

Knowledge about the magnetic field and plasma environment is important
for almost all physical processes in the solar atmosphere. Precise
measurements of the magnetic field vector are done routinely only in
the photosphere, e.g. by SDO/HMI. These measurements are used as
boundary condition for modelling the solar chromosphere and corona,
whereas some model assumptions have to be made. In the low-plasma-beta
corona the Lorentz-force vanishes and the magnetic field
is reconstructed with a nonlinear force-free model. In the mixed-beta
chromosphere plasma forces have to be taken into account with the
help of a magnetostatic model. And finally for modelling the global
corona far beyond the source surface the solar wind flow has to
be incorporated within a stationary MHD model.
To do so, we generalize a nonlinear force-free and magneto-static optimization
code by the inclusion of a field aligned compressible plasma flow.
Applications are the implementation of the solar wind on
global scale. This allows to reconstruct the coronal magnetic field further
outwards than with potential field, nonlinear force-free and magneto-static models.
This way the model might help in future to provide the magnetic connectivity
for joint observations of remote sensing and in-situ instruments on Solar
Orbiter and Parker Solar Probe.

How to cite: Wiegelmann, T., Neukirch, T., Nickeler, D., and Chifu, I.: An optimization principle for computing stationary MHD equilibria with solar wind flow, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3029, https://doi.org/10.5194/egusphere-egu2020-3029, 2020.

EGU2020-18832 | Displays | ST1.9

Possible Generation Mechanism for Alfvenic Velocity Spikes and Magnetic Field Switchbacks as Observed by PSP

Xingyu Zhu, Jiansen He, Die Duan, Lei Zhang, Liping Yang, Chuanpeng Hou, and Wang Ying
According to Parker's theory in the 1950s, the magnetic lines of force extending from the sun to the interplanetary appear to be Archimedean spirals. From 1960 to 1970, it was found that the interplanetary magnetic field not only follows the Archimedes spiral structure, but also has the characteristics of Alfvenic turbulence. How do these Alfvenic turbulence occur? What will be the characteristics when getting close to the Sun? Parker Solar Probe at 0.17au has found that there are often intermittent Alfvenic pulses (or called Alfvenic velocity spikes) in the solar wind. These pulses are high enough that the disturbed magnetic lines may even turn back. What's more interesting is that there is always a compressibility disturbance along with the Alfven pulse: the temperature and density inside and outside the Alfven pulse are different, the internal temperature is often higher than the external temperature, some of the internal density is higher than the external and some is lower than the external. The Alfven pulse often shows asymmetry on both sides: the magnetic field and velocity on one side are "clean" jumps, while on the other side are multiple small-scale disturbances of variables in the transition boundary layer. In view of this new phenomenon of magnetic field line switch back with compressed Alfven pulse, how it is generated is raising a hot debate. It is thought that the exchange magnetic reconnection of the solar atmosphere may be the underlying physical mechanism. But in the traditional exchange magnetic reconnection image, after reconnection, the zigzag magnetic field line can easily become smooth, which can not maintain the distortion of the magnetic field line, and may not be able to explain the observed Alfven pulses. In this work, we propose a new model called "Excitation of Alfven Pulses by Continuous Intermittent Interchange Reconnection with Guide Field Discontinuity" (EAP-CIIR-GFD). By analyzing and comparing the simulation results and observation results, we find that the model can explain the following observation features: (1) Alfven disturbance is pulse type and asymmetric; (2) Alfven pulse is compressible with the enhancement of internal temperature and the increase or decrease of the internal density; (3) Alfven pulse can cause serious distortion of the magnetic field line. Improvements to the model will also be discussed in the report.

How to cite: Zhu, X., He, J., Duan, D., Zhang, L., Yang, L., Hou, C., and Ying, W.: Possible Generation Mechanism for Alfvenic Velocity Spikes and Magnetic Field Switchbacks as Observed by PSP, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18832, https://doi.org/10.5194/egusphere-egu2020-18832, 2020.

EGU2020-48 | Displays | ST1.9 | Highlight

Kinetic Vlasov simulations of contact discontinuities

Takayuki Umeda, Naru Tsujine, and Yasuhiro Nariyuki

The stability of contact discontinuities formed by the relaxation of two Maxwellian plasmas with different number densities but the same plasma thermal pressure is studied by means of a one-dimensional electrostatic full-Vlasov simulation. Our simulation runs with various combinations of ion-to-electron ratios of the high-density and low-density regions showed that transition layers of density and temperature without jump in the plasma thermal pressure are obtained when the electron temperatures in the high-density and low-density regions are almost equal to each other. However, the stable structure of the contact discontinuity with a sharp transition layer on the Debye scale is not maintained. It is suggested that non-Maxwellian velocity distributions are necessary for the stable structure of contact discontinuities. A direct comparison between full- and hybrid-Vlasov simulations is also made.

How to cite: Umeda, T., Tsujine, N., and Nariyuki, Y.: Kinetic Vlasov simulations of contact discontinuities, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-48, https://doi.org/10.5194/egusphere-egu2020-48, 2020.

EGU2020-1175 | Displays | ST1.9

Role of Whistler Waves in Regulation of the Heat Flux in the Solar Wind

Ilya Kuzichev, Ivan Vasko, Angel Rualdo Soto-Chavez, and Anton Artemyev

The electron heat flux is one of the leading terms in energy flow processes in the collisionless or weakly-collisional solar wind plasma. The very first observations demonstrated that the collisional Spitzer-HÓ“rm law could not describe the heat flux in the solar wind well. In particular, in-situ observations at 1AU showed that the heat flux was suppressed below the collisional value. Different mechanisms of the heat flux regulation in the solar wind were proposed. One of these possible mechanisms is the wave-particle interaction with whistler-mode waves produced by the so-called whistler heat flux instability (WHFI). This instability operates in plasmas with at least two counter-streaming electron populations. Recent observations indicated that the WHFI operates in the solar wind producing predominantly quasi-parallel whistler waves with the amplitudes up to several percent of the background magnetic field. But whether such whistler waves can regulate the heat flux still remained an open question.

We present the results of simulation of the whistler generation and nonlinear evolution using the 1D full Particle-in-Cell code TRISTAN-MP. This code models self-consistent dynamics of ions and two counter-streaming electron populations:  warm (core) electrons and hot (halo) electrons. We performed two sets of simulations. In the first set, we studied the wave generation for the classical WHFI, so both core and halo electron distributions were taken to be isotropic. We found a positive correlation between the plasma beta and the saturated wave amplitude. For the heat flux, the correlation changes from positive to a negative one at some value of the heat flux. The observed wave amplitudes and correlations are consistent with the observations. Our calculations show that the electron heat flux does not change substantially in the course of the WHFI development; hence such waves are unlikely to contribute significantly to the heat flux regulation in the solar wind.

The classical WHFI drives only those whistler waves that propagate along the halo electron drift direction (consequently, parallel with respect to background magnetic field). Such waves interact resonantly with electrons that move in the opposite direction; hence, only a relatively small fraction of hot halo electrons is affected by these waves. On the contrary, anti-parallel whistler waves would interact with a substantial fraction of halo electrons. Thus, they could influence the heat flux more significantly. To test this hypothesis, we performed the second set of simulations with anisotropic halo electrons. Anisotropic distribution drives both parallel and anti-parallel waves. Our calculations demonstrate that anti-parallel whistler waves can decrease the heat flux. This indicates that the waves generated via combined whistler anisotropy and heat flux instabilities might contribute to regulation of the heat flux in the solar wind.

The work was supported by NSF grant 1502923. I. Kuzichev would also like to acknowledge the support of the RBSPICE Instrument project by JHU/APL sub-contract 937836 to the New Jersey Institute of Technology under NASA Prime contract NAS5-01072. Computational facility: Cheyenne supercomputer (doi:10.5065/D6RX99HX) provided by NCAR’s Computational and Information Systems Laboratory, sponsored by NSF

How to cite: Kuzichev, I., Vasko, I., Soto-Chavez, A. R., and Artemyev, A.: Role of Whistler Waves in Regulation of the Heat Flux in the Solar Wind , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1175, https://doi.org/10.5194/egusphere-egu2020-1175, 2020.

Magnetohydrodynamic waves in a stratified rotating plasma in a gravitational field in the Boussinesq approximation are studied. The theory of flows on the f -plane, on the non-traditional f-plane (taking into account the horizontal component of the Coriolis force), on the beta -plane, and on the non-traditional beta -plane is developed. In each considered case linear solutions of systems of three-dimensional magnetohydrodynamic equations in the Boussinesq approximation are obtained in form of magnetic inertio-gravity waves, magnetostrophic waves, and magneto-Rossby waves. For equations of a rotating stratified plasma without taking into account sphericity (in the approximation of the f-plane and the non-traditional f- plane), dispersion relations describe three-dimensional magnetic inertio-gravity waves and three-dimensional magnetostrophic waves. In the case of propagating only along the vertical component of the wave vector, their dispersion relations describe two types of magnetic waves, the first of which is a special case of magnetic inerto-gravity waves propagating only vertically, and the second is a special case of magnetostrophic waves propagating only vertically. In addition, it was found that dispersion relations describing wave propagation taking into account sphericity in a first approximation (on the beta-plane and on the non-traditional beta- plane) along the vertical component of the wave vector have a similar particular form. In the case of wave propagation in a horizontal plane, magnetic inertio-gravity waves turn into Alfvén waves, and magnetostrophic waves turn into magnetogravitational waves. In addition, for waves on a non-traditional f-plane, the influence of the horizontal component of the Coriolis force on the existence of various types of three-wave interactions is shown. For equations of a rotating stratified plasma on the beta-plane and on the non-traditional beta-plane dispersion relations for horizontal waves are found in form of magnetogravitational waves (similar to waves on the f- plane) and various types of magneto-Rossby waves. In addition, the equivalence of the low-frequency mode of the magneto-Rossby wave in the Boussinesq approximation and in the magnetohydrodynamic shallow water approximation was shown. The dispersion curves of all the detected wave types are qualitatively analyzed to identify the fulfillment of the synchronism condition, which ensures the presence of three-wave interactions. A system of amplitude equations for interacting waves and the increments of two types of instability that occur in the system (decay and amplification) are obtained using the method of multiscale expansions. The difference in the coefficients and differential operators in the three-wave interaction system is shown for each of the found types of three-wave interactions.

This research was supported by the Russian Foundation for Basic Research (project no. 19-02-00016)

How to cite: Fedotova, M. and Petrosyan, A.: Linear and nonlinear waves in three-dimensional stratified rotating astrophysical flows in the Boussinesq approximation, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1540, https://doi.org/10.5194/egusphere-egu2020-1540, 2020.

A significant number of observed flows in geophysics, astrophysics, and laboratory experiments are in a state of magnetohydrodynamic turbulence. Among them are flows in the Earth’s outer core, in plasma shells of Earth, planets, and satellites of the solar system with strong magnetic fields, as well as flows in the Sun, stars, and astrophysical disks. Despite significant advances in the study of turbulence under the conditions typical of thermonuclear fusion devices, studies of the fundamental properties of homogeneous turbulence in rotating magnetohydrodynamic flows are still fragmentary and mainly concern turbulence in astrophysical disks, the solar tachocline and convective region of the Sun, and two-dimensional magnetohydrodynamic flows on the β-plane. Only in a few exceptional works were the properties of magnetohydrodynamic turbulence studied by simple analytical methods using Fourier series for similarity parameters, characteristic of the Earth’s core.

The aim of this work is to study the influence of the interaction of Alfvén wave packets on the dynamics of homogeneous turbulence. The method of calculation o magnetohydrodynamic turbulence we developed allows numerical simulation at large characteristic times and large external magnetic fields. The proposed method of setting the initial conditions for the velocity field makes it possible to satisfy the divergence-free, homogeneity, and turbulence isotropy conditions, as well as to set an arbitrary spectral distribution of the energy at the initial time without additional calculations. Numerical experiments demonstrate a nontrivial behavior of turbulent kinetic and magnetic energies. It is shown that periodic imbalance in energies occurs in the system in the form of conversion of kinetic energy into magnetic energy and vice versa. The analysis of the results shows that the detected nontrivial temporal dynamics of turbulence is caused by the periodic collisions of Alfvén wave packets.

This work was supported by the Russian Foundation for Basic Research (project no. 19-02-00016).

How to cite: Sirazov, R. and Petrosyan, A.: Periodic imbalances of kinetic and magnetic energies in rotating magnetohydrodynamic turbulent flows, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3454, https://doi.org/10.5194/egusphere-egu2020-3454, 2020.

EGU2020-4497 | Displays | ST1.9

Inverse cascade of kinetic energy in two-dimensional β-Plane magnetohydrodynamic turbulence

Timofey Zinyakov and Arakel Petrosyan

Numerical studies of two-dimensional β-plane homogeneous magnetohydrodynamic turbulence are presented. The study of the fundamental properties of such turbulence allows understanding the evolution of various astrophysical objects from the Sun and stars to planetary systems, galaxies, and galaxy clusters. Energy spectra and cascade process in two-dimensional β-plane MHD are studied.

In this work the equations of two-dimensional magnetohydrodynamics with the Coriolis force in the β-plane approximation are used for the qualitative analysis and numerical simulation of processes in plasma astrophysics. The equations are solved on a square box of edge size 2π with periodic boundary conditions applying a the pseudospectral method using the 2/3 rule for dealiasing. The results of numerical simulation of two-dimensional β-plane MHD turbulence with a spatial resolution of 1024 × 1024 and 4096 × 4096 with different Rossby parameters β and different Reynolds numbers are presented.

It is found that only unsteady zonal flows with complex temporal dynamics are formed in two-dimensional β-plane magnetohydrodynamic turbulence. It is shown that flow nonstationarity is due to the appearance of isotropic magnetic islands caused by the Lorentz force in the system. The formation of Iroshnikov–Kraichnan spectrum is shown in the early stages of evolution of two-dimensional β-plane magnetohydrodynamic turbulence. The self-similarity of the decay of Iroshnikov–Kraichnan spectrum is studied. On long time scale violation of self-similarity of the decay and formation of Kolmogorov spectrum is discovered. The inverse cascade of kinetic energy, which is characteristic of the detected Kolmogorov spectrum, provides the formation of zonal flows.

This work was supported by the Russian Foundation for Basic Research (project no. 19-02-00016).

How to cite: Zinyakov, T. and Petrosyan, A.: Inverse cascade of kinetic energy in two-dimensional β-Plane magnetohydrodynamic turbulence, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4497, https://doi.org/10.5194/egusphere-egu2020-4497, 2020.

In this report, we present a prominence observed by New Vacuum Solar Telescope (NVST) in Hα wavelength.  We use morphological approach to identify the rising or descending knots in the prominence. The rising knots are often found on the top of the prominence, while more knots are seen to descend from anywhere of the prominence.

The optical flow, referring to the apparent proper motion of a feature across the image plane, may be used to determine the velocity field from two images. The technique of local correlation tracking (LCT) optical flow has been widely used in the solar research. The Demon algorithm, which has been  used to match medical image, performs image-to-image matching by determining the optical flow between two images. We have examined the performance of the two methods applying the Hα images, and we noted that the Demon algorithm outperforms traditional LCT  methods.

The result of Demon optical flow allows us to estimate the velocity and acceleration of the moving knots. The descending speed of the knots near the solar surface is higher than that far away from the solar surface. This indicate that most of knots are more possible to descend across the horizontal magnetic field.

How to cite: Bi, Y.: Dynamics of moving knots in a solar prominence observed by New Vacuum Solar Telescope, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-8362, https://doi.org/10.5194/egusphere-egu2020-8362, 2020.

EGU2020-8646 | Displays | ST1.9

Rapid distortion theory for homogeneous shear-driven MHD turbulence

Sergei Safonov and Arakel Petrosyan

In this report we study statistical properties of astrophysical turbulent plasma flows subjected to large scale velocity shear and an external magnetic field using Rapid Distortion Theory (RDT). The problem of shear-driven turbulence arises in several important physical systems, such as the solar wind and ionized atmospheres of exoplanets. Rapid distortion theory is a linearization method for Reynolds-averaged Navier-Stockes equations. Its main assumption is that the turbulence responds to the external distortion by velocity shear so fast, that inertial forces result in a negligible change in velocity field statistics at small time scales. This allows to linearize equations and to derive equations for second moments of turbulence. We apply RDT approach to incompressible homogeneous MHD turbulence distorted with an external magnetic field and a linear velocity shear in cases of rotating and non-rotating plasma. It is shown that even with a strong nonlinearity many properties of turbulence can be qualitatively studied using a linear theory. A closed system of linear equations is derived for energy, helicity and polarization of velocity and magnetic field correlations. Structural analysis is conducted showing the change of energy distribution between components of spectral tensor of turbulence. Development of initially isotropic turbulence and transition to anisotropy are studied. Model equations for fluid, current and cross helicity are derived. Differences in cases of rotating and non-rotating flows are discussed. This work was supported by the Russian Foundation for Basic Research (project no. 19-02-00016).

How to cite: Safonov, S. and Petrosyan, A.: Rapid distortion theory for homogeneous shear-driven MHD turbulence, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-8646, https://doi.org/10.5194/egusphere-egu2020-8646, 2020.

EGU2020-11902 | Displays | ST1.9

Non-linear waves interactions in rotating shallow water magnetohydrodynamics

Dmitry Klimachkov and Arakel Petrosyan

This study is devoted to the development of the nonlinear theory of the magneto-Poincare waves and magnetostrophic waves in rotating layers of astrophysical and space plasma in the shallow-water approximation. These waves determine the large-scale dynamics of the various astrophysical and space objects such as solar tachocline, as well as  magnetoactive atmospheres of exoplanets trapped by tides of a carrier star, neutron stars atmospheres and the flows in accretion disks of neutron stars. For this purpose we derived magnetohydrodynamic shallow water equations with a rotation and presence of an external vertical magnetic field. The system is obtained from conventional magnetohydrodynamic equations for incompressible inviscid heavy plasma layer with free surface in an external vertical magnetic field. The pressure is assumed to be hydrostatic, and the height of the plasma layer is considered to be much smaller than horizontal scales of the flow. The magnetohydrodynamic equations in the shallow-water approximation play equally important role in the space and astrophysical plasma flows like classical shallow-water equations in the fluid dynamics of a neutral fluid. The magnetohydrodynamic shallow water equations with an external vertical magnetic field are modified by supplementing them with the equation for the vertical component of the magnetic field and divergence-free condition for magnetic field contains its vertical component. Thus the velocity field remains two-dimensional while the magnetic field becomes three-dimensional. It is shown that the presence of a vertical magnetic field significantly changes the dynamics of the wave processes in astrophysical plasma compared to the neutral fluid and plasma layer in a horizontal magnetic field.  We have investigated the interaction of Magneto-Poincare waves and magnetostrophic waves in the magnetohydrodynamic shallow water flows in external vertical magnetic field and in horizontal (toroidal and poloidal) magnetic field. In the absence of the horizontal magnetic field the dynamics of plasma appears to be similar to the neutral fluid dynamics and it is shown that there are four-waves interactions in this case. Using the asymptotic multiscale method we obtained the non-linear amplitude equations for the three interacting Magneto-Poincare waves and magnetostrophic waves. The analysis of the amplitude equations shows that there are two types of instabilities for four different types of three-waves configurations. These instabilities occur in both cases: in the external vertical magnetic field and in the horizontal magnetic field. For all types of instabilities the growth rates are found. In the absence of the vertical magnetic field we obtained the non-linear amplitude equations for the four interacting waves. It is shown that the resulting system of equations has the first integrals that describe the mechanism of energy transfer among interacting waves of small amplitude. This work was supported by the Russian Foundation for Basic Research (project no. 19-02-00016).

How to cite: Klimachkov, D. and Petrosyan, A.: Non-linear waves interactions in rotating shallow water magnetohydrodynamics, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11902, https://doi.org/10.5194/egusphere-egu2020-11902, 2020.

EGU2020-12100 | Displays | ST1.9

Influence of He++ and shock geometry on interplanetary shocks in the solar wind: 2D Hybrid simulations

Luis Preisser, Xochitl Blanco-Cano, Domenico Trotta, David Burgess, and Primoz Kajdic

Alpha particles (He++) are the most important minor ion species in the solar wind, constituting typically about 5% of the total ion number density. When crossing an interplanetary shock protons and He++ particles are accelerated differently due to their different charge-to-mass ratio. This behavior can produce changes in the velocity distribution function (VDF) for both species in the immediate downstream region generating anisotropy in the temperature which is considered to be the energy source for various phenomena such as ion cyclotron and mirror mode waves for example. How these changes in temperature anisotropy and shock structure depend on the percentage of He++ particles and the geometry of the shock is not completely understood. In this work we perform various 2D local hybrid simulations (particle ions, massless fluid electrons) with similar characteristics (e.g., Mach number) to observed interplanetary shocks for both quasi-parallel and quasi-perpendicular geometries including self-consistently different percentages of He++ particles. We find that the change of the initial θBn leads to variations of the efficiency with which particles can escape to the upstream region facilitating or not the formation of compressive structures in the magnetic field that will produce increments in perpendicular temperature. The regions where both temperature anisotropy and compressive fluctuations appear tend to be more extended and reach higher values as the He++ content in the simulations increase.

How to cite: Preisser, L., Blanco-Cano, X., Trotta, D., Burgess, D., and Kajdic, P.: Influence of He++ and shock geometry on interplanetary shocks in the solar wind: 2D Hybrid simulations, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-12100, https://doi.org/10.5194/egusphere-egu2020-12100, 2020.

The solar wind in the heliosheath beyond the termination shock (TS) is a non-equilibrium collisionless plasma consisting of thermal solar wind ions, suprathermal pickup ions (PUI) and electrons. In such multi-ion plasma, two fast magnetosonic wave modes exist: the low-frequency fast mode that propagates in the thermal ion component and the high-frequency fast mode that propagates in the suprathermal PUI component [Zieger et al., 2015]. Both fast modes are dispersive on fluid and ion scales, which results in nonlinear dispersive shock waves. In this talk, we briefly review the theory of dispersive shock waves in multi-ion collisionless plasma. We present high-resolution three-fluid simulations of the TS and the heliosheath up to 2.2 AU downstream of the TS. We show that downstream propagating nonlinear magnetosonic waves grow until they steepen into shocklets (thin current sheets), overturn, and start to propagate backward in the frame of the downstream propagating wave, as predicted by theory [McKenzie et al., 1993; Dubinin et al., 2006]. The counter-propagating nonlinear waves result in fast magnetosonic turbulence far downstream of the shock. Since the high-frequency fast mode is positive dispersive on fluid scale, energy is transferred from small scales to large scales (inverse energy cascade). Thermal solar wind ions are preferentially heated by the turbulence. Forward and reverse shocklets in the heliosheath can efficiently accelerate both ions and electrons to high energies through the shock drift acceleration mechanism. We validate our three-fluid simulations with in-situ high-resolution Voyager 2 magnetic field and plasma observations at the TS and in the heliosheath. Our simulations reproduce the magnetic turbulence spectrum with a spectral slope of -5/3 observed by Voyager 2 in frequency domain [Fraternale et al., 2019]. However, since Taylor’s hypothesis is not true for fast magnetosonic perturbations in the heliosheath, the inertial range of the turbulence spectrum is not a Kolmogorov spectrum in wave number domain. 

How to cite: Zieger, B.: Inverse Energy Cascade of Fast Magnetosonic Turbulence in the Heliosheath, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-12219, https://doi.org/10.5194/egusphere-egu2020-12219, 2020.

EGU2020-13622 | Displays | ST1.9 | Highlight

Growth rate evaluation for the decay instability in space plasmas

Horia Comisel, Yasuhito Narita, and Uwe Motschmann

How to cite: Comisel, H., Narita, Y., and Motschmann, U.: Growth rate evaluation for the decay instability in space plasmas, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-13622, https://doi.org/10.5194/egusphere-egu2020-13622, 2020.

Solar magnetic field is a key paramters to understand the solar activity and its influence to the interplanetary space in the solar system. The solar magnetic field measurement is always an enormous challenge to the solar community. We firstly overview the history of solar magnetic field measurement since last early century and analyze the difficulty and progress of pratical methods. Then we introduce an infrared system for the accurate measurement of solar magnetic field (AIMS) and its current progress, which is supported by National Natural Science Foundation of China and also the current ongoing space based projects (ASO-S/FMG) to measure the solar magnetic field in China.

How to cite: Deng, Y.: Introduction to the current status of solar magnetic field measurements in China, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-13638, https://doi.org/10.5194/egusphere-egu2020-13638, 2020.

EGU2020-18602 | Displays | ST1.9 | Highlight

On the invariants of velocity and magnetic field gradient tensors in MHD theory

Giuseppe Consolini, Virgilio Quattrociocchi, Massimo Materassi, Tommaso Alberti, and Mirko Stumpo

In the framework of MHD turbulence, the velocity and magnetic field topological features can be characterized by three quantities invariant under rotations, which are defined by the velocity and magnetic field gradient tensors. These quantities provide information about field structures and dissipative features. 
In this work we present a preliminary derivation of the evolution of the invariant quantities of the velocity and magnetic field gradient tensors in the framework of MHD theory, using a Lagrangian point of view. This work can be considered as a first step useful to characterize and describe the evolution of the fields structures in  heliospheric space plasmas. Furthermore, some examples of the statistical features of magnetic field gradient tensor invariants, in the inertial and dissipation ranges, are also shown and discussed. 

How to cite: Consolini, G., Quattrociocchi, V., Materassi, M., Alberti, T., and Stumpo, M.: On the invariants of velocity and magnetic field gradient tensors in MHD theory, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18602, https://doi.org/10.5194/egusphere-egu2020-18602, 2020.

EGU2020-18835 | Displays | ST1.9

Relative magnetic helicity dissipation during the major flares

Quan Wang, Shangbin Yang, Mei Zhang, and Thomas Wiegelmann

    Magnetic helicity is conserved in ideal magnetic fluid and is still approximately conserved in the process of fast magnetic reconnection when the magnetic Reynolds number is large enough. We can derive the magnetic helicity injecting into corona from the magnetic helicity flux through photoshpere. A statistical research is carried out to investigate the dissipation of magnetic helicity during the major flares. We choose 69M-up flares from 16 major flare-productive active regions in 24th cycle to research the helicity in corona. Among these flares, 19 is X-up flares. We utilize Differential Affine Velocity Estimator for Vector Magnetograms (DAVE4VM) and 12-min successive vector magnetograms from Helioseismic and Magnetic Imager (HMI) on board the Solar Dynamics Observatory (SDO) to derive the flux of magnetic helicity through photosphere. At the same time, we extrapolate the vector magnetic field in corona to calculate the relative helicity by the suppose of Non-linear Force Free Field (NLFFF). The calculation window is 12-18 minutes before and after flares. A well correlation is shown between the magnetic free energy and magnetic helicity, the threshold of triggering M-up flare is the change of magnetic helicity above 2×1042Mx2 and the change of magnetic free energy above 3 × 1031erg . Considering one fifth of magnetic helicity injecting into corona, the dissipation of magnetic helicity during the flares is 6-7 % , which is corresponding to the result of previous numerical simulation results, which strongly support that the magnetic helicity is approximate conserved during the major flares.

How to cite: Wang, Q., Yang, S., Zhang, M., and Wiegelmann, T.: Relative magnetic helicity dissipation during the major flares, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18835, https://doi.org/10.5194/egusphere-egu2020-18835, 2020.

EGU2020-18905 | Displays | ST1.9

MHD simulations of an Uranus type rotating magnetosphere

Filippo Pantellini and Léa Griton

The characteristic relaxation time of the Uranus magnetosphere is of the order  of the planet's rotation period. This is also the case for Jupiter or Saturn. However, the specificity of Uranus (and to a lesser extent of  Neptune) is that the rotation axis and the magnetic dipole axis are separated by  a large angle (~60°) the consequence of which is the development of a highly dynamic and complex magnetospheric tail. In addition, and contrary to all other planets of the solar system, the rotation axis of Uranus happens to be quasi-parallel to the ecliptic plane which also implies a strong variability of the magnetospheric structure as a function of the season. The magnetosphere of Uranus is thus a particularly challenging case for global plasma simulations, even in the frame of MHD. We present MHD simulations of a Uranus type magnetosphere at both equinox (solar wind is orthogonal to the planetary rotation axis) and solstice (solar wind is orthogonal to the planetary rotation axis) configurations. The main differences between the two configurations will be discussed. 

How to cite: Pantellini, F. and Griton, L.: MHD simulations of an Uranus type rotating magnetosphere, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18905, https://doi.org/10.5194/egusphere-egu2020-18905, 2020.

EGU2020-20301 | Displays | ST1.9

Non-adiabatic interaction of ions with solar wind discontinuities

Alexander Vinogradov, Anton Artemyev, Ivan Vasko, Alexei Vasiliev, and Anatoly Petrukovich

According to Helios, Ulysses, New Horizons measurements at a wide range of distances from the Sun, radial evolution of solar wind ion temperature significantly deviates from the adiabatic expansion model:  additional heating of the solar wind plasma is required to describe observational data. Solution of the solar wind heating problem is extremely important both for understanding the structure of the heliosphere and for adequately describing the atmospheres of distant stars. Solar wind magnetic field is turbulent and this turbulence is dominated by numerous small-scale high-amplitude coherent structures – such as quasi-1D discontinuities. Modern theoretical models predict that quasi-1D discontinuities can play important role in solar wind heating. We collected the statistics of MMS observations of thin quasi-1D discontinuities in the solar wind to reveal their characteristics. Analyzing observational data, we construct the discontinuity model and use it to consider non-adiabatic interaction of ions with solar wind discontinuities. We mainly focus on discontinuity roles in solar wind ion scattering and thermalization. This presentation shows how discontinuity configuration affects the scattering rates.

How to cite: Vinogradov, A., Artemyev, A., Vasko, I., Vasiliev, A., and Petrukovich, A.: Non-adiabatic interaction of ions with solar wind discontinuities, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-20301, https://doi.org/10.5194/egusphere-egu2020-20301, 2020.

EGU2020-21114 | Displays | ST1.9

Electron Kinetic Instability Driven by Electron Temperature Anisotropy and Electron Beam in the Solar Wind

Jinsong Zhao, Heyu Sun, Wen Liu, Huasheng Xie, and Dejin Wu

Electron temperature anisotropy instabilities are believed to constrain the distributions of the electron parallel and perpendicular temperatures in the solar wind. When the electron perpendicular temperature is larger than the parallel temperature, the whistler instability is normally stronger than the electron mirror instability. While the electron parallel temperature is larger than the perpendicular temperature, the electron oblique firehose instability dominates the parallel firehose instability. Therefore, previous studies proposed the whistler and electron oblique firehose instabilities constraint on the electron dynamics in the solar wind. Based on the fact that there always exists the differential drift velocity among different electron populations, we consider the electron kinetic instability in the plasmas containing the electron anisotropic component and the electron beam component. Consequently, we give a comprehensive electron kinetic instability analysis in the solar wind. Furthermore, we propose that the electron acoustic/magneto-acoustic instability can arise in the low electron beta regime, and the whistler electron beam instability can be triggered in a wide beta regime. These two instabilities can provide a constraint on the electron beam velocity. Moreover, we find a new instability in the regime of the electron beta ~ 1, and this instability produces obliquely-propagating fast-magnetosonic/whistler waves. These results would be helpful for distinguishing the electron instability and for analyzing the constraint mechanism on the electron temperature distribution in the solar wind.

How to cite: Zhao, J., Sun, H., Liu, W., Xie, H., and Wu, D.: Electron Kinetic Instability Driven by Electron Temperature Anisotropy and Electron Beam in the Solar Wind, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21114, https://doi.org/10.5194/egusphere-egu2020-21114, 2020.

ST2.1 – Open Session on the Magnetosphere

EGU2020-9211 | Displays | ST2.1

Asymmetries in the Earth's dayside magnetosheath: results from global hybrid-Vlasov simulations

Lucile Turc, Vertti Tarvus, Andrew Dimmock, Markus Battarbee, Urs Ganse, Andreas Johlander, Maxime Grandin, Yann Pfau-Kempf, Maxime Dubart, and Minna Palmroth

The magnetosheath is the region bounded by the bow shock and the magnetopause which is home to shocked solar wind plasma. At the interface between the solar wind and the magnetosphere, the magnetosheath plays a key role in the coupling between these two media. Previous works have revealed pronounced dawn-dusk asymmetries in the magnetosheath properties, with for example the magnetic field strength and flow velocity being larger on the dusk side, while the plasma is denser, hotter and more turbulent on the dawn side. The dependence of these asymmetries on the upstream parameters remains however largely unknown. One of the main sources of these asymmetries is the bow shock configuration, which is typically quasi-parallel on the dawn side and quasi-perpendicular on the dusk side of the terrestrial magnetosheath because of the Parker-spiral orientation of the interplanetary magnetic field (IMF) at Earth. Most of these previous studies rely on collections of spacecraft measurements associated with a wide range of upstream conditions that have been processed to obtain the average values of the magnetosheath parameters. In this work, we use a different approach and quantify the magnetosheath asymmetries in global hybrid-Vlasov simulations performed with the Vlasiator model. We concentrate on three parameters: the magnetic field strength, the plasma density and the flow velocity. We find that the Vlasiator model reproduces accurately the polarity of the asymmetries, but that their level tends to be higher than in spacecraft measurements, probably due to the different processing methods. We investigate how the asymmetries change when the IMF becomes more radial and when the Alfvén Mach number decreases. When the IMF makes a 30° angle with the Sun-Earth line instead of 45°, we find a stronger magnetic field asymmetry and a larger variability of the magnetosheath density. In contrast, a lower Alfvén Mach number leads to a decrease of the magnetic field asymmetry level and of the variability of the magnetosheath density and velocity, likely due to weaker foreshock processes.

How to cite: Turc, L., Tarvus, V., Dimmock, A., Battarbee, M., Ganse, U., Johlander, A., Grandin, M., Pfau-Kempf, Y., Dubart, M., and Palmroth, M.: Asymmetries in the Earth's dayside magnetosheath: results from global hybrid-Vlasov simulations, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-9211, https://doi.org/10.5194/egusphere-egu2020-9211, 2020.

During magnetic reconnection, magnetic energy is explosively converted to particle energy and consequently electrons are accelerated to hundreds of keV that are dangerous to spacecraft and astronauts. To date, how and where the acceleration happens during reconnection is still unknown. Also, how efficient can the acceleration be remains a puzzle. Using spacecraft measurements (e.g., Cluster and MMS) and numerical simulations, many attempts have been made to answer these questions during the last twenty years. In this talk, I will briefly review these progresses and then show our recent results in understanding these issues. Specifically, I will (1) report a super-efficient electron acceleration by magnetic reconnection in the Earth’s magnetotail, during which electron fluxes are enhanced by 10000 times within 30 seconds; (2) discuss the mechanisms leading to super-efficient electron acceleration; (3) report the first evidence of electron acceleration at a reconnecting magnetopause, during which the acceleration process is nonadiabatic; and (4) report electron acceleration in the

How to cite: Fu, H.: Energetic electron acceleration during magnetic reconnection, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1945, https://doi.org/10.5194/egusphere-egu2020-1945, 2020.

EGU2020-5786 | Displays | ST2.1

Origins and Evolution of the Electron and Ion Populations of the Magnetopause’s Boundary Layers

Jean Berchem, Giovanni Lapenta, Robert Richard, William Paterson, and C. Philippe Escoubet

Increasingly sophisticated instruments and simulations have revealed a wide variety of plasma processes and multiscale structures at the dayside magnetopause. In this presentation, we focus on the origins and evolution of the plasma populations observed in the magnetopause boundary layers. We present the results of Particle-In-Cell (PIC) simulations encompassing large volumes of the dayside magnetosphere. The implicit 3D PIC code used in the study was initialized from a global MHD state of the magnetosphere for southward interplanetary field conditions.  Three-dimensional plots of the perpendicular slippage indicates that reconnection occurs over most of the dayside magnetopause. However, the simulation reveals that the reconnection region has a much more filamentary structure than the X-line expected from the extrapolation of 2D models and that multiscale structures thread the reconnection outflow. In particular, the simulation indicates the formation of multiple layers of electrons with significant field-aligned velocities along the main magnetopause current layer. We use velocity distribution functions at different locations in the reconnection outflow to characterize the origins and evolution of the electron and ionpopulations of the magnetosheath and magnetospheric boundary layers and compare them with observations from the MMS and Cluster spacecraft.

How to cite: Berchem, J., Lapenta, G., Richard, R., Paterson, W., and Escoubet, C. P.: Origins and Evolution of the Electron and Ion Populations of the Magnetopause’s Boundary Layers, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5786, https://doi.org/10.5194/egusphere-egu2020-5786, 2020.

EGU2020-21014 | Displays | ST2.1

Evolution of Turbulence in the Kelvin–Helmholtz Instability mediated by the Magnetopause and its Boundary Layer
not presented

Francesca Di Mare, Luca Sorriso-Valvo, Alessandro Retino', Francesco Malara, and Hiroshi Hasegawa

The turbulence at the interface between the solar wind and the Earth’s magnetosphere, mediated by the magnetopause and its boundary layer are investigated by using Geotail and THEMIS spacecraft data during ongoing Kelvin-Helmholtz instability (KHI). The efficient transfer of energy across scales for which the turbulence is responsible, achieves the connection between the macroscopic flow and the microscopic dissipation of this energy. This boundary layer is thought to be the result of the observed plasma transfer, driven by the development of the KHI, originating from the velocity shear between the solar wind and the almost static near-Earth plasma. A collection of 20 events spatially located on the tail-flank magnetopause, selected from previously studied by Hasegawa et al. 2006 and Lin et al. 2014, have been tested against standard diagnostics for intermittent turbulence. In light of the results obtained, we have investigated the behaviour of several parameters as a function of the progressive departure along the Geocentric Solar Magnetosphere coordinates, which roughly represent the direction in which we expect the KHI vortices to evolve towards fully developed turbulence. It appears that a fluctuating behaviour of the parameters exist, visible as a decreasing, quasi-periodic modulation with an associated periodicity, estimated to correspond to approximately 6.4 Earth Radii. Such observed wavelength is consistent with the estimated vortices roll-up wavelength reported in the literature for these events. If the turbulence is pre-existent, it is possible that the KHI modulates its properties along the magnetosheath, as we observed. On the other hand, if we assume that the KHI has been initiated near the magnetospheric nose and develops along the flanks, then the different intervals we study may be sampling the plasma at different stages of evolution of the KH-generated turbulence, after the instability has injected energy in a cascading process as large-scale structures.

How to cite: Di Mare, F., Sorriso-Valvo, L., Retino', A., Malara, F., and Hasegawa, H.: Evolution of Turbulence in the Kelvin–Helmholtz Instability mediated by the Magnetopause and its Boundary Layer, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21014, https://doi.org/10.5194/egusphere-egu2020-21014, 2020.

EGU2020-11901 | Displays | ST2.1

Magnetotail flows near lunar orbit and their relation to substorms

Stefan Kiehas, Andrei Runov, Vassilis Angelopoulos, and Daniil Korovinskiy

We perform a five year statistical study of fast flows in the Earth's magnetotail observed by ARTEMIS to investigate their occurrence rate, dawn-dusk asymmetry and relation with magnetospheric substorms. Almost half of the observed flows are directed earthward and their percentage decreases with increasing flow speed. While no clear dawn-dusk asymmetry is observed for earthward directed flows, about 60% of the tailward flows occur in the dusk sector. For tailward flows this asymmetry is similar for different AL thresholds. However, earthward flows become strongly asymmetric towards dusk for higher AL thresholds. A correlation of flow events with the AL index also shows a clear correlation of tailward flows with a decrease in AL, while such a correlation can not be seen for earthward flows. 

How to cite: Kiehas, S., Runov, A., Angelopoulos, V., and Korovinskiy, D.: Magnetotail flows near lunar orbit and their relation to substorms, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11901, https://doi.org/10.5194/egusphere-egu2020-11901, 2020.

Usually, for the plasma pressure estimation in the plasma sheet  ion observations in the energy range up to ~40 keV are used. However, the thermal part of the distribution function can pass beyond the high energy threshold of an instrument during active events like dipolarizations. In such cases the entire ion population is not measured and the ion pressure can be underestimated. We study this problem by using Cluster mission observations provided  by two instruments: thermal plasma instrument - CODIF (up to 38 keV) and suprathermal instrument - RAPID (from 40 up to 1500 keV). We analyzed 11 dipolarization events and showed that in all events the maximum of ion energy flux was shifted to high energy threshold of CODIF instrument. Simultaneously, the energy flux increase in suprathermal energy range was observed by RAPID. For H+ and O+ ion components we calculate the pressure of suprathermal population and showed that the total pressure estimated by using both CODIF and RAPID instruments at some intervals exceeds the pressure estimated only from CODIF data up to 5 times. The superposed epoch analysis applied to 11 dipolarization events from our data base showed that the total pressure of H+ and O+ ion components can be in 2-5 times underestimated in the course of dipolarization.

How to cite: Malykhin, A., Grigorenko, E., Kronberg, E., and Daly, P.: Сomparison of ion pressure variations derived from Cluster/CODIF and the combined Cluster/CODIF&RAPID data during prolonged dipolarizations in the near Earth magnetotail , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1488, https://doi.org/10.5194/egusphere-egu2020-1488, 2020.

EGU2020-10783 | Displays | ST2.1 | Highlight

The SMILE mission: A novel way to explore solar-terrestrial interactions

Graziella Branduardi-Raymont, Chi Wang, C. Philippe Escoubet, Steve Sembay, Eric Donovan, Lei Dai, Lei Li, Jing Li, David Agnolon, Walfried Raab, Jonathan Rae, Andy Read, Emma L. Spanswick, Jenny A. Carter, Hyunju Connor, Tianran Sun, Andrey Samsonov, and David G. Sibeck

The coupling between the solar wind and the Earth's magnetosphere-ionosphere system, and the geospace dynamics that result, comprise some of the key questions in space plasma physics. In situ measurements by a fleet of solar wind and magnetospheric missions, current and planned, can provide the most detailed observations of the Sun-Earth connections. However, we are still unable to quantify the global effects of the drivers of such connections, and to monitor their evolution with time. This information is the key missing link for developing a comprehensive understanding of how the Sun gives rise to and controls the Earth's plasma environment and space weather.

SMILE (Solar wind Magnetosphere Ionosphere Link Explorer) is a novel self-standing mission dedicated to observing the solar wind - magnetosphere coupling via simultaneous X-ray imaging of the magnetosheath and polar cusps (large spatial scales at the magnetopause), UV imaging of global auroral distributions (mesoscale structures in the ionosphere) and in situ solar wind/magnetosheath plasma and magnetic field measurements. X-ray imaging of the magnetosheath and cusps is made possible by the X-ray emission produced in the process of solar wind charge exchange, first observed at comets, and subsequently found to occur in the vicinity of the Earth's magnetosphere. One of the science aims of SMILE is to track the substorm cycle, via X-ray imaging on the dayside and by following its consequences on the nightside with UV imaging. 

SMILE is a collaborative mission between ESA and the Chinese Academy of Sciences (CAS) that was selected in November 2015, adopted into ESA’s Cosmic Vision Programme in March 2019, and is due for launch at the end of 2023. The science that SMILE will deliver, as well as the ongoing technical developments and scientific preparations, and the current status of the mission, will be presented.

 

How to cite: Branduardi-Raymont, G., Wang, C., Escoubet, C. P., Sembay, S., Donovan, E., Dai, L., Li, L., Li, J., Agnolon, D., Raab, W., Rae, J., Read, A., Spanswick, E. L., Carter, J. A., Connor, H., Sun, T., Samsonov, A., and Sibeck, D. G.: The SMILE mission: A novel way to explore solar-terrestrial interactions , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-10783, https://doi.org/10.5194/egusphere-egu2020-10783, 2020.

EGU2020-13572 | Displays | ST2.1

Helium in the Earth's foreshock: a global Vlasiator survey

Markus Battarbee, Xóchitl Blanco-Cano, Lucile Turc, Primoz Kajdic, Vertti Tarvus, Andreas Johlander, Markku Alho, Thiago Brito, Mojtaba Akhavan-Tafti, Maxime Dubart, Urs Ganse, Maxime Grandin, Tomas Karlsson, Yann Pfau-Kempf, Savvas Raptis, Jonas Suni, and Minna Palmroth

The foreshock is a region of space in front of the Earth's bow shock, extending along the interplanetary magnetic field. It is permeated by ions and electrons reflected at the shock, low-frequency waves, and various plasma transients. The ion foreshock is dominated by a number of proton populations such as field-aligned beams, gyrating distributions and diffuse ions, as well as proton-excited waves. As the solar wind can contain a significant fraction of helium, it is of great interest to investigate how alpha-particles (He2+) are reflected into forming their own foreshock. We investigate the extent of the helium foreshock in relation to foreshock ultra-low frequency waves and protons using Vlasiator, a global hybrid-Vlasov simulation. We confirm a number of historical spacecraft observations at the foreshock regions associated with field-aligned beams, gyrating ion distributions, and specularly reflected particles, performing the first numerical global survey of the helium foreshock. We present wavelet analysis at multiple positions within the foreshock and evaluate the dynamics of gyrating ion populations in response to the transverse and compressive wave components. We also present Magnetosphere Multiscale (MMS) spacecraft crossings of the foreshock edge and compare Hot Plasma Composition Analyzer (HPCA) measurements of energetic ions with our simulation data, showing the variability of the foreshock edge suprathermal ion profiles.

How to cite: Battarbee, M., Blanco-Cano, X., Turc, L., Kajdic, P., Tarvus, V., Johlander, A., Alho, M., Brito, T., Akhavan-Tafti, M., Dubart, M., Ganse, U., Grandin, M., Karlsson, T., Pfau-Kempf, Y., Raptis, S., Suni, J., and Palmroth, M.: Helium in the Earth's foreshock: a global Vlasiator survey, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-13572, https://doi.org/10.5194/egusphere-egu2020-13572, 2020.

When a shock is moving through a cluster of spacecraft, the normal N to the shock and the velocity of the shock along N can be determined from the crossing times of the different spacecraft assuming that the shock is planar and moves without deformation or rotation during the time interval of the encounter. For a cluster of four spacecraft there are six pairs of spacecraft, each one giving raise to a scalar equation relating the vector position R from the first to the second spacecraft, the normal vector N and the time lag Dt : R.N=VDt. This over-determined system of six equations is solved by computing the pseudo inverse of the matrix M acting on the normal vector on the lhs of the equation. Thus the system is modified by attributing a priori a positive weight to each equation (wj, j=1 to 6) the sum being constrained to 1. Then a statistical ensemble of 6-uplets (wj, j=1 to 6) is built ; for each element of this ensemble we compute the condition number of matrix M and we look for the 6-uplet giving the lowest condition number. This procedure warrants the best accuracy of the pseudo-inverse of M and hence the best estimate of the normal vector N. Adding random perturbations to M and to the time lags allows to estimate the uncertainties on N and V through simulations. This optimized timing method is applied to reanalyze some crossings of the terrestrial bow-shock by CLUSTER and the results are compared to the results obtained by the standard method using the reciprocal vectors defined in the ISSI report SR-008 « Multi-Spacecraft Analysis Methods Revisited » published in 2008. A similar method has been applied to the determination of wave vectors of chorus elements observed by MMS in the inner magntosphere.

How to cite: Chanteur, G. M.: Reanalysis of Some CLUSTER Bow-Shock Crossings With an Optimized Timing Method, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11440, https://doi.org/10.5194/egusphere-egu2020-11440, 2020.

EGU2020-13632 | Displays | ST2.1

Statistical study of foreshock transients in a global hybrid-Vlasov magnetospheric simulation

Vertti Tarvus, Lucile Turc, Markus Battarbee, Xochitl Blanco-Cano, Primoz Kajdic, Jonas Suni, Markku Alho, Maxime Dubart, Urs Ganse, Maxime Grandin, Andreas Johlander, Yann Pfau-Kempf, Konstantinos Papadakis, and Minna Palmroth

Upstream of Earth's bow shock lies the foreshock, a region permeated by bow shock-reflected electrons and ions propagating against the incoming solar wind. The interaction between the reflected ions and the solar wind leads to instabilities, which generate Ultra Low Frequency (ULF) waves in the foreshock. Another feature of the foreshock are various propagating transient structures. A particular type of transients are foreshock cavitons, which are characterized as simultaneous depressions of plasma density and magnetic field bounded by edges where these parameters are enhanced.
    Cavitons are proposed to form as a consequence of the non-linear evolution of two ULF wave types. They are carried by the solar wind towards the shock, but have been found to propagate sunward in the solar wind rest frame. Studies have shown that cavitons can accumulate reflected suprathermal ions inside them as they approach the bow shock, causing significant heating and bulk flow deflection in their interiors. These signatures resemble those of Hot Flow Anomalies (HFAs), transients which are associated with interplanetary magnetic field (IMF) discontinuities interacting with the bow shock. As the evolution of cavitons is independent of IMF discontinuities, the hot, evolved transients are classified as spontaneous HFAs (SHFAs). SHFAs arriving to the shock have been found to cause perturbations to the shock surface and the magnetosheath downstream of it.
    In this work, a numerical statistical study of cavitons and SHFAs is conducted with Vlasiator, a global hybrid-Vlasov code. Individual transients are tracked, allowing us to examine their formation rate, propagation characteristics and evolution in addition to their physical properties. Our results show that cavitons and SHFAs form in a uniform region near the bow shock, and there is a distinct distance to the shock within which cavitons can become SHFAs. The density and magnetic field depressions inside cavitons appear well correlated, although shallow compared to spacecraft measurements. We find that both transient types propagate sunwards in the solar wind rest frame, agreeing with earlier studies. Our statistical data set allows us to calculate the propagation velocity, which shows a similar value for all tracked transients. Our results also suggest that the velocity has a southward component. 

How to cite: Tarvus, V., Turc, L., Battarbee, M., Blanco-Cano, X., Kajdic, P., Suni, J., Alho, M., Dubart, M., Ganse, U., Grandin, M., Johlander, A., Pfau-Kempf, Y., Papadakis, K., and Palmroth, M.: Statistical study of foreshock transients in a global hybrid-Vlasov magnetospheric simulation, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-13632, https://doi.org/10.5194/egusphere-egu2020-13632, 2020.

EGU2020-5246 | Displays | ST2.1

Energy conversion at the terrestrial bow shock

Maria Hamrin, Ramon Lopez, Pauline Dredger, Herbert Gunell, Oleksandr Goncharov, and Timo Pitkänen

At Earth’s bow shock, the supersonic solar wind is slowed down and deflected around the magnetosphere. To many this is "just a bow shock", a simple and quite passive element of solar-terrestrial physics. However, it has recently been realized that the bow shock plays a significantly more important role with currents on the bow shock connecting through the magnetosheath to the magnetospheric current systems. The bow shock current cannot close locally, since the magnetic field compression in the magnetosheath cannot be maintained globally. The bow shock current is inevitably a generator current extracting mechanical energy from the supersonic solar wind, and feeding it to other processes such as acceleration of the magnetosheath flow, local particle acceleration at the bow shock and dissipation in the distant ionosphere. Here we use data from the first dayside season of the Magnetospheric Multiscale (MMS) mission to investigate the generator properties of the terrestrial bow shock. Typically, the main shock ramp shows clear generator properties, but for some of the more turbulent bow shocks, generator properties may also be observed slightly downstream the ramp. This may be due to effects from shock motions and shock nonstationaity and reformation. Moreover, sometimes a weaker load can be seen in the upstream foot region due to local particle acceleration. We also find that the generator capacity of the bow shock decreases with decreasing bow shock angle as well as with increasing upstream plasma beta and solar Mach number. A better understanding of the energy conversion properties of the terrestrial bow shock will be useful also for the understanding of other astrophysical shock currents. The currents must close somewhere and deposit energy somewhere.

How to cite: Hamrin, M., Lopez, R., Dredger, P., Gunell, H., Goncharov, O., and Pitkänen, T.: Energy conversion at the terrestrial bow shock, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5246, https://doi.org/10.5194/egusphere-egu2020-5246, 2020.

EGU2020-7352 | Displays | ST2.1

Geoeffectiveness of Magnetosheath Jets

Linus Norenius, Maria Hamrin, Oleksandr Goncharov, Herbert Gunell, Tomas Karlsson, Hermann Opgenoorth, and Siung Chong

The study on high speed plasma flows in the Earth’s magnetosheath, or commonly known as jets, has been a popular topic for discussion in recent decades. These jets can often be characterised by increases in the dynamic pressure compared to the background plasma. They can propagate through the magnetosheath and impact the magnetopause, causing indentations and possibly triggering waves on the magnetopause and contribute to energy and mass transfer into the magnetosphere. Previous studies suggest that the effects from these impacts are detectable inside the magnetosphere at geostationary orbit, and even at ground level causing geoeffective responses. Case studies show indications where ground based magnetometers, GMAGs, have observed magnetic pulses as a result of impacting jets. By using data from the MMS mission and GMAGs, we conduct an observational study with a larger set of jets compared to previous works. The geoeffectiveness of these jets will be investigated and the properties of the responses in the GMAG observations will be discussed.

How to cite: Norenius, L., Hamrin, M., Goncharov, O., Gunell, H., Karlsson, T., Opgenoorth, H., and Chong, S.: Geoeffectiveness of Magnetosheath Jets, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7352, https://doi.org/10.5194/egusphere-egu2020-7352, 2020.

EGU2020-1498 | Displays | ST2.1

Is the relation between the solar wind dynamic pressure and the magnetopause standoff distance so simple?

Andrey Samsonov and Graziella Branduardi-Raymont

The relation between the solar wind dynamic pressure and magnetopause standoff distance is usually supposed to be RSUB~Pd-1/N. The simple pressure balance condition gives N=6, however N varies in empirical magnetopause models from 4.8 to 7.7. Using several MHD models, we simulate the magnetospheric response to increases in the dynamic pressure by varying separately the solar wind density or the velocity. We obtain different values of N depending on which parameter, density or velocity, has been varied and for which IMF orientation. The changes in the standoff distance are smaller (higher N) for a density increase and greater (smaller N) for a velocity increase for southward IMF. We explain this result by enhancement of the Region 1 current that moves the magnetopause closer to the Earth for a high solar wind velocity. We suggest for developers of new empirical magnetopause models in the future to replace the simple relation between RSUB and Pd with a fixed N by a more complicated relation which would separate inputs in the dynamic pressure from the density and velocity taking into account the IMF orientation.

How to cite: Samsonov, A. and Branduardi-Raymont, G.: Is the relation between the solar wind dynamic pressure and the magnetopause standoff distance so simple?, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1498, https://doi.org/10.5194/egusphere-egu2020-1498, 2020.

EGU2020-21093 | Displays | ST2.1

Role of non-diagonal pressure tensor components in balance of magnetopause current sheet

Egor Yushkov, Anton Artemyev, and Anatoly Petrukovich

We study the current sheet model separating a strong magnetic field area from the intense solar wind. We use the ideal MHD equations for ideas proposed by D. Nickeler and T. Wiegelmann to describe the transition region with plasma flows inclined to the boundary field. We show that balance in this case can be supported by nondiagonal components of modified pressure tensor. We discuss the possible application of the results to a description of the Earth’s night-side magnetopause boundary and study influence of solar wind characteristics on magnetopause current structure. We show problems that follow from ideal mhd-approach and from our assumptions about stationarity of two-dimensional CS on examples of magnetopause crossings by MMS mission. We speculate about further model development to day-side and magnetopause flanks application. This work is supported by the RFBR grant N 18-02-00218.

How to cite: Yushkov, E., Artemyev, A., and Petrukovich, A.: Role of non-diagonal pressure tensor components in balance of magnetopause current sheet, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21093, https://doi.org/10.5194/egusphere-egu2020-21093, 2020.

EGU2020-7443 | Displays | ST2.1

Mid-altitude cusp dynamics and properties during the IMF By dominated intervals

Yulia Bogdanova, C.-Philippe Escoubet, Robert Fear, Karlheinz Trattner, Jean Berchem, Andrew Fazakerley, and Frederic Pitout

Observations inside the cusp can be used as distant monitoring of the large-scale geometry and properties of the magnetic reconnection at the magnetopause. The recent modelling and observations of the cusp and flux transfer events in the vicinity of the magnetopause show that the reconnection can occur along the X-line extended over many hours of magnetic local time (MLT), comprising sites of both component and anti-parallel reconnection scenarios. Such observations are in contradiction to the statistical DMSP studies showing that the cusp is rather limited in magnetic local time with an average size 2.5 hours of MLT. Moreover, some past observations indicate that the cusp is moving in response to the changes of the IMF By component, suggesting that the cusp is formed due to anti-parallel reconnection along the X-line limited in MLT.

In this presentation we analyse several events of the mid-altitude cusp observations during the Cluster campaign when the satellites cross the cusp mainly along the longitude in a string-of-pearls configuration during an Interplanetary Magnetic Field (IMF) configuration with a stable and dominant IMF By-component. During this particular Cluster orbit it was possible to define the dawn and dusk cusp boundaries and to study plasma parameters inside different parts of the cusp region. The observations will be discussed in terms of the cusp extension, cusp motion, and possible formation of the ‘double’ cusp structures. Finally, we will consider what these observations reveal about the large-scale reconnection geometry at the magnetopause.

How to cite: Bogdanova, Y., Escoubet, C.-P., Fear, R., Trattner, K., Berchem, J., Fazakerley, A., and Pitout, F.: Mid-altitude cusp dynamics and properties during the IMF By dominated intervals, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7443, https://doi.org/10.5194/egusphere-egu2020-7443, 2020.

EGU2020-5823 | Displays | ST2.1

Particle Acceleration in Earth’s Global Magnetosphere: a Multiple Step Process

Robert L. Richard, David Schriver, Jean Berchem, Mostafa El-Alaoui, Giovanni Lapenta, and Raymond J. Walker

Particle velocity distribution functions measured by spacecraft show that suprathermal ion and electron populations are a common feature of Earth’s magnetosphere.  An outstanding question has been to determine the acceleration processes that lead to the formation of these suprathermal particle populations. Very often, it has been challenging to explain the high levels of energy reached by these particles by simply invoking local processes such as magnetic reconnection. In this presentation, we investigate the hypothesis that suprathermal particle populations increase if the acceleration occurs over multiple steps through different acceleration mechanisms at different spatial locations in Earth’s magnetosphere.  For example, particles transported to the magnetotail which have been accelerated first in the dayside reconnection region could be further accelerated in the tail reconnection regions and then gain additional energy through Fermi and/or betatron acceleration as they convected back to the dayside magnetopause. Since local kinetic processes dominate the acceleration of ions and electrons in the magnetosphere, it has been difficult to validate that hypothesis. Multiple reconnection sites and different possible acceleration regions are too distant to be included in a single kinetic simulation and global hybrid simulations cannot describe electron acceleration.  To address this research problem we leverage our simulation capabilities by combining three different simulation techniques: global magnetohydrodynamic (MHD) simulations, large-scale kinetic (LSK) particle tracing simulations, and large-scale particle in cell (PIC) simulations.  First, we carry out an MHD simulation driven by upstream solar wind and interplanetary magnetic field conditions for a specific time interval featuring active magnetospheric reconnection.  Then we use an implicit PIC simulation of dayside reconnection with initial and boundary conditions from the MHD simulation.  Next, we follow suprathermal particles from the PIC simulation globally through the MHD fields using LSK to assess their transport into the magnetotail. A final step is to perform a PIC simulation embedded in the MHD simulation of magnetotail process including the suprathermal particles arriving from the dayside as determined from the LSK simulation.  Preliminary results indicate that particles energized by dayside reconnection are more likely to reach the magnetotail reconnection region. In addition, the development of enhanced high-energy tails in the particle distributions is promoted by previous energization steps during particle transport to the magnetotail reconnection region.

How to cite: Richard, R. L., Schriver, D., Berchem, J., El-Alaoui, M., Lapenta, G., and Walker, R. J.: Particle Acceleration in Earth’s Global Magnetosphere: a Multiple Step Process, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5823, https://doi.org/10.5194/egusphere-egu2020-5823, 2020.

EGU2020-6210 | Displays | ST2.1

Particle Acceleration and Transport in the Magnetotail

Mostafa El-ALaoui, Jean Berchem, Robert L. Richard, David Schriver, Giovanni Lapenta, and Raymond J. Walker

An outstanding problem of magnetospheric physics is to determine the energization of particles transported from the nightside to the dayside. To address this research problem, we leverage our simulation capabilities by combining three different simulation techniques: global magnetohydrodynamic (MHD) simulations, large-scale kinetic (LSK) particle tracing simulations, and large-scale particle in cell (PIC) simulations. First, we model a magnetotail reconnection event using an iPic3D simulation with initial and boundary conditions given by a global MHD simulation. The iPic3D simulation system includes the region of fast outflows emanating from the reconnection site that drives the formation of dipolarization fronts.Then, we follow millions of test particles that exit the iPic3D system using the electromagnetic fields from the MHD simulation as they convect to the dayside and quantify the different acceleration and transport mechanisms.

How to cite: El-ALaoui, M., Berchem, J., Richard, R. L., Schriver, D., Lapenta, G., and Walker, R. J.: Particle Acceleration and Transport in the Magnetotail, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6210, https://doi.org/10.5194/egusphere-egu2020-6210, 2020.

EGU2020-9851 | Displays | ST2.1

Statistical magnetospheric location of auroral omega bands obtained by empirical magnetic field models

Varvara Andreeva, Sergey Apatenkov, Evgeny Gordeev, Noora Partamies, and Kirsti Kauristie

Omega bands are curved aurora forms, which appear as rows of inverted Greek letter Ω drifting eastward and may result in substantial magnetic field variations on the ground. Since they were reported for the first time more than 50 years ago, their ionospheric signatures were thoroughly studied to the present moment. In contrast, magnetospheric processes resulting in the omega-bands generation are poorly understood, mostly due to a small number of conjugated spacecraft observations. Therefore, the only possibility to statistically study magnetospheric features of the omega bands is to use different models.

The goal of the present work is to find a characteristic magnetic field configuration corresponding to this type of aurora. We used the list of omega bands (Partamies et al., 2017), observed in the Fennoscandian Lapland in the period 1997-2007, the MIRACLE all-sky camera data, and new empirical magnetic field model (Tsyganenko and Andreeva, 2016) to identify the magnetospheric equatorial location of the observed omega structures. This work presents the most extensive statistical study of the omega bands projections; in previous papers only a case-study mapping based on few events was described. We found that for 90% of the omega bands aurora its possible source is located on the radial distances from the Earth 6-13 Re in the morning sector (2-4 h MLT), with the average position at R=8 Re and 3 MLT. We also estimated a minimal life-time of the omega bands source in the magnetosphere. This study has been funded by the Russian Science Foundation Grant 19-77-10016.

Partamies, N., Weygand, J. M., and Juusola, L.: Statistical study of auroral omega bands, Ann. Geophys., 35, 1069–1083, https://doi.org/10.5194/angeo-35-1069-2017, 2017.
Tsyganenko, N. A., and V. A. Andreeva (2016), An empirical RBF model of the magnetosphere parameterized by interplanetary and ground-based drivers, J. Geophys. Res. Space Physics, 121, doi:10.1002/2016JA023217.

How to cite: Andreeva, V., Apatenkov, S., Gordeev, E., Partamies, N., and Kauristie, K.: Statistical magnetospheric location of auroral omega bands obtained by empirical magnetic field models, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-9851, https://doi.org/10.5194/egusphere-egu2020-9851, 2020.

EGU2020-4003 | Displays | ST2.1

Roles of electrons and ions in formation of the current in mirror mode structures in the terrestrial plasma sheet: MMS observations

Guoqiang Wang, Tielong Zhang, Mingyu Wu, Daniel Schmid, Yufei Hao, Zonghao Pan, and Martin Volwerk

Currents are believed to exist in mirror mode structures and to be self-consistent with the magnetic field depression. Here, we investigate a train of mirror mode structures in the terrestrial plasma sheet on 11 August 2017 measured by the Magnetospheric Multiscale mission. We find that bipolar current densities exist in the cross-section of two hole-like mirror mode structures, referred to as magnetic dips. The bipolar current in the magnetic dip with a size of ~2.2 ρi (the ion gyro radius) is mainly contributed by variations of the electron velocity, which is mainly formed by the magnetic gradient-curvature drift. For another magnetic dip with a size of ~6.6 ρi, the bipolar current is mainly caused by an ion bipolar velocity, which can be explained by the collective behaviors of the ion drift motions. These observations suggest that the electrons and ions play different roles in the formation of currents in magnetic dips with different sizes.

How to cite: Wang, G., Zhang, T., Wu, M., Schmid, D., Hao, Y., Pan, Z., and Volwerk, M.: Roles of electrons and ions in formation of the current in mirror mode structures in the terrestrial plasma sheet: MMS observations, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4003, https://doi.org/10.5194/egusphere-egu2020-4003, 2020.

EGU2020-4516 | Displays | ST2.1

Characterization of the Pc5 frequency range power spectrum at low latitude in 22 years of geomagnetic field observations.

Alessandro Colonico, Simone Di Matteo, and Umberto Villante

An important aspect of the interaction between the solar wind (SW) and the Earth’s magnetosphere concerns the possible relationship between SW and magnetospheric fluctuations under different SW conditions. In recent investigations (Di Matteo and Villante, 2017,2018) we revealed the critical role of the analytical methods and the spectral analysis techniques in the identification of fluctuations between ≈1-5 mHz in the SW parameters as well as in the magnetospheric field measurements at the geostationary orbit and developed a new approach, based on the joint use of the Welch and the Multitaper methods, for a more robust identification of these oscillations in both regions. Here, we extend the analysis to ground measurements, analyzing 22 years of magnetic field measurements along the H and D components at low latitude (L’Aquila, Italy, λ≈36.3°, L≈1.6). We found that, in general, the much steeper spectrum of the geomagnetic fluctuations with respect to the ones estimated in the SW parameters and magnetospheric field, might deeply influence the identification of real events. We then examined, for the entire period, consecutive two hours intervals through the day during low geomagnetic activity conditions (Dst>-50), and, for each interval, we carefully evaluated the characteristics of the background spectrum. As a matter of fact, in the ≈1-5 mHz frequency range the spectral indices of both components typically range between -3.5 and -2 with a steeper spectrum in the night sector when the fluctuations power is lower. Simulations of red noise representations, with spectral indices similar to the observed ones, combined with the Sq variation show a systematic reduction of the rate of identification of real events up to ≈2 mHz.

Ref.

Di Matteo, S., and U. Villante, J. Geophys.Res. Space Physics, 122, 4905–4920, doi:10.1002/2017JA023936.

Di Matteo, S., and U. Villante, Journal of Geophysical Research: Space Physics, 123, doi.org/10.1002/2017JA024922.

How to cite: Colonico, A., Di Matteo, S., and Villante, U.: Characterization of the Pc5 frequency range power spectrum at low latitude in 22 years of geomagnetic field observations., EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4516, https://doi.org/10.5194/egusphere-egu2020-4516, 2020.

The geomagnetic cutoff rigidity R (momentum per unit charge) is the threshold rigidity below which the particle flux becomes zero due to geomagnetic shielding. The properties of the geomagnetic screen vary greatly during magnetic storms, depending on the dynamic interaction of the solar wind (SW) magnetic fields with the magnetospheric fields and currents. The correlation between the variations of geomagnetic cutoff rigidity ΔR and interplanetary parameters and geomagnetic activity indexes during various phases of the superstorm on November 7 – 8, 2004 has been calculated. On the scale of the entire storm the most geoeffеctive parameters were Dst, Kp, and SW speed, while other parameters, including total interplanetary magnetic field B and Bz component, were effective at different phases of the storm.

How to cite: Vernova, E., Ptitsyna, N., Danilova, O., and Tyasto, M.: Correlation between the variations of cosmic ray geomagnetic thresholds and interplanetary parameters during various phases of solar disturbance in November 2004, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-9971, https://doi.org/10.5194/egusphere-egu2020-9971, 2020.

EGU2020-4488 | Displays | ST2.1

Study on the variation of energetic particle pitch angle caused by NWC VLF transmitter

Wei Chu, Song Xu, ZhenXia Zhang, Jianping Huang, Zhima Zeren, and Xuhui Shen

Based on the observation data collected by the Energetic Particles Detector Package(HEPP) on board CSES satellite during the period of 2018 and 2019.We analyzed the characterizes of pitch angle spectrum of energetic electron precipitated caused by NWC. Our analysis revealed in details the transient properties of the space electrons induced by the man-made VLF wave emitted by the transmitter at NWC.The center location of the NWC electron flux locates in the north hemisphere other than in the south hemisphere during both quiet and disturbance period which is surprising.And the central location of NWC electron belt move westwards during the geomagnetic storm.The pitch angle distributions of the precipitation electron have the maximum flux at about 60-70 degree other than at 90 degree.The pitch angle distributions presented here are examined for evidence of the transportation mechanism especially for the electron loss mechanism.

 

How to cite: Chu, W., Xu, S., Zhang, Z., Huang, J., Zeren, Z., and Shen, X.: Study on the variation of energetic particle pitch angle caused by NWC VLF transmitter, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4488, https://doi.org/10.5194/egusphere-egu2020-4488, 2020.

ST2.2 – Dayside Magnetosphere Interactions

EGU2020-4367 | Displays | ST2.2

Foreshock Transients and Their Geoeffects

Hui Zhang

Foreshock transients are frequently observed upstream from the bow shock (such as Hot Flow Anomalies, foreshock cavities, and foreshock bubbles). They play a significant role in the mass, energy and momentum transport from the solar wind into the magnetosphere and impact the whole magnetosphere-ionosphere system. This presentation will discuss the great progress made recently toward answering some specific outstanding science questions. Some outstanding questions are listed below. What are the physical differences and relationships between different transient phenomena at the bow shock? What are the formation conditions for the transient phenomena at the bow shock? How do the magnetosphere and ionosphere respond to transient phenomena generated at bow shock? How do transient phenomena at the bow shock evolve with time?

How to cite: Zhang, H.: Foreshock Transients and Their Geoeffects, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4367, https://doi.org/10.5194/egusphere-egu2020-4367, 2020.

EGU2020-6535 | Displays | ST2.2

Ion Scale Flux Rope Observed at the Trailing Edge of the Hot Flow Anomaly

Shi-Chen Bai, Quanqi Shi, Terry Liu, Hui Zhang, Chao Yue, Wei-Jie Sun, Anmin Tian, Alexander Degeling, Jacob Bortnik, Jonathan Rae, and Mengmeng Wang

  Magnetic reconnection occurring during the development of a Hot flow anomaly (HFA) has been generated in hybrid simulation, but has never been observed by spacecraft. Using MMS we report an ion scale flux rope like structure, which is Earthward moving, embedded within the trailing edge of a hot flow anomaly (HFA) upstream from the quasi-parallel bow shock. The driver discontinuity of the HFA, a tangential discontinuity, is observed in the solar wind, but no flux rope signatures are observed around it. This suggests that the earthward moving flux rope was generated inside the HFA. This flux rope is close to a one-dimensional structure and expands due to a strong magnetic pressure gradient force. Solar wind ions are decelerated inside the flux rope by the static electric field likely caused by the charge separation of solar wind particles. Our observations imply that magnetic reconnection may have occurred inside the HFA. Reconnection and flux ropes may play a role in particle acceleration/heating inside foreshock transients.

How to cite: Bai, S.-C., Shi, Q., Liu, T., Zhang, H., Yue, C., Sun, W.-J., Tian, A., Degeling, A., Bortnik, J., Rae, J., and Wang, M.: Ion Scale Flux Rope Observed at the Trailing Edge of the Hot Flow Anomaly, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6535, https://doi.org/10.5194/egusphere-egu2020-6535, 2020.

EGU2020-9300 | Displays | ST2.2

Observations and simulations of foreshock waves during magnetic clouds

Lucile Turc, Owen Roberts, Martin Archer, Minna Palmroth, Markus Battarbee, Thiago Brito, Urs Ganse, Maxime Grandin, Yann Pfau-Kempf, Philippe Escoubet, and Iannis Dandouras

The foreshock is a region of intense wave activity, situated upstream of the quasi-parallel sector of the terrestrial bow shock. The most common type of waves in the Earth's ion foreshock are quasi-monochromatic fast magnetosonic waves with a period of about 30 s. In this study, we investigate how the foreshock wave field is modified when magnetic clouds, a subset of coronal mass ejections driving the most intense geomagnetic storms, interact with near-Earth space. Using observations from the Cluster constellation, we find that the average period of the fast magnetosonic waves is significantly shorter than the typical 30 s during magnetic clouds, due to the high magnetic field strength inside those structures, consistent with previous works. We also show that the quasi-monochromatic waves are replaced by a superposition of waves at different frequencies. Numerical simulations performed with the hybrid-Vlasov model Vlasiator consistently show that an enhanced upstream magnetic field results in less monochromatic wave activity in the foreshock. The global view of the foreshock wave field provided by the simulation further reveals that the waves are significantly smaller during magnetic clouds, both in the direction parallel and perpendicular to the wave vector. We estimate the transverse extent of the waves using a multi-spacecraft analysis technique and find a good agreement between the numerical simulations and the spacecraft measurements. This suggests that the foreshock wave field is structured over smaller scales during magnetic clouds. These modifications of the foreshock wave properties are likely to affect the regions downstream - the bow shock, the magnetosheath and possibly the magnetosphere - as foreshock waves are advected earthward by the solar wind.

How to cite: Turc, L., Roberts, O., Archer, M., Palmroth, M., Battarbee, M., Brito, T., Ganse, U., Grandin, M., Pfau-Kempf, Y., Escoubet, P., and Dandouras, I.: Observations and simulations of foreshock waves during magnetic clouds, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-9300, https://doi.org/10.5194/egusphere-egu2020-9300, 2020.

EGU2020-4394 | Displays | ST2.2

The observational evidence of electron mirror mode

Shutao Yao, Quanqi Shi, Zhonghua Yao, Ruilong Guo, Qiugang Zong, Xiaogang Wang, Degeling Alex, Jonathan Rae, Christopher Russell, Anmin Tian, Hui Zhang, Hongqiao Hu, Ji Liu, Han Liu, Bing Li, and Baebara Giles

The mirror modes are fundamental process in space, and play important roles in solar physics, planetary, interplanetary, astrophysical and laboratory plasmas over the past half century. Although theoretical studies and numerical simulations further revealed their kinetic effects, they are generally regarded as magnetohydrodynamics (MHD) scale process. However, if the electron distribution is anisotropic, the electrons could become unstable and excite kinetic scale mirror modes to remove the free energy. This instability was presented for more than thirty years, but so far few unambiguous observational evidence has been found. In this study, we provide high-resolution Magnetospheric Multiscale (MMS) observations of electron mirror mode structures. These structures: (1) are train-like features similar to the MHD-scale mirror-mode; (2) are anti-correlation between electron and magnetic pressure; (3) satisfy electron trapping conditions and theoretical excitation of the mirror modes; (4) are “frozen” in the plasma flow frame. They were observed during the Corotating Interaction Region events (CIRs) near the Earth’s foreshock and its downstream turbulence, and could involve with the interaction between Earth’s magnetosphere and solar wind.

How to cite: Yao, S., Shi, Q., Yao, Z., Guo, R., Zong, Q., Wang, X., Alex, D., Rae, J., Russell, C., Tian, A., Zhang, H., Hu, H., Liu, J., Liu, H., Li, B., and Giles, B.: The observational evidence of electron mirror mode, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4394, https://doi.org/10.5194/egusphere-egu2020-4394, 2020.

EGU2020-3687 | Displays | ST2.2

ULF waves in the foreshock formed by the radial IMF: their effect on solar wind sheath-like deflection

Olga Gutynska, Jaroslav Urbář, Jana Šafránková, and Zdeněk Němeček

Particle reflection at the bow shock provides a source of free energy to drive local instabilities and turbulence within the foreshock. A variety of low-frequency fluctuations (up to 16 mHz) results from the interactions of back-streaming ions with the incoming solar wind flow. We report observations of low-frequency magnetosonic waves observed during intervals of a radial interplanetary magnetic field in the foreshock. A case study of simultaneous dual THEMIS spacecraft observations of asymmetrical fluctuations in Vy is complemented by a statistical study of similar solar wind deflections in the foreshock.  Our moment calculations do not include the reflected particles as well as heavier ions, revealed the modulation of a solar wind core and deflection of the solar wind in the foreshock. This effect decreases with the distance from the bow shock. We conclude that large asymmetrical Vy velocity component fluctuations are typical for the foreshock formed by the radial IMF. The asymmetry of fluctuations changes the mean direction of the incoming solar wind flow within the foreshock leading to preconditioning prior to its encounter with the bow shock.

How to cite: Gutynska, O., Urbář, J., Šafránková, J., and Němeček, Z.: ULF waves in the foreshock formed by the radial IMF: their effect on solar wind sheath-like deflection, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3687, https://doi.org/10.5194/egusphere-egu2020-3687, 2020.

EGU2020-10305 | Displays | ST2.2

MMS observations of wave activity in the particle foreshock bubble foreshock region

Mengmeng Wang and Quanqi Shi

Foreshock bubbles (FBs) are kinetic transient phenomena formed due to the interaction between IMF discontinuities and backstreaming energetic ions in Earth’s foreshock region. FBs can be driven by both rotational discontinuities and tangential discontinuities and are typically observed under higher solar wind speed conditions. They play important roles in the solar wind-magnetosphere coupling because of very large dynamic pressure variations associated with them. The trailing edge of an FB is usually a fast shock which forms due to the expansion of the thermal plasma in the core. Using data from Magnetospheric Multiscale (MMS) mission, we investigate an FB structure with a particle foreshock region upstream its trailing edge. Distinct wave activity is observed in the particle foreshock region and wave analysis shows that the waves with periods of a few seconds may be generated by shock-reflected ion instabilities. The ions reflected at FB shock are observed and the acceleration mechanism needs to be analyzed.

How to cite: Wang, M. and Shi, Q.: MMS observations of wave activity in the particle foreshock bubble foreshock region, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-10305, https://doi.org/10.5194/egusphere-egu2020-10305, 2020.

The Earth’s magnetosphere occasionally experiences sudden movements from localized sources. For example, the impact of the interplanetary shock on the magnetosphere starts from a localized region on the dayside magnetopause, where the perturbations rapidly propagate inside the magnetosphere as the pressure front moves farther away from the Sun. The impulses generated from these sources propagate through the inhomogeneous plasma and can be detected in many corners of the magnetosphere. These impulses often mark the beginning of large-scale reconfigurations in the magnetosphere and the ionosphere, such as magnetic/ionospheric storms and substorms. The propagation of these impulses, such as that through MHD waves, is fast but not instantaneous. The propagation paths in the highly inhomogeneous magnetosphere may not be straightforward. Nonetheless, past studies have demonstrated that the impulse propagation in the dayside magnetosphere can be characterized by the Tamao model.

In this study, we examine the signatures of sudden impulses in the data from a network of spacecraft in the magnetosphere, including THEMIS, Van Allen Probes, MMS, Geotail, and GOES. The ACE and Wind data are also used for solar wind conditions. Observations from Polar, FAST, GOES, Cluster, Swarm, IMP-8, and ground-based magnetometers are also examined whenever they are available. The observations of impulse propagation time will be compared against the modeled Tamao travel time to understand how much the two agree with each other and how the comparison varies with the properties of the solar wind discontinuity.

How to cite: Flores, E. and Chi, P.: Multi-point Observations of Sudden Impulses and Implications for Signal Travel Time in the Magnetosphere, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-12703, https://doi.org/10.5194/egusphere-egu2020-12703, 2020.

EGU2020-2816 | Displays | ST2.2

TCV-like event induced by positive-negative pulse pair of solar wind dynamic pressure

Anmin Tian, Alexander Degeling, Quanqi Shi, and Zanyang Xing

Both simulations and observations had shown that step function-like increase/decrease of solar wind dynamic pressure pulse would excite flow vortex pairs in the dawn and dusk high latitude ionosphere simultaneously. However, some plasma structures, hot flow anomaly, sheath jets etc. existing in the solar wind or magnetosheath are often accompanied with spike-like changes of the dynamic pressure. Whether they can drive the ionospheric vortices or not is still unclear. In this work we report a traveling convection vortex like (TCV-like) event that was induced by a positive-negative pulse pair of dynamic pressure(△p/p~1) accompanying a large scale (~9min) magnetic hole in the solar wind. It is found that following the magnetic hole, two traveling convection vortices first in anticlockwise then in clockwise rotation were detected by geomagnetic stations located along the 10:30MLT meridian. Meanwhile, another pair of ionospheric vortices azimuthally seen up to 3 MLT first in clockwise then in anticlockwise rotation were appeared in the afternoon sector (~14MLT) centered at ~75MLAT with a trend of poleward moving. The duskside vortices were also confirmed by SuperDARN radar data. The processes following magnetosphere struck by a positive-negative pulse pair were simulated and it found that two pairs of flow vortices in the dawn and dusk magnetosphere may provide the field-aligned currents(FACs) required for the flow/current vortices observed in ionosphere. This work provides a way to understand how the momentum and energy injects to the ionosphere under spike-like dynamic pressures imposing on the magnetosphere.

How to cite: Tian, A., Degeling, A., Shi, Q., and Xing, Z.: TCV-like event induced by positive-negative pulse pair of solar wind dynamic pressure, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2816, https://doi.org/10.5194/egusphere-egu2020-2816, 2020.

EGU2020-13703 | Displays | ST2.2

ULF waves and their influence on radiation belt dynamics in Earth's magnetosphere

Robert Rankin and Alexander Degeling

Recent observations from the Van Allen Probes mission have established that Pc3-5 ultra-low-frequency (ULF) waves can energize ions and electrons via drift-resonance and drift-bounce resonance. The extent to which these waves contribute to the space weather of the belts is relatively poorly understood and requires sophisticated modelling and characterization of the dominant wave modes that arise in the development and recovery phase of geomagnetic storms. Despite more than four decades of observations and theoretical analysis of ULF waves, there is no framework for accurately assessing the global distribution of ULF waves and their influence on the ring current. 
In this presentation, we describe a new global model of ULF waves that incorporates non-dipolar geomagnetic fields. The model is constrained using the GCPM of cold plasma density model and a specification of the ionosphere using the IRI and MSIS models. An algorithm is applied to adjust the initial plasma state to a quasi-static equilibrium that is then driven by a global convection electric field and ULF wave source. For specific observations by the Van Allen Probes and ARASE mission, the effect of these ULF waves on radiation belt ions and electrons is evaluated utilizing test-particle methodology and Liouville's theorem, which enables the phase space density to be followed and compared one-for-one with the satellite observations.  

How to cite: Rankin, R. and Degeling, A.: ULF waves and their influence on radiation belt dynamics in Earth's magnetosphere, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-13703, https://doi.org/10.5194/egusphere-egu2020-13703, 2020.

EGU2020-5698 | Displays | ST2.2

Electron drift echoes induced by negative solar wind dynamic pressure pulses

Xiaohan Ma, Qiugang Zong, Yixin Hao, Seth Claudepierre, and Ying Liu

Sudden dropouts of the relativistic electron fluxes with drift echoes are closely related to a positive solar wind dynamic pressure pulse, such as an interplanetary shock impact on the magnetosphere. In this study, we further examine how magnetospheric energetic particles response to a negative solar wind dynamic pressure pulse on the 11th May 2017. During this event, sudden dropouts of energetic electron fluxes with an energy of 200 keV∼750 keV and enhancements of the relativistic electron fluxes of 0.85 MeV∼2.7 MeV were observed simultaneously by both Van Allen Probes. The periodic electron flux dropout-recovery or enhancement-decay signatures, which are attributed to electron drift behaviors, exhibited energy dependence. Based on the electron phase space density profile and the induced electric field variation, we interpreted this phenomenon as the consequence of radially outward transportationss of electrons caused by the electric field impulse induced by the negative dynamic pressure pulse.

How to cite: Ma, X., Zong, Q., Hao, Y., Claudepierre, S., and Liu, Y.: Electron drift echoes induced by negative solar wind dynamic pressure pulses, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5698, https://doi.org/10.5194/egusphere-egu2020-5698, 2020.

EGU2020-18504 | Displays | ST2.2

Determining the global coherence of plasmaspheric hiss waves in the magnetosphere

Shuai Zhang, Jonathan Rae, Clare Watt, Alexander Degeling, Anmin Tian, and Quanqi Shi

Plasmaspheric hiss waves is important in the radiation belt. Previous papers have shown that considering the variability of wave parameters will improve the effectiveness of modeling wave-particle interactions in the Radiation Belt, but less is known about how rapidly (and by how much) wave characteristics vary. We use measurements from the Van Allen Probe mission to study the correlation and ratio of wave amplitudes over a range of frequencies covering the plasmaspheric hiss band as a function of separation and time delay between two satellites. A total of 1851 events with small separation (<1RE) were found. The statistical results show that, as separation between spacecraft increase, the characteristics of hiss change in both correlation of the wavepacket and amplitude. Moreover, we find that the coherence between spacecraft is strong at low-L, and decreases strongly with increasing L. We investigate the coherence of plasmaspheric hiss on geomagnetic indices and solar wind driving. We discuss the ramifications of our results with relevance to understanding the global characteristics of plasmaspheric hiss waves.

How to cite: Zhang, S., Rae, J., Watt, C., Degeling, A., Tian, A., and Shi, Q.: Determining the global coherence of plasmaspheric hiss waves in the magnetosphere, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18504, https://doi.org/10.5194/egusphere-egu2020-18504, 2020.

EGU2020-4520 | Displays | ST2.2

Newly Formed Energy Dispersion Signatures of Low-energy Proton, Oxygen and Helium Ions in the Inner Magnetosphere

Jie Ren, Qiugang Zong, Chao Yue, and Xuzhi Zhou

EGU2020-6406 | Displays | ST2.2

Recent observations of magnetic cavities: from MHD to kinetic scale

Quanqi Shi and Et al

Magnetic cavities, also termed magnetic holes, dips or depression structures, have an observable magnetic field decrease in a short time span and have been widely observed in the solar wind plasmas, comet magnetospheres, terrestrial/planetary magnetosheaths, magnetospheric cusps and magnetotail plasmas since 1970s. In early observations, the structures were found in MHD scale, from tens to thousands of ρi (proton gyroradius) with corresponding temporal scales from seconds to tens of minutes. Later, kinetic scale magnetic cavities were detected in the earth’s magnetotail and magnetosheath, with size less than ρi and sometimes close to several ρe (electron gyroradius) and often associated with a significant electron vortex around the structure. Surprisingly, it has been found that such a small structure contains an abundance of phenomena, including different kinds of ion and electron distributions, electron or ion vortices, various types of waves, and even particle acceleration and declarations. In this presentation, we will show our recent observations of magnetic cavities from MHD scale to kinetic scale in the solar wind, magnetosheath, cusp and magnetotail. In the magnetosheath, downstream of the bow shock, the mirror mode instability can generate magnetic dip and peak trains. Using data from the new NASA satellite constellation MMS, we have found that electrons exhibit a new ‘donut’ shaped distribution function related to particle deceleration processes. Using boundary normal and velocity determination techniques, we found that MHD scale magnetic cavity structures can expand or shrink, and they can enter the cusp regions along with the entry plasmas. In the turbulent magnetosheath and quiet magnetotail, we have observed kinetic scale magnetic cavity structures with scales comparable or less than one ρi. An EMHD model and other theories will also be introduced and compared. We found that in the sheath the electron scale magnetic cavity has a circular cross section and it is a magnetic bottle in 3-D. We have also found that these structures shrink due to increases in the surrounding magnetic field, and this shrinkage of the small scale magnetic cavity can induce an electric field that accelerates the electrons to a significantly higher energy. Qualitatively distinct from other acceleration mechanisms, this process indicates a new type of non-adiabetic acceleration, and has been confirmed by the observed electron distribution function and test particle simulations. This discovery in space physics also has implications for understanding energy conversion in astrophysical plasmas, the origin of cosmic high-energy particles and plasma turbulence.

How to cite: Shi, Q. and al, E.: Recent observations of magnetic cavities: from MHD to kinetic scale, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6406, https://doi.org/10.5194/egusphere-egu2020-6406, 2020.

EGU2020-5026 | Displays | ST2.2

On the scale sizes of magnetosheath jets

Ferdinand Plaschke and Heli Hietala

The subsolar magnetosheath is oftentimes permeated by jets. These are localized entities of enhanced dynamic pressure with respect to the ambient plasma. Magnetosheath jets are thought to arise from bow shock ripples and/or foreshock structures. They can easily propagate through the entire magnetosheath and impact on the magnetopause, where they can cause large amplitude indentations, launch magnetopause surface waves, or modulate magnetopause reconnection. The scale size distributions of magnetosheath jets observed by single spacecraft are relatively well modeled by exponential functions with characteristic scales of 0.71 Earth radii (RE) and 1.34 RE in the directions parallel and perpendicular to the jet propagation direction, respectively. However, these functions do not represent the actual, true jet scale size distributions, because of two reasons: (1) Spacecraft are much more likely to observe large scale jets rather than small scale jets. Hence, the observed scale size distributions are biased towards larger scales. (2) The distributions modeled by exponential functions highly overestimate observation probabilities of jets of smallest scales (on the order of 0.1 RE). We overcome both shortcomings by replacing the exponential functions by log-normal functions, which can be corrected for the bias. By re-analyzing THEMIS multi-spacecraft data, we obtain, for the first time, unbiased, i.e., actual jet scale size distributions. Our results reveal a large population of jets of smallest scales that have not been accounted for, so far. Consequently, we find median scale sizes of jets to be about an order of magnitude smaller than previously thought: 0.15 and 0.12 RE in the parallel and perpendicular directions, respectively.

How to cite: Plaschke, F. and Hietala, H.: On the scale sizes of magnetosheath jets, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5026, https://doi.org/10.5194/egusphere-egu2020-5026, 2020.

EGU2020-5101 | Displays | ST2.2

Magnetosheath high speed jets observed simultaneously by Cluster and MMS

C.-Philippe Escoubet and the Cluster-MMS team

The supersonic solar wind is decelerated and thermalized when it encounters the Earth's magnetosphere and cross the bow shock. Sometimes, however, due to discontinuities in the solar wind, bow shock ripples or ionised dust clouds carried by the solar wind, high speed jets (HSJs) are observed in the magnetosheath. These HSJs have typically a Vx component larger than 200 km s-1 and their dynamic pressure can be a few times the solar wind dynamic pressure. They are typically observed downstream from the quasi-parallel bow shock and have a typical size around one Earth radius (RE) in XGSE. We use a conjunction of Cluster and MMS, crossing simultaneously the magnetopause, to study the characteristics of these HSJs and their impact on the magnetopause. Over one hour-fifteen minutes interval in the magnetosheath, Cluster observed 21 HSJs. During the same period, MMS observed 12 HSJs and entered the magnetosphere several times. A jet was observed simultaneously by both MMS and Cluster and it is very likely that they were two distinct HSJs. This shows that HSJs are not localised into small regions but could span a region larger than 10 RE, especially when the quasi-parallel shock is covering the entire dayside magnetosphere under radial IMF. During this period, two and six magnetopause crossings were observed respectively on Cluster and MMS with a significant angle between the observation and the expected normal deduced from models. The angles observed range between from 11° up to 114°. One inbound magnetopause crossing observed by Cluster (magnetopause moving out at 142 km s-1) was observed simultaneous to an outbound magnetopause crossing observed by MMS (magnetopause moving in at -83 km s-1), showing that the magnetopause can have multiple local indentation places, most likely independent from each other. Under the continuous impacts of HSJs, the magnetopause is deformed significantly and can even move in opposite directions at different places. It can therefore not be considered as a smooth surface anymore but more as surface full of local indents. Four dust impacts were observed on MMS, although not at the time when HSJs are observed, showing that dust clouds would have been present during the observations. No dust cloud in the form of Interplanetary Field Enhancements was however observed in the solar wind which may exclude large clouds of dust as a cause of HSJs. Radial IMF and Alfvén Mach number above 10 would fulfill the criteria for the creation of bow shock ripples and the subsequent crossing of HSJs in the magnetosheath.

How to cite: Escoubet, C.-P. and the Cluster-MMS team: Magnetosheath high speed jets observed simultaneously by Cluster and MMS, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5101, https://doi.org/10.5194/egusphere-egu2020-5101, 2020.

EGU2020-2508 | Displays | ST2.2 | Highlight

Particle acceleration by transient structures around Earth’s bow shock

Terry Zixu Liu, Vassilis Angelopoulos, Heli Hietala, San Lu, and Drew Turner

Upstream of Earth’s bow shock, the foreshock is filled with particles that have been reflected at the bow shock and are streaming away from it. Interaction of these particles with solar wind particles and discontinuities within this region can cause foreshock transients to form. Downstream of Earth’s bow shock, localized magnetosheath jets with high dynamic pressure are frequently observed. When such a fast magnetosheath jet compresses the ambient magnetosheath plasma, an earthward compressional bow wave/shock can form. Here we present that foreshock transients and magnetosheath jets can accelerate particles through shock drift acceleration, Fermi acceleration, and the betatron acceleration. Foreshock transients and magnetosheath jets therefore can increase the particle acceleration efficiency of the parent shock by providing additional acceleration. The shock environment relevant for particle acceleration is not just the shock itself, but also the nonlinear transient structures both upstream and downstream of it.

How to cite: Liu, T. Z., Angelopoulos, V., Hietala, H., Lu, S., and Turner, D.: Particle acceleration by transient structures around Earth’s bow shock, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2508, https://doi.org/10.5194/egusphere-egu2020-2508, 2020.

EGU2020-11030 | Displays | ST2.2

Magnetic field within magnetosheath jets during northward and southward interplanetary magnetic field conditions

Laura Vuorinen, Heli Hietala, and Ferdinand Plaschke

Downstream of the Earth's quasi-parallel shock, transients with higher earthward velocities than the surrounding magnetosheath plasma are often observed. These transients have been named magnetosheath jets. Due to their high dynamic pressure, jets can cause multiple types of effects when colliding into the magnetopause. Recently, jets have been linked to triggering magnetopause reconnection in case studies by Hietala et al. (2018) and Nykyri et al. (2019). Jets have been proposed to affect magnetopause reconnection in multiple ways. Jets can compress the magnetopause and make it thin enough for reconnection to occur. Jets could also affect the magnetic shear either by indenting the magnetopause or via the magnetic field of the jets themselves. Here we want to study whether the magnetic field of jets can statistically affect magnetopause reconnection. In particular, we are interested in whether jets could enhance reconnection during more quiet northward IMF conditions.

We statistically study the magnetic field within jets in the subsolar magnetosheath using measurements from the five Time History of Events and Macroscale Interactions during Substorms (THEMIS) spacecraft and OMNI solar wind data from 2008–2011. We investigate jets next to the magnetopause and find that the magnetic field within jets is statistically different compared to the non-jet magnetosheath. Our results suggest that during southward IMF, the non-jet magnetosheath magnetic field itself has more variation than the jets. This suggests that jets should have no statistical, neither enhancing nor suppressing, effect on reconnection during southward IMF. However, during northward IMF, the magnetic field within jets is statistically favorable for enhancing magnetic reconnection at the subsolar magnetopause as around 70 % of these jets exhibit southward fields close to the magnetopause.

How to cite: Vuorinen, L., Hietala, H., and Plaschke, F.: Magnetic field within magnetosheath jets during northward and southward interplanetary magnetic field conditions, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11030, https://doi.org/10.5194/egusphere-egu2020-11030, 2020.

EGU2020-3335 | Displays | ST2.2

Modification of the magnetosheath due to the high-speed jets propagation.

Oleksandr Goncharov, Herbert Gunell, Maria Hamrin, Linus Norenius, and Olga Gutynska

Plasmoids, defined as plasma entities with a higher anti-sunward velocity component than the surrounding plasma, have been observed in the magnetosheath in recent years. Among other denominations, plasmoids are also called “magnetosheath jets” and can be classified by transient localized enhancements in dynamic pressure. Propagating through the magnetosheath, jets do not only affect the magnetopause and magnetosphere. Jets pushed slower ambient magnetosheath plasma out of their way. As a result, plasma moves around the jets, and it is slowed down or could even be pushed in the sunward direction. Consequently, jets may create anomalous flows and be a source of additional turbulence. Using the magnetosheath measurements by the Magnetospheric Multiscale (MMS) and THEMIS spacecraft, and comparing several criteria, we have identified several thousand events in the wide range of bow shock distances. Previous statistical studies have shown that jet occurrence is almost exclusively controlled by the angle between the IMF and the Earth–Sun line (cone angle), and jets are predominantly observed when this cone angle is small. However, high-speed jets downstream of the quasi-perpendicular bow shock are very common. Our statistical analysis shows differences of jets evolution in the quasi-parallel and quasi-perpendicular magnetosheath regions. We discuss their properties, nature and relation to anomalies regions in the magnetosheath.

How to cite: Goncharov, O., Gunell, H., Hamrin, M., Norenius, L., and Gutynska, O.: Modification of the magnetosheath due to the high-speed jets propagation., EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3335, https://doi.org/10.5194/egusphere-egu2020-3335, 2020.

EGU2020-2443 | Displays | ST2.2

Variations of Pressure Profiles from the Bow Shock to Magnetopause

Gilbert Pi, Zdeněk Němeček, and Jana Šafránková

Numerous simulation results have shown that the spatial profiles of a thermal pressure from the bow shock to the magnetopause are determined by the upstream interplanetary magnetic field (IMF) orientation. The southward IMF conditions lead to an increasing trend of thermal pressure with a maximum near the magnetopause. In contrast, the thermal pressure increases on the plasma entry to the  magnetosheath, but this trend turns to a decreasing one after passing a middle point between the bow shock and magnetopause during northward IMF intervals. In the present study, we show the observation results, both particular events and statistics, to check the variations of pressure profiles in the magnetosheath and their relation to upstream IMF conditions. THEMIS-C observartions during 2007–2009 are used. The profiles near the Sun–Earth line and the global pressure distribution in the dayside equatorial magnetosheath are shown.

How to cite: Pi, G., Němeček, Z., and Šafránková, J.: Variations of Pressure Profiles from the Bow Shock to Magnetopause, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2443, https://doi.org/10.5194/egusphere-egu2020-2443, 2020.

EGU2020-2719 | Displays | ST2.2

Electron acceleration in small-size magnetic holes

Ji Liu, Shutao Yao, Quanqi Shi, Xiaogang Wang, Qiugang Zong, Yongyong Feng, Han Liu, Ruilong Guo, Zhonghua Yao, Jonathan Iain Rae, Alexander William Degeling, Anmin Tian, and Lloyd Woodham

The magnetic-to-particle energy conversion is one of the most fundamental physics processes to laboratory, space and astrophysical contexts. Adiabatic acceleration processes in moderate varying environment merely play significant roles to generate devastating cosmic rays and spectacular aurorae, etc. More commonly, when the violent variation or strongly inhomogeneity in electromagnetic field distorts the trajectory of the particles, non-adiabatic acceleration processes function more transiently and drastically on particle energization trigger explosive phenomena like sudden solar flares. However, without high-resolution simultaneous measurements on plasma and field at previous space missions, the small/fast scale of the non-adiabatic processes make it difficult to be analyzed to reach a comprehensive understanding to most of the underlying non-adiabatic acceleration mechanisms in space and astrophysical contexts. Here, using MMS data with unprecedented high temporal resolutions, we report such finding of acceleration for electrons trapped in a kinetic-size magnetic holes which at the same time is the acceleration region, and demonstrate the validity of the acceleration process by numerical simulation, achieving the reproduction for the observation.

How to cite: Liu, J., Yao, S., Shi, Q., Wang, X., Zong, Q., Feng, Y., Liu, H., Guo, R., Yao, Z., Rae, J. I., Degeling, A. W., Tian, A., and Woodham, L.: Electron acceleration in small-size magnetic holes, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2719, https://doi.org/10.5194/egusphere-egu2020-2719, 2020.

EGU2020-3683 | Displays | ST2.2

Subsolar magnetopause under an inverse gradient of the magnetic field: Statistical study

Kostiantyn Grygorov, Zdeněk Němeček, Jana Šafránková, and Jiří Šimůnek

The magnetopause is usually at the point where the pressure of the magnetospheric magnetic field is balanced by a sum of the thermal plasma and magnetic pressures on the magnetosheath side. However, statistics from THEMIS magnetopause crossings have showed that about 2 % of them exhibit a larger magnetic field in the magnetosheath than in the magnetosphere in the subsolar region (YGSM < 5 RE) and thus, the pressure from the magnetosheath side seems to be uncompensated. In our study, we compare parameters of those unusual crossings with the rest of our statistic in that region with motivation to highlight the possible sources and mechanisms of this apparent pressure imbalance, which can be caused either by specific upstream solar wind conditions or by the state of the magnetosphere. We also compare our THEMIS results with the sets of magnetopause crossings observed by other spacecraft (e.g., Cluster, MMS).

How to cite: Grygorov, K., Němeček, Z., Šafránková, J., and Šimůnek, J.: Subsolar magnetopause under an inverse gradient of the magnetic field: Statistical study, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3683, https://doi.org/10.5194/egusphere-egu2020-3683, 2020.

EGU2020-21977 | Displays | ST2.2

Do Statistical models capture magnetopause dynamics during sudden magnetospheric compressions?

Frances Staples, Jonathan Rae, Colin Forsyth, Ashley Smith, Kyle Murphy, Katie Raymer, Ferdinand Plaschke, Nathan Case, Craig Rodger, James Wild, Steve Milan, and Suzanne Imber

Under steady-state conditions the magnetopause location is described as a pressure balance between internal magnetic pressures and the external dynamic pressure of the solar wind. The question is, does this approximation hold during more dynamic solar wind features?

Under more extreme solar wind driving, such as high solar wind pressures or strong southward-directed interplanetary magnetic fields, this boundary is significantly more compressed than in steady-state, playing a significant role in the depletion of magnetospheric plasma from the Van Allen Radiation Belts, via magnetopause shadowing. Large step-changes in solar wind conditions enable the real magnetopause to have a significant time-dependence which empirical models cannot capture.

We use a database of ~20,000 magnetopause crossings, to determine how the measured magnetopause differs from a statistical model, and under which conditions. We find that observed magnetopause is on average 6% closer to the radiation belts,  with a maximum of 42%, during periods of sudden dynamic pressure enhancement, such as during storm sudden commencement. Our results demonstrate that empirical magnetopause models such as the Shue et al. [1998] model should be used cautiously to interpret energetic electron losses by magnetopause shadowing. 

How to cite: Staples, F., Rae, J., Forsyth, C., Smith, A., Murphy, K., Raymer, K., Plaschke, F., Case, N., Rodger, C., Wild, J., Milan, S., and Imber, S.: Do Statistical models capture magnetopause dynamics during sudden magnetospheric compressions? , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21977, https://doi.org/10.5194/egusphere-egu2020-21977, 2020.

EGU2020-1890 | Displays | ST2.2

Unusual location of the geotail magnetopause at lunar distance: ARTEMIS observation

Wensai Shang, Binbin Tang, Quanqi Shi, Anmin Tian, Xiaoyan Zhou, Zhonghua Yao, Alex W. Degeling, Iain Jonathan Rae, Suiyan Fu, Jianyong Lu, Zuyin Pu, Andrew N. Fazakerley, Malcolm M. Dunlop, Gabor Facsko, Jiang Liu, and Ming Wang

The Earth’s magnetopause is highly variable in location and shape, and is modulated by solar wind conditions. On 8 March 2012, the ARTEMIS probes were located near the tail current sheet when an interplanetary shock arrived under northward interplanetary magnetic field (IMF) conditions, and recorded an abrupt tail compression at ~(-60, 0, -5) RE in Geocentric Solar Ecliptic (GSE) coordinate in the deep magnetotail. Approximately 10 minutes later, the probes crossed the magnetopause many times within an hour after the oblique interplanetary shock passed by. The solar wind velocity vector downstream from the shock was not directed along the Sun-Earth line, but had a significant Y component. We propose that the compressed tail was pushed aside by the appreciable solar wind flow in the Y direction. Using a virtual spacecraft in a global magnetohydrodynamic (MHD) simulation, we reproduce the sequence of magnetopause crossings in the X-Y plane observed by ARTEMIS probes under oblique shock conditions, demonstrating that the compressed magnetopause is sharply deflected at lunar distances in response to the shock and solar wind VY effects. The results of the two different global MHD simulations show that the shocked magnetotail at lunar distances is mainly controlled by the solar wind direction with a timescale of about a quarter hour, which appears to be consistent with the windsock effect. The results also provide some references for investigating interactions between the solar wind/magnetosheath and lunar nearside surface during full moon time intervals, which should not happen in general.

How to cite: Shang, W., Tang, B., Shi, Q., Tian, A., Zhou, X., Yao, Z., Degeling, A. W., Rae, I. J., Fu, S., Lu, J., Pu, Z., Fazakerley, A. N., Dunlop, M. M., Facsko, G., Liu, J., and Wang, M.: Unusual location of the geotail magnetopause at lunar distance: ARTEMIS observation, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1890, https://doi.org/10.5194/egusphere-egu2020-1890, 2020.

EGU2020-4478 | Displays | ST2.2

Transpolar arcs under a long-duration radial IMF interval: A case study

Jong-Sun Park, Quan Qi Shi, Motoharu Nowada, Jih-Hong Shue, Khan-Hyuk Kim, Dong-Hun Lee, Qiu-Gang Zong, Alexander W. Degeling, An Min Tian, Timo Pitkänen, Yongliang Zhang, I. Jonathan Rae, Shichen Bai, and Shutao Yao

Although the responses of the transpolar arcs (TPAs) to the north-south or dawn-dusk interplanetary magnetic field (IMF) orientations are relatively well known, the effects of the Sun-Earth IMF component on the TPA formation are still poorly understood. On 29 October 2005, the IMF pointed nearly earthward over seven hours from 08:20 to 15:40 UT. In this time interval, the Defense Meteorological Satellite Program (DMSP) satellite and the Thermosphere Ionosphere Mesosphere Energetics and Dynamics (TIMED) satellite observed two clear TPA structures (one near the magnetic pole and the other near the dawnside auroral oval) in the northern hemisphere and one clear TPA structure in the dawnside southern hemisphere. Precipitating particle data reveal that the TPA in the southern hemisphere and that near the dawnside auroral oval in the northern hemisphere are associated with precipitating electrons and ions, but the TPA near the magnetic pole in the northern hemisphere is associated with electron-only precipitation. These observational results imply that the formation of TPAs is not limited to northward IMF conditions and that the TPAs could be located not only on open field lines connected to the northward draped IMFs over one hemisphere magnetopause, but also on closed field lines rooted on both hemispheres even under the radial IMF conditions.

How to cite: Park, J.-S., Shi, Q. Q., Nowada, M., Shue, J.-H., Kim, K.-H., Lee, D.-H., Zong, Q.-G., Degeling, A. W., Tian, A. M., Pitkänen, T., Zhang, Y., Rae, I. J., Bai, S., and Yao, S.: Transpolar arcs under a long-duration radial IMF interval: A case study, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4478, https://doi.org/10.5194/egusphere-egu2020-4478, 2020.

EGU2020-12369 | Displays | ST2.2

DMSP/SSUSI observations of the high-latitude dayside aurora (HiLDA

Lei Cai, Anita Kullen, Yongliang Zhang, Tomas Karlsson, and Andris Vaivads

High-latitude dayside aurora (HiLDA) are large-scale discrete arcs or spot-like aurora poleward of the cusp, observed previously in the northern hemisphere by the Viking UV imager [Murphree et al., 1990] and by the IMAGE FUV [Frey et al., 2003]. The particular interest on HiLDA is to understand its formation related to the dayside reconnection and the resulted field-aligned currents (FACs) configuration in the polar cap (open field line region). In addition, the occurrence of HiLDA in the southern hemisphere is not well known.

In this study, we investigate the properties of HiLDA using DMSP/SSUSI images from the satellites F16, F17, F18, and F19. The combined data with auroral images from DMSP/SSUSI, ion drift velocity from SSIES, magnetic field perturbations from SSM, and energetic particle spectrum from SSJ make it possible to study the electrodynamics in the vicinity of the HiLDA and its connection the dayside cusp. HiLDA is formed due to monoenergetic electron precipitation (inverted-V structures) with the absence of ion precipitation. The field-aligned potential drop can be up to tens of keV. Applying the current-voltage relation, we suggest accelerated polar rain as the source of HiLDA, indirectly controlled by the solar wind/magnetosheath plasma population. The upward field-aligned current associated with the potential drop is a part of the cusp current system, produced by the dayside reconnection. Both lobe reconnection and reconnection on the duskside flanks play a role in the formation of HiLDA.

The occurrence of HiLDA is highly associated with the sunlit hemisphere and IMF By dominated conditions. Our results agree with previous observations, which show that HiLDA occurs during positive By dominated conditions in the northern summer hemisphere. We also confirmed that HiLDA occurs during negative By dominated conditions in the southern hemisphere. In addition, the fine structures of HiLDA are studied.

References

Murphree, J. S., Elphinstone, R. D., Hearn, D., and Cogger, L. L. ( 1990), Large‐scale high‐latitude dayside auroral emissions, J. Geophys. Res., 95( A3), 23452354, doi:.

Frey, H. U., Immel, T. J., Lu, G., Bonnell, J., Fuselier, S. A., Mende, S. B., Hubert, B., Østgaard, N., and Le, G. ( 2003), Properties of localized, high latitude, dayside aurora, J. Geophys. Res., 108, 8008, doi:, A4.

How to cite: Cai, L., Kullen, A., Zhang, Y., Karlsson, T., and Vaivads, A.: DMSP/SSUSI observations of the high-latitude dayside aurora (HiLDA, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-12369, https://doi.org/10.5194/egusphere-egu2020-12369, 2020.

ST2.3 – Magnetic reconnection and associated multi-scale coupling in space, astrophysics and laboratorial plasmas

EGU2020-3757 | Displays | ST2.3 | Highlight

Energy Conversion in the Electron Stagnation Region of Magnetopause Reconnection

James Burch, James Webster, Kristina Pritchard, Kevin Genestreti, Michael Hesse, Paul Cassak, Roy Torbert, Barbara Giles, Robert Ergun, Christopher Russell, Robert Strangeway, Kyoung-Joo Hwang, Kyunghwan Dokgo, and Stephen Fuselier

For reconnection at the Earth’s day side, which is asymmetric, the main energy conversion occurs on closed field lines in the electron stagnation region. Energy conversion, as measured by JE, occurs where out-of-plane electric field components are embedded within larger regions of out-of-plane current, which is carried by strong electron flows in the M direction of the LMN coordinate system. Bracketing these energy conversion sites are electron jet reversals (along L and -L) and converging  electron flows (along N and -N). These electron flows are like those that surround reconnection X lines, however, in these cases they occur completely within closed field lines. The question then is what, if anything, this energy conversion has to do with local reconnection of magnetic field lines. This paper reports on a study of two events observed by MMS on December 29, 2016 and April 15, 2018. The electron inflows have velocities between 0.05 VeA and 0.1 VeA, (VeA = electron Alfvén speed), which are consistent with predicted reconnection rates. Laboratory measurements and 3D simulation results offer some clues about how reconnecting current sheets can evolve in a uniform background magnetic field.

How to cite: Burch, J., Webster, J., Pritchard, K., Genestreti, K., Hesse, M., Cassak, P., Torbert, R., Giles, B., Ergun, R., Russell, C., Strangeway, R., Hwang, K.-J., Dokgo, K., and Fuselier, S.: Energy Conversion in the Electron Stagnation Region of Magnetopause Reconnection, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3757, https://doi.org/10.5194/egusphere-egu2020-3757, 2020.

EGU2020-3699 | Displays | ST2.3 | Highlight

Local kinetic processes determining macroscopic properties of interlinked magnetic flux tubes

Kyoung-joo Hwang, Jim Burch, Christopher Russell, Eunjin Choi, Kyunghwan Dokgo, Robert Fear, Stephen Fuselier, Steve Petrinec, David Sibeck, Hiroshi Hasegawa, Huishan Fu, Marit Øieroset, Philippe Escoubet, Barbara Giles, Robert Strangeway, Yuri Khotyaintsev, Daniel Graham, Daniel Gershman, Craig Pollock, and Robert Ergun and the MMS science working group

One of the most important transient phenomena affecting the solar wind-Earth’s magnetosphere coupling is non-steady dayside magnetic reconnection, observationally evidenced by a transient structure consisting of a bipolar magnetic-field component normal to the magnetopause. This signature, termed a flux-transfer-event (FTE), has been recently found to often consist of two interlinked flux tubes. The recent observations, particularly from the MMS spacecraft, showed a reconnecting current sheet between the interlaced flux tubes. However, local kinetic processes between the flux tubes have not been understood in the context of the broader FTE structure and evolution. An FTE observed by MMS on 18 December, 2017 comprised two flux tubes of different topology. One includes field lines with their ends connected to the northern and southern hemispheres while the other includes field lines that are connected to the magnetosheath (and ultimately the Sun). Evidence for reconnection occurring at the interface of the two flux tubes indicates how interacting flux tubes evolve into a flux rope having helical magnetic topology connecting either both to the Earth or being completely open. This study proposes a new aspect of how micro-to-meso-scale dynamics occurring within FTEs determines the macroscale characteristics and evolution of the structures.

How to cite: Hwang, K., Burch, J., Russell, C., Choi, E., Dokgo, K., Fear, R., Fuselier, S., Petrinec, S., Sibeck, D., Hasegawa, H., Fu, H., Øieroset, M., Escoubet, P., Giles, B., Strangeway, R., Khotyaintsev, Y., Graham, D., Gershman, D., Pollock, C., and Ergun, R. and the MMS science working group: Local kinetic processes determining macroscopic properties of interlinked magnetic flux tubes, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3699, https://doi.org/10.5194/egusphere-egu2020-3699, 2020.

EGU2020-2239 | Displays | ST2.3 | Highlight

Flux Transfer Events are Made in Pairs

Christopher Russell and Robert Strangeway

Flux transfer events are transient magnetized plasma structures that are self-balancing, rope-like phenomena that appear when the interplanetary magnetic field is southward. Using measurements of particles and magnetic fields on the MMS spacecraft, we find that these structures contain magnetospheric energetic electrons in exactly half of their observations, independent of external conditions or locations. This implies that two flux ropes are created for each event, one connected to the magnetosphere and one not connected. We show that this dual nature occurs independent of solar wind properties and location of observation. These observations are consistent with a recent model of flux transfer event generation.

How to cite: Russell, C. and Strangeway, R.: Flux Transfer Events are Made in Pairs, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2239, https://doi.org/10.5194/egusphere-egu2020-2239, 2020.

EGU2020-4027 | Displays | ST2.3

Magnetic reconnection induced by the Kelvin-Helmholtz vortex at the Earth’s magnetopause during southward IMF

Takuma Nakamura, Ferdinand Plaschke, Hiroshi Hasegawa, Yi-Hsin Liu, Kyoung-Joo Hwang, Kevin Alexander Blasl, and Rumi Nakamura

When the magnetic field is oriented nearly perpendicular to the direction of the plasma shear flow, the flow easily satisfies the super-Alfvénic unstable condition for the Kelvin-Helmholtz (KH) instability. This configuration is realized at the Earth’s low-latitude magnetopause when the interplanetary magnetic field (IMF) is strongly northward or southward. Indeed, clear signatures of the KH waves have been frequently observed during periods of the northward IMF. However, these signatures have been much less frequently observed during the southward IMF. In this work, we performed the first 3-D fully kinetic simulation of the KH instability at the magnetopause under the southward IMF condition. The simulation demonstrates that magnetic reconnection, with a typical fast rate on the order of 0.1, is induced at multiple locations along the vortex edge in an early non-linear growth phase of the KH instability. The reconnection outflow jet, which grows in the direction nearly perpendicular to the initial shear flow, significantly disrupt the flow of the non-linear KH vortex. On the other hand, the shear and vortex flow strongly bends and twists the reconnected field lines towards the direction out of the reconnection plane. The resulting coupling of the complex field and flow patterns within the magnetopause boundary layer leads to a quick decay of the vortex structure. These simulation results suggest that clear signatures of the KH waves are expected to be observed only for a limited phase during periods of the southward IMF, which may explain the difference in the observation probability of KH waves between northward and southward IMFs.

How to cite: Nakamura, T., Plaschke, F., Hasegawa, H., Liu, Y.-H., Hwang, K.-J., Blasl, K. A., and Nakamura, R.: Magnetic reconnection induced by the Kelvin-Helmholtz vortex at the Earth’s magnetopause during southward IMF, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4027, https://doi.org/10.5194/egusphere-egu2020-4027, 2020.

EGU2020-11373 | Displays | ST2.3

Magnetic mirror structures associated with magnetopause flux ropes investigated with Mangnetospheric Multiscale misson (MMS)

Sadie Robertson, Jonathan Eastwood, Julia Stawarz, Heli Hietala, Tai Phan, Benoit Lavraud, James Burch, Barbra Giles, Daniel Gershman, Roy Torbert, Per Arne Lindqvist, Robert Ergun, Christopher Russell, and Robert Strangeway

Magnetic reconnection is a fundamental plasma physics process which governs energy and mass transfer from the solar wind into the Earth’s magnetosphere. Electron acceleration during reconnection has been widely investigated with multiple mechanisms proposed. Many of these mechanisms involve flux ropes: twisted magnetic field structures formed during reconnection. Drake et al. 2006 suggest that contracting magnetic islands (or flux ropes in 3D) could trap and energise electrons by a Fermi acceleration process.

Whilst previous missions have observed and characterised flux ropes, the temporal resolution of the data was typically not great enough to study structures in detail, particularly on electron scales. Here we investigate magnetopause flux ropes using data from NASA’s four spacecraft Magnetospheric Multiscale mission (MMS). MMS measures the thermal electron and ion 3D distribution at 30 msec and 150 msec time resolution, respectively, and at spacecraft separations down to a few kilometers.

We focus on electron pitch angle distributions and examine how they can be used to investigate magnetopause flux ropes. In particular, the distributions are used to identify electron trapping in magnetic mirror structures on the magnetospheric edge of the flux ropes. These features are found to have extended 3D structure along the body of the flux rope. We evaluate possible formation mechanisms, such as the mirror instability, and potential electron acceleration mechanisms, such as betatron and Fermi acceleration. Magnetic mirror structures could represent an important particle acceleration feature for flux ropes and magnetic reconnection.

How to cite: Robertson, S., Eastwood, J., Stawarz, J., Hietala, H., Phan, T., Lavraud, B., Burch, J., Giles, B., Gershman, D., Torbert, R., Lindqvist, P. A., Ergun, R., Russell, C., and Strangeway, R.: Magnetic mirror structures associated with magnetopause flux ropes investigated with Mangnetospheric Multiscale misson (MMS), EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11373, https://doi.org/10.5194/egusphere-egu2020-11373, 2020.

EGU2020-3156 | Displays | ST2.3

The location of Component Reconnection at the Earth’s Magnetopause During Dominant IMF By and Large Dipole Tilt Conditions

Karlheinz Trattner, Stephen Fuselier, Steven Petrinec, James Burch, Paul Cassak, Robert Ergun, Barbara Giles, and Roy Torbert

The interplanetary magnetic field (IMF) convected with the solar wind drapes around the region of space dominated by Earth’s geomagnetic field and undergoes a process called magnetic reconnection at the magnetopause; the boundary layer that separates these two distinct regimes. Magnetic reconnection changes the topology of magnetic field lines and is known to convert magnetic energy into kinetic energy and heat. This fundamental process occurs in many environments, spanning from laboratory plasmas to the heliosphere, the solar atmosphere, and to astrophysical phenomena. Magnetic reconnection at the Earth’s magnetopause has been observed at various times and places as either anti-parallel and/or component reconnection. A model known as the Maximum Magnetic Shear Model combines these two scenarios, creating long reconnection lines crossing the dayside magnetopause along a ridge of maximum magnetic shear. 
The connection points between the anti-parallel and the component reconnection segments of the reconnection line are known as ‘Knee’ regions. Using observations from the MMS satellites, it was shown that the location of the Knee region depends strongly on the local draping conditions of the IMF across the magnetopause, with certain draping conditions causing a deflection of the location along the anti-parallel reconnection region. This study discusses an event that shows that the entire component reconnection X-line crossing the dayside magnetopause can be affected by this deflection. This result emphasizes the importance of anti-parallel reconnection that seems to control where component reconnection is occurring. 

How to cite: Trattner, K., Fuselier, S., Petrinec, S., Burch, J., Cassak, P., Ergun, R., Giles, B., and Torbert, R.: The location of Component Reconnection at the Earth’s Magnetopause During Dominant IMF By and Large Dipole Tilt Conditions, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3156, https://doi.org/10.5194/egusphere-egu2020-3156, 2020.

EGU2020-16473 | Displays | ST2.3

Particle-In-Cell simulations of magnetic reconnection in the presence of a cold shear flow

Susanne Flø Spinnangr, Paul Tenfjord, Michael Hesse, Cecilia Norgren, and Norah Kwagala

Our group has done extensive research on the fluid and kinetic effect of cold ion populations on the reconnection process, in an effort to identify factors that can lead to the onset or stopping of magnetic reconnection. Recent fully kinetic studies involving cold protons or oxygen have shown that flows of cold particles significantly modify the reconnection process, and that the nature of this modification is dependent on the configuration of these flows and the constituent ions of the flows. In this study we want to investigate how the reconnection process is affected by a shear flow of cold protons outside of the current sheet, using a 2.5D Particle-In-Cell simulation. The effect of shear flows on magnetic reconnection has investigated earlier, indicating a signifficant modification of the reconnection process. However, it is not clear how these effects will be influenced by the additional scale lengths introduced into the system by a cold ion flow. In particular we want to investigate how the current sheet and diffusion regions are altered by a cold shear flow on a kinetic level, and how the reconnection process is altered on ion scales and beyond. Preliminary results indicate that the shear flow introduces a tilt of the current sheet, which appears to be consistent with earlier studies. Results will be compared to our group’s earlier results involving symmetric and asymmetric flows of cold particles in the inflow regions, as well as existing simulations and observations of magnetic reconnection including warm shear flows.

How to cite: Flø Spinnangr, S., Tenfjord, P., Hesse, M., Norgren, C., and Kwagala, N.: Particle-In-Cell simulations of magnetic reconnection in the presence of a cold shear flow, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-16473, https://doi.org/10.5194/egusphere-egu2020-16473, 2020.

EGU2020-5692 | Displays | ST2.3

The Relationship Between Electron-Only Magnetic Reconnection and Turbulence in Earth’s Magnetosheath

Julia E. Stawarz, Jonathan P. Eastwood, Tai Phan, Imogen L. Gingell, Alfred Mallet, Michael A. Shay, Prayash Sharma Pyakurel, James L. Burch, Robert E. Ergun, Barbara L. Giles, Daniel J. Gershman, Olivier Le Contel, Per-Arne Lindqvist, Robert J. Strangeway, Roy B. Torbert, Matthew R. Argall, David Fischer, and Werner Magnes

The Earth’s magnetosheath is filled with small-scale current sheets arising from turbulent dynamics in the plasma. Previous observations and simulations have provided evidence that such current sheets can be sites for magnetic reconnection. Recently, observations from the Magnetospheric Multiscale (MMS) mission have revealed that a novel form of “electron-only” reconnection can occur at these small-scale, turbulence-driven current sheets, in which ions do not appear to couple to the reconnected magnetic field to form ion jets. The presence of electron-only reconnection may facilitate dissipation of the turbulence, thereby influencing the partition of energy between ions and electrons, and can alter the nonlinear dynamics of the turbulence itself. In this study, we perform a survey of turbulent intervals in the Earth’s magnetosheath as observed by MMS in order to determine how common magnetic reconnection is in the turbulent magnetosheath and how it impacts the small-scale turbulent dynamics. The magnetic correlation length, which dictates the length of the turbulent current sheets, is short enough in most of the examined intervals for reconnection with reduced or absent ion jets to occur. Magnetic reconnection is found to be a common feature within these intervals, with a significant fraction of reconnecting current sheets showing evidence of sub-Alfvénic ion jets and super- Alfvénic electron jets, consistent with electron-only reconnection. Moreover, a subset of the intervals exhibit changes in the behavior of the small-scale magnetic power spectra, which may be related to the reconnecting current sheets. The results of the survey are compared with recent theoretical work on electron-only reconnection in turbulent plasmas.

How to cite: Stawarz, J. E., Eastwood, J. P., Phan, T., Gingell, I. L., Mallet, A., Shay, M. A., Sharma Pyakurel, P., Burch, J. L., Ergun, R. E., Giles, B. L., Gershman, D. J., Le Contel, O., Lindqvist, P.-A., Strangeway, R. J., Torbert, R. B., Argall, M. R., Fischer, D., and Magnes, W.: The Relationship Between Electron-Only Magnetic Reconnection and Turbulence in Earth’s Magnetosheath, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5692, https://doi.org/10.5194/egusphere-egu2020-5692, 2020.

Satellite observations with high-resolution measurements have demonstrated the existence of intermittent current sheets and occurrence of magnetic reconnection in a quasi-parallel magnetosheath behind the terrestrial bow shock. In this Letter, by performing a three-dimensional (3-D) global hybrid simulation, we investigated the characteristics of the quasi-parallel magnetosheath of the bow shock, which is formed due to the interaction of the solar wind with the earth’s magnetosphere. Current sheets with widths of several ion inertial lengths are found to be produced in the magnetosheath after the upstream large amplitude electromagnetic waves penetrate through the shock and are then compressed in the downstream. Magnetic reconnection consequently occurs in these current sheets, where high-speed ion flow jets are identified in the outflow region. Simultaneously, flux ropes with the extension (along the   direction) of about several earth’s radii are also observed. Our simulation shed new insight on the mechanism for the occurrence of magnetic reconnection in the quasi-parallel shocked magnetosheath.

How to cite: Lu, Q., Wang, H., and Wang, X.: Turbulence-driven magnetic reconnection in the magnetosheath downstream of a quasi-parallel shock:a three-dimensional global hybrid simulation, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21406, https://doi.org/10.5194/egusphere-egu2020-21406, 2020.

EGU2020-1866 | Displays | ST2.3 | Highlight

A new model to explain energetic electrons behind dipolarization front

Huishan Fu, Mingjie Zhao, Yue Yu, and Zhe Wang

Dipolarization front—a sharp boundary leading reconnection jets and producing colorful auroras—plays a crucial role in the magnetotail energy conversion. Behind this front, sometimes energetic electrons appear, whereas sometimes they vanish. The reason causing such uncertainty is still a mystery, owing to the lack of high-resolution measurements. Here we propose a novel model to uncover this mystery: we find that behind the front there exists a magnetic bottle with time-varying belly but steady neck. When the belly is expanding—like a man getting fat—the magnetic bottle is formed and energetic electrons are trapped; when the belly is contracting—like a man getting slim—the magnetic bottle disappears and energetic electrons are expelled. This model clearly explains how energetic electrons are trapped in the Earth’s magnetotail and in principle it can be applied to other planetary magnetotails. 

How to cite: Fu, H., Zhao, M., Yu, Y., and Wang, Z.: A new model to explain energetic electrons behind dipolarization front, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1866, https://doi.org/10.5194/egusphere-egu2020-1866, 2020.

EGU2020-8550 | Displays | ST2.3

Energy conversion by electron beam-driven waves in a compressed reconnection separatrix

Justin Holmes, Rumi Nakamura, Owen Roberts, Daniel Schmid, Takuma Nakamura, and Zoltan Vörös

We investigate magnetic compression near the reconnection separatrix observed by Magnetospheric MultiScale (MMS) on July 11th 2017. A clear transition between inflow and outflow in both ions and electrons is observed across an ion gyro-scale region of enhanced magnetic field. Multispacecraft techniques for magnetic curvature and local gradients along with timing of highly-correlated wave packets are used to determine the spatial configuration of the compressed region. Structure of the system is found to be inherently three dimensional; electron beam-driven modes propagating parallel to the magnetic field are observed concurrent with perpendicular-propagating lower hybrid waves. Larger scale surface waves are also present behind the compression front. Transforming to a deHoffmann-Teller frame across the boundary results in a distinctly non-rotational discontinuity with structure similar to a quasi-2D, Petschek-like slow shock. However, MHD jump conditions are not satisfied, indicating kinetic dissipation may occur within the thin layer. The largest amplitude measurements of $\mathbf{J}\cdot\mathbf{E}$ energy conversion are associated with an inflowing electron beam and parallel electric fields near the magnetic peak. Spikes in $\mathbf{J}\cdot\mathbf{E}$ are predominantly negative, suggesting electron-scale mixing between the reconnection inflow and outflow is partially responsible for the observed magnetic compression.

How to cite: Holmes, J., Nakamura, R., Roberts, O., Schmid, D., Nakamura, T., and Vörös, Z.: Energy conversion by electron beam-driven waves in a compressed reconnection separatrix, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-8550, https://doi.org/10.5194/egusphere-egu2020-8550, 2020.

EGU2020-1809 | Displays | ST2.3

Lower hybrid waves at the magnetosheath separatrix region

Binbin Tang, Wenya Li, Daniel Graham, Chi Wang, and Yuri Khotyaintsev and the MMS team
Lower hybrid waves are investigated at the magnetosheath separatrix region in asymmetric guide-field reconnection at Earth’s magnetopause by using MMS observations. These waves are found in a limited region, depending on the density gradient across the separatrix, and they are driven by the lower hybrid drift instability. Properties of these waves are presented: (1) the waves propagate towards the x-line due to the out-of-plane magnetic field, consistent with the electron drift direction; (2) the wave potential is about 20% of the electron temperature. These drift waves effectively produce cross-field particle diffusion, enabling the entry of magnetosheath electrons into the exhaust region.

How to cite: Tang, B., Li, W., Graham, D., Wang, C., and Khotyaintsev, Y. and the MMS team: Lower hybrid waves at the magnetosheath separatrix region, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1809, https://doi.org/10.5194/egusphere-egu2020-1809, 2020.

EGU2020-3728 | Displays | ST2.3

Electron Bernstein waves Driven by the Parallel Electron Crescent in the Reconnection Exhaust Region

Kyunghwan Dokgo, Kyoung-Joo Hwang, James L. Burch, Peter H. Yoon, Daniel B. Graham, and Wenya Li

The recently launched NASA’s Magnetosphere Multiscale (MMS) mission enables investigations of multi-scale phenomena in the reconnection process. Especially, the MMS spacecraft revealed that high-frequency waves of electron time scales exist near the electron diffusion region (EDR) due to complex electron distributions. As such waves are generated near the EDR, they could significantly affect the environment of the EDR via wave-particle interactions.

 We investigated the September 19, 2015 event when the MMS spacecraft crossed the reconnection exhaust region. The MMS spacecraft observed a parallel electron crescent, which is known to be generated by the cyclotron turning due to the normal magnetic field in the reconnection exhaust region. At the same time, highly discrete waves were observed in the power spectrum of the electric field. The wave frequency ranged between 6  ~ 14 Fce (Fce: electron cyclotron frequency), and the power of perpendicular components was larger than the parallel component. Therefore, they featured electron Bernstein waves. By modeling the parallel electron crescent as a sum of 18 ring-shaped electron distributions, we calculate the linear dispersion relation using a numerical solver. The linear growth rates agreed with the power spectrum of the electric field, which means that the parallel electron crescent locally drove the electron Bernstein waves. Together with previous studies of high-frequency waves, our work could provide a diagram of high-frequency wave distributions in the reconnection geometry.

How to cite: Dokgo, K., Hwang, K.-J., Burch, J. L., Yoon, P. H., Graham, D. B., and Li, W.: Electron Bernstein waves Driven by the Parallel Electron Crescent in the Reconnection Exhaust Region, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3728, https://doi.org/10.5194/egusphere-egu2020-3728, 2020.

EGU2020-9760 | Displays | ST2.3

The effect of plasmaspheric material on magnetopause reconnection

Stephen Fuselier, Stein Haaland, Paul Tenfjord, David Malaspina, James Burch, Michael Denton, Barbara Giles, Karlheinz Trattner, Steven Petrinec, Robert Strangeway, and Sergio Toledo-Redondo

The Earth’s plasmasphere contains cold (~eV energy) dense (>100 cm-3) plasma of ionospheric origin. The primary ion constituents of the plasmasphere are Hand He+, and a lower concentration of O+. The outer part of the plasmasphere, especially on the duskside of the Earth, drains away into the dayside outer magnetosphere when geomagnetic activity increases. Because of its high density and low temperature, this plasma has the potential to modify magnetic reconnection at the magnetopause. To investigate the effect of plasmaspheric material at the magnetopause, Magnetospheric Multiscale (MMS) data are surveyed to identify magnetopause crossings with the highest He+densities. Plasma wave, ion, and ion composition data are used to determine densities and mass densities of this plasmaspheric material and the magnetosheath plasma adjacent to the magnetopause. These measurements are combined with magnetic field measurements to determine how the highest density plasmaspheric material in the MMS era may affect reconnection at the magnetopause.

How to cite: Fuselier, S., Haaland, S., Tenfjord, P., Malaspina, D., Burch, J., Denton, M., Giles, B., Trattner, K., Petrinec, S., Strangeway, R., and Toledo-Redondo, S.: The effect of plasmaspheric material on magnetopause reconnection, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-9760, https://doi.org/10.5194/egusphere-egu2020-9760, 2020.

EGU2020-2507 | Displays | ST2.3

Nonideal Electric Field Observed in the Separatrix Region of a Magnetotail Reconnection Event

Xiancai Yu, Rongsheng Wang, and Quanming Lu

The microphysics in the separatrix region (SR) plays an important role for the energy conversion in reconnection. Based on the Magnetospheric Multiscale observations in the magnetotail, we present a complete crossing of the current sheet with ongoing magnetic reconnection. The field‐aligned inflowing electrons were observed in both separatrix regions (SRs) and their energy extended up to several times of the thermal energy. Along the SR, a net parallel electrostatic potential was estimated and could be the reason for the inflowing electron streaming. In the northern SR, the electron frozen‐in condition was violated and nonideal electric field was inferred to be caused by the gradient of the electron pressure tensor. The nongyrotropic electron distribution and significant energy dissipation were observed at the same region. The observations indicate that the inner electron diffusion region can extend along the separatrices or some electron‐scale instability can be destabilized in the SR. 

How to cite: Yu, X., Wang, R., and Lu, Q.: Nonideal Electric Field Observed in the Separatrix Region of a Magnetotail Reconnection Event, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2507, https://doi.org/10.5194/egusphere-egu2020-2507, 2020.

By measurements of the Magnetospheric Multiscale (MMS) mission in the magnetotail from -24 to -15 RE , we identified 40 ion Bursty Bulk Flow events (BBFs) and investigated the electron behaviors during these BBFs. The ion flows peaked near the center of the plasma sheet and had a sharp flow boundary. The electron flow profile is distinct from the ion flows of the BBFs. Inside the BBFs, the strongest earthward electron flows are observed in the ion flow boundary, away from the current sheet center. Further away from the peak of the earthward electron flows, the tailward electron flows are observed in the edges of the ion flows, are mainly field-aligned with low energy, and are stronger than the earthward flows. It seems that the tailward low-energy electrons are energized at some places tailward of the spacecraft and then ejected towards Earth, consistent with the magnetic reconnection scenario in the magnetotail. The implication to the understanding of the astrophysical jets is suggested.

How to cite: Zhang, M. and Lu, Q.: Observation of the tailward electron flows commonly detected at the flow boundary of the earthward ion Bursty Bulk Flows in the magnetotail, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1672, https://doi.org/10.5194/egusphere-egu2020-1672, 2020.

EGU2020-22152 | Displays | ST2.3

The magnetic field quantization in pulsar

Chaudhary Rozina, Tsintsadze LevanNodar, and Nodar Tsintsadze

Magnetic field quantization is an important issue for degenerate environments such as neutron star, radio pulsars and magnetars etc., due to the fact that these stars have magnetic field even more than the quantum critical field strength of the order of 4.4×10¹³G, accordingly the cyclotron energy may be equal or even much more than the Fermi energy of degenerate particles. We shall formulate here the exotic physics of strongly magnetized neutron star. The effect of quantized anisotropic magnetic pressure, arising due to a strong magnetic field is studied on the growth rate of Jeans instability of quantum electron–ion and classical dusty plasma.  Here we shall formulate the dispersion equations to govern the propagation of the gravitational waves both in perpendicular and parallel directions to the magnetic field, respectively.  We will depict here that the quantized magnetic field will result in Jeans anisotropic instability such that for perpendicular propagation, the quantized magnetic pressure will stabilize Jeans instability, whereas for the parallel propagation the plasma become more unstable.  We also intend to calculate the corresponding Jeans wave number in the absence of tunneling. The Madelung term leads to the inhomogeneity of the plasma medium. Numerical results are presented to show the effect of the anisotropic magnetic pressure on the Jeans instability.

How to cite: Rozina, C., LevanNodar, T., and Tsintsadze, N.: The magnetic field quantization in pulsar, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-22152, https://doi.org/10.5194/egusphere-egu2020-22152, 2020.

EGU2020-21853 | Displays | ST2.3

Energetic Electron Acceleration in Unconfined Reconnection Jets

Guo Chen, Huishan Fu, Ying Zhang, Xiaocan Li, Yasong Ge, Aimin Du, Chengming Liu, and Yin Xu

Magnetic reconnection in astronomical objects such as solar corona and the Earth’s magnetotail theoretically produces a fast jet toward the object (known as a confined jet as it connects to the object through magnetic field lines) and a fast jet departing the object (known as an unconfined jet as it propagates freely in space). So far, energetic electron acceleration has been observed in the confined jet but never in the unconfined jet, arousing a controversy about whether or not reconnection jets can intrinsically accelerate electrons. Our study is focused on the electron acceleration in unconfined reconnection jet based on Cluster observations and VPIC simulations.

How to cite: Chen, G., Fu, H., Zhang, Y., Li, X., Ge, Y., Du, A., Liu, C., and Xu, Y.: Energetic Electron Acceleration in Unconfined Reconnection Jets, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21853, https://doi.org/10.5194/egusphere-egu2020-21853, 2020.

EGU2020-3254 | Displays | ST2.3

MMS-Cluster conjugate observation of disturbance in the current sheet associated with localized fast flow in the near-Earth magnetotail

Rumi Nakamura, Wolfgang Baumjohann, Joachim Birn, Jim Burch, Chris Carr, Iannis Dandouras, Philippe Escoubet, Andrew Fazakerley, Barbara Giles, Marina Kubyshkina, Olivier Le Contel, Tsugunobu Nagai, Takuma Nakamura, Evgeny Panov, Chris Russell, Victor Sergeev, and Roy Torbert

We report the evolution of the current sheet associated with a localized flow burst in the near-Earth magnetotail on Sep. 8, 2018 around 14 UT when MMS (Magnetospheric Multiscale) and Cluster at about X=17 RE, separated mainly in the dawn-dusk direction at a distance of about 4 RE, encountered at duskside and dawnside part of a dipolarization front, respectively.  We analyzed the mesoscale current sheet disturbances based on multi-point data analysis between Cluster and MMS. It is shown that the current sheet thickens associated with the passage of the dipolarization front confirming results from previous statistical studies. The thickness of the current sheet, however, decreased subsequently, before recovering toward the original configuration. MMS observed enhanced field aligned currents exclusively during this thinning of the current sheet at the off-equatorial region. Multiple layers of small-scale, intense field-aligned currents accompanied by enhanced Hall-currents were detected at this region.  Based on these mesoscale and microscale multipoint observations, we infer the current structures around the localized flow and discuss the role of these mesoscale flow processes in the larger-scale magnetotail dynamics.

 

 

How to cite: Nakamura, R., Baumjohann, W., Birn, J., Burch, J., Carr, C., Dandouras, I., Escoubet, P., Fazakerley, A., Giles, B., Kubyshkina, M., Le Contel, O., Nagai, T., Nakamura, T., Panov, E., Russell, C., Sergeev, V., and Torbert, R.: MMS-Cluster conjugate observation of disturbance in the current sheet associated with localized fast flow in the near-Earth magnetotail, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3254, https://doi.org/10.5194/egusphere-egu2020-3254, 2020.

EGU2020-3523 | Displays | ST2.3

Scaling of magnetic reconnection with a limited x-line extent

Kai Huang, Yi-Hsin Liu, Quanming Lu, and Michael Hesse

Contrary to all the 2D models, where the reconnection x-line extent is infinitely long, we study magnetic reconnection in the opposite limit. The scaling of the average reconnection rate and outflow speed are modeled as a function of the x-line extent. An internal x-line asymmetry along the current direction develops because of the flux transport by electrons beneath the ion kinetic scale, and it plays an important role in suppressing reconnection in the short x-line limit; the average reconnection rate drops because of the limited active region, and the outflow speed reduction is associated with the reduction of the J×B force, that is caused by the phase shift between the J and B profiles, also as a consequence of this flux transport.

How to cite: Huang, K., Liu, Y.-H., Lu, Q., and Hesse, M.: Scaling of magnetic reconnection with a limited x-line extent, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3523, https://doi.org/10.5194/egusphere-egu2020-3523, 2020.

EGU2020-4002 | Displays | ST2.3

Statistical properties of ions in bursty bulk flows

Mingyu Wu, Zonghao Pan, Yangjun Chen, and Tielong Zhang

With the observations of THEMIS and MMS Mission, we have investigated the properties of ions in bursty bulk flows (BBFs). Based on analysis of 315 BBF events, we can obtain the statistical features of ions in the BBFs. The results can be summarized as follows: (1) the occurrence rate of BBFs is related with AE index, which is also confirmed by previous studies; (2) the ion number density in the duskside is nearly at the same level with that in the dawnside; (3) in the region -10RE > XGSM> -15RE(where REis the earth radius), the ion temperature in the duskside is much higher than that in the dawnside; (4) the ion temperature anisotropy T/T∥ is weaker as BBFs close to the Earth; (5) corresponds to cold electrons (Te < 1.5 keV), the ratio of the ion and electron temperature Ti/Te can reach 10-15 and the temperature of ions and electrons have a linear correlation.

How to cite: Wu, M., Pan, Z., Chen, Y., and Zhang, T.: Statistical properties of ions in bursty bulk flows, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4002, https://doi.org/10.5194/egusphere-egu2020-4002, 2020.

EGU2020-4615 | Displays | ST2.3

MMS observations of reconnection separatrix region in the magnetotail at different distances from the active neutral X-line

Victor Sergeev, Sergey Apatenkov, Rumi Nakamura, Simon Wellenzohn, Ferdinand Plaschke, Wolfgang Baumjohann, Yuri Khotyaintsev, Jim Burch, Roy Torbert, Christopher Russell, and Barbara Giles

The region surrounding the reconnection separatrix consists of the multitude of particle and wave transient features (electron, cold and hot ion beams, Hall E&B fields, kinetic Alfven and LH waves, e-holes etc) whose pattern and intensities may vary depending on the stage of reconnection process as well as on the distance from the active neutral line (XNL), whose characterization from observations is not a trivial task. We explore quick MMS entries into the plasma sheet boundary layer from the lobe in 2017 and 2018 tail seasons which potentially could be the crossings of the active separatrix as suggested by energy dispersed beams and polar rain gap features. By combining  the observations of beam dispersion with the measured plasma convection and PSBL motion (obtained using the timing method) we attempt to separate  temporal and spatial (velocity filter) contributions  to the observed beam energy dispersion and evaluate the MMS distance from the XNL. In this report we discuss similarities and differences of separatrix manifestations  observed far from the XNL (at distances exceeding several tens Re) and those found close to it (where the outermost electron beam directed toward the XNL is seen).  One of surprizes was that we were often able to identify the intense Hall-like E&B field structures at very large distances from the XNL.  

How to cite: Sergeev, V., Apatenkov, S., Nakamura, R., Wellenzohn, S., Plaschke, F., Baumjohann, W., Khotyaintsev, Y., Burch, J., Torbert, R., Russell, C., and Giles, B.: MMS observations of reconnection separatrix region in the magnetotail at different distances from the active neutral X-line , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4615, https://doi.org/10.5194/egusphere-egu2020-4615, 2020.

EGU2020-6493 | Displays | ST2.3

Deceleration and deflection of solar wind ions by periodic shocks

Aimin Du and Lican Shan

Interacting with a supersonic solar wind, the escaping ions result in a series of phenomena in the Martian space environment. Observations from MAVEN magnetometer and plasma detector revealed a serial of small-amplitude quasi-monochromatic waves upstream of the Martian bow shock. Those waves have a dominant frequency at the local proton gyrofrequency. The waves evolve into periodic shock structures as they are convected downstream by the high-speed solar wind flow. We found those structures deflected and decelerated solar wind ions through magnetic mirror topology. A consequence of the effect is a significant loss of solar wind ion energy, accompanying with pitch angle scattering.

How to cite: Du, A. and Shan, L.: Deceleration and deflection of solar wind ions by periodic shocks, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6493, https://doi.org/10.5194/egusphere-egu2020-6493, 2020.

EGU2020-8673 | Displays | ST2.3

Grad-Shafranov reconstruction of the in-plane magnetic field potential in the X-point vicinity: boundary-layer approximation

Daniil Korovinskiy, Andrey Divin, Vladimir Semenov, Nikolai Erkaev, and Stefan Kiehas

The problem of steady symmetrical two-dimensional magnetic reconnection is addressed in terms of the EMHD approximation. In the immediate vicinity of the X-point, this approach has been proven to be an appropriate frame for the reconstruction problem, expressed, particularly, by the Poisson equation for the magnetic potential A, where the right-hand side contains the out-of-plane electron current density with reversed sign. With boundary conditions fixed at some curve (the satellite trajectory), and assuming the right-hand side to be a function of A, one arrives at an ill-posed problem for the Grad-Shafranov equation. The further simplification of the problem may be achieved by using the boundary layer approximation, since magnetic configuration in reconnection region is highly stretched. The benchmark reconstruction of PIC-simulation data, using four numerical techniques, has shown that the main contribution for inaccuracy arises from replacing the Poisson equation by the Grad-Shafranov one. A boundary layer approximation, in turn, does not affect the accuracy significantly; in some cases this approach can appear even the most appropriate. 

How to cite: Korovinskiy, D., Divin, A., Semenov, V., Erkaev, N., and Kiehas, S.: Grad-Shafranov reconstruction of the in-plane magnetic field potential in the X-point vicinity: boundary-layer approximation, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-8673, https://doi.org/10.5194/egusphere-egu2020-8673, 2020.

EGU2020-8693 | Displays | ST2.3

MMS Observations of Short-Period Current Sheet Flapping

Louis Richard, Yuri Khotyaintsev, Daniel Graham, Christopher Russell, and Olivier Le Contel

Flapping motions of current sheets are commonly observed in the magnetotail. Various wave modes can correspond to these oscillations such as kink-like flapping or steady flapping (e.g Wei2019). The period of such oscillating phenomena is usually longer than 100s and a typical observations consist only of a few crossings (e.g. Zhang2002). Here, we present a short period (T≈25s) flapping event observed by Magnetospheric Multiscale (MMS) mission at the dusk side plasmasheet on September 14, 2019. Using the multispacecraft observations, the direction of flapping as well as the direction of propagation of the current sheet are determined using the minimum variance, the timing method and the spatiotemporal derivative (Shi2005). It appears that the three methods give similar results with a direction of propagation of the current sheet which mainly lies in the ecliptic plane with a flapping velocity up to 500km/s. Based on the obtained wavelength and the variations of the direction of propagation we discuss which of the wave modes can explain the flapping.

How to cite: Richard, L., Khotyaintsev, Y., Graham, D., Russell, C., and Le Contel, O.: MMS Observations of Short-Period Current Sheet Flapping, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-8693, https://doi.org/10.5194/egusphere-egu2020-8693, 2020.

EGU2020-4023 | Displays | ST2.3

magnetic reconnection onset from electron phase to ion phase

Rongsheng Wang

It is still unresolved that how magnetic reconnection is triggered in the collisionless environment. In this talk, we will present that the reconnection onset consists of two phases: the electron phase and ion phase. In the electron phase, the electrons are significantly energized and super-alfvenic electron jets are created while the ion bulk flows haven't been formed and the ions haven't been heated. Later on, the ion jets are produced together with the electron jets in the ion phase. The main reason for such two phases is discussed. A particle-in-cell simulation was performed to realize these two phases during reconnection onset. 

 

How to cite: Wang, R.: magnetic reconnection onset from electron phase to ion phase, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4023, https://doi.org/10.5194/egusphere-egu2020-4023, 2020.

EGU2020-8780 | Displays | ST2.3

Unsteady energy dissipation in the magnetic reconnection diffusion region

Xiangcheng Dong, Malcolm Dunlop, Tieyan Wang, Barbara Giles, Roy Torbert, Christopher Russell, and James Burch

Magnetic reconnection is a universal physical process during which energy can be transferred from the electromagnetic field to the plasma. Energy dissipation in the diffusion region has always been a significant issue for understanding this energy transport. Using the four MMS spacecraft data, we investigate a magnetic reconnection diffusion region event at the magnetopause. Similar magnetic field and electric current behavior between each spacecraft indicates the formation of a quasi 2D structure. However, we find that the energy dissipation results of each spacecraft are different. Further analysis indicates that the reconnection electric field, EM, plays a key role in this process. Thus, we suggest that the energy dissipation of magnetic reconnection is unsteady on this spatial or temporal scale, even under stable diffusion conditions.

How to cite: Dong, X., Dunlop, M., Wang, T., Giles, B., Torbert, R., Russell, C., and Burch, J.: Unsteady energy dissipation in the magnetic reconnection diffusion region, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-8780, https://doi.org/10.5194/egusphere-egu2020-8780, 2020.

EGU2020-11451 | Displays | ST2.3

Reconnection site and ion scale turbulence generation

Andris Vaivads, Chengming Liu, Yuri V. Khotyaintsev, Daniel B. Graham, Per-Arne Lindqvist, Roy B. Torbert, Jim L. Burch, Christopher T. Russell, Olivier Le Contel, Barbara L. Giles, and Daniel J. Gershman

We analyze in detail a reconnection site observed by the Magnetospheric Multiscale (MMS) mission in the magnetotail. The interval around the X-line is identified based on the ion jet reversal, Hall electric fields and other reconnection signatures. At the reconnection site strong electric fields with amplitudes above 100mV/m are observed. In addition, the region shows strong turbulent variations on ion scales, including magnetic island-like structures. We discuss the cause of strong electric fields, their relation to ion scale structures and associated particle acceleration in this region. Of particular interest is the relation of the reconnection site to the generation of kinetic Alfven waves.

How to cite: Vaivads, A., Liu, C., Khotyaintsev, Y. V., Graham, D. B., Lindqvist, P.-A., Torbert, R. B., Burch, J. L., Russell, C. T., Contel, O. L., Giles, B. L., and Gershman, D. J.: Reconnection site and ion scale turbulence generation, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11451, https://doi.org/10.5194/egusphere-egu2020-11451, 2020.

EGU2020-13506 | Displays | ST2.3

Current sheet structure close to a reconnection point observed by MMS

Diana Rojas Castillo, Rumi Nakamura, and Takuma K.M. Nakamura

The typical picture of magnetic reconnection in the magnetosphere includes a classic Harris-type current sheet, where the current density is maximum at the magnetic equator (Bx=0). However, observations have shown that the magnetotail current sheet structure is much more complicated than this simple view. Therefore, revealing the structure of the current sheet is of importance to understand the reconnection process. Based on the four-point MMS high-resolution data, we present observations of a multiple reconnection event for which we study the structure of the current sheet as well as some of its characteristic scales. We show that the CS structure is highly dynamic during the reconnection process, changing from a bifurcated shape away from the reconnection site, to a more symmetric (Harris-type) structure near the X-line.

How to cite: Rojas Castillo, D., Nakamura, R., and Nakamura, T. K. M.: Current sheet structure close to a reconnection point observed by MMS, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-13506, https://doi.org/10.5194/egusphere-egu2020-13506, 2020.

EGU2020-811 | Displays | ST2.3

First Evidence of Flux Transfer Events Caused by Mangetosheath Jets

Simon Thor, Anita Kullen, Tomas Karlsson, and Savvas Raptis

Magnetosheath jets are local enhancements of dynamic pressure above the background level. Hietala et al. (2018) recently presented observational evidence of a jet collision with the magnetopause causing magnetic field line reconnection. In the present study, we show data which, for the first time, strongly indicates that magnetosheath jets can even create localized transient reconnection events, so-called flux transfer events (FTEs).

FTEs are commonly observed in cascades with an average separation time of 8-10 minutes, but may also appear as isolated events. Despite the fact that FTEs have gained major attraction during recent years, the formation process of FTEs is not yet fully understood. We showed in a recent statistical study (Kullen, Thor, and Karlsson; 2019) that isolated FTEs and FTE cascades occur during different IMF conditions and are differently distributed along the magnetopause. The results of the statistical study strongly suggest that the majority of the FTEs formed along the expected reconnection region for each respective IMF condition. However, for a subset of isolated FTEs, we proposed a different formation process. These events may have been caused by magnetosheath jets, as they occur during IMF conditions favorable for jet formation. Simulation results by Karimabadi et al. (2014) has shown that such a creation mechanism is possible. In his simulation, a magnetosheath jet collides with the magnetopause, creating an FTE.

In the present investigation, FTEs that may have been caused by magnetosheath jets were identified. To achieve this, we examined measurements from all four Cluster satellites, and searched for magnetosheath jets that appear in close proximity to FTEs listed in Wang et al. (2005)’s FTE list. Our results show that approximately 15% of isolated FTEs appear in the vicinity of jets. These FTEs are further examined based on IMF and location across the magnetopause. For two of the FTEs, the associated jet appears close to the magnetopause. We present a detailed data analysis of these two events and discuss a possible formation mechanism for the FTEs, as there is strong evidence that the two FTEs are indeed caused by jets.

How to cite: Thor, S., Kullen, A., Karlsson, T., and Raptis, S.: First Evidence of Flux Transfer Events Caused by Mangetosheath Jets, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-811, https://doi.org/10.5194/egusphere-egu2020-811, 2020.

Using measurements by the Magnetospheric Multiscale (MMS) spacecraft in the magnetotail, we studied electron distribution functions across an electron diffusion region. The dependence of the non-gyrotropic distribution on the energy and vertical distance from the EDR mid-plane was revealed for the first time. The non-gyrotropic distribution was observed everywhere except for an extremely narrow layer right at the EDR mid-plane. The energy of the non-gyrotropic distribution increased with growth of the vertical distance from the mid-plane. For the electrons within certain energy range, they exhibited the non-gyrotropic distribution at the distance further away from the mid-plane than that expected from the meandering motion. The correlation between the crescent-shaped distribution with multiple stripes and the large Hall electric field was established. It appears that the measured non-gyrotropic distribution and the crescent-shaped distribution were caused by the meandering motion and the Hall electric field together.

How to cite: Li, X. and Lu, Q.: Observation of non-gyrotropic electron distribution across the electron diffusion region in the magnetotail reconnection, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1549, https://doi.org/10.5194/egusphere-egu2020-1549, 2020.

Magnetic reconnection is a fundamental plasma process, by which magnetic energy is explosively released in the current sheet to energize charged particles and to create bi-directional Alfvénic plasma jets. A long-outstanding issue is how the stored magnetic energy is rapidly released in the process. Numerical simulations and observations show that formation and interaction of magnetic flux ropes dominate the evolution of the reconnecting current sheet. Accordingly, most volume of the reconnecting current sheet is occupied by the flux ropes and energy dissipation primarily occurs along their edges via the flux rope coalescence. Here, for the first time, we present in-situ evidence of magnetic reconnection inside the filamentary currents which was driven possibly by electron vortices inside the flux ropes. Our results reveal an important new way for energy dissipation in magnetic reconnection.

How to cite: Wang, S. and Lu, Q.: Direct evidence of secondary reconnection inside filamentary currents of magnetic flux ropes in magnetic reconnection, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1671, https://doi.org/10.5194/egusphere-egu2020-1671, 2020.

EGU2020-4750 | Displays | ST2.3

Asymmetric reconnection at the bow shock

Herbert Gunell, Maria Hamrin, Oleksandr Goncharov, Alexandre De Spiegeleer, Stephen Fuselier, Joey Mukherjee, and Andris Vaivads

Can reconnection be triggered as a directional discontinuity (DD) crosses the bow shock? Here we present some unique observations of asymmetric reconnection at a quasi-perpendicular bow shock as an interplanetary DD is crossing it simultaneously with the Magnetospheric Multiscale (MMS) mission. The data show indications of ongoing reconnection at the bow shock southward of the spacecraft. The DD is also observed by several upstream spacecraft (ACE, WIND, Geotail, and THEMIS B) and one downstream in the magnetosheath (Cluster 4), but none of them resolve signatures of ongoing reconnection. We therefore suggest that reconnection was temporarily triggered as the DD was compressed by the shock. Bow shock reconnection is inevitably asymmetric with both the density and the magnetic field strength being higher on one side of the X-line (the magneosheath side) than on the other side where the plasma flow also is supersonic (the solar wind side). Asymmetric reconnection of the bow shock type has never been studied before, and the data discussed here are hence unique.

How to cite: Gunell, H., Hamrin, M., Goncharov, O., De Spiegeleer, A., Fuselier, S., Mukherjee, J., and Vaivads, A.: Asymmetric reconnection at the bow shock, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4750, https://doi.org/10.5194/egusphere-egu2020-4750, 2020.

EGU2020-9881 | Displays | ST2.3

On the identification of Electron Diffusion Regions at the magnetopause with an AI approach

Quentin Lenouvel, Vincent Génot, Philippe Garnier, Sergio Toledo-Redondo, Benoît Lavraud, Roy Torbert, Barbara Giles, and Jim Burch

MMS has already been producing a very large dataset with invaluable information about how the solar wind and the Earth's magnetosphere interact. However, it remains challenging to process all these new data and convert it into scientific knowledge, the ultimate goal of the mission. Data science and machine learning are nowadays a very powerful and successful technology that is employed to many applied and research fields. During this presentation, I shall discuss the tentative use of machine learning for the automatic detection and classification of plasma regions, relevant to the study of magnetic reconnection in the MMS data set, with a focus on the critical but poorly understood electron diffusion region (EDR) at the Earth's dayside magnetopause. We make use of the EDR database and the plasma regions nearby that has been identified by the MMS community and compiled by Webster et al. (2018) as well as the Magnetopause crossings database compiled by the ISSI team, to train a neural network using supervised training techniques. I shall present a list of new EDR candidates found during the phase 1 of MMS and do a case study of some of the strong candidates.

How to cite: Lenouvel, Q., Génot, V., Garnier, P., Toledo-Redondo, S., Lavraud, B., Torbert, R., Giles, B., and Burch, J.: On the identification of Electron Diffusion Regions at the magnetopause with an AI approach, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-9881, https://doi.org/10.5194/egusphere-egu2020-9881, 2020.

EGU2020-3764 | Displays | ST2.3

Magnetic Curvature Analysis on Reconnection Related Structures at Earth’s Magnetopause

Yi Qi, Christopher T. Russell, Robert J. Strangeway, Yingdong Jia, Roy B. Torbert, William R. Paterson, Barbara L. Giles, and James L. Burch

Magnetic reconnection is a mechanism that allows rapid and explosive energy transfer from the magnetic field to the plasma. The magnetopause is the interface between the shocked solar wind plasma and Earth’s magnetosphere. Reconnection enables the transport of momentum from the solar wind into Earth’s magnetosphere. Because of its importance in this regard, magnetic reconnection has been extensively studied in the past and is the primary goal of the ongoing Magnetospheric Multiscale (MMS) mission. During magnetic reconnection, the originally anti-parallel fields annihilate and reconnect in a thinned current sheet. In the vicinity of a reconnection site, a prominently increased curvature of the magnetic field (and smaller radius of curvature) marks the region where the particles start to deviate from their regular gyro-motion and become available for energy conversion. Before MMS, there were no closely separated multi-spacecraft missions capable of resolving these micro-scale curvature features, nor examining particle dynamics with sufficiently fast cadence.

In this study, we use measurements from the four MMS spacecraft to determine the curvature of the field lines and the plasma properties near the reconnection site. We use this method to study FTEs (flux ropes) on the magnetopause, and the interaction between co-existing FTEs. Our study not only improves our understanding of magnetic reconnection, but also resolves the relationship between FTEs and structures on the magnetopause.

How to cite: Qi, Y., Russell, C. T., Strangeway, R. J., Jia, Y., Torbert, R. B., Paterson, W. R., Giles, B. L., and Burch, J. L.: Magnetic Curvature Analysis on Reconnection Related Structures at Earth’s Magnetopause, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3764, https://doi.org/10.5194/egusphere-egu2020-3764, 2020.

ST2.4 – Kinetic plasma processes in the Earth's magnetosphere and magnetosheath

EGU2020-4295 | Displays | ST2.4 | Highlight

Electron Bernstein Waves driven by Electron Crescents near the Electron Diffusion Region

Wenya Li, Daniel Graham, Binbin Tang, Andris Vaivads, Mats Andre, Kyungguk Min, Kaijun Liu, Keizo Fujimoto, Per Arne Lindqvist, Kyunghwan Dokgo, Chi Wang, and James Burch

The Magnetospheric Multiscale spacecraft encounter an electron diffusion region (EDR) of asymmetric magnetic reconnection at Earth's magnetopause. The EDR is characterized by agyrotropic electron velocity distributions on both sides of the neutral line. Various types of plasma waves are produced by the magnetic reconnection in and near the EDR. Here we report large-amplitude electron Bernstein waves (EBWs) at the electron-scale boundary of the Hall current reversal. The finite gyroradius effect of the outflow electrons generates the crescent-shaped agyrotropic electron distributions, which drive the EBWs. The EBWs propagate toward the central EDR. The amplitude of the EBWs is sufficiently large to thermalize and diffuse electrons around the EDR. Our analysis shows that the EBWs contribute to the cross-field diffusion of the electron-scale boundary of the Hall current reversal near the EDR.

How to cite: Li, W., Graham, D., Tang, B., Vaivads, A., Andre, M., Min, K., Liu, K., Fujimoto, K., Lindqvist, P. A., Dokgo, K., Wang, C., and Burch, J.: Electron Bernstein Waves driven by Electron Crescents near the Electron Diffusion Region, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4295, https://doi.org/10.5194/egusphere-egu2020-4295, 2020.

EGU2020-13405 | Displays | ST2.4

In situ spacecraft observations of structured electron diffusion regions during magnetic reconnection

Giulia Cozzani, Alessandro Retinò, Francesco Califano, Alexandra Alexandrova, Yuri Khotyaintsev, Mats André, Filomena Catapano, Huishan Fu, Olivier Le Contel, Andris Vaivads, Narges Ahmadi, and Hugo Breuillard and the MMS Team

Magnetic reconnection is a fundamental energy conversion process in plasmas. It occurs in thin current sheets, where a change in the magnetic field topology leads to rapid heating of plasma, plasma bulk acceleration and acceleration of plasma particles. To allow for magnetic field reconfiguration, both ions and electrons must be demagnetized. The ion and electron demagnetization  take place in the ion and electron diffusion regions respectively, in both cases at kinetic scales. For the first time, Magnetospheric Multiscale (MMS) spacecraft observations, at inter-spacecraft separation comparable to the electron inertial length, allow for a multi-point analysis of the electron diffusion region (EDR). A key question is whether the EDR has a homogeneous or patchy structure. 

Here we report MMS observations at the magnetopause providing evidence of inhomogeneous current densities and energy conversion over a few (∼ 3 de) electron inertial lengths suggesting that the EDR can be structured at electron scales. In particular, the energy conversion is patchy and changing sign in the vicinity of the reconnection site implying that the EDR comprises regions where energy is transferred from the field to the plasma and regions with the opposite energy transition, which is unexpected during reconnection. The origin of the patchy energy conversion appears to be connected to the large ve,N ∼ ve,M directed from the magnetosphere to magnetosheath. These observations are consistent with recent high-resolution and low-noise kinetic simulations of asymmetric reconnection. Patchy energy conversion is observed also in an EDR at the magnetotail, where the inter-spacecraft separation was ∼ 1 de. Electric field measurements are different among the spacecraft suggesting inhomogeneities at the electron scale. However, in this case the current density appear homogeneous in the EDR suggesting that the structuring may be sourced from a different kind of electron dynamics in the magnetotail.

How to cite: Cozzani, G., Retinò, A., Califano, F., Alexandrova, A., Khotyaintsev, Y., André, M., Catapano, F., Fu, H., Le Contel, O., Vaivads, A., Ahmadi, N., and Breuillard, H. and the MMS Team: In situ spacecraft observations of structured electron diffusion regions during magnetic reconnection, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-13405, https://doi.org/10.5194/egusphere-egu2020-13405, 2020.

EGU2020-3846 | Displays | ST2.4

Electron- and proton-scale nested magnetic cavities: Manifestation of kinetic theta-pinch equilibrium in space plasmas

Jinghuan Li, Fan Yang, Xu-Zhi Zhou, Qiu-Gang Zong, Anton V. Artemyev, Robert Rankin, Quanqi Shi, Shutao Yao, Han Liu, Jiansen He, Zuyin Pu, and Chijie Xiao

Magnetic cavities, sometimes referred to as magnetic holes, are ubiquitous in space and astrophysical plasmas characterized by localized regions with depressed magnetic field strength, strongly anisotropic particle distributions, and enhanced plasma pressure. Typical cavity sizes range from fluid to ion and sub-ion kinetic scales, with recent observations also identifying nested cavities that may indicate cross-scale energy cascades. Although heavily investigated in space, magnetic cavities have analogs in laboratory plasmas, the classical theta-pinches. Here, we develop an equilibrium solution of the Vlasov-Maxwell equations in cylindrical coordinates (in similar format to theta-pinch models), to reconstruct the cross-scale profiles of magnetic cavities observed by the four-spacecraft MMS mission. The kinetic model uses input parameters derived from single-spacecraft measurements to successfully reproduce signatures of magnetic cavities from all observing spacecraft. The reconstructed profiles demonstrate that near the electron-scale cavity boundary, the decoupled electron and proton motions generate a radial electric field that contributes to electron vortex formation that has been previously attributed mostly to diamagnetic effects. At larger scales, the diminishing electric field implies that diamagnetic motion is solely responsible for proton vortices.

How to cite: Li, J., Yang, F., Zhou, X.-Z., Zong, Q.-G., Artemyev, A. V., Rankin, R., Shi, Q., Yao, S., Liu, H., He, J., Pu, Z., and Xiao, C.: Electron- and proton-scale nested magnetic cavities: Manifestation of kinetic theta-pinch equilibrium in space plasmas, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3846, https://doi.org/10.5194/egusphere-egu2020-3846, 2020.

EGU2020-2848 | Displays | ST2.4 | Highlight

Disturbance of the front region of magnetic reconnection outflow jets due to the lower-hybrid drift instability

Takuma Nakamura, Takayuki Umeda, Rumi Nakamura, Huishan Fu, and Mitsuo Oka

Magnetic reconnection is a key process in collisionless plasmas that converts magnetic energy to plasma kinetic energies through changes in the magnetic field topology. The energy conversion in this process is believed to cause various explosive phenomena in space such as auroral substorms in the Earth’s magnetosphere and solar flares. Here, a 3D fully kinetic simulation shows that the lower-hybrid drift instability (LHDI) disturbs the front of magnetic reconnection outflow jets and additionally causes the energy dissipation. The peak energy dissipation at the jet fronts is comparable to the values seen near the center of the reconnection region where the topology change during reconnection occurs, indicating that the LHDI turbulence has a substantial effect on the energetics of reconnection. The result is well consistent with a disturbance observed at the dipolarization front (DF) in the Earth’s magnetotail by the Magnetospheric Multiscale (MMS) mission. A fully kinetic dispersion relation solver, validated by the MMS observations, further predicts that the disturbance of the reconnection jet front could occur over different parameter regimes in space plasmas including the Earth’s DF and solar flares.

How to cite: Nakamura, T., Umeda, T., Nakamura, R., Fu, H., and Oka, M.: Disturbance of the front region of magnetic reconnection outflow jets due to the lower-hybrid drift instability, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2848, https://doi.org/10.5194/egusphere-egu2020-2848, 2020.

EGU2020-16698 | Displays | ST2.4

A multi-spacecraft analysis of energy transfer associated with near-Earth magnetic reconnection

Sid Fadanelli, Benoit Lavraud, and Francesco Califano

We present an analysis of energy transfers in a reconnecting near-Earth plasma, obtained by interpreting MMS data within the framework of multi-fluid plasma theory. In our analysis, energy transfers are calculated and examined locally. This way, correlations between different mechanisms of energy exchange can be retrieved in all spatial and temporal detail provided by the high-frequency, multi-point sampling capacity of the four MMS satellites.
In particular, compressional effects are separated from effective sources in the energy density evolution equations, allowing to distinguish whether some effective energy transfer is occurring locally. A large database of MMS encounters with reconnecting current sheets is exploited in order to assess the statistical validity of all results presented.

How to cite: Fadanelli, S., Lavraud, B., and Califano, F.: A multi-spacecraft analysis of energy transfer associated with near-Earth magnetic reconnection, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-16698, https://doi.org/10.5194/egusphere-egu2020-16698, 2020.

EGU2020-11510 | Displays | ST2.4

Effect of shock ripples on electron acceleration and reflection at the quasi-perpendicular bow shock

Daniel Graham, Yuri Khotyaintsev, Andris Vaivads, Mats Andre, Ahmad Lalti, Andrew Dimmock, and Andreas Johlander

At Earth’s bow shock electrons can be reflected and accelerated along magnetic fields lines, which can then form electron beams and excite Langmuir and beam-mode waves. These electron beams form when the shock normal angle is close to 90 degrees. However, recent observations have shown that quasi-perpendicular shocks can be non-stationary and exhibit ripples, which can modify the local shock-normal angle and cross-shock potential. We use Magnetospheric Multiscale (MMS) data to investigate the effects of shock ripples on the accelerated electrons observed in the electron foreshock. We compare the results with test-particle simulations to determine the effect of shock ripples on electron acceleration. We discuss the implications of these results for the generation of plasma frequency waves and radio emission in the electron foreshock region. 

How to cite: Graham, D., Khotyaintsev, Y., Vaivads, A., Andre, M., Lalti, A., Dimmock, A., and Johlander, A.: Effect of shock ripples on electron acceleration and reflection at the quasi-perpendicular bow shock, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11510, https://doi.org/10.5194/egusphere-egu2020-11510, 2020.

EGU2020-11777 | Displays | ST2.4

Magnetosheath kinetic structure: Mirror mode and jets during southward IP magnetic field

Xochitl Blanco-Cano, Luis Preisser, Diana Rojas-Castillo, and Primoz Kajdic

Earth's magnetosheath is permeated by a variety of plasma waves, nonlinear structures and ion distributions.  Understanding solar wind interaction with Earth's magnetic field requires a detailed knowledge of the magnetosheath as the interface between both regions, including its kinetic micro-structure. In this work we study an extended interval (45 min) with southward magnetic field (Bz< 0) observed by MMS in the dayside magnetosheath. We use magnetic field and plasma data to study the properties of three transient enhancements in dynamic pressure identified as jets. We also calculate instability thresholds and investigate wave characteristics inside and outside of the jets. The characteristics of these jets are variable, which suggest different origins. While two of them can be classified as V-jets with large increment in velocity with almost no density increment the third one is an N-jet showing large enhancements in density with almost no velocity increment. The N-jet lasts seven times longer than the V-jets and occurs just at the region where the negative Bz becomes positive. Ion distributions inside the jets are more isotropic (Tperp ≈Tparallel) compared with the surrounding plasma where Tperp > Tparallel. FFT and minimum variance analysis show that fluctuations inside the N-jet tend to have larger transversal components, although they propagate at large angles to the background field. In contrast, waves in regions surrounding the jets are compressive and can be identified as elliptically polarized mirror mode waves. We have also show that the mirror instability threshold CM is positive inside these intervals.

How to cite: Blanco-Cano, X., Preisser, L., Rojas-Castillo, D., and Kajdic, P.: Magnetosheath kinetic structure: Mirror mode and jets during southward IP magnetic field, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11777, https://doi.org/10.5194/egusphere-egu2020-11777, 2020.

EGU2020-18886 | Displays | ST2.4

Acceleration of cold ions at separatrices of symmetric collisionless magnetic reconnection

Evgeny Gordeev, Andrey Divin, Ivan Zaitsev, Vladimir Semenov, Yuri Khotyaintsev, and Stefano Markidis

Separatrices of magnetic reconnection host intense perpendicular Hall electric fields produced by decoupling of ion and electron components and associated with the in-plane electrostatic potential drop between inflow and outflow regions. The width of these structures is several local electron inertial lengths, which is small enough to demagnetize ions as they cross the layer. We investigate temperature dependence of ion acceleration at separatrices by means of 2D Particle-in-Cell (PIC) simulations of magnetic reconnection with only cold or hot ion background population. The separatrix Hall electric field is balanced by the inertia term in cold background simulations, the effect indicative of the quasi-steady local perpendicular acceleration. The electric field introduces a cross-field beam of unmagnetized particles which makes the temperature strongly non-gyrotropic and susceptible to sub-ion scale instabilities. This acceleration mechanism nearly vanishes for hot ion background simulations. Particle-in-cell simulations are complemented by one-dimensional test particle calculations, which show that the hot ion particles experience scattering in energies after crossing the accelerating layer, whereas cold ions are uniformly energized up to the energies comparable to the electrostatic potential drop between the inflow and outflow regions.

How to cite: Gordeev, E., Divin, A., Zaitsev, I., Semenov, V., Khotyaintsev, Y., and Markidis, S.: Acceleration of cold ions at separatrices of symmetric collisionless magnetic reconnection, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18886, https://doi.org/10.5194/egusphere-egu2020-18886, 2020.

EGU2020-3653 | Displays | ST2.4

Ionospheric ions in the magnetosphere: Important at large and small scales

Mats André, Sergio Toledo-Redondo, and Andrew W Yau

Cold (eV) ions of ionospheric origin dominate the number density of most of the volume of the magnetosphere during most of the time. Supersonic flows of cold positive ions are common and can cause a negatively charged wake behind a positively charged spacecraft. The associated induced electric field can be observed and can be used to study the cold ions. We present observations from the Cluster and MMS spacecraft showing how a charged satellite, and also individual charged wire booms of  an electric field instrument, can be used to investigate cold ion populations. Ionospheric ions affect large scales, including the Alfvén velocity and  thus energy transport with waves and the magnetic reconnection rate. These ions also affect small-scale kinetic plasma physics, including the Hall physics and wave instabilities associated with magnetic reconnection. Concerning large scales, we summarize observations from several spacecraft and show that a typical total outflow rate of ionospheric ions is 1026 ions/s and that many of these ions stay cold also after a long time in the magnetosphere.  Concerning small scales, we show examples of how cold ions modify the Hall physics of thin current sheets, including magnetic reconnection separatrices. On small kinetic scales the cold ions introduce a new length-scale, a gyro radius between the gyro radii of hot (keV) ions and electrons. The Hall currents carried by electrons can be partially cancelled by the cold ions when electrons and the magnetized cold ions ExB drift together. Also, close to a reconnection X-line an additional diffusion region can be formed (regions associated with hot and cold ions, and with electrons, total of three).

How to cite: André, M., Toledo-Redondo, S., and Yau, A. W.: Ionospheric ions in the magnetosphere: Important at large and small scales , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3653, https://doi.org/10.5194/egusphere-egu2020-3653, 2020.

EGU2020-21818 | Displays | ST2.4

Cold ion dynamics and interaction with EMIC waves near the Earth's magnetopause

Sergio Toledo-Redondo, Justin Lee, Sarah Vines, Drew Turner, Robert Allen, Wenya Li, Scott Boardsen, Mats Andre, Stephen Fuselier, Benoit Lavraud, Daniel Gershman, Adolfo Viñas, Olivier Lecontel, Barbara Giles, and James Burch

The Earth’s magnetosphere is constantly supplied by plasma coming from the solar wind and from the ionosphere. The ionospheric supply is typically cold and contains heavy ions, which can be often found in most parts of the magnetosphere.

Electromagnetic Ion Cyclotron (EMIC) waves occur in the outer magnetosphere, often in association with ionospheric ions, and serve as a coupling mechanism to the ionosphere and inner magnetosphere. Using the MMS spacecraft, we investigate the dynamics of these waves when ionospheric ions are present, and resolve their motion and energy exchange with the electromagnetic fields below the ion scale. We find that ring current ions and ionospheric ions have different dynamics inside an EMIC wave packet near the magnetopause, affecting the dispersion relation of the wave. We compare the observations to linear dispersion theory, and find excellent agreement between both. Cold ions are accelerated and drain energy from the wave packet, and modify the intrinsic properties such as the wave normal angle and the polarization of the wave.

 

 

 

 

How to cite: Toledo-Redondo, S., Lee, J., Vines, S., Turner, D., Allen, R., Li, W., Boardsen, S., Andre, M., Fuselier, S., Lavraud, B., Gershman, D., Viñas, A., Lecontel, O., Giles, B., and Burch, J.: Cold ion dynamics and interaction with EMIC waves near the Earth's magnetopause, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21818, https://doi.org/10.5194/egusphere-egu2020-21818, 2020.

EGU2020-509 | Displays | ST2.4

Kinetic-scale plasma turbulence evolving in the magnetosheath: case study

Liudmila Rakhmanova, Maria Riazantseva, Georgy Zastenker, and Yuri Yermolaev

Large set of in-situ measurements with high time resolution in the Earth's magnetosheath provides a great opportunity to explore influence of kinetic processes on the turbulent cascade in the collisionless plasma. Recent statistical studies reveal dependence of characteristics of the turbulent spectra on position of the viewing point behind the bow shock. Detailed analysis of dynamics of the turbulence inside the magnetosheath requires a case study prepared in several points. Present study deals with in-situ measurements of kinetic-scale fluctuations in two points located close to one stream line in different parts of the magnetosheath. We analyze fluctuation spectra of ion flux value and magnetic field magnitude in the frequency range 0.01-2 Hz obtained simultaneously from Spektr-R and Themis spacecraft. The range of frequencies corresponds to transition from magnetohydrodynamic range of scales to the scales where kinetic effects become dominant. We demonstrate deviation of turbulent cascade from the shape predicted typically by the models of developed turbulence in the vicinity of the bow shock and in the subsolar magnetosheath. We show the recovery of the spectral shape during plasma propagation toward the tail. Also, we consider influence of the upstream solar wind conditions on the evolution of turbulence in the magnetosheath.

How to cite: Rakhmanova, L., Riazantseva, M., Zastenker, G., and Yermolaev, Y.: Kinetic-scale plasma turbulence evolving in the magnetosheath: case study, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-509, https://doi.org/10.5194/egusphere-egu2020-509, 2020.

EGU2020-20941 | Displays | ST2.4

Minor Ion and Electron Characteristics within Magnetosheath Flux Transfer Events Observed by the Magnetospheric Multiscale Mission

Steven Petrinec, James Burch, Michael Chandler, Charlie Farrugia, Stephen Fuselier, Barbara Giles, Roman Gomez, Joey Mukherjee, William Paterson, Christopher Russell, David Sibeck, Robert Strangeway, Roy Torbert, Karlheinz Trattner, Sarah Vines, and Cong Zhao

Several dayside magnetosheath flux transfer events (FTEs) have been observed at high temporal resolution by the four-spacecraft MMS mission. In this study, we examine ion energy spectrograms, ion moments, and ion distribution functions for several long duration magnetosheath FTEs observed by MMS. For these cases, the spacecraft were positioned at similar locations (i.e., south of the equatorial plane, post-noon local time sector). The ion observations are placed in context with electron energy spectrograms parallel and anti-parallel to the observed magnetic field and the location of MMS relative to the predicted reconnection line location as determined from convected solar wind conditions. This combined set of observations provide important information on the formation, topologies, and evolution of FTEs.

How to cite: Petrinec, S., Burch, J., Chandler, M., Farrugia, C., Fuselier, S., Giles, B., Gomez, R., Mukherjee, J., Paterson, W., Russell, C., Sibeck, D., Strangeway, R., Torbert, R., Trattner, K., Vines, S., and Zhao, C.: Minor Ion and Electron Characteristics within Magnetosheath Flux Transfer Events Observed by the Magnetospheric Multiscale Mission, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-20941, https://doi.org/10.5194/egusphere-egu2020-20941, 2020.

EGU2020-15878 | Displays | ST2.4 | Highlight

MMS Observations of FTE-Type Structures with Internal Magnetic Reconnection

Rungployphan Kieokaew, Benoit Lavraud, and Naïs Fargette

A bipolar magnetic variation Bn with enhanced core and total fields in spacecraft data are recognized as a Flux Transfer Event (FTE) signature, which corresponds to the passage of a magnetic flux rope structure. Recent literature reported Magnetospheric Multiscale (MMS) observations of FTE signatures with magnetic reconnection signatures at the central current sheet. Among reported cases, electron pitch angle distributions (ePAD) in the suprathermal energy range show different features on either side of the reconnecting current sheet, indicating different magnetic connectivities. This structure is interpreted as interlinked/interlaced flux tubes, possibly formed by converging jets toward the central current sheet that in turn enhance magnetic flux pile-up and facilitate reconnection at the current sheet separating the two flux tubes. By surveying similar events using MMS data, we found some FTE-type structures with reconnection signatures at the central current sheet but with homogeneous ePAD of suprathermal electrons across the structures. Thus, these structures are inconsistent with interlinked flux tubes, but rather a regular flux rope. This leads to a question of how reconnection can occur in those single flux ropes, and their relation with interlinked flux tubes. In this work, we investigate properties of these structures and their related upstream solar-wind conditions. Formation mechanisms of such structures and how reconnection can occur will be discussed.

How to cite: Kieokaew, R., Lavraud, B., and Fargette, N.: MMS Observations of FTE-Type Structures with Internal Magnetic Reconnection, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-15878, https://doi.org/10.5194/egusphere-egu2020-15878, 2020.

EGU2020-7452 | Displays | ST2.4 | Highlight

Effect of whistler precursor waves on energy dissipation in supercritical quasi-perpendicular collisionless shocks.

Ahmad Lalti, Yuri Khotyaintsev, Daniel Graham, Andris Vaivads, Andreas Johlander, Roy Torbert, Barbara Giles, Chris Russell, and Jim Burch

The process of transforming the bulk kinetic energy of solar wind into the random motion of the plasma particles is still an open question. One of the proposed mechanisms for energy dissipation in such shocks is wave-particle interactions. Specifically reflected ions at the foot of the shock could interact with the solar wind plasma in an unstable way causing an increase in the temperature of the upstream plasma. Phase standing Whistler precursor waves upstream of the shock front could play a major role in enhancing energy dissipation. We analyze multiple shock crossing events encountered by the Magnetospheric Multiscale (MMS) multi-spacecraft Mission, with Alfvenic Mach numbers around 4 and a θBn around 80 degrees. We use these events to study the effect of such waves on energy dissipation at quasi perpendicular shocks.  Using spectral analysis and by calculating the poynting flux of the waves, we investigate the upstream shock energy transport by whistler waves, then we discuss the consequences of these results on the wave particle interaction as a mechanism for stabilizing such high Mach number shocks.

How to cite: Lalti, A., Khotyaintsev, Y., Graham, D., Vaivads, A., Johlander, A., Torbert, R., Giles, B., Russell, C., and Burch, J.: Effect of whistler precursor waves on energy dissipation in supercritical quasi-perpendicular collisionless shocks., EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7452, https://doi.org/10.5194/egusphere-egu2020-7452, 2020.

EGU2020-7680 | Displays | ST2.4

Electron anisotropy driven by kinetic Alfven waves in the Earth magnetotail

Alexander Lukin, Anton Artemyev, Evgeny Panov, Anatoly Petrukovich, and Rumi Nakamura

Thermal and subthermal electron populations in the Earth’s magnetotail is usually characterized by pronounced field-aligned anisotropy that contributes to generation of strong electric currents within the magnetotail current sheet. Formation of this anisotropy requires electron field-aligned acceleration, and thus likely involves field-aligned electric fields. Such fields can be carried by various electromagnetic waves generated by fast plasma flows interacting with ambient magnetotail plasma. In this presentation we consider one of the most intense observed wave emissions, kinetic Alfven waves, that accompany all fast plasma flows in the magnetotail.

Using two tail seasons (2018, 2019) of MMS observations we have collected statistics of 80 fast plasma flows (or BBF) events with distinctive enhancement of intensity of broadband electromagnetic waves sharing properties of kinetic Alfven waves. We show that a direct correlation the intensity of electric fields of kinetic Alfven waves and electron anisotropy distribution: the parallel electron anisotropy significantly increases with magnitude of the wave parallel electric field. The energy range of this electron anisotropic population is well within the range of resonant energies for observed kinetic Alfven waves. Our results show that kinetic Alfven waves can significantly contribute to shaping the magnetotail electron population.

How to cite: Lukin, A., Artemyev, A., Panov, E., Petrukovich, A., and Nakamura, R.: Electron anisotropy driven by kinetic Alfven waves in the Earth magnetotail, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7680, https://doi.org/10.5194/egusphere-egu2020-7680, 2020.

EGU2020-8260 | Displays | ST2.4

Observations of Magnetotail Interchange Heads' Signatures at Later Stage of Development

Evgeny V. Panov, San Lu, and Philip L. Pritchett

How to cite: Panov, E. V., Lu, S., and Pritchett, P. L.: Observations of Magnetotail Interchange Heads' Signatures at Later Stage of Development, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-8260, https://doi.org/10.5194/egusphere-egu2020-8260, 2020.

EGU2020-11967 | Displays | ST2.4

Electron holes in the Earth's magnetotail current sheet: role of magnetic field gradients and electron anisotropy

Pavel Shustov, Ilya Kuzichev, Ivan Vasko, Anton Artemyev, and Anatoliy Petrukovich

Electron holes are nonlinear electrostatic structures that are often observed in the vicinity of the magnetotail energy release regions, e.g. magnetic reconnection. In this work we develop 1.5D Vlasov code simulations of the electron hole dynamics in the magnetic field configuration typical of the current sheet of the Earth's magnetotail. We consider the propagation of electron holes along magnetic field lines in the inhomogeneous magnetic field of the current sheet with realistically anisotropic electron distribution function. We demonstrate that electron holes generated near the equatorial plane of the current sheet brake as they propagate toward the boundaries of the current sheets. This effect is stronger for higher magnetic field gradient and larger electron field-aligned anisotropy. These simulations demonstrate that slow electron holes observed in the plasma sheet boundary layer may appear due to that effect of electron hole braking.

How to cite: Shustov, P., Kuzichev, I., Vasko, I., Artemyev, A., and Petrukovich, A.: Electron holes in the Earth's magnetotail current sheet: role of magnetic field gradients and electron anisotropy, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11967, https://doi.org/10.5194/egusphere-egu2020-11967, 2020.

EGU2020-18357 | Displays | ST2.4

MMS/Cluster joint measurements at the vicinity of the plasma sheet boundary layer

Olivier Le Contel, Alessandro Retino, Alexandra Alexandrova, Thomas Chust, Konrad Steinvall, Soboh Alqeeq, Patrick Canu, Dominique Fontaine, iannis Dandouras, Christopher Carr, Sergio Toledo, Andrew Fazakerley, Natasha Doss, Stefan Kiehas, Rumi Nakamura, Yuri Khotyaintsev, Frederick Wilder, Narges Ahmadi, Daniel Gershman, and Robert Strangeway and the Cluster/MMS team

On 28th of August 2018 at 5:30 UT, MMS and Cluster were located in the magnetotail at about 16 earth radii (RE). They both suddenly crossed plasma interfaces. Located in the post midnight sector, Cluster transitioned from a cold plasma sheet to a hot plasma sheet whereas MMS, located at 4 RE duskward of Cluster, transitioned from a similar cold plasma sheet to the lobe region via a very short period in a hot plasma sheet. At 05:50 UT MMS returned to a hot plasma sheet and detected a quasi-parallel earthward flow ~ 400 km/s and increased energetic ion and electron fluxes. We use measurements from both missions during this conjunction to describe the possible macroscale evolution of the magnetotail as well as some associated kinetic processes. In particular, we analyze fast and slow non linear electrostatic waves propagating tailward which are detected in the so called electron boundary layer as well as in the hot plasma sheet. We discuss their possible generation mechanisms and link with the large scale evolution of the magnetotail. Finally, we investigate possible effects related to the dawn-dusk asymmetry of the magnetotail.

How to cite: Le Contel, O., Retino, A., Alexandrova, A., Chust, T., Steinvall, K., Alqeeq, S., Canu, P., Fontaine, D., Dandouras, I., Carr, C., Toledo, S., Fazakerley, A., Doss, N., Kiehas, S., Nakamura, R., Khotyaintsev, Y., Wilder, F., Ahmadi, N., Gershman, D., and Strangeway, R. and the Cluster/MMS team: MMS/Cluster joint measurements at the vicinity of the plasma sheet boundary layer, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18357, https://doi.org/10.5194/egusphere-egu2020-18357, 2020.

EGU2020-19750 | Displays | ST2.4

Analysis of energy conversion processes at kinetic scales associated with a series of dipolarization fronts observed by MMS during a substorm

Soboh Alqeeq, Olivier Le Contel, Patrick Canu, Alessandro Retino, Thomas Chust, and Laurent Mirioni and the MMS team

In July 2017, the MMS constellation was in the magnetotail with an apogee of 25 Earth radii
and an average inter-satellite distance of 10 km (i.e. at electron scales). On 23 July around
16:19 UT, MMS was located at the edge of the current sheet which was in a quasi-static
state. Then, MMS suddenly entered in the central plasma sheet and detected the local onset
of a small substorm as indicated by the AE index (~400 nT). Fast earthward plasma flows
were measured for about 1 hour starting with a period of quasi-steady flow and followed by
a saw-tooth like series of fast flows associated with dipolarization fronts. This plasma
transport sequence finished with a flow reversal still occurring close to the magnetic
equator. In the present study, we investigate the energy conversion processes at ion and
electron scales for these different phases with particular attention on the processes in the
vicinity of the dipolarization fronts.

How to cite: Alqeeq, S., Le Contel, O., Canu, P., Retino, A., Chust, T., and Mirioni, L. and the MMS team: Analysis of energy conversion processes at kinetic scales associated with a series of dipolarization fronts observed by MMS during a substorm, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-19750, https://doi.org/10.5194/egusphere-egu2020-19750, 2020.

ST2.5 – Global magnetospheric dynamics in simulations and observations

EGU2020-5502 | Displays | ST2.5

How does the magnetosphere go to sleep?

Therese Moretto Jorgensen, Michael Hesse, Lutz Rastaetter, Susanne Vennerstrom, and Paul Tenfjord

Energy and circulation in the Earth’s magnetosphere and ionosphere are largely determined by conditions in the solar wind and interplanetary magnetic field. When the driving from the solar wind is turned off (to a minimum), we expect the activity to die down but exactly how this happens is not known.  Utilizing global MHD modelling, we have addressed the questions of what constitutes the quietest state for the magnetosphere and how it is approached following a northward turning in the IMF that minimizes the driving. We observed an exponential decay with a decay time of about 1 hr in several integrated parameters related to different aspects of magnetospheric activity, including the total field-aligned current into and out of the ionosphere.  The time rate of change for the cessation of activity was also measured in total field aligned current estimates from the AMPERE project, adding observational support to this finding.  Events of distinct northward turnings of the interplanetary magnetic field were identified, with prolonged periods of stable southward driving conditions followed by northward interplanetary magnetic field conditions. A well-defined exponential decay could be identified in the total hemispheric field-aligned current following the northward turning with a generic decay constant of 0.9, corresponding to an e-folding time of 1.1 hr. A possible physical explanation for the exponential decay follows from considering what needs to happen for the convection in the magnetosphere to slow down, or stop, namely the unwinding of the field-aligned current carrying flux tubes in the coupled magnetosphere-ionosphere system. A statistical analysis of the ensemble of events also reveals both a seasonal and a day/night variation in the decay parameter, with faster decay observed in the winter than in the summer hemisphere and on the nightside than on the dayside. These results can be understood in terms of stronger/weaker line tying of the ionospheric foot points of magnetospheric field lines for higher/lower conductivity.  Additional global modeling results with varying conductance scenarios for the ionosphere confirm this interpretation.   

How to cite: Moretto Jorgensen, T., Hesse, M., Rastaetter, L., Vennerstrom, S., and Tenfjord, P.: How does the magnetosphere go to sleep?, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5502, https://doi.org/10.5194/egusphere-egu2020-5502, 2020.

EGU2020-3023 | Displays | ST2.5

Hybrid-Vlasov simulation of auroral proton precipitation in the cusps: Comparison of northward and southward interplanetary magnetic field driving

Maxime Grandin, Lucile Turc, Markus Battarbee, Urs Ganse, Andreas Johlander, Yann Pfau-Kempf, Maxime Dubart, and Minna Palmroth

We present the first hybrid-Vlasov simulations of proton precipitation in the polar cusps. We use two runs from the Vlasiator model to compare cusp proton precipitation fluxes during southward and northward interplanetary magnetic field (IMF) driving. The simulations reproduce well-known features of cusp precipitation, such as a reverse dispersion of precipitating proton energies, with proton energies increasing with increasing geomagnetic latitude under northward IMF driving, and a nonreversed dispersion under southward IMF driving. The cusp location is also found more poleward in the northward IMF simulation than in the southward IMF simulation. In addition, we find that the precipitation takes place in the form of successive bursts during southward IMF driving, those bursts being associated with the transit of flux transfer events in the vicinity of the cusp. In the northward IMF simulation, dual lobe reconnection takes place. As a consequence, in addition to the high-latitude precipitation footprint associated with the lobe reconnection from the same hemisphere, we observe lower-latitude precipitating protons which originate from the opposite hemisphere’s lobe reconnection site. The proton velocity distribution functions along the newly closed dayside magnetic field lines exhibit multiple proton beams travelling parallel and antiparallel to the magnetic field direction, which is consistent with observations with the Cluster spacecraft. We suggest that precipitating protons originating from the opposite hemisphere’s lobe reconnection site, albeit infrequent, could be observed in a situation of dual lobe reconnection.

How to cite: Grandin, M., Turc, L., Battarbee, M., Ganse, U., Johlander, A., Pfau-Kempf, Y., Dubart, M., and Palmroth, M.: Hybrid-Vlasov simulation of auroral proton precipitation in the cusps: Comparison of northward and southward interplanetary magnetic field driving, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3023, https://doi.org/10.5194/egusphere-egu2020-3023, 2020.

EGU2020-10877 | Displays | ST2.5

Imaging the Earth’s magnetic environment in soft X-rays with SMILE

Graziella Branduardi-Raymont, Steve Sembay, Tianran Sun, Hyunju Connor, and Andrey Samsonov

It is a relatively recent discovery that charge exchange soft X-ray emission is produced in the interaction of solar wind high charge ions with neutrals in the Earth’s exosphere; this has led to the realization that imaging this emission will provide us with a global and novel way to study solar-terrestrial interactions.

In particular X-ray imaging will provide us with the means of establishing the location of the magnetopause and the morphology of the magnetospheric cusps. Variations of the magnetopause standoff distance indicate global magnetospheric compressions and expansions, both in response to solar wind variations and internal magnetospheric processes.

Soft X-ray imaging is one of the main objectives of SMILE (Solar wind Magnetosphere Ionosphere Link Explorer), a joint space mission by ESA and the Chinese Academy of Sciences, which is under development and is due for launch in 2023. This presentation will introduce the scientific aims of SMILE, show simulations of the expected images to be returned by SMILE’s Soft X-ray Imager for different solar wind conditions, and will discuss some of the techniques that will be applied in order to extract the positions of the Earth’s magnetic boundaries, such as the magnetopause standoff distance.

How to cite: Branduardi-Raymont, G., Sembay, S., Sun, T., Connor, H., and Samsonov, A.: Imaging the Earth’s magnetic environment in soft X-rays with SMILE, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-10877, https://doi.org/10.5194/egusphere-egu2020-10877, 2020.

EGU2020-19932 | Displays | ST2.5

On the origins of an explicit IMF By dependence on solar wind - magnetosphere coupling

Jone Peter Reistad, Anders Ohma, Karl Magnus Laundal, Therese Moretto, Steve Milan, and Nikolai Østgaard

Presently, all empirical coupling functions quantifying the solar wind - magnetosphere energy- or magnetic flux conversion, assume that the coupling is independent of the sign of the dawn-dusk component (By) of the Interplanetary Magnetic Field (IMF). In this paper we present observations strongly suggesting an explicit IMF By effect on the solar wind - magnetosphere coupling. When the Earth's dipole is tilted in the direction corresponding to northern winter, positive IMF By is found to on average lead to a larger polar cap than when IMF By is negative during otherwise similar conditions. This explicit IMF By effect is found to reverse when the Earth's dipole is inclined in the opposite direction (northern summer), and is consistently observed from both hemispheres using the Active Magnetosphere and Planetary Electrodynamics Response Experiment (AMPERE) to infer the size of the region 1/2 current system. Two interpretations are presented: 1) The dayside reconnection rate is affected by the combination of dipole tilt and IMF By sign in a manner explaining the observations 2) The combination of dipole tilt and IMF By sign affect the global conditions for maintaining a given nightside reconnection rate. The observations as well as idealized magnetohydrodynamic (MHD) model runs are analyzed and discussed in light of the two different interpretations in order to enhance our understanding of this explicit IMF By effect.

How to cite: Reistad, J. P., Ohma, A., Laundal, K. M., Moretto, T., Milan, S., and Østgaard, N.: On the origins of an explicit IMF By dependence on solar wind - magnetosphere coupling, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-19932, https://doi.org/10.5194/egusphere-egu2020-19932, 2020.

EGU2020-2591 | Displays | ST2.5 | Highlight

Substorm onset latitude and the steadiness of magnetospheric convection

Steve Milan, Jenny Carter, Maria-Theresia Walach, Harneet Sangha, and Brian Anderson

We study the role of substorms and steady magnetospheric convection (SMC) in magnetic flux transport in the magnetosphere, using observations of field-aligned currents (FACs) by the Active Magnetosphere and Planetary Electrodynamics Response Experiment (AMPERE).  We identify two classes of substorm, with onsets above and below 65o magnetic latitude, which display different nightside FAC morphologies.  We show that the low-latitude onsets develop a poleward-expanding auroral bulge, and identify these as substorms that manifest ionospheric convection-braking in the auroral bulge region.  We show that the high-latitude substorms, which do not experience braking, can evolve into SMC events if the interplanetary magnetic field (IMF) remains southwards for a prolonged period following onset.  Our results provide a new explanation for the differing modes of response of the terrestrial system to solar wind-magnetosphere-ionosphere coupling, as understood in the context of the expanding/contracting polar cap paradigm, by invoking friction between the ionosphere and atmosphere.

How to cite: Milan, S., Carter, J., Walach, M.-T., Sangha, H., and Anderson, B.: Substorm onset latitude and the steadiness of magnetospheric convection, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2591, https://doi.org/10.5194/egusphere-egu2020-2591, 2020.

The presence of heavy ions has a profound impact on the temporal response of the magnetosphere to internal and external forcing, and plays a key role in plasma entry and transport processes within the terrestrial magnetosphere.

Numerous studies focused on the transport and energization of O+ through the ionosphere-magnetosphere system; however, relatively few have considered the contribution of N+ to the near-Earth plasma, even though past observations have established that N+ is a significant ion species in the ionosphere and its presence in the magnetosphere is significant. In spite of only 12% mass difference, N+ and O+ have different ionization potentials, scale heights and charge exchange cross sections. The latter, together with the geocoronal density distribution, plays a significant role in the formation of ENAs, which in turn controls the energy budget of the inner magnetosphere, and the overall loss of the ring current. Therefore, the outflow of N+ from the ionosphere, in addition to that of O+, affects the global structure and properties of the current sheet, the mass loading of the magnetosphere, and it leads to changes in the local properties of the plasma, which in turn can influence waves propagation.

 

This study involves an integrated computational view of geospace, that solves and tracks the evolution of all relevant ion species, to systematically assess their regional and global influence on the various loss and acceleration mechanisms operating throughout the terrestrial magnetosphere. We employ the newly developed Seven Ion Polar Wind Outflow Model (7iPWOM), which in addition to tracking the transport of H+, He+ and O+, now solves for the heating and transport of N+, N2+, NO+ and O2+ in Earth’s polar wind. The 7iPWOM is coupled with a two-stream model of superthermal electrons (GLobal airglow, or GLOW) to account for the attenuated radiation, electron beam energy dissipation, and secondary electron impact. We show that during various solar conditions, the polar wind outflow solution using 7iPWOM improves significantly when compared with OGO observations.

 

In addition, numerical simulations using the kinetic drift Hot Electron Ions Drift Integrator (HEIDI) model suggest that the contribution of outflowing N+ to the ring current dynamics is significant, as the presence of N+alters the development and the decay rate of the ring current. Electron transfer collisions are far more efficient at removing N+ the system, compared with the removal of O+ ions. Synthetic TWINS-like mass separated ENA images show that the presence on nitrogen ions in the ring current, even in small amounts, significantly alters the ENA fluxes, and the peak of oxygen ENA fluxes can vary for up to an order of magnitude, depending on the magnetosphere composition. These findings can explain recent observations of faster than expected decay of high energy oxygen ions, as measured by the RBSPICE instrument on board of the Van Allen Probe spacecraft. We speculate that the abundance of oxygen has been mis-estimated, as it is likely that some of the oxygen measurements to actually be include comparable abundances of nitrogen ions.

How to cite: Ilie, R., Lin, M.-Y., Glocer, A., and Bashir, M. F.: Tracking the Differential Transport and Acceleration of Nitrogen and Oxygen Ions from the Terrestrial Ionosphere to the Inner Magnetosphere , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-10158, https://doi.org/10.5194/egusphere-egu2020-10158, 2020.

EGU2020-8824 | Displays | ST2.5

Plasmoid releases in the Saturn's magnetosphere

Emmanuel Chané

In this work, the interactions between the solar wind and the magnetosphere of Saturn are studied via state-of-the-art global MHD simulations, focusing on the release of plasmoids in the magnetotail. We analyze in detail the occurrence rate, the size, the speed and the evolution of the plasmoids in the simulations and compare the results with in-situ measurements. In our simulations, the multi-species three-dimensional MHD equations are solved with the code MPI-AMRVAC on a spherical non-uniform mesh ranging from 3 Rs (inner boundary) to 200 Rs (outer boundary). In order to simulate the magnetosphere-ionosphere coupling, to accelerate the ionospheric plasma up to rigid corotation and to close the electrical current systems, ion-neutral collisions are introduced in the MHD equations in the ionospheric region near the inner boundary. The strong mass-loading associated with the moon Enceladus is also included as an axisymmetric torus centered at 5.5 Rs.

How to cite: Chané, E.: Plasmoid releases in the Saturn's magnetosphere, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-8824, https://doi.org/10.5194/egusphere-egu2020-8824, 2020.

EGU2020-5163 | Displays | ST2.5

Dependence of magnetopause reconnection events on interplanetary parameters

Walter Gonzalez and Daiki Koga

Magnetic reconnection permits topological rearrangements of the interplanetary and magnetospheric magnetic fields and the entry of solar wind mass, energy, and momentum into the magnetosphere. Thus, magnetic reconnection is a key issue to understand space weather. However, it hasnot been fully understood yet under which interplanetary/magnetosheath conditions magnetic reconnection takes place more effectively at the dayside magnetopause. For this purpose,  in the present study 25 dayside magnetopause reconnection events are investigated using the Time History of Events and Macroscale Interactions during Substorms ( THEMIS ) spacecraft  observations. It was found, (1) that the reconnection electric field is proportional to the interplanetary electric field, (2) that the reconnection electric field is inversely proportional to the solar wind-Alfvén Mach number,  (3) that thereconnection outflow speed is proportional to the solar wind Alfvén speed, and (4) that the reconnection outflow speed is  inversely proportional to the magnetosheath plasma beta. Finally, it is shown that the range of magnetic shear angles for which magnetic reconnection should occur is restricted to large shears as the magnetosheath flow direction becomes more perpendicular to the direction of the local magnetopause normal vector. Since these results refer to fairly typical solar wind-Alfvén Mach number condition, they may not apply to more extreme cases.

How to cite: Gonzalez, W. and Koga, D.: Dependence of magnetopause reconnection events on interplanetary parameters, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5163, https://doi.org/10.5194/egusphere-egu2020-5163, 2020.

EGU2020-6780 | Displays | ST2.5

Spatial resolution dependence of ion-scale waves in a global-hybrid Vlasov simulation

Maxime Dubart, Urs Ganse, Adnane Osmane, Markus Battarbee, Maxime Grandin, Andreas Johlander, Yann Pfau-Kempf, Lucile Turc, and Minna Palmroth

Plasma waves are ubiquitous in the Earth's magnetosheath. The most observed waves arise from instabilities generated by temperature anisotropy on the ions and electrons, such as the mirror and proton cyclotron instabilities. Along with observations, space physics is increasingly relying on the support of numerical simulations to understand these waves and instabilities. However, numerical simulations come with resolution limitations. We investigate here the spatial resolution dependence of the mirror and proton cyclotron instabilities in a global-hybrid Vlasov simulation with the use of the Vlasiator model. We compare the proton velocity distribution functions, power spectrum and growth rate of the instabilities in a simulation with three different spatial resolutions. We find that the proton cyclotron instability is absent at the lowest resolution and that the mirror instability is dominating, increasing the overall temperature anisotropy of the simulation. We also conducted a test at higher resolution and found out that this does not improve the description of the proton cyclotron instability significantly enough to justify this increase in resolution at the cost of numerical resources in future simulations. These results will be used for a future sub-grid model in order to mimic the energy dissipation processes at work at smaller scales without increasing the resolution of the simulation.

How to cite: Dubart, M., Ganse, U., Osmane, A., Battarbee, M., Grandin, M., Johlander, A., Pfau-Kempf, Y., Turc, L., and Palmroth, M.: Spatial resolution dependence of ion-scale waves in a global-hybrid Vlasov simulation, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6780, https://doi.org/10.5194/egusphere-egu2020-6780, 2020.

 CLUSTER experimental observations of  Lavraud et al. (2005) have evidenced the presence of a particular layer (so –called herein Alfven Transition Layer or ATL) almost adjacent to the upper edge of the stagnant exterior cusp (SEC), through which the plasma flow transits from super-(from magnetosheath) to sub- (to SEC) Alfvenic regime as the interplanetary magnetic field (IMF) is northward. Three dimensional globa PIC simulations have been recently used  (Cai et al., 2015) to analyze the main features of the cusp for an IMF configuration similar that in the observations. These simulations have allowed us to complete the global view of the cusp region  (in particular the features not accessible by MHD approach).  A  detailed analysis has allowed to retrieve the features of the ATL which reveals to be associated to the complicated 3D particles entry into the cusp region and exhibit an internal conic depletion region (CDR) where the ion fluxes concentrate and are very strong (which suggests very local ion precipitation). Moreover, simulation results show that the ATL expands towards areas out and even far from the cusp region and outside the meridian plane.

                     In the present work, the study is extended for different Ma regimes of the solar wind, as the IMF stays in northward  configuration. Results show the impact of this Ma variation on the 3D features of the overall magnetosphere and in particular on the cusp region, i.e. (i) on the 3D ATL structures/spatial scales, (ii) on the extension of the region surrounded by the ATL, and (iii) on the structures, the spatial scales and the dynamics of the CDR itself.

 

 

How to cite: Cai, D. and Lembege, B.: Impact of the low/high Alfven Mach number regime of the solar wind on the Aflven transition Layer of the cusp for IMF North: 3D global PIC simulation., EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3870, https://doi.org/10.5194/egusphere-egu2020-3870, 2020.

EGU2020-16461 | Displays | ST2.5

Timescales of Ionospheric Field-Aligned Currents during a Geomagnetic Storm: Global Magnetospheric Simulations

Joseph Eggington, John Coxon, Robert Shore, Ravindra Desai, Lars Mejnertsen, Jonathan Eastwood, and Jeremy Chittenden

Geomagnetic storms generate a complex and highly time-dependent response in the magnetosphere-ionosphere system. Enhancement in field-aligned currents (FACs) can be very localised, and so accurately predicting the stormtime response of the ionosphere is crucial in forecasting the potential impacts of a severe space weather event at a given location on the Earth. Global MHD simulations provide a means to model ionospheric conditions in real-time for a given geomagnetic storm, allowing direct comparison to space- and ground-based observations from which the observations can be placed in global context to better understand the physical drivers behind the system's response.                   

Using the Gorgon MHD code and driving with upstream data from the ACE spacecraft, we simulate the state of the magnetosphere-ionosphere system during a geomagnetic storm commencing on 3rd May 2014. To elucidate the characteristic timescales of the system response during this event, we adopt a novel approach originally applied by Shore et al. (2019) to ground magnetic field data from SuperMAG, and by Coxon et al. (2019) to FAC data from AMPERE. In this method the simulated FAC at each point on the ionospheric grid is cross-correlated with solar wind time-series for time lags of up to several hours, and the lag with the strongest correlation is identified.

From this we construct maps of the characteristic response timescale and strength of correlation in the ionosphere to IMF By and Bz, and interpret these results in terms of the varying stormtime FAC morphology by comparing the simulation results to observations by AMPERE and SuperMAG during this same event. Finally, we identify sources of asymmetry in the ionospheric response, such as that between day/night and north/south, relating these to asymmetries in magnetospheric dynamics such as magnetopause and magnetotail reconnection, and changes in global convection as the system reconfigures. This will reveal the importance of different aspects of magnetosphere-ionosphere system in influencing the coupling timescales, as well as the role of onset time in determining the potential impacts of a severe event.

References:

Shore, R. M., Freeman, M. P., Coxon, J. C., Thomas, E. G., Gjerloev, J. W., & Olsen, N. (2019). Spatial variation in the responses of the surface external and induced magnetic field to the solar wind. Journal of Geophysical Research: Space Physics, 124. https://doi.org/10.1029/2019JA026543

Coxon, J. C., Shore, R. M., Freeman, M. P., Fear, R. C., Browett, S. D., Smith, A. W., et al. (2019). Timescales of Birkeland currents driven by the IMF. Geophysical Research Letters, 46, 7893– 7901. https://doi.org/10.1029/2018GL081658

How to cite: Eggington, J., Coxon, J., Shore, R., Desai, R., Mejnertsen, L., Eastwood, J., and Chittenden, J.: Timescales of Ionospheric Field-Aligned Currents during a Geomagnetic Storm: Global Magnetospheric Simulations, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-16461, https://doi.org/10.5194/egusphere-egu2020-16461, 2020.

EGU2020-20250 | Displays | ST2.5

How tail reconnection affects the asymmetric state of the magnetosphere in the LFM model

Anders Ohma, Nikolai Østgaard, Jone Peter Reistad, Karl M. Laundal, and Paul Tenfjord

The IMF By component is a source of numerous asymmetric features in our magnetospheric system, e.g. north-south asymmetries in the aurora, the magnetospheric and ionospheric current systems and the plasma convection. Several recent studies have shown that asymmetries in the lobe pressure play a major role in inducing these asymmetries. It has also been reported that enhanced tail reconnection affects the dynamics of the system by reducing the north-south asymmetries imposed by the IMF. A possible interpretation of these observations is that enhanced reconnection in the near-Earth tail reduces the pressure in the lobes and thus suppresses the cause of the initial asymmetry. In this study, we present the results from global MHD simulations using the LFM model to further investigate how enhanced tail reconnection affects the asymmetric state of the system. A relaxation of the asymmetry in the closed magnetosphere is seen in the model when the reconnection rate in the tail increases, consistent with observations, and we use the simulation output to gain further insight into the physical mechanism(s) responsible for the return to a more symmetric state.

How to cite: Ohma, A., Østgaard, N., Reistad, J. P., Laundal, K. M., and Tenfjord, P.: How tail reconnection affects the asymmetric state of the magnetosphere in the LFM model, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-20250, https://doi.org/10.5194/egusphere-egu2020-20250, 2020.

EGU2020-22329 | Displays | ST2.5

Solar wind-magnetosphere coupling in the form of recurrent substorms with one-hour periodicity

Andreas Keiling, Masahito Nosé, and Vassillis Angelopoulos

The magnetospheric substorm is a response mode of the magnetosphere to solar wind driving. It has been shown that substorms can show repetitive behavior (that is, three or more substorms following each other with a quasi-period). The most common period is approximately three hours. A conclusive and satisfactory answer to the cause of this periodicity has not yet been given. Very limited mentioning of a shorter recurrence period, namely around one hour, has sparsely been appeared in the literature. In this presentation, we report on this lesser studied periodicity, giving observational examples from the THEMIS fleet. We compare the observations with global magnetosphere MHD simulations (BATS-R-US) of solar wind-magnetosphere coupling that incorporate kinetic corrections at the reconnection site. The similarity is striking, suggesting that indeed kinetic effects in tail reconnection are responsible - at least in some cases - for this periodic behavior of the magnetosphere.

How to cite: Keiling, A., Nosé, M., and Angelopoulos, V.: Solar wind-magnetosphere coupling in the form of recurrent substorms with one-hour periodicity, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-22329, https://doi.org/10.5194/egusphere-egu2020-22329, 2020.

Understanding the transport of hot plasma from tail towards the inner magnetosphere is of great importance to improve our perception of the near-Earth space environment. In accordance with the recent observations, the contribution of bursty bulk flows (BBFs)/bubbles in the inner plasma sheet especially in the storm-time ring current formation is nonnegligible. These high-speed plasma flows with depleted flux tube/entropy are likely formed in the mid tail due to magnetic reconnection and injected earthward as a result of interchange instability. In this presentation, we investigate the interplay of these meso-scale structures on the average magnetic field and plasma distribution in various regions of the plasma sheet, using the Inertialized Rice Convection Model (RCM-I). We will discuss the comparison of our simulation results with the observational statistics and data-based empirical models.

How to cite: Sadeghzadeh, S. and Yang, J.: Interplay of bubble injections in the plasma sheet dynamics as inferred from RCM-I simulations, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2120, https://doi.org/10.5194/egusphere-egu2020-2120, 2020.

EGU2020-3312 | Displays | ST2.5

Vortical flow in the plasma sheet: Non-linear growth of flow burst surface wave?

Ghai Siung Chong, Alexandre De Spiegeleer, Maria Hamrin, Timo Pitkanen, Sae Aizawa, Liisa Juusola, and Laila Andersson

In contrast to the simple conventional plasma flow convection governed by the Dungey Cycle, past studies have revealed that the plasma flows in the magnetotail region are more complicated, hosting high-speed bursty and meandering vortical flows. We have utilized magnetic field and plasma data from the Cluster mission to investigate a high speed earthward propagating flow burst with a peak velocity of ~530 km/s in the magnetotail plasma sheet (XGSM ~ -17RE) on 20 September 2002. In the vicinity of this flow burst, a vortical flow, whose plasma vectors are first directed tailward then earthward, is also observed. The plasma data shows that the plasma population in the vortical flow is likely to originate from the associated flow burst. In addition, the boundaries of both structures are also found to be tangential discontinuities, clearly surrounded by the ambient slow moving plasma sheet. Inside the vortical flow, there exists a region where plasma originating from the flow burst and ambient plasma sheet are mixed. The local segment of inbound boundary crossing of the vortical flow is shown to have a thickness that is non-uniform. Coupled with the flow evolution in the vortical flow, these characteristics are consistent to a boundary crossing of a vortical flow. The magnetic field on the flow burst is quasi-perpendicular to the large velocity shear (~460 km/s) across the flow burst boundary. These results suggest that the formation of vortical flow can arise from the development and subsequent growth of flow burst boundary wave as a result of Kelvin-Helmholtz instability. In summary, this article presents a detailed observational study of a vortical flow and the formation of which would serve as the first direct observational consequence of an excited and growing flow burst boundary wave. Continuous scattering of the detached vortices may play an important role in the braking mechanism of earthward propagating flow bursts. 

How to cite: Chong, G. S., De Spiegeleer, A., Hamrin, M., Pitkanen, T., Aizawa, S., Juusola, L., and Andersson, L.: Vortical flow in the plasma sheet: Non-linear growth of flow burst surface wave?, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3312, https://doi.org/10.5194/egusphere-egu2020-3312, 2020.

EGU2020-4006 | Displays | ST2.5

Statistical Properties of Field-Aligned Currents in the Plasma Sheet Boundary Layer

Yuanqiang Chen, Mingyu Wu, Guoqiang Wang, Zonghao Pan, and Tielong Zhang

Field-aligned currents (FACs), also known as Birkeland currents, are the agents by which momentum and energy can be transferred to the ionosphere from solar wind and the magnetosphere, exhibiting a seasonal variation as that of ionospheric conductance at low altitude. By using magnetic field and plasma measurements from the Magntospheric Multiscale (MMS), we estimated the properties of the small-scale FACs in the plasma sheet boundary layer (PSBL) region. The occurrence rates of those FACs are larger near the midnight plane and near the flank region; they are also larger in the northern (summer) hemisphere than in the southern hemisphere, especially for the earthward FACs. Different distribution patterns as a function of plasma β are found for the Beam-type FACs and the Flow-type FACs (accompanied with observable perpendicular currents). The latter are closer to central plasma sheet (higher β) and their occurrence rate decreases linearly toward tail lobe (lower β), while the former mainly appear within the β range of 0.1 to 1. FAC magnitudes show little dependence on plasma β, while they would increase when approaching Earth generally. The occurrence rate and magnitude of FACs both increase from low to high geomagnetic activity, consistent with observation at ionospheric altitude. The main carriers for FACs in PSBL are thermal electrons, while cold electrons sometimes could also have contribution, especially under high geomagnetic activity. This study shows that FACs in the PSBL exhibit an asymmetry of occurrence rate between the northern and southern hemisphere and different signatures under low and high geomagnetic activity, which are consistent with FACs at ionospheric altitude. This demonstrates that FACs are significant in magnetosphere-ionosphere coupling and illustrates the possible ionospheric feedback effects to magnetosphere in the nightside.

How to cite: Chen, Y., Wu, M., Wang, G., Pan, Z., and Zhang, T.: Statistical Properties of Field-Aligned Currents in the Plasma Sheet Boundary Layer, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4006, https://doi.org/10.5194/egusphere-egu2020-4006, 2020.

EGU2020-10882 | Displays | ST2.5

Explanation of global plasmapause characteristics in the frame of interchange instability mechanism

Giuli Verbanac, Mario Bandic, and Viviane Pierrard

Recent statistical studies based on CLUSTER, CRRES, and THEMIS satellite data have provided insight into global plasmapause characteristics: start of erosion between 21-07 MLT and eastward azimuthal propagation. The observed plasmapause behavior is found to agree with the theory of the interchange instability mechanism. We present the results of the plasmapause characteristics obtained with simulations based on this mechanism.

Here we aim to obtain the same plasmapause characteristics that we previously obtained with simulations using real values of geomagnetic Kp index (which are the proxies for the convection electric field), but using synthetic Kp changes. We show that for that, completely unexpected, instead of many combinations of Kp changes occurring at different UT times (generated for instance with Monte Carlo methods), only 3 Kp jumps occurring at one UT time, leads to the same plasmapause characteristics obtained with simulations using the real Kp values. Therefore, two plasmapause datasets are constructed by setting the following input in the simulations: (a) real values of the geomagnetic Kp index, (b) certain types of time-dependent changes in the Kp (Kp jumps). The Kp jumps include sharp Kp increase, sharp Kp decrease, short time burst enhancement (increase-decrease within 3 hours) in Kp and their combinations in order to obtain plumes, shoulders, and notches, the structures most often observed in nature. The modeled plasmapause is cross-correlated with the Kp index at different 1-hour MLT bins.

We have shown that the cross-correlation curves provide deep insight into the physical processes related to the plasmapause dynamic and evolution. In single events, plasmapause may undergo complex and different dynamics. Here, we show that global plasmapause motions and deformation in time may be simply explained, at least in the statistical sense. Accordingly, we will demonstrate and discuss that three plasmapause structures and their combinations statistically leave the same imprint in the passage through a specific MLT sector as a combination of the plasmapauses created with a large number of the real Kp changes.  

How to cite: Verbanac, G., Bandic, M., and Pierrard, V.: Explanation of global plasmapause characteristics in the frame of interchange instability mechanism, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-10882, https://doi.org/10.5194/egusphere-egu2020-10882, 2020.

EGU2020-265 | Displays | ST2.5

The Plasmasphere During Major Geomagnetic Storms: Analysis Of Trapped Particles In The Outer Radiation Belt

Jessy Matar, Benoit Hubert, Stan Cowley, Steve Milan, Zhonghua Yao, Ruilong Guo, Jerry Goldstein, and Bill Sandel

The coupling between the Earth’s magnetic field and the interplanetary magnetic field (IMF) transported by the solar wind results in a cycle of magnetic field lines opening and closing generally known as the Dungey substorm cycle, mostly governed by the process of magnetic reconnection. The geomagnetic field lines can therefore have either a closed or an open topology, i.e. lower latitude field lines are closed (map from southern ionosphere to the northern), while higher latitude field lines are open (map from one polar ionosphere into interplanetary space). Closed field lines can trap electrically charged particles that bounce between mirror points located in the North and South hemispheres while drifting in longitude around the Earth, forming the plasmasphere, the radiation belts and the ring current. The outer boundary of the plasmasphere is the plasmapause. Its location is mostly driven by the interplay of the corotation electric field of ionospheric origin, and the convection electric field that results from the interaction between the IMF and the geomagnetic field. At times of prolonged intense coupling between these fields, the response of the magnetosphere becomes global and a geomagnetic storm develops. The ring current created by the motion of the trapped energetic particles intensifies and then decays as the storm abates. This study aims to find a possible relationship between the evolution of the trapped population and the process of magnetic reconnection during storm times. The EUV instrument on board the NASA-IMAGE spacecraft observed the distribution of the trapped helium ions (He+) in the plasmasphere. We consider several cases of intense geomagnetic storms observed by the IMAGE satellite. We identify the plasmapause location (Lpp) during those cases. We find a strong correlation between the Dst index and Lpp. The ring current and the trapped particles are expected to vary during storms. We use the Tsyganenko magnetic field model to map the electric potential between the Heppner-Maynard boundary (HMB) in the ionosphere and the magnetosphere and estimate the voltage and electric field in the vicinity of the plasmapause. The ionospheric electric field is deduced from the ionospheric convection velocity measured by the SuperDARN (SD) radar network at high latitudes. The tangential electric field component of the moving plasmapause boundary is estimated from IMAGE-EUV observations of the plasmasphere and is compared with expectations based on the SD data. We combine measurements of the trapped population from IMAGE-EUV and IMAGE-FUV observations of the aurora to better understand and quantify the variability of the Earth's outer radiation belt during strong storms. The auroral precipitation at ionospheric latitude is studied using FUV imaging and compared to the He+ response during the storms.

How to cite: Matar, J., Hubert, B., Cowley, S., Milan, S., Yao, Z., Guo, R., Goldstein, J., and Sandel, B.: The Plasmasphere During Major Geomagnetic Storms: Analysis Of Trapped Particles In The Outer Radiation Belt, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-265, https://doi.org/10.5194/egusphere-egu2020-265, 2020.

EGU2020-2126 | Displays | ST2.5

Spatial Distribution of Particle Precipitation in Terms of Energy Channels under Different Geomagnetic Conditions

Han-Wen Shen, Jih-Hong Shue, John Dombeck, and Hsien-Ming Li

The geomagnetic activity can modulate the number and energy fluxes of precipitation and their spatial distributions. Most previous studies examined precipitation in terms of energy spectrum types associated with quasi-static potential structures (QSPS) acceleration, Alfvénic acceleration, and wave scattering under various geomagnetic conditions. In this study, we instead categorize precipitation according to energy channels of particles. The spatial distribution of the precipitation for various energy channels is also derived under different geomagnetic conditions. Our results indicate that regardless of active and quiet times, low-energy (high-energy) precipitation is mostly distributed on the dayside (nightside). By comparing with past results, we infer that electron precipitation is mainly caused by QSPS and Alfvénic acceleration for most cases; however, the high-energy electrons during quiet times are predominantly created by wave scattering. For high-energy precipitation, the dawn-dusk asymmetry of the spatial distribution during active times is found to be opposite of that during quiet times. Based on their spatial distributions, we suggest that the high-energy precipitation during quiet times is dominated by the curvature and gradient drifts, while that during active times is mainly affected by physical processes related to substorms in the magnetotail.

How to cite: Shen, H.-W., Shue, J.-H., Dombeck, J., and Li, H.-M.: Spatial Distribution of Particle Precipitation in Terms of Energy Channels under Different Geomagnetic Conditions, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2126, https://doi.org/10.5194/egusphere-egu2020-2126, 2020.

EGU2020-7689 | Displays | ST2.5

Intense dB/dt variations driven by near-Earth Bursty Bulk Flows (BBFs): A case study

Dong Wei, Malcolm Dunlop, Junying Yang, Yiqun Yu, and Tieyan Wang

During geomagnetically disturbed times, geomagnetically induced currents (GICs) flow in power systems potentially causing damage to the system. The largest GICs are often produced when the surface geomagnetic field abruptly changes (for example, an induced rate of change of the horizontal magnetic field component, dH/dt). It is well established that intense dB/dt variations take place in the main phase of a geomagnetic storm, particularly while magnetic substorms occur during the active period. However, there are currently few studies that report intense dB/dt variations which are directly driven by bursty bulk flows (BBFs) at geosynchronous orbit. In this study, we investigate the characteristics and response in the magnetosphere-ionosphere system during the recovery phase of a geomagnetic storm that occurred on 7 January 2015 by using a multi-point approach combining space-borne Cluster and SWARM measurements, and a group of ground-based magnetometer observations. The locations of Cluster and SWARM map to the same conjugate region as the magnetometer ground stations at the time of the BBF. The measurements show that corresponding signals in all measurements occur simultaneously in this region. Our results suggest that the most intense dB/dt (dH/dt) variations are associated with R1-type FACs that are driven by BBFs at geosynchronous orbit around substorm onset.

How to cite: Wei, D., Dunlop, M., Yang, J., Yu, Y., and Wang, T.: Intense dB/dt variations driven by near-Earth Bursty Bulk Flows (BBFs): A case study, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7689, https://doi.org/10.5194/egusphere-egu2020-7689, 2020.

EGU2020-9947 | Displays | ST2.5

About determination of coordinates of sources of geomagnetic perturbations according to the world network of magnetic observatories

Beibit Zhumabayev, Ivan Vassilyev, Vladimir Protsenko, and Saltanat Zhumabayeva

A method for determining the coordinates of geomagnetic perturbation sources based on joint data processing of the world network of magnetic observatories is proposed. A large statistical material showed the relationship of large geomagnetic storms with the interaction of two or more magnetic clouds formed as a result of coronal mass ejections. To determine the coordinates of the sources of perturbations, it is proposed to use the data of magnetic observatories of the "INTERMAGNET" international network, which has more than 100 observation points distributed around the world and equipped with modern identical hardware. The results of geomagnetic field measurement obtained by magnetic observatories are brought to a single coordinate system. It was achieved by rotation of the axes of local stations, which allows determining the coordinates of the sources of perturbations and evaluating the accuracy of specifying the coordinate system of each local observatory.

How to cite: Zhumabayev, B., Vassilyev, I., Protsenko, V., and Zhumabayeva, S.: About determination of coordinates of sources of geomagnetic perturbations according to the world network of magnetic observatories, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-9947, https://doi.org/10.5194/egusphere-egu2020-9947, 2020.

EGU2020-20011 | Displays | ST2.5

Investigations on the power-law burst lifetime distribution characteristics of the magnetospheric system

Prince Prasad, Santhosh Kumar G, and Sumesh Gopinath

The waiting time distributions and associated statistical relationships can be considered as a general strategy for analyzing space weather and inner magnetospheric processes to a large extent. It measures the distribution of delay times between subsequent hopping events in such processes. In a physical system the time duration between two events is called a waiting-time, like the time between avalanches. The burst lifetime can be considered as the time duration when magnitude of fluctuations are above a given threshold intensity.  If a characteristic time scale is absent then the probability densities vary with power-law relations having a scaling exponent. The burst lifetime distribution of the substorm index called as the Wp index (Wave and planetary), which reflects Pi2 wave power at low-latitude is considered for the present analysis. Our analysis shows that the lifetime probability distributions of Wp index yield power-law exponents. Even though power-law exponents are observed in magnetospheric proxies for different solar activity periods, not many studies were made to analyze whether these features will repeat or differ depending on sunspot cycle. We compare the variations of power-law exponents of Wp index and other magnetospheric proxies, such as AE index, during solar maxima and solar minima. Thus the study classifies the activity bursts in Wp and other magnetospheric proxies that may have different dynamical critical scaling features. We also expect that the study sheds light into certain stochastic aspects of scaling properties of the magnetosphere which are not developed as global phenomena, but in turn generated due to inherent localized properties of the magnetosphere.

How to cite: Prasad, P., Kumar G, S., and Gopinath, S.: Investigations on the power-law burst lifetime distribution characteristics of the magnetospheric system , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-20011, https://doi.org/10.5194/egusphere-egu2020-20011, 2020.

The Earth's magnetosheath is luminous in the soft X-ray band, due to the solar wind charge exchange (SWCX) process. SWCX occurs when a heavy solar wind ion with a high charge state encounters with a neutral component. The heavy ion obtains an electron and gets into an excited state. It then decays to the ground state and emits a photon in the soft X-ray band. Considering that the X-ray emission from the magnetosheath is higher compared to that from the magnetosphere, information about the boundary positions can be derived from an X-ray image of the magnetosheath.

 

The solar wind - magnetosphere - ionosphere link explorer (SMILE) is a mission jointly supported by ESA and CAS, which aims at exploring the dynamics in the whole system. Soft X-ray Imager (SXI) is expected to provide X-ray images of the magnetosphere. The Modeling Working Group (MWG) is one of the four working groups of SMILE. Studies about the modeling of X-ray emissions as well as the method to derive the boundary positions are two main topics of the MWG. The main progress of MWG will be summarized here. 

How to cite: Sun, T.: Modeling the X-ray emissions from the geo-space environment , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21675, https://doi.org/10.5194/egusphere-egu2020-21675, 2020.

ST2.6 – Inner-magnetosphere Interactions and Coupling

Whistler-mode chorus emissions are generated at the equator in the parallel direction to the magnetic field, and propagate toward higher latitudes changing the wave normal angle gradually to oblique directions. Interaction between the wave and energetic electrons through Landau resonance becomes effective in the oblique propagation. As observed from the guiding center of a Landau resonant electron moving with the parallel phase velocity, the wave phase becomes stationary. With the perpendicular wave number and the deviation of the particle position from the guiding center, the electron see a wave phase of a right-handed circulary polaraized wave, which causes efficient acceleration by the perpendicular component of the wave electric field [1]. The interaction time between the resonant electron and the wave packet is maximized with the frequency close to half the cyclotron frequency, because the parallel phase velocity becomes nearly equal to the parallel group velocity. The efficient acceleration of resonant electrons causes damping of the wave at half the cyclotron frequency. Although our previous model assumed that the nonlinear wave damping was due to the parallel wave electric field in the presence of the gradient of magnetic field [2], we have confirmed that the nonlinear trapping due to the perpendicular components of the wave fields plays the major role in the electron acceleration and resultant wave damping in the nonuniform magnetic field [3]. In addition to the nonlinear damping, propagation characteristics of upper and and lower band chorus wave packets are much different. The Gendrin angle, at which the group velocity takes the parallel direction, exists only for the lower band chorus, while the group velocity of the upper band chorus takes highly oblique directions [4], and this difference enhances separation of the two bands in space. A single chorus element can be generated at the equator forming a long-lasting rising tone emission covering half the cyclotron frequency. As the wave packet propagates away from the equator, it splits into lower band and upper band wave packets because of the nonlinear damping through Landau resonance at half the cyclotron frequency, and the wave packets propagate in different directions.

References 
[1] Omura, Y., Hsieh, Y.-K., Foster, J., et al., (2019),  Cyclotron acceleration of relativistic electrons through Landau resonance with obliquely propagating whistler-mode chorus emissions, J. Geophys., Res.: Space Physics, 124, 2795–2810.
[2] Omura, Y., Hikishima, M., Katoh, Y., et al.. (2009), Nonlinear mechanisms of lower band and upper band VLF chorus emissions in the magnetosphere, J. Geophys. Res., 114, A07217.
[3] Hsieh, Y.-K., & Omura, Y. (2018), Nonlinear damping of oblique whistler mode waves via Landau resonance, J. Geophys. Res.: Space Physics,123, 7462–7472. 
[4] Hsieh, Y.-K, & Omura, Y. (2017). Study of wave-particle interactions for whistler mode waves at oblique angles by utilizing the gyroaveraging method, Radio Science, 52, 1268–1281.

How to cite: Omura, Y. and Hsieh, Y.-K.: Generation of lower band and upper band whistler-mode chorus emissions and associated electron acceleration in the inner magnetosphere, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2143, https://doi.org/10.5194/egusphere-egu2020-2143, 2020.

EGU2020-8921 | Displays | ST2.6

Ion injection triggered EMIC wave activity and its association with enhanced convection periods

Remya Bhanu, David Sibeck, Mike Ruohoniemi, Bharat Kunduri, Alexa Halford, Geoffery Reeves, and Virupakshi Reddy

Electromagnetic ion cyclotron (EMIC) waves are found to be most prevalent during geomagnetic storms and solar wind pressure pulses which provide the necessary free energy for the wave growth. However, they have also been regularly observed
in the absence of these two drivers. These non-storm time and non-pressure pulse EMIC events are very well associated with individual night side injections during substorms. However, not all substorm injections elicit wave activity. Our study aims to determine which substorm trigger wave activity. EMIC events excited during substorm injections are examined and various plasma parameters that are responsible for wave growth are studied. We find that injections that are associated with EMIC waves are also associated with enhanced high latitude ionospheric convection, which are manifestations of strong magnetospheric electric fields. The convective signatures occur at local times similar to those of the observed wave activity.

How to cite: Bhanu, R., Sibeck, D., Ruohoniemi, M., Kunduri, B., Halford, A., Reeves, G., and Reddy, V.: Ion injection triggered EMIC wave activity and its association with enhanced convection periods , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-8921, https://doi.org/10.5194/egusphere-egu2020-8921, 2020.

EGU2020-16970 | Displays | ST2.6 | Highlight

A combined neural network- and physics-based approach for modeling the plasmasphere dynamics

Irina Zhelavskaya, Nikita Aseev, Yuri Shprits, and Maria Spasojevic

Plasmasphere is a torus of cold plasma surrounding the Earth and is a very dynamic region. Its dynamics is driven by space weather. Having an accurate model of the plasmasphere is very important for wave-particle interactions and radiation belt modeling. In recent years, feedforward neural networks (NNs) have been successfully applied to reconstruct the global plasmasphere dynamics in the equatorial plane [Bortnik et al., 2016, Zhelavskaya et al., 2017, Chu et al., 2017]. These neural network-based models have been able to capture the large-scale dynamics of the plasmasphere, such as plume formation and the erosion of the plasmasphere on the night side. However, NNs have one limitation. When data is abundant, NNs perform really well. In contrast, when the coverage is limited or non-existent, as during geomagnetic storms, NNs do not perform well. The reason is that since these data are underrepresented in the training set, NNs cannot learn from the limited number of examples. This limitation can be overcome by employing physics-based modeling during such intervals. Physics-based models perform stably during high geomagnetic activity time periods if initialized and configured correctly. In this work, we show the combined approach to model the global plasmasphere dynamics that utilizes advantages of both neural network- and physics-based modeling and produces accurate global plasma density reconstruction during extreme events. We present examples of the global plasma density reconstruction for a number of extreme geomagnetic storms that occured in the past including the Halloween storm in 2003. We validate the global density reconstructions by comparing them to the IMAGE EUV images of the He+ particles distribution in the Earth’s plasmasphere for the same time periods.

How to cite: Zhelavskaya, I., Aseev, N., Shprits, Y., and Spasojevic, M.: A combined neural network- and physics-based approach for modeling the plasmasphere dynamics , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-16970, https://doi.org/10.5194/egusphere-egu2020-16970, 2020.

EGU2020-5002 | Displays | ST2.6 | Highlight

Electron Flux and Precipitation During ICME Case Studies

Harriet E. George, Emilia Kilpua, Adnane Osmane, Timo Asikainen, Craig J. Rodger, Milla Kalliokosi, and Minna Palmroth

Interplanetary coronal mass ejections (ICMEs) can dramatically affect electrons in the outer radiation belt. Electron energy flux and location varies over a range of timescales during these events, depending on ICME characteristics. This highly complex response means that electron flux within the outer radiation belt and precipitation into the upper atmosphere during ICMEs is not yet fully understood. This study analyses the electron response to two ICMEs, which occurred near the maximum of Solar Cycle 24. Both ICMEs had leading shocks and sheaths, followed by magnetic flux ropes in the ejecta. The magnetic field in these flux ropes rotated throughout the events, with opposite rotation in each event. The field rotated from south to north during the first event, while the second event had rotation from north to south. Data from Van Allen Probes were used to study electron flux variation in the outer radiation belt, while POES data were used for electron precipitation into the upper atmosphere. Qualitative analysis of these data was carried out in order to characterise the temporal and spatial variations in electron flux and precipitation throughout these two events, with particular focus on the effects of the sheath and rotating magnetic field in the ICME ejecta. In both events, we observe enhanced precipitation at mid-latitudes during the southward portion of the ejecta, with greater enhancements taking place in lower energy electron populations. By contrast, flux of outer radiation belt electron populations differs significantly between the two ICMEs, highlighting the complexity of the electron flux response to these space weather events.

How to cite: George, H. E., Kilpua, E., Osmane, A., Asikainen, T., Rodger, C. J., Kalliokosi, M., and Palmroth, M.: Electron Flux and Precipitation During ICME Case Studies, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5002, https://doi.org/10.5194/egusphere-egu2020-5002, 2020.

EGU2020-3181 | Displays | ST2.6 | Highlight

Modeling particle precipitation and effects on the ionospheric conductivity

Yiqun Yu, Xingbin Tian, Minghui Zhu, and Shreedevi Pr

Particle precipitation originated from the magnetosphere provides important energy source to the upper atmosphere, leading to ionization and enhancement of conductivity, which in turn changes the electric potential in the MI system to influence the plasma convection in the magnetosphere. In this study, we simulate ring current particle precipitation caused by several important loss mechanisms, including electron precipitation due to whistler wave scattering, ion precipitation due to EMIC wave diffusion and field line curvature scattering. These physical mechanisms are implemented in the kinetic ring current model via diffusion equation with associated pitch angle diffusion coefficients. The precipitation is subsequently input to a two-stream transport model at the top of ionosphere in order to examine its impact on the ionsopheric conductivity. It is found that during intense storm time, electron precipitation of tens of keV dominates in the dawn sector and leads to significant enhancement of conductivity at low altitudes. On the other hand, proton precipitation on the nightside mostly occurs for energy below 10 keV, and contributes to ionization above 100 km, resulting in enhancement of conductivity there. Consequently, the height profile of both Pedersen and Hall conductivity exhibits two layers, potentially complicating the current closure in the ionosphere system.

How to cite: Yu, Y., Tian, X., Zhu, M., and Pr, S.: Modeling particle precipitation and effects on the ionospheric conductivity, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3181, https://doi.org/10.5194/egusphere-egu2020-3181, 2020.

EGU2020-632 | Displays | ST2.6

Identification of interplanetary parameter schemes which drive the variability of the magnetospheric radiation environment

Christos Katsavrias, Afroditi Nasi, Constantinos Papadimitriou, Sigiava Aminalragia-Giamini, Ingmar Sandberg, Piers Jiggens, and Ioannis A. Daglis

The energetic particles of the outer radiation belt are highly variable in space, time and energy, due to the complex interplay between various mechanisms that contribute to their energization and/or loss. Previous studies have focused on the influence of solar wind and magnetospheric processes on the electron population dynamics, showing that the eventual effect of the various interplanetary drivers results from different combinations of IMF and solar wind parameters. Yet, all of these studies were limited in temporal, spatial and energy coverage. In this work, we take advantage of a large dataset, which includes multipoint measurements of electron fluxes covering a large energy range and various orbits (e.g. Van Allen Probes, GOES, HIMAWARI, SREM monitors, etc.), as well as approximately the whole solar cycle 24 to deduce specific interplanetary parameter schemes that drive enhancements or depletions of relativistic electrons in the outer radiation belt. Our study also investigates parameters which are correlated to the Solar Energetic Particle (SEP) environment with the long-term goal of connecting the two sets of results for coherent merging of environment models.

This work is supported by ESA’s Science Core Technology Programme (CTP) under contract No. 4000127282/19/IB/gg.

How to cite: Katsavrias, C., Nasi, A., Papadimitriou, C., Aminalragia-Giamini, S., Sandberg, I., Jiggens, P., and Daglis, I. A.: Identification of interplanetary parameter schemes which drive the variability of the magnetospheric radiation environment , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-632, https://doi.org/10.5194/egusphere-egu2020-632, 2020.

EGU2020-20204 | Displays | ST2.6

How Coherent are Flux Variations in the Outer Van Allen Radiation Belt?

Samuel Walton, Colin Forsyth, Iain Jonathan Rae, Clare Watt, Richard Horne, Rhys Thompson, Craig Rodger, Mark Clilverd, and Maria Walach

The electron population inside Earth’s outer radiation belt is highly variable and typically linked to geomagnetic activity such as storms and substorms. These variations can differ with radial distance, such that the fluxes at the outer boundary are different from those in the heart of the belt. Using data from the Proton Electron Telescope (PET) on board NASA’s Solar Anomalous Magnetospheric Particle Explorer (SAMPEX), we have examined the correlation between electron fluxes at all L's within the radiation belts for a range of geomagnetic conditions, as well as longer-term averages. Our analysis shows that fluxes at L≈2-4 and L≈4-10 are well correlated within these regions, with coefficients in excess of 80%, however, the correlation between these two regions is low. These correlations vary between storm-times and quiet-times. We examine whether, and to what extent this correlation is related to the level of enhancement of the outer radiation belt during geomagnetic storms, and whether the plasmapause plays any role defining the different regions of correlated flux.

How to cite: Walton, S., Forsyth, C., Rae, I. J., Watt, C., Horne, R., Thompson, R., Rodger, C., Clilverd, M., and Walach, M.: How Coherent are Flux Variations in the Outer Van Allen Radiation Belt?, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-20204, https://doi.org/10.5194/egusphere-egu2020-20204, 2020.

EGU2020-1987 | Displays | ST2.6

Drifting Electron Holes Occurring During Geomagnetically Quiet Times: BD-IES Observations

Zhi-Yang Liu, Qiu-Gang Zong, and Hong Zou

Drifting electron holes (DEHs), manifesting as sudden but mild dropout in electron flux, are a common phenomenon seen in the Earth's magnetosphere. It manifests the change of the state of the magnetosphere. However, previous studies primarily focus on DEHs during geomagnetically active time (e.g., substorm). Not until recently have quiet time DEHs been reported. In this paper, we present a systematic study on the quiet time DEHs. BeiDa Imaging Electron Spectrometer (BD-IES) measurements from 2015 to 2017 are investigated. Twenty-two DEH events are identified. The DEHs cover the whole energy range of BD-IES (50–600 keV). Generally, the DEHs are positively dispersive with respect to energy. Time-of-flight analysis suggests the dispersion results from electron drift motion and gives the location where the DEHs originated from. Statistics reveal the DEHs primarily originated from the postmidnight magnetosphere. In addition, superposed epoch analysis applied to geomagnetic indices and solar wind parameters indicates these DEH events occurred during geomagnetically quiet time. No storm or substorm activity could be identified. However, an investigation into nightside midlatitude ground magnetic records suggests these quiet time DEHs were accompanied by Pi2 pulsations. The DEH-Pi2 connection indicates a possible DEH-bursty bulk flow (BBF) connection, since nightside midlatitude Pi2 activity is generally attributed to magnetotail BBFs. This connection is also supported by a case study of coordinated magnetotail observations from Magnetospheric Multiscale spacecraft. Therefore, we suggest the quiet time DEHs could be caused by magnetotail BBFs, similar to the substorm time DEHs.

How to cite: Liu, Z.-Y., Zong, Q.-G., and Zou, H.: Drifting Electron Holes Occurring During Geomagnetically Quiet Times: BD-IES Observations, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1987, https://doi.org/10.5194/egusphere-egu2020-1987, 2020.

EGU2020-6462 | Displays | ST2.6

A New Approach to Monitoring the Interplanetary Shock Induced Pulse: TEC Measurements by the GNSS Receiver Network

Xingran Chen, Quanhan Li, Qiugang Zong, and Yongqiang Hao

We revisit the typical interplanetary shock event on November 7, 2004, with high resolution total electron content (TEC) measurements obtained by the distributed Global Navigation Satellite System (GNSS) receivers. TEC impulses were observed after the IP shock impinged on the dayside agnetosphere at ~18:27 UT. In view of the similarity of the wave form and the time-delay characteristics, the TEC impulses were regarded as responses to the IP shock, despite the small amplitude (in the order of 0.4 TECU). Particularly, the peak of the TEC impulse was first observed by the receivers located around 120°W geographic longitude (corresponding to noon magnetic local time), while receivers at both sides recorded the impulse sequentially afterwards. From the timedelay of the TEC impulse, we derive the propagation velocity of the shock induced pulse. The angular velocity of the pulse is estimated to be ~2 degree per second, which is in the same order as the propagation speed of a typical shock pulse in the magnetosphere. Our results present global observational features of the shock pulse and provide new aspects to understand the ionospheric-magnetospheric dynamics in response to IP shocks.

How to cite: Chen, X., Li, Q., Zong, Q., and Hao, Y.: A New Approach to Monitoring the Interplanetary Shock Induced Pulse: TEC Measurements by the GNSS Receiver Network, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6462, https://doi.org/10.5194/egusphere-egu2020-6462, 2020.

EGU2020-17757 | Displays | ST2.6 | Highlight

A Comparison of Radial Diffusion Coefficients in 1-D and 3-D Long-Term Radiation Belt Simulations

Alexander Drozdov, Hayley Allison, Yuri Shprits, and Nikita Aseev

Radial diffusion is one of the dominant physical mechanisms that drives acceleration andloss of the radiation belt electrons due to wave-particle interactions with ultra-low frequency (ULF) waves, which makes it very important for radiation belt modeling and forecasting.  We investigate the sensitivity of several parameterizations of the radial diffusion including Brautigam and Albert (2000), Ozeke et al. (2014), Ali et al. (2016), and Liu et al. (2016) on long-term radiation belt modeling using the Versatile Electron Radiation Belt (VERB) code.  Following previous studies, we first perform 1-D radial diffusion simulations.  To take into account effects of local acceleration and loss, we perform additional 3-D simulations, including pitch-angle, energy and mixed diffusion.

How to cite: Drozdov, A., Allison, H., Shprits, Y., and Aseev, N.: A Comparison of Radial Diffusion Coefficients in 1-D and 3-D Long-Term Radiation Belt Simulations, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-17757, https://doi.org/10.5194/egusphere-egu2020-17757, 2020.

EGU2020-17946 | Displays | ST2.6 | Highlight

Controlling Effect of Wave Models and Plasma Boundaries on the Dynamic Evolution of Relativistic Radiation Belt Electrons

Dedong Wang, Yuri Shprits, Irina Zhelavskaya, Alexander Drozdov, Nikita Aseev, Frederic Effenberger, Angelica Castillo, and Sebastian Cervantes

Modeling and observations have shown that energy diffusion by chorus waves is an important source of acceleration of electrons to relativistic energies. By performing long‐term simulations using the three‐dimensional Versatile Electron Radiation Belt (VERB-3D) code, we test how the latitudinal dependence of chorus waves can affect the dynamics of the radiation belt electrons. Results show that the variability of chorus waves at high latitudes is critical for modeling of megaelectron volt (MeV) electrons. We show that, depending on the latitudinal distribution of chorus waves under different geomagnetic conditions, they cannot only produce a net acceleration but also a net loss of MeV electrons. Decrease in high‐latitude chorus waves can tip the balance between acceleration and loss toward acceleration, or alternatively, the increase in high‐latitude waves can result in a net loss of MeV electrons. Variations in high‐latitude chorus may account for some of the variability of MeV electrons.

Our simulation results also show that the position of the plasmapause plays a significant role in the dynamic evolution of relativistic electrons. The magnetopause shadowing effect is included by using last closed drift shell (LCDS), and it is shown to significantly contribute to the dropouts of relativistic electrons at high L*.

How to cite: Wang, D., Shprits, Y., Zhelavskaya, I., Drozdov, A., Aseev, N., Effenberger, F., Castillo, A., and Cervantes, S.: Controlling Effect of Wave Models and Plasma Boundaries on the Dynamic Evolution of Relativistic Radiation Belt Electrons, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-17946, https://doi.org/10.5194/egusphere-egu2020-17946, 2020.

EGU2020-19607 | Displays | ST2.6 | Highlight

The dynamics of the inner boundary of the outer radiation belt during geomagnetic storms

Xiaofei Shi, Jie Ren, and Qiugang Zong

We present a statistical study of energy-dependent and L shell-dependent inner boundary of the outer radiation belt during 37 isolated geomagnetic storms using observations from Van Allen Probes from 2013 to 2017. There are mutual transformations between "V-shaped" and "S-shaped" inner boundaries during different storm phases, resulting from the competition among electron loss, radial transport and local acceleration. The radial position, onset time, Est (the minimum energy at Lst where the inner boundary starts to exhibit an S-shaped form), and the radial width of S-shaped boundary (ΔL) are quantitatively defined according to the formation of a reversed energy spectrum (electron flux going up with increasing energies from hundreds of keV to ~1 MeV) from a kappa-like spectrum (electron flux steeply falling with increasing energies). The case and statistical results present that (1) The inner boundary has repeatable features associated with storms: the inner boundary is transformed from S-shaped to V-shaped form in several hours during the storm commencement and main phase, and retains in the V-shaped form for several days until it evolves into S-shaped during late recovery phase; (2) ΔL shows positive correlation with SYM-H index; (3) The duration of the V-shaped form is positively correlated with the storm intensity and the duration of the recovery phase; (4) The minimum energy Est are mainly distributed in the range of 100-550 keV. All these findings have important implications for understanding the dynamics of energetic electrons in the slot region and the outer radiation belt during geomagnetic storms.

How to cite: Shi, X., Ren, J., and Zong, Q.: The dynamics of the inner boundary of the outer radiation belt during geomagnetic storms, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-19607, https://doi.org/10.5194/egusphere-egu2020-19607, 2020.

EGU2020-19053 | Displays | ST2.6

A Neural Network Model of Three-dimensional Magnetospheric Chorus Waves

Yingjie Guo, Binbin Ni, Dedong Wang, Yuri Shprits, Song Fu, Xing Cao, and Xudong Gu

The evolution of chorus waves is important in the inner magnetosphere since it is closely related to the loss and acceleration of radiation belt electrons. In this study, we develop neural-network-based models for upper-band chorus (UBC; 0.5 fce < f <  fce ) waves and lower-band chorus (LBC; 0.05 fce < f < 0.5 fce) waves, where fce is the equatorial electron gyrofrequency. We establish a root-mean-square amplitude database for both UBC and LBC using Van Allen Probe levels 2 and 3 data products from the EMFISIS payload between October 1, 2012 and January 14, 2018. Based on the database, we construct an artificial neural network with corresponding L, magnetic local time, magnetic latitude, solar wind parameters and geomagnetic indices on different time windows as model inputs. Additionally, we adopt several different feature selection techniques to determine the most important features of magnetospheric chorus waves, reduce training or running time and improve the model accuracy. Our study suggests that the model results using the machine learning technique have the great potential to highly improve current understanding of the radiation belt dynamics.

How to cite: Guo, Y., Ni, B., Wang, D., Shprits, Y., Fu, S., Cao, X., and Gu, X.: A Neural Network Model of Three-dimensional Magnetospheric Chorus Waves, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-19053, https://doi.org/10.5194/egusphere-egu2020-19053, 2020.

Electron pitch angle distribution (PAD) is a critical parameter in the study of the dynamics of the radiation belt electrons. It is well known that solar wind pressure has an impact on the PAD of the geomagnetically trapped electrons. Using the Van Allen Probes' data, we find that the MeV electron PAD at 4.5<L*<5.5 became narrowing (PAD is mainly concentrated at 90 degree) for over three days during a prolonged enhancement of the solar wind number density on November 27-30, 2015. During that period, the EMIC waves are observed by Van Allen Probe-A and ground stations on the afternoon and dusk MLTs at L>4. Meanwile, the precipitations of tens of keV protons and MeV electrons are observed by POES satellites. Additionally, there is a growing dip in electron phase space density at L*~5, indicating a local loss caused by the wave-particle interaction. The narrowing of the electron PAD is energy-dependent and the PAD is more anisotropic for electrons with higher energy, which is consistent with the wave-particle interaction with the EMIC waves. Furthermore, previous studies have shown that high solar wind density can lead to a hot and dense plasma sheet. The inward penetration of a dense plasma-sheet down to 4 Re has been confirmed by THEMIS spacecraft. We suggest that the overlap of the plasma sheet and the plasmasphere provide a favorable condition for exciting EMIC waves and the loss of small pitch angle electrons by EMIC waves can lead to the electron PAD narrowing. 

 

How to cite: Xie, L., Xiong, Y., Fu, S., and Pu, Z.: Ultra-relativistic electron’s pitch angle distribution narrowing associated with the solar wind density enhancement, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-13017, https://doi.org/10.5194/egusphere-egu2020-13017, 2020.

Much evidence has indicated that charge exchange with the neutral atoms is an important loss mechanism of the ring current ions, especially during the slow recovery phase of a geomagnetic storm. Most of the studies, however, were focused on the global effect of the charge exchange on the ring current decay. The effect on different magnetic local times and L shells has not been achieved. In this study, based on the in-situ energetic ion data (Level 3) from RBSPICE onboard two Van Allen Probes, we study the contribution of the charge exchange, calculated from the differential flux of ions, to the local ring current decay at different magnetic local times and radial distance. Results indicate that the charge exchange effect on the ring current decay shows clear MLT and L dependence. Our study provides important information of spatial distribution of the ring current loss evolution, which could be as a reference during the ring current modeling.

How to cite: Li, S. and Luo, H.: MLT Dependence of Contribution of Charge Exchange Loss to the Storm Time Ring Current Decay: Van Allen Probes Observations, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21176, https://doi.org/10.5194/egusphere-egu2020-21176, 2020.

EGU2020-19284 | Displays | ST2.6

Global Morphology of Lower-band Chorus Wave Intensity Reconstructed Using multi-year POES Electron Measurements

Yang Zhang, Binbin Ni, Xudong Gu, Yuri Shprits, Song Fu, Xing Cao, and Zheng Xiang

Magnetospheric chorus is known to play a significant role in the acceleration and loss of radiation belt electrons. Interactions of chorus waves with radiation belt particles are commonly evaluated using quasi-linear diffusion codes that rely on statistical models, which might not accurately provide the instantaneous global wave distribution from limited in-situ wave measurements. Thus, a novel technique capable of inferring wave amplitudes from POES particle measurements, with an extensive coverage of L-shell and magnetic local time, has been established to obtain event-specific, global dynamic evolutions of chorus waves. This study, using 5 years of POES electron data, further improves the technique, and enables us to subsequently infer the chorus wave amplitudes for all useful data points (removing the electrons which were in the drift loss cone) and to construct the global distribution of lower-band chorus wave intensity. The results obtained from the improved technique reproduce Van Allen Probes in-situ observations of chorus waves reasonably well and reconstruct the major features of the global distribution of chorus waves. We demonstrate that such a data-based, dynamic model can provide near-real-time estimates of chorus wave intensity on a global scale for any time period when POES data are available, which cannot be obtained from in-situ wave measurements by equatorial satellites alone, but is crucial for quantifying the  dynamics of the radiation belt electrons.

How to cite: Zhang, Y., Ni, B., Gu, X., Shprits, Y., Fu, S., Cao, X., and Xiang, Z.: Global Morphology of Lower-band Chorus Wave Intensity Reconstructed Using multi-year POES Electron Measurements, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-19284, https://doi.org/10.5194/egusphere-egu2020-19284, 2020.

EGU2020-7657 | Displays | ST2.6

Calculation of corotation electric field based on Van Allen Probes measurements

Wenlong Liu and Zhao Zhang

Corotation electric field is important in the inner magnetosphere topology, which was usually calculated by assuming 24h corotation period. However, some studies suggested that plasmasphere corotation lag exists which leads to the decrease of corotation electric field. In this study, we use electric field measurements from Van Allen Probes mission from 2013 to 2017 to statistically calculate the distribution of large-scale electric field in the inner magnetosphere. A new method is subsequently developed to separate corotation electric field from convection electric field. Our research shows electric field is inversely proportional to the square of L, and, with the assumption of dipole magnetic field, the rotation period of plasmasphere is estimated as 27h, consistent to the results by Sandel et al. [2003] and Burch et al. [2004] with EUV imaging of the plasmasphere. Based on the research, a new empirical model of innermagnetospheric corotation electric field was estibalished, which is significant for a more accurate understanding the large-scale electric field in the inner magnetosphere.

How to cite: Liu, W. and Zhang, Z.: Calculation of corotation electric field based on Van Allen Probes measurements, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7657, https://doi.org/10.5194/egusphere-egu2020-7657, 2020.

EGU2020-1294 | Displays | ST2.6 | Highlight

Episodic occurrence of field-aligned energetic ions on the dayside

Chao Yue, Jacob Bortnik, Shasha Zou, Yukitoshi Nishimura, and John C. Foster

The tens of keV ion populations observed in the ring current region at L~ 3- 7, generally have pancake-shaped pitch angle distributions (PADs), that is, peaked at 90 degrees. These pancake PADs are formed due to a combination of betatron and Fermi acceleration when they are transported from the tail plasma sheet, where the major ring current plasma originates. However, in this study, by using the Van Allen Probe observations from 2012 to 2018 on the dayside, unexpectedly we have found that about 5% of the time, protons with energies of ~30 to 50 keV show two distinct populations according to their PADs, having an additional population of field-aligned ions overlapping with the original pancake population. The newly appearing field-aligned populations have higher occurrence rates at ~12-16 MLT during geomagnetically active times. In particular, we have studied eight such events in detail and traced back these ions to their source regions according to the energy-dependent dispersion signatures caused by the differences in drift velocities. We found that the source regions are located around 12 to 18 MLT which coincides with the high occurrence rate region of 12-16 MLT. Based on the ionospheric and LANL geosynchronous observations of these eight events, it is suggested that these energetic ions with field-aligned PADs most probably are accelerated in the post-noon sector in association with ionospheric disturbances that are triggered by tail injection. These results provide evidence of another important source of the ring current ions.

How to cite: Yue, C., Bortnik, J., Zou, S., Nishimura, Y., and Foster, J. C.: Episodic occurrence of field-aligned energetic ions on the dayside , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1294, https://doi.org/10.5194/egusphere-egu2020-1294, 2020.

EGU2020-2034 | Displays | ST2.6

Roles of magnetospheric convection on nonlinear drift resonance between electrons and ULF waves

Xuzhi Zhou, Li Li, Yoshiharu Omura, Qiugang Zong, Suiyan Fu, Robert Rankin, and Alex Degeling

In the Earth's inner magnetosphere, charged particles can be accelerated and transported by ultralow frequency (ULF) waves via drift resonance. We investigate the effects of magnetospheric convection on the nonlinear drift resonance process, which provides an inhomogeneity factor S to externally drive the pendulum equation that describes the particle motion in the ULF wave  field. The S factor, defined as the ratio of the driving amplitude to the square of the pendulum trapping frequency, is found to vary with magnetic local time and as a consequence, oscillates quasi-periodically at the particle drift frequency. To better understand the particle behavior governed by the driven pendulum equation, we carry out simulations to obtain the evolution of electron distribution functions in energy and L-shell phase space. We find that resonant electrons can remain trapped by the low-m ULF waves under strong convection electric  field, whereas for high-m ULF waves, the electrons trajectories can be significantly modified. More interestingly, the electron drift frequency is close to the nonlinear trapping frequency for intermediate-m ULF waves, which corresponds to chaotic motion of resonant electrons. These  findings shed new light on the nature of particle coherent and diffusive transport in the inner magnetosphere.

How to cite: Zhou, X., Li, L., Omura, Y., Zong, Q., Fu, S., Rankin, R., and Degeling, A.: Roles of magnetospheric convection on nonlinear drift resonance between electrons and ULF waves, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2034, https://doi.org/10.5194/egusphere-egu2020-2034, 2020.

Previous studies have demonstrated that the field line resonance (FLR) frequencies detected on closed magnetospheric field lines can be used to estimate the plasma mass density in the inner magnetosphere. This method, also known as “normal-mode magnetoseismology,” can act as a virtual instrument that turns spacecraft measurements of magnetic and/or electric field into plasma mass density, which is a fundamental physical quantity that is difficult to measure directly but important to investigations involving the MHD timescales, reconnection rates, or instability/wave growth rates.

In this study, we use normal-mode magnetoseismology to help investigate the characteristics of the oxygen torus, which is the narrow region of enhanced O+ density in the vicinity of the plasmapause that may form during the storm recovery phase. The formation of the oxygen torus is still an outstanding question, and the geomagnetic mass spectrometer effect and the direct ring current heating of the ionosphere have been proposed as two possible causes. We identify the location and timing of oxygen torus occurrence by examining the FLR-inferred plasma mass densities in Magnetospheric Multiscale (MMS) and Van Allen Probes (RBSP) observations and compare them with the charge densities derived from the upper hybrid resonance frequency detected by the respective plasma wave experiments on the spacecraft. We find that, while MMS and RBSP could both observe clear enhancements of heavy ions during a magnetic storm, the degree and the width of O+ enhancement can vary with location. The timing of oxygen torus occurrence may differ from storm to storm. In RBSP measurements, we also compare the bulk densities with the partial densities of low-energy ions detected by the HOPE instrument. While the average ion mass can be greater for 30 eV – 1 keV ions than that for the bulk plasma in the oxygen torus, it is evident that the majority of the ions in the oxygen torus are below 30 eV, confirming the need to examine the bulk mass and charge densities through electromagnetic sounding methods.

How to cite: Wilcox, B., Chi, P., Takahashi, K., and Denton, R.: Normal-mode Magnetoseismology as a Virtual Plasma Mass Density Instrument and Its Use in Investigation of Oxygen Torus during Magnetic Storms, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-12323, https://doi.org/10.5194/egusphere-egu2020-12323, 2020.

EGU2020-4357 | Displays | ST2.6

Multi-event analysis of SAPS Wave Structures observed by the SuperDARN Hokkaido Pair of radars

Nozomu Nishitani, Tomoaki Hori, and Mariko Teramoto

The SuperDARN Hokkaido Pair (HOP) of radars data with special operation modes are used to study the wavy variations of plasma flow embedded in larger-scale, fast flow structures at subauroral latitudes (SAPS). Because of the limited number of examples studied so far, their generation mechanism is not fully understood yet. In this paper we focus mainly on the events on Sep 08, 2017 and Aug. 26, 2018. Both events occurred near the peak of large geomagnetic storms. These events were registered by the SuperDARN radars with higher temporal resolution (3 and 12 seconds respectively) camping beams. Using both camping beam data and 2-dimensional data (with 1 to 2 min temporal resolution) enable us to examine the period, wavelength and propagation speed of these wave structures. In addition, using the data with the new fitting algorithm (fitacf Ver. 3) we have more extended coverage of the echo regions. We notice that  both events were observed during geomagnetic storms (minimum Dst: -124 nT and -174 nT) and the wave structures have limited spatial extent in magnetic local time. On the other hand, there are several differences between these events such as period, propagation speed and geomagnetic latitude. Their possible generation mechanisms will be discussed.

How to cite: Nishitani, N., Hori, T., and Teramoto, M.: Multi-event analysis of SAPS Wave Structures observed by the SuperDARN Hokkaido Pair of radars, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4357, https://doi.org/10.5194/egusphere-egu2020-4357, 2020.

EGU2020-4580 | Displays | ST2.6

Presence of cavity resonances in the inner magnetosphere

Harri Laakso

In the inner magnetosphere there are sharp plasma boundaries that can cause resonance cavities. The four Cluster satellites move in a string-of-pearls configuration at perigee (at L=4-5) so that they are spatially well separated but their separation is still short that at least some of them are simultaneously at different positions inside the cavity. In the presence of cavity resonance of a half wavelength, all spacecraft inside the cavity observe the same wave mode in the same phase. In this talk we analyze and present a number of cavity resonances observed by the Cluster spacecraft. Typical observed mode frequencies are between 4 - 14 mHz, depending on the size of the cavity. It appears that the occurrence of cavity resonances is well correlated with changes in geomagnetic activity and they are quite common. They tend to occur at 12-16 MLT and 21-23 MLT. These ULF waves may have a significant impact on radiation belt particles as they cover a large L shell range.

How to cite: Laakso, H.: Presence of cavity resonances in the inner magnetosphere, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4580, https://doi.org/10.5194/egusphere-egu2020-4580, 2020.

EGU2020-6312 | Displays | ST2.6

Variations of Poynting Flux in the Northern Hemisphere during Quiet Times

Xiao-Xin Zhang, Chao Yu, Wenbin Wang, and Fei He

Poynting flux energy is deposited from the magnetosphere in high latitudes, and measures the electromagnetic energy transmitted between the magnetosphere and the ionosphere. Little attention has been paid on the seasonal variation of the longitudinal pattern of the Poynting flux. Here, using long-term measurements of the ion drifts and the magnetic field by the DMSP satellite in the topside ionosphere, a statistical investigation of the longitudinal distributions of the Poynting flux in polar region during quiet times is conducted. Both case study and statistics show that there is a local maximum in downward Poynting flux in the pre-noon sector. Generally, the maximum is centered around geographic longitude of 120° west and geographic latitude of 80°, meaning that the total energy transferred into the ionosphere is the greatest in this region. The longitudinal distribution of the Poynting flux also exhibit clear seasonal variations with the longitudinal asymmetry the most significant in norther summer. The results could provide some new sights in future investigations of magnetosphere-ionosphere coupling in the polar region with observations and simulations.

How to cite: Zhang, X.-X., Yu, C., Wang, W., and He, F.: Variations of Poynting Flux in the Northern Hemisphere during Quiet Times, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6312, https://doi.org/10.5194/egusphere-egu2020-6312, 2020.

ST2.7 – Plasma waves, energetic particles and their interactions throughout planetary magnetospheres

EGU2020-5801 | Displays | ST2.7 | Highlight

Substorm Injections as a Source of Relativistic Electrons in Earth’s Outer Radiation Belt

Drew Turner, Ian Cohen, Kareem Sorathia, Sasha Ukhorskiy, Geoff Reeves, Jean-Francois Ripoll, Christine Gabrielse, Joseph Fennell, and J. Bernard Blake

Earth’s magnetotail plasma sheet plays a crucial role in the variability of Earth’s outer electron radiation belt. Typically, injections of energetic electrons from Earth’s magnetotail into the outer radiation belt and inner magnetosphere during periods of substorm activity are not observed exceeding ~300 keV.  Consistent with that, phase space density radial distributions of electrons typically indicate that for electrons below ~300 keV, there is a source of electrons in the plasma sheet while for electrons with energies above that, there is a local source within the outer radiation belt itself.  However, here we ask the question: is this always the case or can the plasma sheet provide a direct source of relativistic (> ~500 keV) electrons into Earth’s outer radiation belt via substorm injection? Using phase space density analysis for fixed values of electron first and second adiabatic invariants, we use energetic electron data from NASA’s Van Allen Probes and Magnetospheric Multiscale (MMS) missions during periods in which MMS observed energetic electron injections in the plasma sheet while Van Allen Probes concurrently observed injections into the outer radiation belt. We report on cases that indicate there was a sufficient source of up to >1 MeV electrons in the electron injections in the plasma sheet as observed by MMS, yet Van Allen Probes did not see those energies injected inside of geosynchronous orbit.  From global insight with recent test-particle simulations in global, dynamic magnetospheric fields, we offer an explanation for why the highest-energy electrons might not be able to inject into the outer belt even while the lower energy (< ~300 keV) electrons do. Two other intriguing points that we will discuss concerning these results are: i) what acceleration mechanism is capable of producing such abundance of relativistic electrons at such large radial distances (X-GSE < -10 RE) in Earth’s magnetotail? and ii) during what conditions (if any) might injections of relativistic electrons be able to penetrate into the outer belt?

How to cite: Turner, D., Cohen, I., Sorathia, K., Ukhorskiy, S., Reeves, G., Ripoll, J.-F., Gabrielse, C., Fennell, J., and Blake, J. B.: Substorm Injections as a Source of Relativistic Electrons in Earth’s Outer Radiation Belt, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5801, https://doi.org/10.5194/egusphere-egu2020-5801, 2020.

EGU2020-2729 | Displays | ST2.7

The Detection and Consequences of Coherent Electromagnetic Plasma Waves: Prediction of Rapid L = 2-3 Electron Slot Formation

Bruce Tsurutani, Sang A Park, Jolene Pickett, Gurbax Lakhina, and Abhijit Sen

Low frequency (LF) ~22 Hz to 200 Hz plasmaspheric hiss was studied using a year of Polar
plasma wave data occurring during solar cycle minimum. The waves are found to be most intense in the noon and early dusk sectors. When only the most intense LF (ILF) hiss was examined, they are found to be substorm dependent and most prominent in the noon sector. The noon sector ILF waves were also determined to be independent of solar wind ram pressure. The ILF hiss intensity is independent of magnetic latitude. ILF hiss is found to be highly coherent in nature. ILF hiss propagates at all angles relative to
the ambient magnetic field. Circular, elliptical, and linear/highly elliptically polarized hiss have been detected, with elliptical polarization the dominant characteristic. A case of linear polarized ILF hiss that occurred deep in the plasmasphere during geomagnetic quiet was noted. The waveforms and polarizations of ILF hiss are similar to those of intense high frequency hiss. We propose the hypothesis that ~10–100 keV substorm injected electrons gradient drift to dayside minimum B pockets close to the magnetopause to generate LF chorus. The closeness of this chorus to low altitude entry points into the plasmasphere will minimize wave damping and allow intense noon‐sector ILF hiss. The coherency of ILF hiss leads the authors to predict energetic electron precipitation into the midlatitude ionosphere and the electron slot formation during substorms. Several means of testing the above hypotheses are discussed.
 
References
[1] Tsurutani, B.T., S.A. Park, B.J. Falkowski, J. Bortnik, G.S. Lakhina, A. Sen, J.S. Pickett, R. Hajra, M. Parrot, and P. Henri (2020), Low frequency (f < 200 Hz) Polar plasmasheric hiss: Coherent and intense, J. Geophys. Res. Spa. Phys., in press. 

How to cite: Tsurutani, B., Park, S. A., Pickett, J., Lakhina, G., and Sen, A.: The Detection and Consequences of Coherent Electromagnetic Plasma Waves: Prediction of Rapid L = 2-3 Electron Slot Formation, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2729, https://doi.org/10.5194/egusphere-egu2020-2729, 2020.

EGU2020-18091 | Displays | ST2.7 | Highlight

The Impacts of Substorms on the Ring Current

Jasmine Sandhu, Jonathan Rae, Maria-Theresia Walach, Clare Watt, Mervyn Freeman, Matina Gkioulidou, Colin Forsyth, Geoffrey Reeves, Harlan Spence, David Hartley, Nigel Meredith, and Johnathan Ross

Substorms are a highly dynamic process that results in the global redistribution of energy within the magnetosphere. The occurrence of a substorm can provide the inner magnetosphere with hot ions and consequently intensify the ring current population. However, substorms are a highly variable phenomenon that can occur as an isolated event or as part of a sequence. In this study we investigate how substorms shape the energy content, anisotropy, and storm time behaviour of the ring current population.

Using ion observations (H+, O+, and He+) from the RBSPICE and HOPE instruments onboard the Van Allen Probes, we quantify how the total ring current energy content and ring current anisotropy changes during the substorm process. A statistical analysis demonstrates the impact of a typical substorm energises the ring current by 12% on average. The features of the energy enhancement correlate well with the expected properties of particle injections into the inner magnetosphere, and large enhancements in the O+ contribution to the energy content suggest important compositional variations.

Analysis also shows that the ring current ions experience significant isotropisation following substorm onset. Although previously attributed to enhanced EMIC wave activity, a consideration of different drivers of the isotropisation identifies that although EMIC wave activity plays a role, the properties of the injected and convected population is the dominant driver.

Finally, we explore the storm time variations of the ring current, revealing important information on the role of substorms in storm dynamics. A superposed epoch analysis of ring current energy content shows large enhancements particularly in the premidnight sector during the main phase, and a reduction in both local time asymmetry and intensity during the recovery phase. A comparison with estimated energy content using the Sym-H index was conducted. In agreement with previous results, the Sym-H index significantly overestimates energy content. A new finding is an observed temporal discrepancy, where estimates maximise ~ 12 hours earlier than the in-situ observations. We assert that an observed enhancement in substorm activity coincident with the Sym-H recovery is responsible. The results highlight the drawbacks of ring current indices and emphasise the impacts of substorms on the ring current population.

How to cite: Sandhu, J., Rae, J., Walach, M.-T., Watt, C., Freeman, M., Gkioulidou, M., Forsyth, C., Reeves, G., Spence, H., Hartley, D., Meredith, N., and Ross, J.: The Impacts of Substorms on the Ring Current, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18091, https://doi.org/10.5194/egusphere-egu2020-18091, 2020.

EGU2020-11657 | Displays | ST2.7

MMS Observations of the Charge State and Mass Dependent Energization of Heavy Ions During Injections in the Earth’s Magnetotail

Sam Bingham, Ian Cohen, Barry Mauk, Don Mitchell, Drew Turner, and Stephen Fuselier

Particle injections transport particles from the Earth’s magnetotail to the inner magnetosphere. During this process, ions in the injections are substantially energized. The physical processes behind this energization are still under debate. Recent results from the Van Allen Probes mission at radial distances < 6 RE have shown that higher mass ions (helium and oxygen) with high charge states are often found at substantially higher energies than protons (up to MeV energies compared to a couple hundred keV) in the inner magnetosphere. Here we present results from the Magnetospheric Multiscale (MMS) mission over a broad range of radial distances (between 7-25 RE) where the energization of injected ions is charge state dependent. We demonstrate with these observations that injected ions exhibit behavior which is well ordered by energy per charge due to the gradient/curvature drift’s impact on particle trajectories as they drift in the direction of transient electric fields. The charge state dependent energization leads to the dominance of multiple charge state heavy ions, as opposed to H+, above ~250 keV throughout the Earth’s inner and middle magnetosphere. Additionally, there are also cases with hints of non-adiabatic energization observed in O+ between ~100-250 keV, where O+ potentially gets some extra-energization compared to H+ due differences in their respective gyroradii. However, the highest energy ions (> 300 keV oxygen and helium) are still likely of solar wind origin and primarily accelerated due to their higher charge-state. In the process of these results we demonstrate the utility of a technique for deducing ion charge-states using instrumentation that does not directly discriminate by charge state.

How to cite: Bingham, S., Cohen, I., Mauk, B., Mitchell, D., Turner, D., and Fuselier, S.: MMS Observations of the Charge State and Mass Dependent Energization of Heavy Ions During Injections in the Earth’s Magnetotail, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11657, https://doi.org/10.5194/egusphere-egu2020-11657, 2020.

EGU2020-279 | Displays | ST2.7

The Angular Distribution of Whistler-Mode Chorus and the Importance of Plumes in the Chorus-Hiss Mechanism

David P. Hartley, Lunjin Chen, Craig Kletzing, Richard Horne, and Ondrej Santolik

Correlations between chorus waves and plasmaspheric hiss have been directly observed, leading to the proposition that the two wave modes are causally linked. Ray tracing simulations have confirmed that chorus waves can propagate into the plasmasphere and be a source of plasmaspheric hiss, but only for a specific set of initial conditions, particularly relating to the orientation of the wave vector at the chorus source. In this study, both survey and burst mode observations from the Van Allen Probes EMFISIS Waves instrument are coupled with ray tracing simulations to determine the fraction of chorus wave power that exists with the conditions required to enter the plasmasphere. In general, it is found that only a small fraction (< 2%) of chorus wave power exists with the required wave vector orientation. An exception is found when the chorus source is located close to a plasmaspheric plume. Here, azimuthal density gradients modify the wave propagation to permit a large fraction, up to 94%, of chorus wave power to access the plasmasphere. Therefore plasmaspheric plumes are identified as an important access region if a significant fraction of chorus wave power is to enter the plasmasphere and be a source of plasmaspheric hiss. To provide context, we note that plumes are most commonly observed on the dusk side whereas chorus wave power typically peak on the dawn side. The post-noon sector, where these two statistical distributions overlap, appears to be key for observing correlations between chorus and hiss. As such, particular attention is devoted to this region.

How to cite: Hartley, D. P., Chen, L., Kletzing, C., Horne, R., and Santolik, O.: The Angular Distribution of Whistler-Mode Chorus and the Importance of Plumes in the Chorus-Hiss Mechanism, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-279, https://doi.org/10.5194/egusphere-egu2020-279, 2020.

EGU2020-4642 | Displays | ST2.7

Global models of the inner electron radiation belt and slot region investigating the effects of VLF transmitter waves

Johnathan Ross, Sarah Glauert, Richard Horne, Nigel Meredith, and Mark Clilverd

Signals from man-made very low frequency (VLF) transmitters can leak from the Earth-ionosphere wave guide into the inner magnetosphere, where they propagate in the whistler mode and contribute to electron dynamics in the inner radiation belt and slot region through wave-particle interactions. These inner regions of the magnetosphere are becoming increasingly important from a satellite perspective. For instance, the newly populated Medium Earth Orbits pass though the slot region, and satellites launched via electric orbit raising are exposed to the inner belt and slot region for extended periods of time.

We have calculated diffusion coefficients associated with wave-particle interactions between radiation belt electrons and waves from each of the strongest VLF transmitters using Van Allen Probe observations. These coefficients are included into global models of the radiation belts to assess the importance of the effects of VLF transmitters individually and collectively on electron populations.

How to cite: Ross, J., Glauert, S., Horne, R., Meredith, N., and Clilverd, M.: Global models of the inner electron radiation belt and slot region investigating the effects of VLF transmitter waves, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4642, https://doi.org/10.5194/egusphere-egu2020-4642, 2020.

EGU2020-12580 | Displays | ST2.7

Timescales of electrons wave-particle interactions with chorus and hiss in the outer radiation belts

Oleksiy Agapitov, Didier Mourenas, Anton Artemyev, Forrest Mozer, and John Bonnell

Electron scattering by chorus and hiss waves is an important mechanism that can lead to fast electron acceleration and loss in the inner magnetosphere. Making use of Van Allen Probes measurements, we present the factors found recently to affect the efficiency and control the predominance of the precipitation or acceleration regimes. The dependence of VLF waves frequency on latitude [1], so that the relative wave frequency goes down, leads to decreasing the electron scattering resonance latitudes. This provides an effective increase of wave amplitude due to whistler-mode wave amplitude distribution on latitude. High latitude wave extent and wave amplitude distribution on latitude determine the regime of scattering (higher latitudes) or acceleration (lower latitudes). Wave normal angle distribution and the existence of the significant oblique whistler population influence efficiency of electron scattering affects significantly the scattering rates and potentially shifts the wave-particle interaction regime during geomagnetic storms from mostly scattering to mostly acceleration [2]. Dynamics of plasma characteristics during disturbed periods, such as ωpece decreases (especially in the night sector) sometimes leading to very short time scales for quasi‐linear MeV electron acceleration in agreement with Van Allen Probes observations [3].  ωpece dynamics in the plasmasphere increases the efficiency of electron scattering by hiss.

 

References

[1] Agapitov et al. (2018) Journal of Geophysical Research, https://doi.org/10.1002/2017JA024843

[2] Artemyev et al., (2016). Space Science Reviews, https://doi.org/10.1007/s11214-016-0252-5

[3] Agapitov et al., (2019) Geophysical Research Letters, https://doi.org/10.1029/2019GL083446

How to cite: Agapitov, O., Mourenas, D., Artemyev, A., Mozer, F., and Bonnell, J.: Timescales of electrons wave-particle interactions with chorus and hiss in the outer radiation belts, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-12580, https://doi.org/10.5194/egusphere-egu2020-12580, 2020.

EGU2020-3354 | Displays | ST2.7

Modeling and Data Assimilation of the Ring Current, Relativistic and Ultra-relativistic Electrons in the Inner Magnetosphere

Yuri Shprits, Nikita Aseev, Alexander Drozdov, Juan Sebastian Cervantes Villa, Angelica Maria Castillo Tibocha, Irina Zhelavskaya, Ruggero Vasile, Frederic Effenberger, Dominika Soergel, Ingo Michaelis, and Anthony Saikin

Dynamics of energetic and relativistic particles have received a lot of attention in recent years. Significant efforts have been focused on the understanding of the acceleration and loss processes of relativistic electrons and their dynamic evolution, as well as the understanding of ring-current injections in variable magnetic and electric fields. More recently, observations have been used systematically with the aid of data assimilation tools that allow to reconstruct the state of the system by blending models and various observations, and also allow to infer unknown physics and quantify various physical processes. In this study, we present an overview of recent modeling efforts with the VERB-3D and VERB-4D codes. We also show data assimilation from ring current to multi-MeV energies. We present a systematic comparative analysis of the dominant acceleration and loss processes for ring current, relativistic, and ultra-relativistic electrons and compare them. In particular, modeling and data assimilation reveal the missing physical processes at these three ranges of energies. Sensitivity simulations show that the background plasma density, location of the magnetopause, accurate description of electric and magnetic fields, and the description of the not well sampled high latitude wave environment play a crucial role for the dynamics of various electron populations in the inner magnetosphere. In summary, we present the recently funded EU Horizon 2020 project led by GFZ that will produce a chain of probabilistic modeling forecasts from the Sun to the inner magnetosphere.

How to cite: Shprits, Y., Aseev, N., Drozdov, A., Cervantes Villa, J. S., Castillo Tibocha, A. M., Zhelavskaya, I., Vasile, R., Effenberger, F., Soergel, D., Michaelis, I., and Saikin, A.: Modeling and Data Assimilation of the Ring Current, Relativistic and Ultra-relativistic Electrons in the Inner Magnetosphere, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3354, https://doi.org/10.5194/egusphere-egu2020-3354, 2020.

EGU2020-6034 | Displays | ST2.7

Differences in inner magnetospheric wave activity, outer Van Allen belt electron dynamics and atmospheric precipitation during CME sheaths and flux ropes

Emilia Kilpua, Milla Kalliokoski, Liisa Juusola, Maxime Grandin, Antti Kero, Drew Turner, Allison Jaynes, Timo Asikainen, Stepan Dubyagin, Harriet George, Heli Hietala, Hannu Koskinen, Adnane Osmane, Minna Palmroth, Noora Partamies, Tuija Pulkkinen, Tero Raita, Lucile Turc, and Rami Vainio

Coronal mass ejection (CME) driven sheath regions are one of the key structures driving strong magnetospheric disturbances, in particular at high latitudes. Sheaths are turbulent and compressed regions that exhibit large-amplitude magnetic field variations and high and variable dynamic pressure. They thus put the magnetosphere under particularly strong solar wind forcing. We show here the results of our recent studies that have investigated the response of inner magnetosphere plasma waves, energy and L-shell resolved outer belt electron variations and precipitation of high-energy electrons to the upper atmosphere during sheath regions. The data come primarily from Van Allen Probes and ground-based riometers. Our results reveal that sheaths drive intense “wave storms” in the inner magnetosphere (ULF, EMIC, chorus, hiss). Lower-energy electron fluxes (source and seed populations) are typically enhanced due to frequent and strong substorms injecting fresh electrons, while relativistic electrons are effectively depleted at wide L-ranges due to scattering by wave-particle interactions and magnetopause shadowing playing in concert. We found that even non-geoeffective sheaths can drive significant wave activity and dramatic changes in the outer belt electron fluxes. The “complex ejecta”, however, that consist of multiple sheaths and distorted CME ejecta can lead to sustained chorus and ULF waves, and as a consequence, effective electron acceleration to high energies. We also report some distinct characteristics in the intensity and Magnetic Local Time distribution of precipitation during sheaths when compared to other large-scale solar wind driver structures. The different precipitation responses likely stem from driver specific characteristics in their ability to excite inner magnetosphere plasma waves.

 

How to cite: Kilpua, E., Kalliokoski, M., Juusola, L., Grandin, M., Kero, A., Turner, D., Jaynes, A., Asikainen, T., Dubyagin, S., George, H., Hietala, H., Koskinen, H., Osmane, A., Palmroth, M., Partamies, N., Pulkkinen, T., Raita, T., Turc, L., and Vainio, R.: Differences in inner magnetospheric wave activity, outer Van Allen belt electron dynamics and atmospheric precipitation during CME sheaths and flux ropes, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6034, https://doi.org/10.5194/egusphere-egu2020-6034, 2020.

EGU2020-9575 | Displays | ST2.7

Eastward Propagating Second Harmonic Poloidal Waves Triggered by Temporary Outward Gradient of Proton Phase Space Density: Van Allen Probe A Observation

Kazuhiro Yamamoto, Masahito Nosé, Kunihiro Keika, David Hartley, Charles Smith, Robert MacDowall, Louis Lanzerotti, Donald Mitchell, Harlan Spence, Geoff Reeves, John Wygant, John Bonnell, and Satoshi Oimatsu

Two wave packets of second harmonic poloidal Pc 4 waves with a wave frequency of ~7 mHz were detected by Van Allen Probe A at a radial distance of ~5.8 RE and magnetic local time of 13 hr near the magnetic equator, where plasmaspheric refilling was in progress. Proton butterfly distributions with energy dispersions were also measured at the same time; the proton fluxes at 10–30 keV oscillated with the same frequency as the Pc 4 waves. Using the ion sounding technique, we find that the Pc 4 waves propagated eastward with an azimuthal wave number (m number) of ~220 and ~260 for each wave packet, respectively. Such eastward propagating high‐m (m > 100) waves were seldom reported in previous studies. The condition of drift‐bounce resonance is well satisfied for the estimated m numbers in both events. Proton phase space density was also examined to understand the wave excitation mechanism. We obtained temporal variations of the energy and radial gradient of the proton phase space density and find that temporal intensification of the radial gradient can generate the two wave packets. The cold electron density around the spacecraft apogee was >100 cm−3 in the present events, and hence the eigenfrequency of the Pc 4 waves became lower. This causes the increase of the m number which satisfies the resonance condition of drift‐bounce resonance for 10–30 keV protons and meets the condition for destabilization due to gyrokinetic effect.

How to cite: Yamamoto, K., Nosé, M., Keika, K., Hartley, D., Smith, C., MacDowall, R., Lanzerotti, L., Mitchell, D., Spence, H., Reeves, G., Wygant, J., Bonnell, J., and Oimatsu, S.: Eastward Propagating Second Harmonic Poloidal Waves Triggered by Temporary Outward Gradient of Proton Phase Space Density: Van Allen Probe A Observation, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-9575, https://doi.org/10.5194/egusphere-egu2020-9575, 2020.

EGU2020-22404 | Displays | ST2.7

Observations and simulations of electron flux oscillations in response to broadband ULF waves

Xinlin Li, Theodoros Sarris, Michael Temerin, Hong Zhao, Leng Ying Khoo, Drew Turner, Wenlong Liu, and Seth Claudepierre

It has recently been demonstrated through simulations and observations that flux oscillations of hundreds-keV electrons are produced in the magnetosphere in association with broadband Ultra Low Frequency (ULF) waves (Sarris et al., JGR, 2017). These oscillations are observed in the form of drift-periodic flux fluctuations, but are not associated with drift echoes following storm- or substorm-related energetic particle injections. They are observed in particular during quiet times, and it has been shown that they could indicate ongoing radial transport processes caused by ULF waves. It has also been shown that the width of electron energy channels is a critical parameter affecting the observed amplitude of flux oscillations, with narrower energy channel widths enabling the observation of higher-amplitude flux oscillations; this potentially explains why such features were not observed regularly before the Van Allen Probes era, as previous spacecraft generally had lower energy resolution. We extend these initial results by investigating the association between the observed flux oscillations with the amplitude of electric and magnetic fluctuations in the ULF range and with Phase Space Density gradients, both of which are expected to also affect radial transport rates.

How to cite: Li, X., Sarris, T., Temerin, M., Zhao, H., Khoo, L. Y., Turner, D., Liu, W., and Claudepierre, S.: Observations and simulations of electron flux oscillations in response to broadband ULF waves, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-22404, https://doi.org/10.5194/egusphere-egu2020-22404, 2020.

EGU2020-11063 | Displays | ST2.7

Understanding the controlling factors of Ultra-Low Frequency waves and their penetration during geomagnetic storms

Jonathan Rae, Kyle Murphy, Clare Watt, Jasmine Sandhu, Samuel Wharton, Alex Degeling, Marina Georgiou, Colin Forsyth, Sarah Bentley, Frances Staples, and Quanqi Shi

Wave-particle interactions play a key role in radiation belt dynamics. Traditionally, Ultra-Low Frequency (ULF) wave-particle interaction is parameterised statistically by a small number of controlling factors for given solar wind driving conditions or geomagnetic activity levels. Here, we investigate solar wind driving of ultra-low frequency (ULF) wave power and the role of the magnetosphere in screening that power from penetrating deep into the inner magnetosphere. We demonstrate that, during enhanced ring current intensity, the Alfvén continuum plummets, allowing lower frequency waves to penetrate deeper into the magnetosphere than during quiet periods. With this penetration, ULF wave power is able to accumulate closer to the Earth than characterised by statistical models. During periods of enhanced solar wind driving such as coronal mass ejection driven storms, where ring current intensities maximise, the observed penetration provides a simple physics-based reason for why storm-time ULF wave power is different compared to non-storm time waves. We demonstrate statistically that the ring current plays a pivotal role in allowing ULF wave energy to access the inner magnetosphere and show a new parameterisation of ULF wave power for radiation belt research purposes that is specifically tuned for geomagnetic storms.

How to cite: Rae, J., Murphy, K., Watt, C., Sandhu, J., Wharton, S., Degeling, A., Georgiou, M., Forsyth, C., Bentley, S., Staples, F., and Shi, Q.: Understanding the controlling factors of Ultra-Low Frequency waves and their penetration during geomagnetic storms, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11063, https://doi.org/10.5194/egusphere-egu2020-11063, 2020.

EGU2020-5642 | Displays | ST2.7

Probabilistic ULF models: how do they improve our understanding of the physics?

Sarah Bentley, Clare Watt, and Rhys Thompson

Probabilistic modelling is used heavily in weather and climate models to accurately represent the full range of possible physical states, thereby improving forecasts and capturing the uncertainty inherent in a complex system. Here, we begin to apply probabilistic modelling to ULF waves. Eventually, we aim to better determine the impact of ULF waves on Earth’s radiation belts; by representing the full probability distribution of radial diffusion coefficients we will represent physical reality more faithfully than solely using the mean or median.

However, to construct such a model, we first need to determine the probability distributions of the radial diffusion coefficient, which varies with the power in the underlying ULF waves. Therefore we present an analysis of the distributions of wave power spectral density for both ground-based magnetometers (CARISMA) and the corresponding in situ observations. We compare these distributions, examine the relationships between them and comment on the new physical insights this probabilistic approach reveals. Differences between distributions seen on the ground and in space give us new insights into the generation and propagation of ULF waves in the magnetosphere. We comment on the consequences of these types of distributions for probabilistic modelling. We also discuss how these distributions change with the driving solar wind; in particular, whether upper and lower bounds of power at the ground determined by the solar wind are seen in space. These bounds may indicate a limit to the ability of the magnetosphere to support ULF waves, and therefore limits on the resulting radial diffusion.

How to cite: Bentley, S., Watt, C., and Thompson, R.: Probabilistic ULF models: how do they improve our understanding of the physics?, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5642, https://doi.org/10.5194/egusphere-egu2020-5642, 2020.

EGU2020-1966 | Displays | ST2.7

Solar Wind induced waves in the skies of Mars: Ionospheric compression, energization, and escape resulting from the impact of ultra-low frequency magnetosonic waves generated upstream of the Martian bow shock

Glyn Collinson, Lynn Wilson III, Nick Omidi, David Sibeck, Jared Espley, Christopher Fowler, David Mitchell, Joseph Grebowsky, Christian Mazelle, Suranga Ruhunusiri, Jasper Halekas, Bruce Jakosky, and Yuki Harada

Using data from the NASA Mars Atmosphere and Voltatile EvolutioN (MAVEN) and ESA Mars Express spacecraft, we show that transient phenomena in the foreshock and solar wind can directly inject energy into the ionosphere of Mars. We demonstrate that the impact of compressive Ultra-Low Frequency (ULF) waves in the solar wind on the induced magnetospheres drive compressional, linearly polarized, magnetosonic ULF waves in the ionosphere, and a localized electromagnetic "ringing" at the local proton gyrofrequency. The pulsations heat and energize ionospheric plasmas. A preliminary survey of events shows that no special upstream conditions are required in the interplanetary magnetic field or solar wind. Elevated ion densities and temperatures in the solar wind near to Mars are consistent with the presence of an additional population of Martian ions, leading to ion-ion instablities, associated wave-particle interactions, and heating of the solar wind. The phenomenon was found to be seasonal, occurring when Mars is near perihelion. Finally, we present simultaneous multipoint observations of the phenomenon, with the Mars Express observing the waves upstream, and MAVEN observing the response in the ionosphere. When these new observations are combined with decades of previous studies, they collectively provide strong evidence for a previously undemonstrated atmospheric loss process at unmagnetized planets: ionospheric escape driven by the direct impact of transient phenomena from the foreshock and solar wind.

How to cite: Collinson, G., Wilson III, L., Omidi, N., Sibeck, D., Espley, J., Fowler, C., Mitchell, D., Grebowsky, J., Mazelle, C., Ruhunusiri, S., Halekas, J., Jakosky, B., and Harada, Y.: Solar Wind induced waves in the skies of Mars: Ionospheric compression, energization, and escape resulting from the impact of ultra-low frequency magnetosonic waves generated upstream of the Martian bow shock, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1966, https://doi.org/10.5194/egusphere-egu2020-1966, 2020.

EGU2020-18264 | Displays | ST2.7

Modelling the Rebuilding the Radiation Belt Following a Drop-out Event from Acceleration of the Seed Population

Hayley Allison, Yuri Shprits, Sarah Glauert, Richard Horne, and Dedong Wang

The Earth’s electron radiation belts are a dynamic environment and can change dramatically on short timescales. From Van Allen Probes observations, we see storm time drop-out events followed by a rapid recovery of the electron flux over a broad range of energies. Substorms can supply a seed population of new electrons to the radiation belt region, which are then energised by a number of processes, rebuilding the belts. However, how the electron flux is replenished across energy space, and the sequence of events leading to flux enhancements, remains an open question. Here we use a 3-D radiation belt model to explore how the seed population is accelerated to 1 MeV on realistic timescales, comparing the output to Van Allen Probes observations. By using a low energy boundary condition derived by POES data we encompass the whole radiation belt region, employing an open outer boundary condition. This approach isolates the contribution of seed population changes and allows electron flux variations over a broad range of L* to be studied. Using the model, we explore the contribution of both local acceleration and radial diffusion and demonstrate that the timing and duration of these two processes, particularly in relation to one another, is important to determine how the radiation belt rebuilds.

How to cite: Allison, H., Shprits, Y., Glauert, S., Horne, R., and Wang, D.: Modelling the Rebuilding the Radiation Belt Following a Drop-out Event from Acceleration of the Seed Population, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18264, https://doi.org/10.5194/egusphere-egu2020-18264, 2020.

EGU2020-1014 | Displays | ST2.7

Association of chorus waves and source/seed electrons with the enhancement of relativistic electrons in the outer Van Allen belt

Afroditi Nasi, Ioannis A. Daglis, Christos Katsavrias, and Wen Li

Local acceleration driven by whistler-mode chorus waves is fundamentally important for the acceleration of seed electrons in the outer radiation belt to relativistic energies. Τhis mechanism strongly depends on substorm activity and on the source electron population injected by the substorms into the inner magnetosphere. In our work we use Van Allen Probes data to investigate the features of source electrons, seed electrons and chorus waves for events of enhancement versus events of depletion of relativistic electrons in the outer Van Allen belt. To that end we calculate the electron phase space density (PSD) for five values of the first adiabatic invariant corresponding to source and seed electrons, and we perform a superposed epoch analysis of 28 geomagnetic disturbance events, out of which, 20 result in enhancement and 8 in depletion of relativistic electron PSD. Our results indicate that events resulting in significant enhancement of relativistic electron PSD in the outer radiation belt are characterized by statistically stronger and more prolonged storm and substorm activity, leading to more efficient injections of source but mostly seed electrons to the inner magnetosphere, and also to more pronounced and long-lasting chorus and Pc5 wave activity. The effect of these parameters in the acceleration of electrons seems to be determined by the abundance of seed electrons at the region of L*=4-5.

How to cite: Nasi, A., Daglis, I. A., Katsavrias, C., and Li, W.: Association of chorus waves and source/seed electrons with the enhancement of relativistic electrons in the outer Van Allen belt, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1014, https://doi.org/10.5194/egusphere-egu2020-1014, 2020.

EGU2020-12266 | Displays | ST2.7

Statistical Study of Pitch Angle Diffusion during Substorm Injections

Reihaneh Ghaffari and Christopher Cully

Energetic Electron Precipitation (EEP) associated with substorm injections typically occurs when magnetospheric waves, particularly whistler-mode waves, resonantly interact with electrons to affect their equatorial pitch angle. This can be considered as a diffusion process that scatters particles into the loss cone. In this study, we investigate whistler-mode wave generation in conjunction with electron injections using in-situ wave measurements by the Themis mission. We calculate the pitch angle diffusion coefficient exerted by the observed wave activity using the quasi-linear diffusion approximation and estimate scattering efficiency in the substorm injection region to constrain where and how much scattering happens typically during these events.

How to cite: Ghaffari, R. and Cully, C.: Statistical Study of Pitch Angle Diffusion during Substorm Injections, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-12266, https://doi.org/10.5194/egusphere-egu2020-12266, 2020.

EGU2020-6892 | Displays | ST2.7

Proton and electron fluxes in the plasma sheet transition region and their dependence on the solar wind parameters

Stepanov Nikita, Viktor Sergeev, Dmitry Sormakov, Stepan Dubyagin, and Andrey Runov

Proton and electron spectra in the plasma sheet usually consist of spectral core and high energy tail. These two populations are formed by different processes, driven by the various combinations of the solar wind parameters.These processes include different time delays and may act differently on protons or electrons. In this work we evaluate empirically the magnitude and the time delay of the impact of different solar wind parameter combinations on the protons and electrons with energies (30-300 keV) and reveal the mechanisms behind these impacts. To do this we build a model of the fluxes at different energy channels in the transition region (nightside central plasma sheet between 6 and 15 Re) for the THEMIS spacecraft observations in 2007-2018. We use normalized values of solar wind parameter combinations (incl. speed, density, pressure, electric field, etc) as inputs of the model, with regression coefficients indicating their impact magnitudes. We investigate different time delays up to 16 hours. The model obtained shows that protons and electrons are controlled differently by solar wind parameters: dynamic pressure is important for protons, whereas solar wind speed and VBs are important for electrons. Larger time delays are required to describe higher energy electron fluxes.

How to cite: Nikita, S., Sergeev, V., Sormakov, D., Dubyagin, S., and Runov, A.: Proton and electron fluxes in the plasma sheet transition region and their dependence on the solar wind parameters, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6892, https://doi.org/10.5194/egusphere-egu2020-6892, 2020.

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CSES monitoring of the interplay between current-sheet and EMIC-wave driven scattering as a proxy of substorm activity

Alexandra Parmentier, Matteo Martucci, Mirko Piersanti, and the CSES-Limadou Collaboration

Plasma injections from Earth’s magnetotail to high-latitude ionosphere pro-
vided by substorm activity are known to play a key role in the MeV-electron
acceleration mechanism by resonating interaction of very-low-frequency (VLF)
chorus waves with seed electrons. On the other hand, non-adiabatic motion
of plasma-sheet protons related to current sheet scattering (CSS) causes pitch-
angle diffusion and precipitation to the ionosphere, inducing the formation of
a characteristic energy-latitude dispersion pattern at the equatorward side of
the auroral isotropy boundary (IB), which gets significantly altered during geo-
magnetic storms due to particle precipitation triggered by electromagnetic ion
cyclotron (EMIC) waves.
For these last two years, a moderate geomagnetic storm activity has been affect-
ing the Earth’s environment, with the notable case of Aug 2018 G3-class storm.
The effects of such disturbances - especially in case of prolonged substorm ac-
tivity during the recovery phase - have been clearly spotted by the entire suite
of detectors on board the China Seismo-Electromagnetic Satellite (CSES-01), a
low-Earth-orbit (LEO) mission launched on Feb 2, 2018.
Here, we present long-term storm-time observations by particle, e.m.-field, and
plasma instrumentation on board CSES-01, namely the High-Energy Particle
Detector (HEPD), the Electric Field Detector (EFD), and the High Precision
Magnetometer (HPM), either developed or data-validated by the Italian LI-
MADOU Collaboration. Thanks to magnetosphere-to-ionosphere mapping, re-
sults from HEPD, EFD, and HPM data analysis help track substorm plasma
injections and consequent magnetosphere re-arrangement on a statistical basis.
This further inscribes CSES-01 into the thematic area of space-weather and
space-climate exploration and modeling, which is especially important in a pe-
riod when many key space-weather instruments have been quit or operate well
beyond the end of their scheduled lifetimes.

How to cite: Parmentier, A., Martucci, M., Piersanti, M., and CSES-Limadou Collaboration, T.: CSES monitoring of the interplay between current-sheet and EMIC-wave driven scattering as a proxy of substorm activity, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2330, https://doi.org/10.5194/egusphere-egu2020-2330, 2020.

EGU2020-1284 | Displays | ST2.7

Second order statistical moments of scattered electromagnetic waves in the conductive magnetized ionospheric plasma

Giorgi Jandieri, Akira Ishimaru, and Jaromir Pistora

The ionosphere is greatly influenced by ionizing radiation including both electromagnetic flux and energetic particles. The ionosphere is immersed in a magnetic field and the interactions of radio waves with the ionosphere are complex and exhibit the following properties: anisotropy, absorption, dispersion, birefringent. The ionospheric effects on radiowave systems depend upon the focus of the treatment. The development of inhomogeneous electron density structures is responsible for radiowave signal fluctuations. A comprehensive treatment of radiowaves propagation in the ionospheric plasma is based on the investigation of the statistical moments of both amplitude and phase fluctuations of scattered radiation. In this paper analytical calculations of the statistical characteristics in the conductive collision magnetized ionospheric plasma have been carried out for the first time using the complex geometrical optics approximation. Stochastic wave equation of the phase fluctuations includes both dielectric permittivity and conductivity tensors which are random functions of the spatial coordinates and time. Using the boundary conditions correlation function of the phase fluctuations has been obtained for arbitrary second order statistical moment of electron density fluctuations (large and small ionospheric plasmonic structures); observation points are spaced at small distance. The index of refraction contains both ordinary and extraordinary waves. Angular power spectrum (broadening, shift of its maximum) of scattered electromagnetic waves is investigated. It was shown that Hall’s, Pedersen, and longitudinal conductivities have a substantial influence on the frequency fluctuation of an incident wave. Doppler spread associated with random ionospheric structure, and Doppler shifts associated with relative motion of the ray path with respect to the elongated plasmonic structures. Spatial-temporal broadening of the spatial spectrum depends on the anisotropy factor of elongated plasma irregularities, inclination angle with respect to the lines of forces of geomagnetic field, collision frequency between plasma particles, conductivity fluctuations, and the movement of ionospheric plasmonic irregularities. Shift of the spectral maximum changes the sign depending on the anisotropy factor of elongated plasma irregularities, inclination angle with respect to the lines of forces of geomagnetic field and conductivity fluctuations. Numerical calculations and spatial-temporal modeling are carried out for both large and small-scale ionospheric plasma irregularities using experimental data and experimentally observing power-law spectrum of electron density fluctuations. The obtained results are useful for solving the reverse problem restoring plasma parameters, in satellite communication and navigation systems that operate in the earth-space regime. The influence of the conductivity fluctuations on the second order statistical moments will open new horizons in understanding and forecasting new phenomena in the upper ionosphere caused due to spatial-temporal parameters fluctuations.

 

How to cite: Jandieri, G., Ishimaru, A., and Pistora, J.: Second order statistical moments of scattered electromagnetic waves in the conductive magnetized ionospheric plasma, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1284, https://doi.org/10.5194/egusphere-egu2020-1284, 2020.

EGU2020-18386 | Displays | ST2.7

Plasmasphere observations with Cluster data supplemented with data from the Dynamics Explorer-1 and Van Allen Probes missions

Fabien Darrouzet, Johan De Keyser, Pierrette Décréau, Dennis Gallagher, Giuli Verbanac, and Mario Bandic

Since 2000 the four Cluster spacecraft have crossed the Earth's plasmasphere along a polar orbit every 2.5 days, with various perigee altitudes (from 1.5 to 4 RE), different configurations (string of pearls, tetrahedron) and changing separations (from 10 to 100 000 km). The resulting dataset allows different types of inner magnetosphere studies and provides insight in plasmasphere dynamics, including changes in plasmapause position. Plasmaspheric plumes can also be studied on a case-by-case basis, in a statistical manner and in relation with wave activity (EMIC, electromagnetic rising tone, whistler waves).

Moreover, data from an old mission, Dynamics Explorer-1, have recently become available. In particular, densities and temperatures for many ions (H+, He+, He++, O+, and O++) have been derived from the RIMS (Retarding Ion Mass Spectrometer) instrument and are available from October 1981 to January 1985. Such composition data, not available from the Cluster satellites, allow in particular to analyze the distributions of those ions in the plasmasphere boundary layer, as a function of magnetic local time and geomagnetic activity.

Finally, since 2012, the two Van Allen Probes satellites are orbiting the inner magnetosphere in the magnetic equatorial plane and with a low perigee, allowing a crossing of the plasmasphere every 9 hours. The EMFISIS (Electric and Magnetic Field Instrument Suite and Integrated Science) instrument onboard both spacecraft can determine the electron density in a very large density range (up to 3000 cm-3) using several methods. This gives a different opportunity to analyze the plasmapause and plasmaspheric plumes from a different perspective.

How to cite: Darrouzet, F., De Keyser, J., Décréau, P., Gallagher, D., Verbanac, G., and Bandic, M.: Plasmasphere observations with Cluster data supplemented with data from the Dynamics Explorer-1 and Van Allen Probes missions, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18386, https://doi.org/10.5194/egusphere-egu2020-18386, 2020.

EGU2020-2432 | Displays | ST2.7

On the upper frequency limit of whistler mode waves observed by low-altitude spacecraft

Frantisek Nemec, Ondřej Santolík, and Michel Parrot

Frequency-latitude plots of electromagnetic wave intensity in the very low frequency range (VLF, up to about 20 kHz) observed by the low altitude DEMETER spacecraft are analyzed. Apart from electromagnetic waves generated by plasma instabilities in the magnetosphere, a significant portion of the detected wave intensity comes from ground-based lightning activity and VLF military transmitters. These whistler mode waves are observed not only close to source locations, but also close to their geomagnetically conjugated points. There appears to be an upper frequency limit of such emissions, where the wave intensity substantially decreases. Its frequency roughly corresponds to half of the equatorial electron cyclotron frequency at a respective magnetic field line, suggesting a relation to wave ducting in ducts with enhanced density. However, it seems to exhibit a non-negligible longitudinal dependence and it is different during the day than during the night. We use a realistic model of the Earth’s magnetic field to explain the observed variations. We interpret the observations in terms of ducted/unducted wave propagation, and we compare the wave intensities in the source hemisphere with those measured in the hemisphere geomagnetically conjugated.

How to cite: Nemec, F., Santolík, O., and Parrot, M.: On the upper frequency limit of whistler mode waves observed by low-altitude spacecraft, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2432, https://doi.org/10.5194/egusphere-egu2020-2432, 2020.

EGU2020-2435 | Displays | ST2.7

Energetic particle flux variations detected at low altitudes by Space Application of Timepix Radiation Monitor (SATRAM)

Stefan Gohl, František Němec, Benedikt Bergmann, and Stanislav Pospíšil

The Space Application of Timepix Radiation Monitor (SATRAM) on board the Proba-V satellite of the European Space Agency (ESA) was launched in May 2013 into a sun-synchronous orbit with an altitude of about 820 km. This technology demonstration payload is based on the Timepix technology developed by the CERN-based Medipix2 Collaboration. It is equipped with a 300 um thick silicon sensor with a pixel pitch of 55 um in a 256 x 256 pixel matrix. The device is sensitive to X-rays and all charged particles. A Monte Carlo simulation was conducted to determine the detector response to electrons (0.5–7 MeV) and protons (10–400 MeV) taking into account the shielding of the detector housing and the satellite. With the help of the simulation, a strategy was developed to estimate omnidirectional electron, proton, and ion fluxes around Earth using stopping power, maximum energy deposition per pixel of the particle track, and the shape of the particle tracks in the sensor. Presented are typical overall dose rates as well as fluxes of individual particle species. A superposed epoch analysis is used to analyze variations of particle fluxes related to geomagnetic storms and interplanetary shock arrivals as a function of time and L-shell.

How to cite: Gohl, S., Němec, F., Bergmann, B., and Pospíšil, S.: Energetic particle flux variations detected at low altitudes by Space Application of Timepix Radiation Monitor (SATRAM), EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2435, https://doi.org/10.5194/egusphere-egu2020-2435, 2020.

EGU2020-11503 | Displays | ST2.7

Equatorial pitch angle distributions in Earth's radiation belts: an empirical model from Van Allen Probes data

Artem Smirnov, Yuri Shprits, Hayley Allison, and Nikita Aseev

Earth’s radiation belts comprise complex and dynamic systems, depending substantially on solar activity. The pitch angle distributions (PADs) play an important role for radiation belts modelling, as they yield information on the particle transport, source and loss processes. Yet, many missions flying in the radiation belts provide omni-directional or uni-directional electron flux measurements and do not resolve pitch angles. We propose an empirical model of the equatorial PADs and a method to retrieve PADs from omni-directional flux measurements at different energies and locations along the inclined orbits. We use the entire dataset of MagEIS and REPT instruments aboard the Van Allen Probes (RBSP) mission to analyze the equatorial pitch angle distributions in the energy range from 30 keV to 6.2 MeV. The fitting method resolves all main types of PADs, including butterfly and cap distributions, and the resulting coefficients are directly related to the PAD shapes. The developed model can be used to obtain pitch angle resolved fluxes for GPS, Arase and other missions. The proposed algorithm is applied to the GPS electron flux data set to obtain the pitch-angle resolved fluxes, which are compared to the RBSP data at a number of GPS-RBSP conjunctions. The proposed model also allows one to reconstruct the pitch-angle resolved data using LEO measurements. The dynamics of the fitting coefficients based on solar activity is discussed with respect to AE, Kp, Dst indices and solar wind parameters: velocity, density and dynamic pressure.

How to cite: Smirnov, A., Shprits, Y., Allison, H., and Aseev, N.: Equatorial pitch angle distributions in Earth's radiation belts: an empirical model from Van Allen Probes data, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11503, https://doi.org/10.5194/egusphere-egu2020-11503, 2020.

EGU2020-2055 | Displays | ST2.7

Chorus acceleration of relativistic electrons in extremely low L-shell during geomagnetic storm

Zhenxia Zhang, Lunjin Chen, Si Liu, Ying Xiong, Xinqiao Li, and Xuhui Shen

Based on data from the Van Allen Probes and ZH-1 satellites, relativistic electron enhancements in extremely low L-shell Regions (reaching L~3) were observed during major geomagnetic storm (minimum Dst`-190 nT).  Contrary to what occurs in the outer belt, such an intense and deep electron penetration event is rare and more interesting. Strong whistler-mode (chorus and hiss) waves, with amplitudes 81-126 pT, were also observed in the extremely low L-shell simultaneously (reaching L~2.5) where the plasmapause was suppressed. The bounce-averaged diffusion coefficient calculations support that the chorus waves can play a significantly important role in diffusing and accelerating the 1-3 MeV electrons even in such low L-shells during storms. This is the first time that the electron acceleration induced by chorus waves in the extremely low L-shell region is reported. This new finding will help to deeply understand the electron acceleration process in radiation belt physics.

How to cite: Zhang, Z., Chen, L., Liu, S., Xiong, Y., Li, X., and Shen, X.: Chorus acceleration of relativistic electrons in extremely low L-shell during geomagnetic storm, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2055, https://doi.org/10.5194/egusphere-egu2020-2055, 2020.

The last decade has shown the prime importance of wave-particle interaction for the accurate modelling of the dynamics of energetic electrons trapped in the Earth’s radiation belts, as well as for other planets, such as Jupiter or Saturn. They have been therefore added in the sum of physical processes modeled in radiation belt codes such as Salammbô, with conclusive results. However, this upgrade of the physical representation is not straightforward and comes at the price of degrading the numerical resolution. In particular, computational instabilities and odd phase space density profiles are observed, impacting the code’s accuracy and its physical relevance. This challenging issue requires the development of a numerical scheme which supports in particular wave-particle cross diffusion terms. Thus, we will present in this talk the new dedicated numerical scheme we have developed and implemented in Salammbô. Then we will focus on quantifying the effect of wave-particle cross diffusion terms on the dynamics of highly energetic trapped electrons, in presenting results for real case storms.

How to cite: Dahmen, N., Maget, V., and Rogier, F.: Evaluating the effect of wave-particle cross diffusion in radiation belts modelling using an innovative and robust numerical scheme, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3562, https://doi.org/10.5194/egusphere-egu2020-3562, 2020.

EGU2020-18676 | Displays | ST2.7

The model of outer radiation belt electron lifetimes based on combined Van Allen Probes and Cluster VLF wave measurements

Homayon Aryan, Oleksiy Agapitov, Anton Artemyev, Michael Balikhin, Didier Mourenas, and Richard Boynton

The flux of highly energetic electrons in the outer radiation belt show a high variability during geomagnetically disturbed conditions. Wave-particle interaction with VLF chorus waves play a significant role in the flux variation of these particles, and quantification of the effects from these interactions is crucially important for accurately modeling the global dynamics of the outer radiation belt and for providing a comprehensive description of electron flux variations over a wide energy range (from the source population of keV electrons to the relativistic core population of the outer radiation belt).  In this study, we use the synthetic model based on the combined database from the Van Allen Probes and Cluster spacecraft VLF measurements (including the recent findings of wave amplitude dependence on geomagnetic latitude, wave normal angle distribution, and variations of wave frequency with latitude) to develop a comprehensive parametric model of electron lifetime in the outer radiation belt as a function of geomagnetic activity, L-shell, and magnetic local time. Results show high local scattering rates during moderate and active conditionslocal scattering is higher on the dawn and night side compared to day side, and electron lifetime is short during active conditions. 

How to cite: Aryan, H., Agapitov, O., Artemyev, A., Balikhin, M., Mourenas, D., and Boynton, R.: The model of outer radiation belt electron lifetimes based on combined Van Allen Probes and Cluster VLF wave measurements , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18676, https://doi.org/10.5194/egusphere-egu2020-18676, 2020.

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System identification models for waves in the inner magnetosphere

Richard Boynton, Homayon Aryan, Walker Simon, and Michael Balikhin

This research develops forecast models of the spatiotemporal evolution of emissions throughout the inner magnetosphere between L=2-6 and at all MLT. The system identification, or machine learning, technique based on Nonlinear AutoRegressive Moving Average eXogenous (NARMAX) models is employed to deduce the forecasting models of the lower band chorus, Hiss, and magnetosonic waves using solar wind and geomagnetic indices as inputs. It is difficult to develop machine leaning based spatiotemporal models of the waves in the inner magnetosphere as the data is sparse and machine learning techniques require large amounts of data to deduce a model. To solve this problem, the spatial co-ordinates at the time of the measurements are included as inputs to the model along with time lags of the solar wind and geomagnetic indices, while the measurement of the waves by the Van Allen Probes are used as the output to train the models. The estimates of the resultant models are compared with separate data to the training data to assess the performance of the models. The models are then used to reconstruct the spatiotemporal waves over the inner magnetosphere, as the waves respond to changes in the solar wind and geomagnetic indices.  

How to cite: Boynton, R., Aryan, H., Simon, W., and Balikhin, M.: System identification models for waves in the inner magnetosphere, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-16544, https://doi.org/10.5194/egusphere-egu2020-16544, 2020.

In situ measurements of electron scale fluctuations by the Van Allen Probes and MMS have demonstrated the ubiquitous occurrence of phase-space holes and various kinetic nonlinear structures in the Earth's magnetosphere. However it remains an open question whether phase-space holes have to be incorporated into global magnetospheric models describing the energisation and acceleration of electrons. In this communication we will review current wave-particle models of electron phase-space holes interacting with energetic electrons (e.g. >1 keV in the Earth's radiation belts)  and present new theoretical results showing that finite correlation times of phase-space holes results in enhanced pitch-angle scattering. The pitch-angle scattering by phase-space holes is shown to be on par with that produced by chorus waves, and in some instances outgrows the chorus contribution. 

 

How to cite: Osmane, A.: Effect of finite correlation time on the wave-particle interactions of nonlinear electrostatic structures with electrons in the Earth's radiation belts., EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21856, https://doi.org/10.5194/egusphere-egu2020-21856, 2020.

EGU2020-2039 | Displays | ST2.7

Periodic modulation of the upper ionosphere by ULF waves as observed by SuperDARN radars and GPS/TEC technique

Vyacheslav Pilipenko, Olga Kozyreva, Emma Bland, and Lisa Baddeley

We compare the simultaneous magnetometer, SuperDARN radar, and GPS observations during Pc5 wave event on March 02, 2002. A possible correspondence between those instruments may help to determine the mechanism of the ionosphere modulation by magnetospheric disturbances. Transient Pc5 pulsations (2.6 mHz) in the morning sector, stimulated by the solar wind density jumps, have been detected simultaneously by ground magnetometers and the Kodiak and King Salmon SuperDARN radars.  Besides that, pulsations with the same periodicity have been found in the rate of total electron content (TEC), dTEC/dt (ROT), variations in several GPS radio paths. The ratio between the spectral amplitudes of the Doppler velocities and magnetic pulsations (X component) on the ground are Vx/Bx~7-12 (m/s)/nT and Vy/Bx~27 (m/s)/nT. The ratio between the oscillation amplitudes of ROT and ionospheric Doppler meridional (Vx) and azimuthal (Vy) velocities are ROT/Vx~0.02-0.07 (dTECu/min)/(m/s) and ROT/Vy~0.004 (dTECu/min)/(m/s). The correspondence between simultaneous periodic variations of the ionospheric Doppler velocity and geomagnetic field can be reasonably well interpreted quantitively on the basis of theory of Alfven wave interaction with the thin ionospheric layer. However, order-of-magnitudes estimates of possible TEC modulation mechanisms show that a responsible mechanism which can interpret the observed ratios has not been found yet. 

How to cite: Pilipenko, V., Kozyreva, O., Bland, E., and Baddeley, L.: Periodic modulation of the upper ionosphere by ULF waves as observed by SuperDARN radars and GPS/TEC technique, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2039, https://doi.org/10.5194/egusphere-egu2020-2039, 2020.

EGU2020-6901 | Displays | ST2.7

ULF waves registered with the Ekaterinburg radar: Statistical analysis and case studies

Maksim Chelpanov, Olga Mager, Pavel Mager, and Dmitri Klimushkin

A midlatitude coherent decameter radar installed near Ekaterinburg, Russia (EKB radar) has been operating since 2012. It is aimed at monitoring dynamics of the ionosphere–magnetosphere system in Eastern Siberia. A special operation mode is used at the radar to study ULF wave activity: three adjacent beams oriented approximately along the magnetic meridian are surveyed with time resolution of 18 s each. A number of wave observation events registered with the radar was analyzed and discussed in several papers. An overview of the main results from these studies is presented here.

A statistical study of more than 30 waves observed in the nightside ionosphere revealed that in the majority of the cases their frequencies are considerably lower than those of field line resonance (FLR) for appropriate magnetic shells and longitudinal sectors (FLR fundamental frequencies for each case were estimated based on spacecraft data). Thus, these waves cannot be associated with the Alfvén mode. It was assumed that at least part of them should be identified with the drift compressional mode. Indeed, in individual cases oscillations exhibited signatures of this mode: in one of the events a linear dependence of frequency on azimuthal wave number m at a fixed magnetic shell was found. Only the drift compressional mode can feature such dependence in the inner magnetosphere. For two other cases merging of drift compressional and Alfvén modes at some critical value of m was shown. A case of simultaneous spacecraft and radar wave observation accompanied by increases in energetic particle fluxes was shown. A modulation with the frequency of this wave was found for flux intensity of those energetic protons, whose phase velocity is close to that of the wave. This implies that the source of the wave was a drift resonance with the substorm injected protons.

How to cite: Chelpanov, M., Mager, O., Mager, P., and Klimushkin, D.: ULF waves registered with the Ekaterinburg radar: Statistical analysis and case studies, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6901, https://doi.org/10.5194/egusphere-egu2020-6901, 2020.

The GOES-16 spacecraft, launched in November 2016, is the first of the GOES-R series next generation NOAA weather satellites. The spacecraft has a similar suite of space weather instruments to previous GOES satellites but with improved magnetometer sampling rate and wider energy range of particle flux observations. Presented are observations of simultaneously occurring Pc 4/5 ULF waves and electromagnetic ion cyclotron (EMIC) waves with a discussion on the relationship between the two wave modes including possible generation mechanisms. The waves were also observed in the particle data and we discuss both adiabatic and non-adiabatic wave-particle effects. Relativistic electron fluxes showed strong adiabatic motion with the magnetic field ULF waves. Estimates of Pc 4/5 ULF wave m-numbers suggest they were high, while ring current energy ion fluxes showed ULF variations with non-zero phasing relative to magnetic field ULF wave. This suggests ULF wave drift resonance with ring current ions. In one event we observed EMIC variations in the ion fluxes around energies that can drift resonate with simultaneously observed Pc 5 waves, suggesting that one particle population may be responsible for generating and/or modifying both observed Pc 5 and EMIC waves. ULF variations were also observed in electron/ion fluxes at lower energies down to 30 eV. We looked into ULF bounce resonance with 30 eV electrons, but the resonance condition did not match the observations. We will also discuss future plans to expand this study of ULF waves and wave-particle interactions using the two newest GOES satellites.

How to cite: Loto'aniu, P.: Observations of simultaneously occurring ULF and Ion Cyclotron Waves by the GOES-16 satellite magnetometer and particle detectors at geostationary orbit, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6164, https://doi.org/10.5194/egusphere-egu2020-6164, 2020.

We use  multipoint magnetic field, plasma  and particle observations to study the spatial, temporal  and spectral characteristics of Pc 4-5 pulsations   observed  in the recovery phase of a strong magnetic storm on January 1, 2016.   The magnetosphere was compressed and periodic increases of the total magnetic field strength occurred every 20-40 min at the times of generation of the pulsations.  The frequencies of the Pc4 pulsations varied  from 14 mHz to 25 mHz with radial distance. An explanation for this behavior can be given in terms of standing Alfvén waves along resonant field lines.  By contrast, Fourier analysis of the magnetic field observations  shows that the compressional  Pc5 pulsations  exhibited  similar spectra at different radial distances.  The long duration of the Pc5 pulsations and their nearly constant frequencies indicate that the plasma conditions in the morning sector of magnetosphere were stable for more than two hours.  The Pc4 and Pc5   pulsations displayed wave properties consistent with the second harmonic waves. The energetic particles   observed by Van Allen Probes and GOES 15  exhibited  a regular periodicity over a  broad range of energies from tens of eV to 2 MeV  with periods  corresponding to  those of the compressional component   of the  ULF magnetic field.   We searched for possible solar wind triggers and discussed generation mechanisms for the compressional Pc5 pulsations  in terms of drift mirror instability and  drift bounce resonance. 

How to cite: Korotova, G., Sibeck, D., and Engebretson, M.: Multipoint observations of spatial and temporal characteristics of Pc 4-5 pulsations in the dayside magnetosphere and particle signatures. , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-20948, https://doi.org/10.5194/egusphere-egu2020-20948, 2020.

EGU2020-2832 | Displays | ST2.7

Selective acceleration of O+ by drift-bounce resonance in the Earth’s magnetosphere: MMS observations

Satoshi Oimatsu, Masahito Nosé, Guan Le, Stephan A Fuselier, Robert E Ergun, Per-Arne Lindqvist, and Dmitry Sormakov

We studied O+drift-bounce resonance using Magnetospheric Multiscale (MMS) data. A case study of an event on 17 February 2016 shows that O+ flux oscillations at ~10–30 keV occurred at MLT ~ 5 hr and L~ 8–9 during a storm recovery phase. These flux oscillations were accompanied by a toroidal Pc5 wave and a high-speed solar wind (~550 km/s). The azimuthal wave number (m-number) of this Pc5 wave was found to be approximately –2. The O+/H+ flux ratio was enhanced at ~10–30 keV corresponding to the O+ flux oscillations without any clear variations of H+ fluxes, indicating the selective acceleration of O+ ions by the drift-bounce resonance. A search for the similar events in the time period from September 2015 to March 2017 yielded 12 events. These events were mainly observed in the dawn to the afternoon region at L~ 7–12 when the solar wind speed is high, and all of them were simultaneously identified on the ground, indicating low m-number. Correlation analysis revealed that the O+/H+ energy density ratio has the highest correlation coefficient with peak power of the electric field in the azimuthal component (Ea). This statistical result supports the selective acceleration of O+ due to the = 2 drift-bounce resonance.

How to cite: Oimatsu, S., Nosé, M., Le, G., Fuselier, S. A., Ergun, R. E., Lindqvist, P.-A., and Sormakov, D.: Selective acceleration of O+ by drift-bounce resonance in the Earth’s magnetosphere: MMS observations, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2832, https://doi.org/10.5194/egusphere-egu2020-2832, 2020.

Low‐energy ions of ionospheric origin with energies below 10s of electron volt dominate most
of the volume and mass of the terrestrial magnetosphere. However, sunlit spacecraft often become
positively charged to several 10s of volts, which prevents low‐energy ions from reaching the particle
detectors on the spacecraft. Magnetospheric Multiscale spacecraft (MMS) observations show that
ultralow‐frequency (ULF) waves drive low‐energy ions to drift in the E × B direction with a drift velocity
equal to VE×B, and low‐energy ions were accelerated to suffificient total energy to be measured by the
MMS/Fast Plasma Investigation Dual Ion Spectrometers. The maximum low‐energy ion energy flflux peak
seen in MMS1's dual ion spectrometer measurements agreed well with the theoretical calculation of H+ ion
E × B drift energy. The density of ions in the energy range below minimum energy threshold was
between 1 and 3 cm−3 in the magnetosphere subsolar region in this event.

How to cite: Li, B.: Magnetospheric Multiscale (MMS) Observations of ULF Waves and Correlated Low-Energy IonMonoenergetic Acceleration, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6858, https://doi.org/10.5194/egusphere-egu2020-6858, 2020.

Several observational studies have shown that ULF oscillations of the solar wind dynamic pressure can drive periodic fluctuations in magnetic field measurements at corresponding frequencies. In this study, we use multi-spacecraft (Cluster, GOES, THEMIS and Van Allen Probes) mission measurements to investigate the propagation of pressure fluctuations-driven pulsations within the Pc5 and Pc4 frequency range (from ~0.5 to 25 mHz) into the magnetosphere. During intervals of slow solar wind — to exclude waves generated by velocity shear at the magnetopause — common periodicities in electromagnetic fields in the magnetosphere and the solar wind driver are first detected in Lomb-Scargle periodograms. Then, using the cross-wavelet transform, we examine the causal relationship and specifically, in cross-wavelet spectra and wavelet transform coherence. Lastly, spatial and temporal variations of wave properties are mapped from beyond the magnetopause to the inner magnetosphere through frequency, polarisation and power signatures of waves detected at the various probes. The observed dependence of wave properties on their localisation offers an excellent source for verification of the role that solar wind dynamic pressure oscillations as driver of ULF waves propagating through the magnetosheath into the dayside and nightside magnetosphere.

How to cite: Georgiou, M., Katsavrias, C., Daglis, I., and Balasis, G.: Ultra-Low Frequency (ULF) waves originating in solar wind dynamic pressure oscillations and propagating through the magnetosheath to the inner magnetosphere, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21129, https://doi.org/10.5194/egusphere-egu2020-21129, 2020.

EGU2020-3146 | Displays | ST2.7

Wave Propagation and Global Implications of Magnetopause Surface Eigenmodes

Martin Archer, Michael Hartinger, Ferdinand Plaschke, and Lutz Rastaetter

Using global magnetohydrodynamic simulations we investigate the recently discovered eigenmode of the magnetopause surface – the natural response of the boundary to impulsive solar wind transients. We show that following the directly driven motion of the magnetopause by a pressure pulse, decaying oscillations of the boundary follow in agreement with theoretical predications and previous simulations of the magnetopause surface eigenmode. Across the equatorial magnetosphere these oscillations originate at the subsolar point and maintain a near-constant frequency through all local times, though into the flanks a secondary higher-frequency signal emerges consistent with the expectations of Kelvin-Helmholtz generated surface waves. Focusing only on the eigenmode shows its amplitude grows with local time away from the subsolar point, with the waves showing no azimuthal propagation in the region 9-15h MLT – surprising given the convecting effect downtail of the magnetosheath flow.  In the noon-midnight meridian the eigenmode is confined to the dayside magnetosphere. Comparing these results to MHD theory, we propose how the structure of the magnetopause surface eigenmode is determined by the properties of the magnetospheric system and how it may influence global dynamics during impulsive events.

How to cite: Archer, M., Hartinger, M., Plaschke, F., and Rastaetter, L.: Wave Propagation and Global Implications of Magnetopause Surface Eigenmodes, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3146, https://doi.org/10.5194/egusphere-egu2020-3146, 2020.

EGU2020-5562 | Displays | ST2.7

Observation and Numerical Simulation of Propagation of ULF Waves From the Ion Foreshock Into the Magnetosphere

Kazue Takahashi, Turc Turc, Emilia Kilpua, Naoko Takahashi, Andrew Dimmock, Primoz Kajdic, Minna Palmroth, Yann Pfau-Kempf, Jan Soucek, Howard Singer, Tetsuo Motoba, and Craig Kletzing

Observational studies have demonstrated that ULF waves excited in the ion foreshock are a main source of Pc3-4 ULF waves detected in the magnetosphere. However, quantitative understanding of the propagation of the waves is not easy, because the waves are generated through a kinetic process in the foreshock, pass through the turbulent magnetosheath, and propagate as fast mode waves and couple to shear Alfven waves within the magnetosphere.  Recent advancement of hybrid numerical simulations of foreshock dynamics motivated us to analyze observational data from multiple sources and compare the results with simulation results. We have selected the time interval 1000-1200 UT on 20 July 2016, when the THEMIS, GOES, and Van Allen Probe spacecraft covered the solar wind, foreshock, magnetosheath, and magnetosphere. The EMMA magnetometers (L=1.6-6.5) were located near noon. We found that the spectrum of the magnetic field magnitude (Bt) in the foreshock exhibits a peak near 90 mHz, which agrees with the theoretical prediction assuming an ion beam instability in the foreshock.  A similar Bt spectrum is found in the dayside outer magnetosphere but not in the magnetosheath or in the nightside magnetosphere.  On the ground, a 90 mHz spectral peak was detected in the H component only at L=2-3. The numerical simulation using the VLASIATOR code shows that the foreshock is formed on the prenoon sector but that the effect of the upstream waves in the magnetosphere is most pronounced at noon. The Bt spectrum of the simulated waves in the outer magnetosphere exhibits a peak at 90 mHz, which is consistent with the observation.

How to cite: Takahashi, K., Turc, T., Kilpua, E., Takahashi, N., Dimmock, A., Kajdic, P., Palmroth, M., Pfau-Kempf, Y., Soucek, J., Singer, H., Motoba, T., and Kletzing, C.: Observation and Numerical Simulation of Propagation of ULF Waves From the Ion Foreshock Into the Magnetosphere, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5562, https://doi.org/10.5194/egusphere-egu2020-5562, 2020.

ST3.1 – Open Session on Ionosphere and Thermosphere

EGU2020-1968 | Displays | ST3.1

“Endurance”, a new NASA mission to gauge Earth’s polar wind ambipolar electric field

Glyn Collinson, Alex Glocer, Robert Pfaff, Robert Michell, Aroh Barjatya, James Clemmons, Frank Eparvier, Suzanne Imber, Mark Lester, David Mitchell, Max King, and Scott Bissett

Earth’s primary ionospheric loss process is the polar wind, which flows outwards along open magnetic field lines above our polar caps. One key component critical to the formation of this outflow is thought to be a weak ambipolar electric field. The potential drop resulting from this electric field is thought to assist terrestrial atmospheric escape since it reduces the potential barrier required for heavier ions (such as O+) to escape and accelerates light ions (such as H+) to escape velocity. Although a key component to atmospheric loss, Earth’s ambipolar electric field has never been measured due to its weak strength.

 

We announce the NASA Endurance mission, launching in 2022, which will attempt to make the first direct in-situ observations of Earth’s ambipolar electric field. Endurance launch from Ny-Ålesund, Svalbard, and soar across the exobase to altitudes greater than 800km. The spacecraft will be equipped with a new type of scientific instrument which will enable the Endurance to measure the total electric potential drop below her. She will also be equipped with a full array of sensors that will enable the science team to self-consistently model the polar wind during the flight to test our current theoretical understanding of the physical processes which generate Earth’s ambipolar electric field.

Endurance will perform groundbreaking discovery science, measuring a fundamental property of Earth for the first time: the strength of the ambipolar electric field generated by its ionosphere. The results will provide us with a better understanding of atmospheric escape at Earth, and why our planet is habitable.

How to cite: Collinson, G., Glocer, A., Pfaff, R., Michell, R., Barjatya, A., Clemmons, J., Eparvier, F., Imber, S., Lester, M., Mitchell, D., King, M., and Bissett, S.: “Endurance”, a new NASA mission to gauge Earth’s polar wind ambipolar electric field, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1968, https://doi.org/10.5194/egusphere-egu2020-1968, 2020.

EGU2020-11789 | Displays | ST3.1

Multi-instrument Observations of Ion-Neutral Coupling in the Dayside Cusp

James Wild, Daniel Billett, Keisuke Hosokawa, Adrian Grocott, Anasuya Aruliah, Yasunobu Ogawa, Satoshi Taguchi, and Mark Lester

Using data from the Scanning Doppler Imager, the Super Dual Auroral Radar Network, the EISCAT Svalbard Radar and an auroral all-sky imager, we examine an instance of F-region neutral winds which have been influenced by the presence of poleward moving auroral forms near the dayside cusp region. We observe a reduction in the time taken for the ion-drag force to re-orientate the neutrals into the direction of the convective plasma (on the order of minutes), compared to before the auroral activity began. Additionally, because the ionosphere near the cusp is influenced much more readily by changes in the solar wind via dayside reconnection, we observe the neutrals responding to an interplanetary magnetic field change within minutes of it occurring. This has implications on the rate that energy is deposited into the ionosphere via Joule heating, which we show to become dampened by the neutral winds.

How to cite: Wild, J., Billett, D., Hosokawa, K., Grocott, A., Aruliah, A., Ogawa, Y., Taguchi, S., and Lester, M.: Multi-instrument Observations of Ion-Neutral Coupling in the Dayside Cusp, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11789, https://doi.org/10.5194/egusphere-egu2020-11789, 2020.

EGU2020-7839 | Displays | ST3.1

First measurements of the Mesospheric Magnetic Field in the Auroral Zone by means of laser

Magnar G. Johnsen, Njål Gulbrandsen, Paul Hillman, Craig Denman, Jürgen Matzka, Volkmar Schultze, and Ulf-Peter Hoppe

In December 2019, for the first time, we were able to remotely measure the magnetic field in the mesospheric sodium layer, in the auroral zone.

By means of laser optical pumping and Larmor-resonance detection, it is possible to use the naturally occurring sodium layer in the mesosphere to measure Earth’s magnetic field magnitude at 90 km above ground. This is an altitude otherwise only accessible by rockets, which only will provide point measurements of very short time scales.

During the winter of 2019-20 we have applied a cw sum-frequency fasor/laser for probing the sodium-atom Larmor resonance at the Artic Lidar Observatory for Mesospheric Research (ALOMAR) at Andøya in northern Norway in order to measure and monitor the magnetic field in situ in the high latitude mesosphere over longer time scales.

The technique, which has been proved earlier at mid-latitudes, has now been confirmed and applied to high latitudes in the auroral zone during disturbed auroral and geomagnetic conditions. The magnetic field in the auroral zone is close to vertical making our measurements a notable achievement since the beam is closer to parallel with the magnetic field, contary to earlier measurements being closer to perpendicular as shown as best by theory.

This opens up for a completely new domain of measurements of externally generated geomagnetic variations related to currents in the magnetosphere-ionosphere system.

Here we report on the instrumental setup, and discuss our measurements of the mesospheric magnetic field.

How to cite: Johnsen, M. G., Gulbrandsen, N., Hillman, P., Denman, C., Matzka, J., Schultze, V., and Hoppe, U.-P.: First measurements of the Mesospheric Magnetic Field in the Auroral Zone by means of laser, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7839, https://doi.org/10.5194/egusphere-egu2020-7839, 2020.

EGU2020-7934 | Displays | ST3.1

Solar flare effect on the ionospheric current in the polar region: a new phenomena

Masatoshi Yamauchi, Magnar Johnsen, and Carl-Fredrik Enell

Solar flares are known to enhance the ionospheric electron density in the D- and E-region, enhancing twin vortex pattern in the dayside (e.g., Curto et al., 1994).  The geomagnetic deviation due to this current system is called as "crochet" or "SFE (solar flare effect)".  For X-flares, the crochet is easily detected as an enhancement in ASY-D index (Sing et al., 2012).  Since the effect is expected stronger at low solar zenith angles where solar radiation is high, high-latitude behavior (> 70° geographic latitudes: GGlat) has not been well studied and simply assumed as minor (such as weak return current).

However, the X flares on 6 September 2017 (X2.2 at 9 UT and X9.3 at 12 UT), caused large non-substorm geomagnetic disturbances at high latitudes, lasting much longer than the burst of electron density enhancement in the the D- and E-region (Yamauchi et al., 2018).  Both the polarity and duration turned out to be different from mid-latitude crochet which is characterized by short-lived (< 30 min) dH<0: dH is positive for over 5 hours with much higher amplitude than the crochet although the event took place near equator.  In addition, this dH showed oscillations on the order of 30 minute.  Since the X-ray intensity during 12-17 UT was higher than X-flare criterion until 17 UT, this long-lasting dH>0 with peak at 74-75 GGLat must also be caused by the X-flare.  The EISCAT radar data showed strong enhancement of convection lasting hours after the flare onset and relevant bursty (< 10 min) enhancement of the electron density.  This is consistent with long-lasting positive dH.  On the other hand, density oscillation period is about 15 min and different from the oscillation period of dH.   

Using Norwegian geomagnetic chain and EISCAT data, we examined X flares (> X2.0) for past two solar cycles, and found that (1) dH>0 at > 70 GGLAT with dH<0 (and positive ASY-D change is quite common) at lower latitude, (2) duration of crochet (dH<0) is shorter at higher latitude as the start timing and amplitude of dH>0 becomes earlier and larger at higher latitude, (3) at some latitude, crochet (dH<0) disappears and dH>0 dominates the entire period much longer than the crochet, and (4) electron density enhancement is spike-like no matter the duration of X-flare.  We interpret this long-lasting dH>0 is caused by independent mechanism from crochet.

Reference
Curto et al. (1994): doi:10.1029/93JA02270
Singh et al. (2012): doi:10.1016/j.jastp.2011.12.010
Yamauchi et al. (2018): doi:10.1029/2018SW00193

How to cite: Yamauchi, M., Johnsen, M., and Enell, C.-F.: Solar flare effect on the ionospheric current in the polar region: a new phenomena, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7934, https://doi.org/10.5194/egusphere-egu2020-7934, 2020.

EGU2020-2389 | Displays | ST3.1 | Highlight

Citizen scientists discover a new auroral form: Dunes provide insight into the upper atmosphere

Minna Palmroth, Maxime Grandin, Matti Helin, Pirjo Koski, Arto Oksanen, Minna Glad, Rami Valonen, Kari Saari, Emma Bruus, Johannes Norberg, Ari Viljanen, Kirsti Kauristie, and Pekka Verronen

Auroral forms are like fingerprints linking optical features to physical phenomena in the near-Earth space. While discovering new forms is rare, recently scientists reported of citizens' observations of STEVE, a pinkish optical manifestation of subauroral ionospheric drifts that were not thought to be visible to the naked eye. Here, we present a new auroral form named "the dunes". On Oct 7, 2018, citizen observers took multiple digital photographs of the same dunes simultaneously from different locations in Finland and Sweden. We develop a triangulation method to analyse the photographs, and conclude that the dunes are a monochromatic wave field with a wavelength of about 45 km within a thin layer at 100 km altitude. Supporting data suggest that the dunes manifest atmospheric waves, possibly mesospheric bores, which are rarely detected, and have not previously been observed via diffuse aurora, nor at auroral latitudes and altitudes. The dunes present a new opportunity to investigate the coupling of the lower/middle atmosphere to the thermosphere and ionosphere. We conclude that the the dunes may provide new insights into the structure of the mesopause as a response to driving by ionospheric energy deposition via Joule heating and electron precipitation. Further, our paper adds to the growing body of work that illustrates the value of citizen scientist images in carrying out quantitative analysis of optical phenomena, especially at small scales at subauroral latitudes. The dune project presents means to create general interest towards physics, emphasising that citizens can take part in scientific work by helping to uncover new phenomena.

How to cite: Palmroth, M., Grandin, M., Helin, M., Koski, P., Oksanen, A., Glad, M., Valonen, R., Saari, K., Bruus, E., Norberg, J., Viljanen, A., Kauristie, K., and Verronen, P.: Citizen scientists discover a new auroral form: Dunes provide insight into the upper atmosphere, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2389, https://doi.org/10.5194/egusphere-egu2020-2389, 2020.

EGU2020-5431 | Displays | ST3.1

A new auroral phenomenon: The anti-black aurora

Amoré Nel and Mike Kosch

Black auroras are small-scale features that show a significant reduction in optical brightness, i.e. reduced flux of particle precipitation, compared to the surrounding diffuse aurora. It typically occurs post-substorm after magnetic midnight. This phenomenon also exhibits lower mean energy than the surrounding brighter aurora it is embedded in. The underlying mechanisms that cause black auroras are not yet fully understood, although several theories have been proposed: a coupled ionospheric-magnetospheric generation mechanism, and a magnetospheric generation mechanism. This shift in particle precipitation energy to a lower mean value is confirmed by using synchronised dual-wavelength optical and EISCAT incoherent scatter radar observations that ran in parallel, and agrees with the magnetospheric generation mechanism theory. Now reported for the first time is an even more elusive small-scale optical structure has been observed occurring paired with ~10% of black aurora patches. A patch or arc segment of enhanced luminosity, distinctly brighter than the diffuse background, which we name the anti-black aurora, may appear adjacent to the black aurora. The anti-black aurora always moves in parallel to the black aurora. The paired phenomenon always drifts with the same average speed in an easterly direction. From the first dual-wavelength observations of anti-black and black aurora pairs, we show that the anti-black and black auroras have a higher and lower mean energy, respectively, of the precipitating electrons compared to the diffuse background.

How to cite: Nel, A. and Kosch, M.: A new auroral phenomenon: The anti-black aurora, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5431, https://doi.org/10.5194/egusphere-egu2020-5431, 2020.

EGU2020-12853 | Displays | ST3.1

Auroral electrodynamics---investigation by a dual sounding rocket experiment

Hassanali Akbari and Robert Pfaff and the Auroral Jets Sounding Rocket Experiment Team

We present results from a 2017 sounding rocket experiment in which two NASA sounding rockets were simultaneously launched into the auroral ionosphere. The rockets included comprehensive instrumentation to measure DC and AC electric fields, magnetic fields, energetic particles, plasma density, and neutral winds, among other parameters, and achieved apogees of 190 and 330 km. This unprecedented collection of in-situ measurements obtained at two altitudes over an auroral arc, along with conjugate ground-based measurements by the Poker Flat incoherent scatter radar and all-sky cameras, enable us to investigate the behavior of an aurora arc and its associated electrodynamics. A prominent feature of our observations is the presence of localized, large-amplitude Alfvén wave structures observed in both the electric field and magnetometers at altitudes as low as 190 km in the vicinity of up- and down-ward current regions. The observations are discussed in the context of ionospheric feedback instability. The results are compared to predictions of previously published numerical studies and other sounding rocket observations.

How to cite: Akbari, H. and Pfaff, R. and the Auroral Jets Sounding Rocket Experiment Team: Auroral electrodynamics---investigation by a dual sounding rocket experiment, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-12853, https://doi.org/10.5194/egusphere-egu2020-12853, 2020.

EGU2020-11558 | Displays | ST3.1

ICEBEAR: Recent Results from a Bistatic Coded Continuous-Wave E-region Coherent Scatter Radar

Devin Huyghebaert, Adam Lozinsky, Glenn Hussey, Kathryn McWilliams, Draven Galeschuk, Jean-Pierre St. Maurice, Miguel Urco, Jorge Chau, and Juha Vierinen

The Ionospheric Continuous-wave E-region Bistatic Experimental Auroral Radar (ICEBEAR) is located in Canada and has a field of view centered at (58°N, 106°W) overlooking the terrestrial auroral zone.  This 49.5 MHz coherent scatter radar measures plasma density irregularities in the E-region ionosphere using a pseudo random noise phase modulated continuous-wave (CW) signal.  ICEBEAR uses this coded CW signal to obtain simultaneous high temporal (1 s) and spatial (1.5 km) resolutions of E-region plasma density turbulence over a 600 km x 600 km field of view, providing insights into the Farley-Buneman plasma density instability and wave-like structures evident in the coherent scatter.  The initial results from ICEBEAR were obtained with a 1D receiving array, providing azimuthal angle of arrival details of the incoming scattered signal.  This azimuthal determination, along with the range determined using the coded signal, allowed the scatter to be mapped in 2D.  A recent reconfiguration of the receiving array has allowed the elevation angle of the received signal to be calculated, providing 3D determination of the location of the plasma density irregularities.  This presentation will demonstrate the capabilities of ICEBEAR, displaying measurements of highly dynamic plasma density irregularities with wave-like behaviour on 1 second time scales.

How to cite: Huyghebaert, D., Lozinsky, A., Hussey, G., McWilliams, K., Galeschuk, D., St. Maurice, J.-P., Urco, M., Chau, J., and Vierinen, J.: ICEBEAR: Recent Results from a Bistatic Coded Continuous-Wave E-region Coherent Scatter Radar, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11558, https://doi.org/10.5194/egusphere-egu2020-11558, 2020.

EGU2020-20711 | Displays | ST3.1 | Highlight

Daedalus: a Candidate ESA Earth Explorer Mission for the Exploration of the Lower Thermosphere-Ionosphere

Theodoros Sarris and the The Daedalus Science Study Team

The Daedalus mission has been proposed to the European Space Agency (ESA) in response to the call for ideas for the Earth Observation programme’s Earth Explorers. It was selected in 2018 as one of three candidates for Earth Explorer 10, and is currently undergoing a Phase-0 Science and Requirements Consolidation Study. The goal of the mission is to quantify the key electrodynamic processes that determine the structure and composition of the Lower Thermosphere-Ionosphere (LTI), focusing in particular on processes related to ion-neutral coupling. Daedalus will perform in-situ measurements of plasma density and temperature, ion drift, neutral density and wind, ion and neutral composition, electric and magnetic fields and precipitating particles. An innovative preliminary mission design allows Daedalus to perform these measurements down to altitudes of 140 km and below. These measurements will quantify the amount of energy locally deposited in the upper atmosphere via Joule heating and energetic particle precipitation, estimates of which currently vary by orders of magnitude between models. At the same time, the instrumentation of Daedalus will enable exploration of the variability and dynamics of the LTI, as well as science questions related to connections between the LTI and the atmosphere below. Daedalus will thus study the most under-explored region of the Earth's environment, the "agnostophere", which is the gateway between Earth’s atmosphere and space. In this presentation an overview of the Daedalus Mission Concept will be given, including the status of the ongoing Phase-0 Study.

How to cite: Sarris, T. and the The Daedalus Science Study Team: Daedalus: a Candidate ESA Earth Explorer Mission for the Exploration of the Lower Thermosphere-Ionosphere, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-20711, https://doi.org/10.5194/egusphere-egu2020-20711, 2020.

EGU2020-6464 | Displays | ST3.1

Recurrent high-speed solar wind co-rotating interaction region imprint on the ionosphere and atmosphere: GPS TEC variations and atmospheric gravity waves

James M. Weygand, Paul Prikryl, Reza Ghoddousi-Fard, Lidia Nikitina, and Bharat S. R. Kunduri

High-speed streams (HSS) from coronal holes dominate solar wind structure in the absence of coronal mass ejections during solar minimum and the descending branch of solar cycle. Prominent and long-lasting coronal holes produce intense co-rotating interaction regions (CIR) on the leading edge of high-speed plasma streams that cause recurrent ionospheric disturbances and geomagnetic storms. Through solar wind coupling to the magnetosphere-ionosphere-atmosphere (MIA) system they affect the ionosphere and neutral atmosphere at high latitudes, and, at mid to low latitudes, by the transmission of the electric fields [1] and propagation of atmospheric gravity waves from the high-latitude lower thermosphere [2].

The high-latitude ionospheric structure, caused by precipitation of energetic particles, strong ionospheric currents and convection, results in changes of the GPS total electron content (TEC) and rapid variations of GPS signal amplitude and phase, called scintillation [3]. The GPS phase scintillation is observed in the ionospheric cusp, polar cap and auroral zone, and is particularly intense during geomagnetic storms, substorms and auroral breakups. Phase scintillation index is computed for a sampling rate of 50 Hz by specialized GPS scintillation receivers from the Canadian High Arctic Ionospheric Network (CHAIN). A proxy index of phase variation is obtained from dual frequency measurements of geodetic-quality GPS receivers sampling at 1 Hz, which include globally distributed receivers of the RT-IGS network that are monitored by the Canadian Geodetic Survey in near-real-time [4]. Temporal and spatial changes of TEC and phase variations following the arrivals of HSS/CIRs [5] are investigated in the context of ionospheric convection and equivalent ionospheric currents derived from  a ground magnetometer network using the spherical elementary current system method [6,7].

The Joule heating and Lorentz forcing in the high-latitude lower thermosphere have long been recognized as sources of internal atmospheric gravity waves (AGWs) [2] that propagate both upward and downward, thus providing vertical coupling between atmospheric layers. In the ionosphere, they are observed as traveling ionospheric disturbances (TIDs) using various techniques, e.g., de-trended GPS TEC maps [8].

In this paper we examine the influence on the Earth’s ionosphere and atmosphere of a long-lasting HSS/CIRs from recurrent coronal holes at the end of solar cycles 23 and 24. The solar wind MIA coupling, as represented by the coupling function [9], was strongly increased during the arrivals of these HSS/CIRs.

 

[1] Kikuchi, T. and K. K. Hashimoto, Geosci. Lett. , 3:4, 2016.

[2] Hocke, K. and K. Schlegel, Ann. Geophys., 14, 917–940, 1996.

[3] Prikryl, P., et al., J. Geophys. Res. Space Physics, 121, 10448–10465, 2016.

[4] Ghoddousi-Fard et al., Advances in Space Research, 52(8), 1397-1405, 2013.

[5] Prikryl et al. Earth, Planets and Space, 66:62, 2014.

[6] Amm O., and A. Viljanen, Earth Planets Space, 51, 431–440, 1999.

[7] Weygand J.M., et al., J. Geophys. Res., 116, A03305, 2011.

[8] Tsugawa T., et al., Geophys. Res. Lett., 34, L22101, 2007.

[9] Newell P. T., et al., J. Geophys. Res., 112, A01206, 2007.

How to cite: Weygand, J. M., Prikryl, P., Ghoddousi-Fard, R., Nikitina, L., and Kunduri, B. S. R.: Recurrent high-speed solar wind co-rotating interaction region imprint on the ionosphere and atmosphere: GPS TEC variations and atmospheric gravity waves, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6464, https://doi.org/10.5194/egusphere-egu2020-6464, 2020.

EGU2020-7769 | Displays | ST3.1

Identification and monitoring techniques of TIDs in the H2020 TechTIDE project

David Altadill, Antoni Segarra, Estefania Blanch, José Miguel Juan, Dalia Buresova, Ivan Galkin, Anna Belehaki, Haris Haralambous, and Claudia Borries

Traveling Ionospheric Disturbances (TIDs) are wave-like propagating irregularities that alter the electron density environment and play an important role spreading radio signals propagating through the ionosphere.

TechTIDE project, funded by the European Commission Horizon 2020 research and innovation program, is establishing a pre-operational system to issue warnings of the occurrence of TIDs over the region extended from Europe to South Africa based on the reliability of a set of TID detection methodologies.

This contribution aims at presenting the different methods and techniques of identification and tracking the activity of TIDs and their respective performance, that serve to feed the warning system of TechTIDE.

How to cite: Altadill, D., Segarra, A., Blanch, E., Juan, J. M., Buresova, D., Galkin, I., Belehaki, A., Haralambous, H., and Borries, C.: Identification and monitoring techniques of TIDs in the H2020 TechTIDE project , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7769, https://doi.org/10.5194/egusphere-egu2020-7769, 2020.

EGU2020-13966 | Displays | ST3.1

Impact of disturbed ionospheric conditions in EGNOS performance

Sergio Magdaleno and Joanna Rupiewicz

The European Geostationary Navigation Overlay Service (EGNOS) is the Europe's regional satellite-based augmentation system (SBAS). It provides an augmentation service to the Global Positioning System (GPS) L1 Coarse/ Acquisition (C/A) civilian signal by providing corrections and integrity information for GPS space vehicles (ephemeris, clock errors) and information to estimate the ionosphere delays affecting the user. This information provided by EGNOS improves the accuracy and reliability of GNSS positioning information while also providing a crucial integrity message. This is especially relevant for civil aviation community, which, thanks to this improvement, can perform precision approaches (APV-I and LPV200) using GNSS, with a clear optimisation of the cost of the infrastructure with no impact in the safety of the operations.

One of the most important figures for EGNOS is the availability of the system, which is characterized by the proportion of time during which reliable navigation information is presented to the crew, autopilot, or other system managing the flight of the aircraft. (ICAO SARPS).

ESSP, as EGNOS Service Provider, monitors the daily availability for these flight operations (APV-I, LPV200), considering the system available when operational requirements defined in ICAO SARPS are met. In this case, EGNOS is considered available when the Protection Levels, an upper bound of the aircraft position error with the specified integrity risk, are lower than the Alarm limits defined by ICAO for these operations.

One of the main degradation sources in the EGNOS availability (and others SBAS) is the ionosphere, especially under disturbance conditions (e.g. geomagnetic storms, scintillation …) (Pintor et al., 2015; Haddad, 2016).

In the frame of the H2020 project - TechTIDE, the impact of disturbed ionospheric conditions in the EGNOS availability has been analysed. TechTIDE project is generating a warning system which will provide Travelling Ionospheric Disturbances (TID) information and some ionospheric activity indicators. These products would be used for the definition of mitigation strategies in some operational systems (EGNOS, N-RTK and HF communications).

As part of TechTIDE project, ESSP has assessed the impact of disturbed ionospheric conditions in EGNOS availability and defined a relationship with an ionospheric activity indicator provided by TechTIDE warning system. This paper presents the outcomes of this assessment.

References:

Haddad, F. (2016). Latest SBAS Performances under Severe and Equatorial Ionosphere Conditions, ICAO Workshop, August, 15-17, 2016.

Pintor, P., Roldan, R., Gomez, J., de la Casa, C., Fidalgo, R. M. (2015). The impact of the high ionospheric activity in the EGNOS performance, Coordinates, March 2015.

How to cite: Magdaleno, S. and Rupiewicz, J.: Impact of disturbed ionospheric conditions in EGNOS performance, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-13966, https://doi.org/10.5194/egusphere-egu2020-13966, 2020.

EGU2020-18657 | Displays | ST3.1

Inter-hemispheric comparison of the ionosphere-plasmasphere system from multi-instrumental/model approach.

Nicolas Bergeot, John Bosco Habarulema, Jean-Marie Chevalier, Tshimangadzo Matamba, Elisa Pinat, Pierre Cilliers, and Dalia Burešová

An increasing demand for a better modelling and understanding of the Ionosphere-Plasmasphere system (I/Ps) is required for both scientific and public practical applications using electromagnetic wave signals reflecting on or passing through this layer. This is the case for the Global Navigation Satellite Systems (GNSS, i.e. GPS, GLONASS, Galileo) and for spacecraft designers and operators who need to have a precise knowledge of the electron density distribution.

Additionally, despite the long-term ionospheric studies that have been on-going for many decades, a number of aspects are still complicated to understand and forecast accurately even in mid-latitude regions during quiet conditions. Performing inter-hemispherical climatological studies in European and South African regions should highlight differences/similarities in I/Ps response during different phases of solar activity and geophysical conditions.

In that frame, the Royal Observatory of Belgium (ROB) and the South African National Space Agency (SANSA) started a collaboration named “Interhemispheric Comparison of the Ionosphere-Plasmasphere System” (BEZA-COM). The goal is to provide inter-hemispheric comparison of the I/Ps implying: (1) a characterization of the climatological behavior of the Total Electron Content (TEC) in the I/Ps, over European, South African, Arctic and Antarctica regions; (2) an identification of the mechanisms that regulate inter-hemispheric differences, asymmetries and commonalities in the I/Ps from low to high-latitudes, (3) study of the different responses of the I/Ps during extreme solar events and induced geomagnetic storms in the two hemispheres.

In this paper, we reprocessed the GNSS data (GPS+GLONASS) of the dense EUREF Permanent GNSS Network (EPN) and South African TRIGNET networks as well as IGS stations for the period 1998-2018. The output consists in vertical Total Electron Content (vTEC), estimated every 15 min., and covering the central European and South African regions. The vTEC is then extracted at two conjugated locations and used to constrain empirical models to highlight the climatological behavior of the ionospheric vTEC over Europe and South Africa. From the results, we will show that the differences are quite significant. To give first answers on these differences, we also compared these models with ionosondes long-term data based models (for foF2 and hmF2) at two conjugated locations (Grahamstown and Průhonice) as well as long-term NRLMSISE O/N2 ratio.

How to cite: Bergeot, N., Habarulema, J. B., Chevalier, J.-M., Matamba, T., Pinat, E., Cilliers, P., and Burešová, D.: Inter-hemispheric comparison of the ionosphere-plasmasphere system from multi-instrumental/model approach. , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18657, https://doi.org/10.5194/egusphere-egu2020-18657, 2020.

EGU2020-21635 | Displays | ST3.1

Total electron content driven data products of SIMuRG

Artem Vesnin, Yury Yasyukevich, Boris Maletckii, Alexander Kiselev, Ilya Zhivetiev, Ilya Edemskiy, and Semen Syrovatskiy

System for the Ionosphere Monitoring and Researching from GNSS (SIMuRG, see https://simurg.iszf.irk.ru) has been developed in ISTP SB RAS. The system servers as proxy for the RINEX data of global GNSS receivers network. SIMuRG automatically downloads, process and visualize GNSS data. Despite of the system takes routine processing task from the researches, which is valuable by itself, it provides newly developed and improved data products. All data products are based on total electron content (TEC) calculated from RINEX and global ionospheric maps GIM. The first data product is ionospheric variations (TEC variations). The variations are widely used for ionospheric studies, but SIMuRG performs calculation using the filtration that suits TEC data the best way. Before new filtration technique was applied major unphysical artifacts were detected in the data. The artifacts could even prevent from correct interpretation of processing results. The variations together with widely used ROTI index which is also implemented in the system helps to study ionospheric variability. The second data product is newly developed “adjusted TEC”. For that we use GIM to force all TEC series from different site-satellite line-of-sights have one reference level. While the reference level is the same, adjusted TEC leaves all the peculiarities exhibited in different TEC series unaffected. Adjusted TEC broaden ionospheric maps capability near the GNSS stations improving time resolution up to 30 seconds and giving better space resolution. The third data product is implementation of D1 method which calculates ionospheric irregularities motion velocity. D1 shows velocity vector while variations show only amplitude of the irregularity (deviation from the background). D1 calculation is designed in the way that it possible to choose scale of the disturbance to study. It makes possible to study the disturbances of different physical origin. D1 is able to show global ionospheric dynamics and can help detect traveling ionospheric disturbances of various scales. The data described above are attribute by the interactive experimental geometry plots, which might consider as one more data product. The geometry plots might be useful since the TEC data cover area of several thousands kilometers across. The fourth data product is global and regional electron content (GEC and REC), see https://simurg.iszf.irk.ru/gec for reference. SIMuRG provides interactive plots of the GEC and REC. While TEC shows the number of electrons in a given direction (surface density), GEC and REC show amount of a plasma in a volume. GEC is weighted sum of the TEC around the globe, REC – in some geographical region. GEC and REC suits for large scale long-living ionospheric variations studies. Using REC we detect after-storm plasma density change in equatorial ionosphere. There is an option to choose region for REC using geographic and geomagnetic coordinates. We also developed the interface for ionospheric events tracking and submission. We hope to use the events database for machine learning purpose. We hope all above newly developed and improved TEC based data products find application among researches.

This work was performed under the Russian Science Foundation Grant No. 17-77-20005.

How to cite: Vesnin, A., Yasyukevich, Y., Maletckii, B., Kiselev, A., Zhivetiev, I., Edemskiy, I., and Syrovatskiy, S.: Total electron content driven data products of SIMuRG, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21635, https://doi.org/10.5194/egusphere-egu2020-21635, 2020.

EGU2020-7016 | Displays | ST3.1

CIR/HSSS-related TID activity and their interhemispheric circulation

Dalia Buresova, John Bosco Habarulema, Jurgen Watermann, Ilya K. Edemskiy, Jaroslav Urbar, David Altadill, Estefania Blanch, Antoni Segara, and Zama Katamzi

The paper presents results of the analysis of the changes in the regular ionospheric variability and TID activity observed during CIR/HSSS-related storms. We analyzed main ionospheric parameters retrieved from manually scaled ionograms, plasma drift measurements and TEC data obtained from several European and African ionospheric stations and GNSS receivers. Most of the observed storm-related TIDs had periods of 60-180 min (LSTIDs). During the analyzed storms we also observed extraordinary spreads and plasma bubbles at the F region heights. The results of the analysis were compared with the TID activity during strong magnetic storms of CME origin along the European-African sector. In order to obtain quantitative information on the likeliness and morphology of interhemispheric circulation of LSTIDs at about 40 events were examined lasting between 8 and 24 hours each. We used exclusively GPS-based detection methods, specifically information on TEC, TEC deviations in space and time from a background reference (dTEC), and the Rate of TEC change in time (ROT), all inferred from GPS receiver networks in Europe and Africa. We conclude that hemispheric conjugacy of LSTID is highly probable while interhemispheric circulation rather unlikely but still occurring during some periods.

How to cite: Buresova, D., Habarulema, J. B., Watermann, J., Edemskiy, I. K., Urbar, J., Altadill, D., Blanch, E., Segara, A., and Katamzi, Z.: CIR/HSSS-related TID activity and their interhemispheric circulation, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7016, https://doi.org/10.5194/egusphere-egu2020-7016, 2020.

EGU2020-9389 | Displays | ST3.1

Global distribution of persistence of total electron content anomaly

Yang-Yi Sun, Chieh-Hong Chen, Jann-Yenq Liu, and Tsung-Yu Wu

Solar activities can disturb the ionosphere globally and induce ionospheric weather phenomena that transit rapidly through a large area. By contrast, sometimes the ionospheric plasma density can remain high or low over a certain location for a few days, which are difficult to be attributed to solar activities. This study shows the location preference of the positive and negative total electron content (TEC) anomalies persisting continuously longer than 24 hours (cross the two terminators) at middle and low latitudes (within ±60ºN geomagnetic latitudes). The TEC is obtained from the global ionospheric map (GIM) of the Center for Orbit Determination in Europe (CODE) (ftp://cddis.gsfc.nasa.gov/pub/gps/products/ionex) under the geomagnetic quiet condition of Kp ≤ 3o during the period of 2005–2018. There are a few (less than 4%) TEC anomalies that can persist over 24 hours. The persistence of the positive TEC anomaly along the ring of fire on the western edge of the Pacific Ocean. The high persistence of the TEC anomalies at midlatitudes suggests that thermospheric neutral wind contributes to the anomaly formation. The temporal and spatial anomalies of the ionospheric electric field, atmospheric electric field (flash), atmospheric gravity wave, and neutral wind over the ring of fire should be further examined for explaining whether the persistence of the TEC anomalies associates with lithospheric activities.

How to cite: Sun, Y.-Y., Chen, C.-H., Liu, J.-Y., and Wu, T.-Y.: Global distribution of persistence of total electron content anomaly, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-9389, https://doi.org/10.5194/egusphere-egu2020-9389, 2020.

EGU2020-2924 | Displays | ST3.1

Studying the ionospheric absorption during large solar flare events in September 2017

Attila Buzas, Veronika Barta, and Daniel Kouba

The most intense external force affecting the ionosphere from above is related to large solar flare events, therefore it is of particular importance to study their impact on the ionosphere. During solar flares, the suddenly increased radiation causes increased ionization and enhanced absorption of radio waves leading to partial or even total radio fade-out lasting for hours in some cases (e. g. [1] [2]).

 

The ionospheric response to large solar flares have been investigated using the ionosonde data measured at Pruhonice (PQ052, 50°, 14.5°) in September 2017, the most active solar period of Solar Cycle 24. A novel method [3] to calculate and investigate the absorption of radio waves propagating in the ionosphere is used to determine the absorption during large solar flare events (M and X class). Subsequently, the absorption data are compared with the indicators derived from the fmin method (fmin, the minimum frequency is considered as a qualitative proxy for the “nondeviative” radio wave absorption occurring in the D-layer). Total and partial radio fade-out and increased values (with 2-5 MHz) of the fmin parameter were experienced during and after the intense solar flares (> M3). The combination of these two methods may prove to be an efficient approach to monitor the ionospheric response to solar flares.

 

[1] Sripathi, S., Balachandran, N., Veenadhari, B., Singh, R., and Emperumal, K.: Response of the equatorial and low-latitude ionosphere to an intense X-class solar flare (X7/2B) as observed on 09 August 2011, J. Geophys. Res.-Space, 118, 2648–2659, 2013.

[2] Barta, V., Sátori, G., Berényi, K. A., Kis, Á., and Williams, E. (2019). Effects of solar flares on the ionosphere as shown by the dynamics of ionograms recorded in Europe and South Africa. Annales Geophysicae, Vol. 37, No. 4, pp. 747-761

[3] Sales, G. S., 2009, HF absorption measurements using routine digisonde data, Conference material, XII. International Digisonde Forum, University of Massachusetts

How to cite: Buzas, A., Barta, V., and Kouba, D.: Studying the ionospheric absorption during large solar flare events in September 2017, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2924, https://doi.org/10.5194/egusphere-egu2020-2924, 2020.

  A remote sensing satellite, FORMOSAT-5, developed by National Space Organization (NSPO) carried a piggyback science payload, Advanced Ionospheric Payload (AIP), for space weather and seismo-ionospheric precursor study.  To meet the science requirements, AIP could be operated in different measurement modes to obtain various plasma parameters.  The first AIP measurement was performed on 7 September 2017 to obtain the first-orbit data and started routine operation in November the same year.  Global ion density and ion velocity/temperature distributions were available every two days and four days, respectively.  AIP was regularly operated in a sampling rate 1,024 Hz to maximize useful science data.  In this poster, global occurrence rates of pre-midnight low-latitude ionospheric plasma density irregularities will be shown from AIP science data collected since winter 2017.  The results indicate that seasonal variations of the occurrence rates during the solar minimum (2017/11-2019/12) are distributed very similar to but have lower magnitudes than those observations by ROCSAT-1/Ionospheric Plasma and Electrodynamics Instrument dataset (1999-2004) during solar maximum.

How to cite: Chen, Y.-W. and Chao, C.-K.: Global Occurrence Rates of Ionospheric Plasma Density Irregularities Observed by Advanced Ionospheric Probe Onboard FORMOSAT-5 Satellite During Solar Minimum, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3210, https://doi.org/10.5194/egusphere-egu2020-3210, 2020.

EGU2020-3368 | Displays | ST3.1

Comparison of D-Region Absorption During Solar Cycle 24

Michael Danielides and Jaroslav Chum

Earth's ionosphere is formed mainly due to solar radiation, precipitating particles and cosmic rays. Its behavior is directly dependent on solar variation and the change of solar activity through out each solar cycle. The solar activity is measured by the number of sunspots and the solar radiation flux expressed by the F10.7 index. The earlier variation in electron density from solar cycle maximum to solar cycle minimum has been noted by Hargreaves (1992). He utilized the F10.7 index as a proxy for Lyman- radiation flux, which ionizes at D-region heights mainly O2 and N2 also NO. Utilizing the IRI model the atmospheric densities of O2 and N2 are assumed to be constant, NO density is the unknown. Also, it is known that the ionospheric reflection height depends on, e.g. diurnal variations [Pal & Chakrabarti, 2010] and other sudden ionospheric disturbances. Its longer term variations are not well enough studied.

Utilizing passive VLF ground based measurements with data coverage for almost the entire solar cycle 24, we compare monthly averaged solar quiet absorption curves fitted by a cosine dependence. This cosine dependence includes fixed parameters based on geography and setup of the instrument. The variables are only the solar zenith angle and the D-region absorption. This approach offers an indirect value of NO density change.

For the present study we utilize VLF monitors, which are located in northern Germany and at Czech Republic. The latter station also offers data from ionospheric sounder and continuous Doppler sounding. A simple 1-D ionospheric model is applied to compute ionospheric electron densities for daytime conditions based on solar F10.7 radiation fluxes.

The aim of this study is a comparison of solar quiet VLF curves of the solar cycle 24 maximum and minimum. Beside the change of NO density, also the variation of height of the D-region reflective layer will be discussed.

How to cite: Danielides, M. and Chum, J.: Comparison of D-Region Absorption During Solar Cycle 24, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3368, https://doi.org/10.5194/egusphere-egu2020-3368, 2020.

EGU2020-4956 | Displays | ST3.1

The link between solar wind structures, geomagnetic indices, and energetic electron precipitation

Josephine Salice, Hilde Nesse Tyssøy, Christine Smith-Johansen, and Eldho Midhun Babu

Energetic electron precipitation (EEP) into the Earth’s atmosphere can collide with gases and deposit their energy there. The collisions between electrons and atmospheric gasses initiate several chemical reactions which can reduce the ozone concentration. Ozone is critically important in the middle atmosphere energy budget as changes in the ozone concentration impact temperature and winds. EEP is not fully understood in terms of how much energy is being deposited and what the associated drivers are.  An accurate quantification of EEP has limitations due to instrumental challenges and therefore imposes limitations of the associated EEP parameterization into climate models. A solution to this problem is a better understanding of the driver processes of energetic electron acceleration and precipitation, alongside optimized measurements. In this study the bounce loss cone fluxes are inferred from EEP measurements by MEPED on board NOAA/POES and EUMETSAT/METOP at tens of keV to relativistic energies. It investigates EEP in contexts of three different solar wind structures: high-speed streams, coronal mass ejections, and ambient or slow interstream solar wind, as well as geomagnetic activity. The study will focus on the year 2010 and aim to understand the context EEP is created in, which will allow a more accurate estimate of the EEP to be applied in atmospheric climate models

How to cite: Salice, J., Tyssøy, H. N., Smith-Johansen, C., and Babu, E. M.: The link between solar wind structures, geomagnetic indices, and energetic electron precipitation, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4956, https://doi.org/10.5194/egusphere-egu2020-4956, 2020.

A FORMOSAT-5 satellite has been launched on 25 August 2017 CST into a 98.28° inclination sun-synchronous circular orbit at 720 km altitude along the 1030/2230 local time sectors.  The orbital coverage provides a great opportunity to survey terrestrial ionosphere from equatorial to polar region every two days.  Advanced Ionospheric Probe (AIP) is a piggyback science payload developed by National Central University for the FORMOSAT-5 satellite to measure ionospheric plasma concentrations, velocities, and temperatures.  It is also capable of measuring ionospheric plasma density irregularities at a sample rate up to 8,192 Hz over a wide range of spatial scales.  In this poster, global ion density distributions observed by FORMOSAT-5/AIP in the pre-midnight sector can be averaged monthly and seasonally from in-situ measurement since November 2017.  Wave-3 and wave-4 patterns are clearly detected from the distributions and varied with season and solar cycle.  It is adversely indicated that FORMOSAT-5/AIP can provide high quality data to identify long-term ionospheric ion density variations.

How to cite: Chao, C.-K.: Global Ion Density Distributions Observed by Advanced Ionospheric Probe Onboard FORMOSAT-5 Satellite, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6421, https://doi.org/10.5194/egusphere-egu2020-6421, 2020.

EGU2020-4963 | Displays | ST3.1

Determining latitudinal extent of energetic electron precipitation using MEPED on-board NOAA POES

Eldho Midhun Babu, Hilde Nesse Tyssøy, Christine Smith-Johnsen, Ville Aleksi Maliniemi, Josephine Alessandra Salice, and Robyn Millan

Energetic electron precipitation (EEP) from the plasma sheet and the radiation belts, can collide with gases in the atmosphere and deposit their energy. EEP increase the production of NOx and HOx, which will catalytically destroy stratospheric ozone, an important element of atmospheric dynamics. The particle precipitation also causes variation in the radiation belt population. Therefore, measurement of latitudinal extend of the precipitation boundaries is important in quantifying atmospheric effects of Sun-Earth interaction and threats to spacecrafts and astronauts in the Earth’s radiation belt.
This study uses measurements by MEPED detectors of six NOAA/POES and EUMETSAT/METOP satellites during the year 2010 to determine the latitudinal boundaries of EEP and its variability with geomagnetic activity and solar wind drivers. Variation of the boundaries with respect to different particle energies and magnetic local time is studied. The result will be a key element for constructing a model of EEP variability to be applied in atmosphere climate models.

How to cite: Babu, E. M., Tyssøy, H. N., Smith-Johnsen, C., Maliniemi, V. A., Salice, J. A., and Millan, R.: Determining latitudinal extent of energetic electron precipitation using MEPED on-board NOAA POES, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4963, https://doi.org/10.5194/egusphere-egu2020-4963, 2020.

EGU2020-12549 | Displays | ST3.1

Interhemispheric conjugate effect in longitude variations of mid-latitude ion density

Yiding Chen, Libo Liu, Huijun Le, and Hui Zhang

Interhemispheric coupling between the northern and southern mid-lattitude ionosphere through the plasmasphere is difficult to confirm directly from observations. A possible result induced by this coupling is interhemispheric conjugacy of the mid-latitude ionosphere. In this paper, interhemispheric conjugate effect in longitude variations of mid-latitude total ion density (Ni) is presented, for the first time, using the Defense Meteorological Satellite Program (DMSP) measurements; northern and southern Ni longitude variations at 21:30 LT are similar between magnetically conjugate mid-latitudes around solar minimum June Solstice of 1996. The conjugate effect after sunset also occurs around the June Solstice in other solar minimum years but disappears when solar activity increases. We suggested that mid-latitude interhemispheric coupling is responsible for the conjugate effect. Neutral wind induced ionospheric transport causes topside longitude variations via upward diffusion at summer mid-latitudes; this further induces similar longitude variations of topside Ni at winter mid-latitudes via the summer to winter interhemispheric coupling. The conjugate effect occurs only inside the plasmapause where magnetic flux tubes are closed and the plasma in these tubes can stably corotate with the Earth. The conjugate effect not only proves mid-latitude interhemispheric coupling through the plasmasphere, but also implies that neutral wind induced transport can affect ionospheric coupling to the plasmasphere at mid-latitudes.

How to cite: Chen, Y., Liu, L., Le, H., and Zhang, H.: Interhemispheric conjugate effect in longitude variations of mid-latitude ion density, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-12549, https://doi.org/10.5194/egusphere-egu2020-12549, 2020.

EGU2020-13374 | Displays | ST3.1

Bayesian filtering for incoherent scatter radar analysis

Habtamu Tesfaw, Ilkka Virtanen, Anita Aikio, Lassi Roininen, and Sari Lasanen

Electron precipitation and ion frictional heating events cause rapid variations in electron temperature, ion temperature and F1 region ion composition of the high-latitude ionosphere. Four plasma parameters: electron density, electron temperature, ion temperature, and plasma bulk velocity, are typically fitted to incoherent scatter radar (ISR) data.

Many ISR data analysis tools extract the plasma parameters using an ion composition profile from an empirical model. The modeled ion composition profile may cause bias in the estimated ion and electron temperature profiles in the F1 region, where both atomic and molecular ions exist with a temporally varying proportion.

In addition, plasma parameter estimation from ISR measurements requires integrating the scattered signal typically for tens of seconds. As a result, the standard ISR observations have not been able to follow the rapid variations in plasma parameters caused by small scale auroral activity.

In this project, we implemented Bayesian filtering technique to the EISCAT’s standard ISR data analysis package, GUISDAP. The technique allows us to control plasma parameter gradients in altitude and time.

The Bayesian filtering implementation enabled us to fit electron density, ion and electron temperatures, ion velocity and ion composition to ISR data with high time resolution. The fitted ion composition removes observed artifacts in ion and electron temperature estimates and the plasma parameters are calculated with 5 s time resolution which was previously unattainable.

Energy spectra of precipitating electrons can be calculated from electron density and electron temperature profiles observed with ISR. We used the unbiased high time-resolved electron density and temperature estimates to improve the accuracy of the estimated energy spectra. The result shows a significant difference compared to previously published results, which were based on the raw electron density (backscattered power) and electron temperature estimates calculated with coarser time resolution.

 

How to cite: Tesfaw, H., Virtanen, I., Aikio, A., Roininen, L., and Lasanen, S.: Bayesian filtering for incoherent scatter radar analysis , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-13374, https://doi.org/10.5194/egusphere-egu2020-13374, 2020.

EGU2020-16800 | Displays | ST3.1

Electrodynamic Coupling and Dissipation of Thermospheric Winds

Stephan C. Buchert

A so far simplified model considers the response of the magnetized ionosphere
to neutral winds and the so created effective electrodynamic coupling in
neutral atmosphere dynamics.  The effect resembels viscosity, but the
geomagnetic field couples winds also over large distances.  As a prominent
example the Sq variations are presented as a system that couples the winds
between hemispheres at magnetically conjugate points. The interaction between
hemispheres tends to force the large scale wind systems towards alignment with
magnetic coordinates and towards mirror symmetry with respect to the magnetic
equator. This is, however, for the Earth's thermosphere, never completed
because the time constant exceeds the 24 hours over which dynamics driven by
the energy input from solar radiation creates new winds.

Wind differences are so reduced and kinetic energy gets dissipated. From
observed magnetic Sq variations we estimate that a typical average dissipation
rate by interhemisphere electrodynamic coupling is roughly 0.1 to 1 % of the
heating rate resulting from the absorption of EUV solar radiation.

The same model applies when a neutral wind varies along the geomagnetic field
within the dynamo layer of the ionosphere, for example due to tides and gravity
waves. As a result such neutral wind variations also tend to get evened out and
Joule heat is produced. At mid and high latitudes so upward propagating gravity
waves get damped when they reach to ionospheric dynamo region.

How to cite: Buchert, S. C.: Electrodynamic Coupling and Dissipation of Thermospheric Winds, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-16800, https://doi.org/10.5194/egusphere-egu2020-16800, 2020.

EGU2020-20550 | Displays | ST3.1

Characteristics of a HSS-driven magnetic storm in the high-latitude ionosphere; A case study of 14th of March 2016 storm

Nada Ellahouny, Anita Aikio, Marcus Pedersen, Heikki Vanhamäki, Ilkka Virtanen, Johannes Norberg, Maxime Grandin, Alexander Kozlovsky, Tero Raita, Kirsti Kauristie, Aurélie Marchaudon, Pierre-Louis Blelly, and Shin-ichiro Oyama

 Solar wind High-Speed Streams (HSSs) affect the auroral ionosphere in many ways, and several separate studies have been conducted of the different effects seen e.g. on aurora, geomagnetic disturbances, F-region behavior, and energetic particle precipitation. In this work, we study an HSS event in the solar cycle (24), which was associated with a co-rotating interaction region (CIR) that hit the Earth’s magnetopause at about 17:20 UT on 14 March 2016. The associated magnetic storm lasted for seven days, and the Dst index reached -56 nT. We use a very comprehensive set of measurements to study the whole period of this storm, following day by day for the magnetic indices and solar wind parameters and relating its consequences on ionospheric plasma parameters. We use EISCAT radar data from Tromsø and Svalbard stations to see the response in plasma parameters at different altitudes, riometer data for cosmic noise absorption, and IMAGE magnetometers to see the intensities of auroral electrojets. TomoScand ionospheric tomography provides us with electron densities over a wide region in Scandinavia and AMPERE data the global field-aligned currents. We identified 13 local substorms in the Scandinavian sector from the IL (IMAGE lower) index. Altogether, there were 11 global substorms, for which the AE index reaches 1000 nT. We discuss the development of currents, as well as E and D region precipitation during the course of this long-duration storm and compare local versus global behavior.

How to cite: Ellahouny, N., Aikio, A., Pedersen, M., Vanhamäki, H., Virtanen, I., Norberg, J., Grandin, M., Kozlovsky, A., Raita, T., Kauristie, K., Marchaudon, A., Blelly, P.-L., and Oyama, S.: Characteristics of a HSS-driven magnetic storm in the high-latitude ionosphere; A case study of 14th of March 2016 storm, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-20550, https://doi.org/10.5194/egusphere-egu2020-20550, 2020.

EGU2020-13921 | Displays | ST3.1

Ionosphere research with a nanosatellite’s radio wave spectrometer

Esa Kallio, Ari-Matti Harri, Anita Aikio, Arno Alho, Mathias Fontell, Riku Jarvinen, Kirsti Kauristie, Antti Kero, Antti Kestilä, Petri Koskimaa, Juha-Matti Lukkari, Olli Knuuttila, Jauaries Loyala, Joonas Niittyniemi, Johannes Norberg, Jouni Rynö, Esa Turunen, and Heikki Vanhamäki

The Suomi100 nanosatellite was launched on Dec. 3, 2018 (http://www.suomi100satelliitti.fi/eng). The 1 Unit (10 cm x 10 cm x 10 cm) polar orbit cubesat will perform geospace, ionosphere and arctic region research with a white light camera and a radio wave spectrometer instrument which operates in the 1-10 MHz frequency range.

Suomi 100 satellite type of nanosatellite, so called CubeSat, provides a cost effective possibility to provide in-situ measurements in the ionosphere. Especially, combined CubeSat observations with ground-based observations give a new view on auroras and associated electromagnetic phenomena. Especially joint CubeSat – ground based observation campaigns enable the possibility of studying the 3D structure of the ionosphere.

Increasing computation capacity has made it possible to perform simulations where properties of the ionosphere, such as propagation of the electromagnetic waves in the medium frequency, MF (0.3-3 MHz) and high frequency, HF (3-30 MHz), ranges is based on a 3D ionosphere model and on first-principles modelling. Electromagnetic waves at those frequencies are strongly affected by ionospheric electrons and, consequently, those frequencies can be used for studying the plasma. On the other hand, even if the ionosphere originally enables long-range telecommunication at MF and HF frequencies, the frequent occurrence of spatio-temporal variations in the ionosphere disturbs communication channels, especially at high latitudes. Therefore, study of the MF and HF waves in the ionosphere has both a strong science and technology interests.

We present computational simulation and measuring principles and techniques to investigate the arctic ionosphere by a polar orbiting CubeSat which radio instrument measures HF and MF waves. We introduce 3D simulations, which have been developed to study the propagation of the radio waves, both ground generated man-made radio waves and space formed space weather related waves, through the 3D arctic ionosphere with a 3D ray tracing simulation. We also introduce the Suomi100 CubeSat mission and its observations.

How to cite: Kallio, E., Harri, A.-M., Aikio, A., Alho, A., Fontell, M., Jarvinen, R., Kauristie, K., Kero, A., Kestilä, A., Koskimaa, P., Lukkari, J.-M., Knuuttila, O., Loyala, J., Niittyniemi, J., Norberg, J., Rynö, J., Turunen, E., and Vanhamäki, H.: Ionosphere research with a nanosatellite’s radio wave spectrometer, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-13921, https://doi.org/10.5194/egusphere-egu2020-13921, 2020.

EGU2020-17726 | Displays | ST3.1

Break up of a polar cap patch in the nightside ionosphere due to a flow channel event

Elizabeth Donegan-Lawley, Alan Wood, Gareth Dorrian, Alexandra Fogg, Timothy Yeoman, and Sean Elvidge

Flow channel events have previously been observed breaking up polar cap patches on the dayside ionosphere but, to the best of our knowledge, have not been observed on the nightside. We report observations of a flow channel event in the evening of the 9th January 2019 under quiet geomagnetic conditions. This multi-instrument study was undertaken using a combination of multiple EISCAT (European Incoherent Scatter) radars, SuperDARN (Super Dual Auroral Radar Network), MSP (Meridian Scanning Photometer) and GNSS (Global Navigation Satellite System) scintillation data. These data were used to build a picture of the evening’s observations from 1800 to 2359 UT. The flow channel event lasted a total of 13 minutes and was responsible for segmenting a polar cap patch. A decrease in electron density was observed, from a patch value of 1.4x1011 m3 to a minimum value of 5x1010 m3. In addition, ion velocities in excess of 1000 ms-1 and ion temperatures of greater than 2000 K were also observed. 

How to cite: Donegan-Lawley, E., Wood, A., Dorrian, G., Fogg, A., Yeoman, T., and Elvidge, S.: Break up of a polar cap patch in the nightside ionosphere due to a flow channel event, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-17726, https://doi.org/10.5194/egusphere-egu2020-17726, 2020.

EGU2020-18592 | Displays | ST3.1

Impact of Solar Wind High Speed Streams on Ionospheric Current Systems

Marcus Pedersen, Heikki Vanhamäki, Anita Aikio, Sebastian Käki, Ari Viljanen, Abiyot Workayehu, Colin Waters, and Jesper Gjerloev

High speed streams (HSS) and associated co-rotating interaction regions (CIR) in the solar wind are one of the major drivers of geomagnetic activity, especially during declining phases of sunspot cycles and near sunspot minima. We have identified 51 HSS/CIR driven geomagnetic storms that coincide with a Dst drop to less than -50nT during the period 2009-2018 and we investigate their impact on ionospheric current systems. Our approach is to study the evolution of the global scale current systems, i.e. the auroral electrojets and Region-1/2 field-aligned currents (FAC), with the SuperMAG magnetometers and AMPERE satellite data, respectively. The events are studied with a superposed epoch analysis centered at the storm onset to see the general behavior of the current system globally and in four different MLT sectors: noon, dusk, midnight and dawn. A minor enhancement of the integrated FAC was observed in the midnight, dawn and dusk sector 3 hours before the storm onset. The largest FAC and variability was observed in the dusk sector, and the integrated FAC maximum occurred in the middle of the storm main phase, 4 hours before the Dst minimum. This result will be compared to the evolution and behavior of the electrojet currents from superMAG. In the future a similar study will be conducted for ICME geomagnetic storms and compared to the HSS/CIR-related storms.

How to cite: Pedersen, M., Vanhamäki, H., Aikio, A., Käki, S., Viljanen, A., Workayehu, A., Waters, C., and Gjerloev, J.: Impact of Solar Wind High Speed Streams on Ionospheric Current Systems , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18592, https://doi.org/10.5194/egusphere-egu2020-18592, 2020.

The relationship between ionospheric parameters and solar activity proxies has broadly been assumed to be stable. However, using data of foF2 from three European stations and foE from two European stations we show that this assumption is not correct. In more recent years the dependence of ionospheric parameters on solar proxies is steeper than in the past. The change is between 1994 and 1997 for foF2 and after 2000 for foE. Also the relationships among solar proxies have changed, which might indicate some solar changes perhaps responsible for the observed changes of the relationship between ionospheric parameters and solar proxies with implications to trend and climatological studies, and modeling.

 

How to cite: Laštovička, J.: The relationship between ionospheric parameters and solar proxies is changing – when?, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3329, https://doi.org/10.5194/egusphere-egu2020-3329, 2020.

EGU2020-5300 | Displays | ST3.1

Localized enhancements of total electron content in Southern Hemisphere

Ilya Edemskiy and Ilya Edemskiy

Localized enhancements of total electron content (TEC) are usually registered during magnetic storms and are often believed to be connected with storm enhanced density (SED) events. Investigating global ionospheric maps we found that such localized TEC enhancements (LTE) could be observed in Southern Hemisphere during both disturbed and quiet time with no clear dependence on parameters of near space. Analysis of occurrence of LTEs in the regions of Indian and Southern Atlantic Oceans showed that part of them (observed during magnetic storms and localized in subpolar latitudes) can be connected with SEDs. Since another part of subpolar LTEs is detected during relatively quiet conditions its generation mechanism should be different despite they have similar spatial distribution. Most of the enhancements are observed in middle latitudes and is detected during all the investigated years. The occurrence rate of LTEs hardly depends on solar activity and the most probable season for LTE detection is April-September (autumn-winter).

Here we investigate reasons of generation both midlatitudinal and subpolar LTEs trying to define the mechanisms of their generation in details.

How to cite: Edemskiy, I. and Edemskiy, I.: Localized enhancements of total electron content in Southern Hemisphere, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5300, https://doi.org/10.5194/egusphere-egu2020-5300, 2020.

EGU2020-8268 | Displays | ST3.1

Interhemispheric comparison of the ionospheric electron density response during geomagnetic storm conditions

John Bosco Habarulema, Nicolas Bergeot, Jean-Marie Chevalier, Elisa Pinat, Dalia Buresova, Tshimangadzo Matamba, and Zama Katamzi-Joseph

The ionospheric electron density response to the occurrence of geomagnetic storms remains one of the challenges that is less understood partially on both short and long-term scales. This is even more complicated given that different locations within the same latitude region (for example in mid-latitudes) at times show different electron density responses as a result of complex dynamic and electrodynamics processes that may be present during one storm duration.  Mid-latitude regions are influenced by storm induced processes originating from both low and high latitudes. Using a combination of ionosonde and Global Navigational Satellite Systems (GNSS) observations, we show differences and or similarities in the electron density response during selected storm periods in both northern and southern hemisphere over the Europe-African sector. Physical mechanisms at play within different storm phases are explored using both observations and empirical modeling efforts.  

How to cite: Habarulema, J. B., Bergeot, N., Chevalier, J.-M., Pinat, E., Buresova, D., Matamba, T., and Katamzi-Joseph, Z.: Interhemispheric comparison of the ionospheric electron density response during geomagnetic storm conditions, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-8268, https://doi.org/10.5194/egusphere-egu2020-8268, 2020.

EGU2020-7842 | Displays | ST3.1

Large Scale TIDs climatology over Europe using HF Interferometry method

Estefania Blanch, Antoni Segarra, David Altadill, Vadym Paznukhov, and Jose Miguel Juan

Travelling Ionospheric Disturbances (TIDs) are ionospheric irregularities that occur as plasma density fluctuations that propagate as waves through the ionosphere over a wide range of velocities and frequencies. It has been demonstrated that Large Scale TIDs (LSTID) can be detected with several ionospheric sensors such as ionosondes and their main characteristics such as velocity, direction of propagation and amplitude can be inferred.

We have applied the recent developed HF Interferometry (HF-Int) method to detect the occurrence and main characteristics of LSTIDs over Europe for different solar activities (2014 – 2019) in order to perform a climatological analysis. HF-Int determines the dominant period of oscillation and the amplitude of the LSTIDs using spectral analysis, and estimates the propagation parameters of the LSTIDs from the measured time delays of the disturbance detected at different sensor sites.

The results show that larger diurnal and seasonal occurrence of LSTID happens near sunrise hours and night-time, especially during equinox. In the morning sector, prevailing velocity propagation is westward influenced by the solar terminator effect and it also depends on the season: during winter the dominant propagation velocity is north-westward and during summer is south-westward. In the evening and night sector, the prevailing propagation velocity is southward suggesting auroral origin of the disturbance. The higher activity at night-time might be the result that neutral winds favour equatorward propagation at night whereas at day might prevent to propagate to low latitudes.

Similar behaviour has been found for high and low solar activity with the difference that during summer at low solar activity, large occurrence of sporadic E layer happens during day time. Then, ionospheric data experience large data gaps at the F region because of screening of the Es (Es Blanketing effect). This results in a poor statistic under such a conditions for daytime summer low solar activity and the number of detected LSTID is lower.

How to cite: Blanch, E., Segarra, A., Altadill, D., Paznukhov, V., and Juan, J. M.: Large Scale TIDs climatology over Europe using HF Interferometry method, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7842, https://doi.org/10.5194/egusphere-egu2020-7842, 2020.

EGU2020-18779 | Displays | ST3.1

Far-ultraviolet Ionospheric Photometer

Ruyi Peng and Liping Fu

As a space-based optical remote sensing method, Far-ultraviolet Ionospheric Photometer with small size, low power consumption, high sensitivity is an important means to detect physical parameters of the ionosphere. Using the Far-ultraviolet Ionospheric Photometer to detect the intensity of ionospheric 135.6nm night airglow can obtain the ionospheric TEC, F2 layer peak electronic density(NmF2), which can be used to study the information on changes in ionospheric space environment,and the impact of the ionosphere on the radio communications, etc.; The ionospheric 135.6nm day airglow and the LBH radiation radiance can be used to obtain the ionospheric O / N2 ratio information, which can be used to study the space weather events and monitor the electromagnetic environment changes in the Earth's space. The FY3-D Ionospheric Photometer(IPM), launched on November 15, 2017, has a detection sensitivity which is greater than 150 counts / s / Rayleigh and a spatial field of view of 1.6 × 3.5 ° with high horizontal spatial resolution that will help to achieve the fine detection of the ionosphere. This report will analyze the FY3-D IPM detection results.At the same time,the report will introduce our research team’s work on the development and application of other payloads in the far ultraviolet band

How to cite: Peng, R. and Fu, L.: Far-ultraviolet Ionospheric Photometer, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18779, https://doi.org/10.5194/egusphere-egu2020-18779, 2020.

Geomagnetic storms cause the largest disturbances in the ionosphere-thermosphere system. We use measurements with satellites and ground based radars to study storm-induced variations in ionospheric plasma drift, ion density, and ion composition at low latitudes. It is found that the storm-time change of ion drift velocity in the equatorial ionosphere can reach 200-300 m/s, the change of ion density can be one or two orders of magnitude, and the change of ion composition can be 50-80%. These extremely large changes in the ionosphere can last for several hours or even a few days during the main and recovery phases of magnetic storms. The longitudinal, latitudinal and hemispheric differences of storm-time ionospheric disturbances are analyzed from measurements of multiple satellites or radar chain. Very long, continuous penetration of interplanetary electric fields to the equatorial ionosphere for 6 or even 14 hours are observed, and the time when disturbance dynamo electric fields become dominant is identified. The interplay of penetration, shielding, and disturbance dynamo electric fields in the storm-time ionosphere will be addressed. Mechanisms responsible for storm-time ionospheric dynamics will be discussed.

How to cite: Huang, C.: Ionospheric dynamic and coupling processes during geomagnetic storms, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-10498, https://doi.org/10.5194/egusphere-egu2020-10498, 2020.

EGU2020-11107 | Displays | ST3.1 | Highlight

Millennial solar irradiance forcing (Hallstatt’s cycle) in the terrestrial temperature variations

Valentina Zharkova, Simon Shepherd, and Elena Popova

In this paper we explore the millennial oscillations (or Hallstatt cycle) of the baseline solar magnetic field, total solar irradiance and baseline terrestrial temperature detected from Principal Component Analysis of the observed solar background magnetic field. We confirm the existence of these oscillations with a period of 2100-2200 years with the similar oscillations detected in carbon 14C isotope abundances and with wavelet analysis of solar irradiance in the past 12 millennia indicating the presence of this  millennial period among a few others. We also test again the idea expressed in our paper Zharkova et al, 2019 that solar inertial motion (SIM) can cause these millennial variations because of a change of the distance between the Sun and Earth. In this paper we use the S-E distance derived from the current JPL ephemeris, finding that currently starting from the Maunder minimum the Sun-Earth  distance is reducing by 0.00025 au per 100 years, or by 0.0025 au per 1000 years.. We present the estimation of variations of solar irradiance caused by this variation of the S-E distance caused by solar inertial motion (SIM) demonstrating these variations to be closely comparable with the observed variations of the solar irradiance measured by the SATIRE payload. We also estimate the baseline temperature variations since Maunder Minimum caused by the increase of solar irradiance caused by the recovery from grand solar minimum and by reduction of the S-E distance caused by  SIM. These estimations show that the Sun will still continue moving towards the Earth in the next 700 years that will result in the increase of the baseline terrestrial temperature by up to 2.5◦C in 2700. These variations of solar irradiance will be over-imposed by the variations of solar activity of 11 cycles and the two grand solar minima occurring in 2020-2053 and 2370-2415 caused by the double dynamo actions inside the Sun.

How to cite: Zharkova, V., Shepherd, S., and Popova, E.: Millennial solar irradiance forcing (Hallstatt’s cycle) in the terrestrial temperature variations, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11107, https://doi.org/10.5194/egusphere-egu2020-11107, 2020.

EGU2020-11369 | Displays | ST3.1

The Role of Field-Aligned Current Closure on the E and F-Region Coupled Thermosphere-Ionosphere

Daniel Billett, Kathryn McWilliams, and Mark Conde

In this study, the behaviour of both E and F-region neutral winds are examined in the vicinity of intense R1 and R2 field-aligned currents (FACs), measured by AMPERE. This is achieved through the dual sampling of both the green (557.5nm) and red (630nm) auroral emissions, sequentially, from a ground based Scanning Doppler Imager (SDI) located in Alaska.

With the addition of plasma velocity data from the Super Dual Auroral Radar Network (SuperDARN) and ionospheric parameters from the Poker Flat Incoheerent Scatter Radar (PFISR), we assess how the large closure of Pedersen currents (implied by the strong FACs) modifies the spatial and temporal structure of the neutral wind at different altitudes. We find that the thermosphere becomes significantly height dependent, which could indicate a broader altitude range where the Pedersen conductivity is more important during intense FAC closure.

How to cite: Billett, D., McWilliams, K., and Conde, M.: The Role of Field-Aligned Current Closure on the E and F-Region Coupled Thermosphere-Ionosphere , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11369, https://doi.org/10.5194/egusphere-egu2020-11369, 2020.

EGU2020-11602 | Displays | ST3.1

Interhemispheric conjugacy of transpolar arcs

Anita Kullen, Simon Thor, and Lei Cai

Most models predict that transpolar arcs (TPAs) occur simultaneously in both hemispheres. Conjugate TPAs are expected to appear in the northern and southern hemisphere on opposite oval sides. However, several observational studies have shown that this is not always the cases. It has been suggested that IMF Bx and/or the Earth dipole tilt may be responsible for non-conjugate TPAs. During strongly negative IMF Bx and/or positive Earth dipole tilt a TPA is expected to occur only in the northern hemisphere (for positive Bx and/or negative dipole tilt only in the southern hemisphere).

In the present work we revisit this question by investigating three previously published and one new TPA dataset regarding the influence of IMF Bx and Earth dipole tilt on interhemispheric TPA occurrence. The results show, the Earth dipole tilt has no statistical effect on TPA conjugacy while IMF Bx may have a small influence. However, this influence is much smaller than previously reported, when normalizing the IMF Bx distribution during TPAs with the average IMF Bx distribution in the solar wind during the time period covered by the respective dataset.

In the second part of this study we present results from the new TPA dataset, which is based on three months of SUSSI DMSP images. Arc location and IMF conditions during conjugate and non-conjugate TPAs are discussed in detail and possible reasons for non-conjugate TPA events are discussed.

How to cite: Kullen, A., Thor, S., and Cai, L.: Interhemispheric conjugacy of transpolar arcs, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11602, https://doi.org/10.5194/egusphere-egu2020-11602, 2020.

EGU2020-12208 | Displays | ST3.1

Features of ionospheric responses to geomagnetic storms of low solar activity period

Iurii Cherniak, Wenbin Wang, and Irina Zakharenkova

During low solar activity periods, geomagnetic disturbances still occur and impact the Earth’s ionosphere. In such conditions, even comparatively weak disturbances can lead to a noticeable ionospheric response. In particular during the extended solar minimum of the 23rd solar cycle, the October 11, 2008 geomagnetic storm of moderate intensity (Dst = -50 nT, maximum Kp=6) caused strong positive ionospheric disturbances. At midlatitudes, the storm-induced enhancement in total electron contain (TEC) exceeded by two times the normal quite time day-to-day variability and the strong density enhancement was registered in the topside ionosphere.

Using a combination of the ground-based and low-Earth-orbit (LEO) observations (ground-based GNSS networks, LEO RO COSMIC, in-situ and onboard GPS CHAMP and Swarm measurements, space-based optical observations), we examined features of ionospheric responses to several weak-to-moderate geomagnetic storms occurred at low solar activity periods of the 23rd and 24th solar cycles (2008 and 2019 years respectively). The ionospheric response was analyzed in terms of the storm-time TEC changes, large and medium scale travelling ionospheric disturbances generation, and auroral plasma irregularities intensity and location. The prominent features obtained were an intensification of ionospheric irregularities occurrence at sub-auroral latitudes and an equatorward expansion of the auroral irregularities oval, differences of TEC variations from quite-time variability, response of the topside ionosphere, and TIDs generation.

The first-principle TIEGCM simulations with a comprehensive data-model comparison was carried out to specify the main drivers responsible for the observed ionospheric responses.

This work is supported by the NASA LWS grant NNX15AB83G.

How to cite: Cherniak, I., Wang, W., and Zakharenkova, I.: Features of ionospheric responses to geomagnetic storms of low solar activity period, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-12208, https://doi.org/10.5194/egusphere-egu2020-12208, 2020.

EGU2020-12474 | Displays | ST3.1

The Polar Wind Modulated by the Spatial Inhomogeneity of the Strength of the Earth’s Magnetic Field

Kun Li, Matthias Förster, Zhaojin Rong, Stein Haaland, Elena Kronberg, Jun Cui, Lihui Chai, and Yong Wei

When the geomagnetic field is weak, the small mirror force allows precipitating charged particles to deposit energy in the ionosphere. This leads to an increase in ionospheric outflow from the Earth’s polar cap region, but such an effect has not been previously observed because the energies of the ions of the polar ionospheric outflow are too low, making it difficult to detect the low-energy ions with a positively charged spacecraft. In this study, we found anti-correlation between ionospheric outflow and the strength of the Earth’s magnetic field. Our results suggest that the electron precipitation through the polar rain can be a main energy source of the polar wind during periods of high levels of solar activity. The decreased magnetic field due to spatial inhomogeneity of the Earth’s magnetic field and its effect on outflow can be used to study the outflow in history when the magnetic field was at similar levels.

How to cite: Li, K., Förster, M., Rong, Z., Haaland, S., Kronberg, E., Cui, J., Chai, L., and Wei, Y.: The Polar Wind Modulated by the Spatial Inhomogeneity of the Strength of the Earth’s Magnetic Field, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-12474, https://doi.org/10.5194/egusphere-egu2020-12474, 2020.

EGU2020-16400 | Displays | ST3.1

Global Ionospheric Response to CIR/HSS Induced Geomagnetic Storms

Catalin Negrea, Costel Munteanu, and Marius Echim

The solar wind is one of the main drivers for the thermosphere-ionosphere, affecting both long-term trends and short-term variability. In this study, we investigate the global ionospheric impact of high-speed solar wind streams/corotating interaction regions (HSS/CIR). Ten such events are identified between December 1st 2007 and April 16th 2008, based on solar wind speed, density and magnetic field measurements. Each event triggered a geomagnetic storm, highlighted by the temporal evolution of the SYM-H and AE geomagnetic indices. The ionospheric response to these storms is investigated using 28 globally distributed ionosonde stations, providing NmF2 and hmF2 measurements. Spectral peaks associated with 27-, 13- and 9-day periodicities are identified at most locations, highlighting the global nature of the ionospheric response. The amplitude of the ionospheric diurnal variability is also shown to vary, to a large extent correlated with the HSS/CIR induced geomagnetic storms.

How to cite: Negrea, C., Munteanu, C., and Echim, M.: Global Ionospheric Response to CIR/HSS Induced Geomagnetic Storms, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-16400, https://doi.org/10.5194/egusphere-egu2020-16400, 2020.

EGU2020-18107 | Displays | ST3.1

Properties and Generation of Large Scale Travelling Ionospheric Disturbances during 8 September 2017

Claudia Borries, Arthur Amaral Ferreira, Chao Xiong, Renato Alves Borges, Jens Mielich, and Daniel Kouba

Large Scale Travelling Ionospheric Disturbances (LSTIDs) are a frequent phenomenon during ionospheric storms, indicating strong electrodynamic processes in high latitudes. LSTIDs are signatures of Atmospheric Gravity Waves (AGW) observed in the changes of the electron density in the ionosphere. During ionospheric storms, large scale AGWs are often generated in the vicinity of the auroral region, where sudden strong heating processes take place.

Many LSTIDs are observed during the ionosphere storm during the September 2017 Space Weather event. In this presentation, the LSTID occurrence on 8th September 2017 is analysed in more detail, based on a TID detection method using ground based Global Navigation Satellite System (GNSS) measurements. Fast LSTIDs are observed in midlatitudes between 0-3 UT and 13-16 UT. Slow LSTIDs are observed between 3-12 UT. A significant strong wave-like TEC perturbation occurred in high latitudes at noon, which vanished at around 50°N. A strong single LSTID in mid-latitudes generated in high latitudes around 18 UT. Consulting IMAGE magnetometer data, ionosonde measurements and Swarm field aligned current measurements, strong heating processes, the extension of the Auroral oval and unusual electrodynamic processes are discussed as source mechanisms for these LSTIDs.

How to cite: Borries, C., Ferreira, A. A., Xiong, C., Borges, R. A., Mielich, J., and Kouba, D.: Properties and Generation of Large Scale Travelling Ionospheric Disturbances during 8 September 2017, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18107, https://doi.org/10.5194/egusphere-egu2020-18107, 2020.

EGU2020-20811 | Displays | ST3.1

Investigating waves and instabilities in the auroral E region via multi-points in-situ from the SPIDER sounding rockets

Gabriel Giono, Nickolay Ivchenko, and Tima Sergienko

On February 2nd 2016 the SPIDER sounding rocket released ten Free Falling Units (FFUs) inside an active westward-travelling auroral electrojet (between 100 to 120 km altitude). Each FFUs carried four electric field probes and four Langmuir probes, respectively on 2 and 1-meter wire booms, as well as a 3-axis fluxgate magnetometer, a gyroscope, an accelerometer and a GPS recorder. The main scientific objective of the project was to study waves and instabilities on various spatial scales, in particular the Farley-Buneman instability, as well as providing an in-situ picture of plasma properties inside the aurora.

Six FFUs were successfully recovered after landing and, despite some mechanical issues on some units, the recorded data showed promising results. Some of these results will be discussed in this presentation, namely (i) the electron density and temperature profiles from two FFUs compared to the incoherent scatter radar measurements from the EISCAT facility, (ii) the hints of different turbulence regimes along the flight seen in the electron density, (iii) the search for Farley-Buneman instability in the electric field data via wavelet analysis, (iv) the observation of electric field waves propagating between two FFUs and the comparison with ground-based observation of the aurora from the ALIS multi-camera system, and finally (v) a global comparison between perturbations seen in the electric field, magnetic field and plasma density and temperature on two FFUs.

These results demonstrated the potential of multi-point in-situ measurements for understanding multi-scale processes in auroras, and preliminary results from the reflight of the rocket to be happening in February 2020 will also be briefly presented.

How to cite: Giono, G., Ivchenko, N., and Sergienko, T.: Investigating waves and instabilities in the auroral E region via multi-points in-situ from the SPIDER sounding rockets, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-20811, https://doi.org/10.5194/egusphere-egu2020-20811, 2020.

EGU2020-21560 | Displays | ST3.1

High-resolution measurements of plasma entry into the polar cap: indication of plasma structuring

Yaqi Jin, Andres Spicher, Magnus Ivarsen, Jøran Moen, and Lasse Clausen

Polar cap patches/tongue of ionization are believed to be the dominant space weather phenomena in the high-latitude ionosphere as they are associated with significant plasma irregularities. These irregularities can greatly degrade satellite-based communication and navigation systems that rely on trans-ionospheric signals. Due to the practical need for a more reliable space weather forecasting system, the plasma structuring of these phenomena are an active area of research in recent years. In the study, we present a case of a tongue of ionization that was formed due to the transport of the high-density plasma from the dayside sunlit ionosphere into the dark polar cap. The tongue of ionization was probed by the first Norwegian scientific satellite NorSat-1 in noon-midnight orbits. Among other payloads, NorSat-1 carries the multi-needle Langmuir probe (m-NLP) system that is capable of measuring electron density at a rate up to 1 kHz. The electron density measurement shows significant irregularities at all scales along the profile of the tongue of ionization. In the dayside auroral oval, the electron density is associated with clear mesoscale (20-80 km) density enhancements, which are likely caused by structured auroral precipitations. We also use data from other satellites (e.g., Swarm and DMSP) to support observations from NorSat-1.

How to cite: Jin, Y., Spicher, A., Ivarsen, M., Moen, J., and Clausen, L.: High-resolution measurements of plasma entry into the polar cap: indication of plasma structuring, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21560, https://doi.org/10.5194/egusphere-egu2020-21560, 2020.

EGU2020-22534 | Displays | ST3.1

Conditions for topside ionline enhancements

Theresa Rexer, Björn Gustavsson, Thomas Leyser, and Mike Rietveld

High frequency (HF) enhanced ion line spectra as a response to magnetic field aligned HF pumping of the polar ionosphere in an O-mode polarization can be observed at the top and bottomside F-region ionosphere under certain conditions. The European Incoherent Scatter (EISCAT) UHF radar was directed in magnetic zenith on 18th and 19th October 2017 while stepping the pump frequency of the EISCAT Heating facility across the double resonance frequency of the fourth harmonic of the electron gyrofrequency and the local upper hybrid frequency, in a 2-min-on, 2-min-off pump cycle, stepping both upward and downward in frequency. We present observations of two separate cases of topside HF enhanced ion lines (THFIL). THFIL simultaneous to bottomside HFIL (BHFIL) and conditioned by the relative proximity to the double resonance frequency, consistent with previous observations \citep{Rexer2018} were observed for heating pulses on 19th October. Recurring THFIL with a second set of characteristics were observed on 18th October, appearing independently from BHFIL and possibly conditioned by the proximity of the topside double resonance frequency. Propagation of the pump wave to the topside ionosphere is consistent with L-mode wave propagation facilitated by density striations in the plasma. We consider the conditions for the occurrence of THFIL for two cases/types of observations. 

How to cite: Rexer, T., Gustavsson, B., Leyser, T., and Rietveld, M.: Conditions for topside ionline enhancements , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-22534, https://doi.org/10.5194/egusphere-egu2020-22534, 2020.

ST3.2 – Wave couplings in the atmosphere-ionosphere system

EGU2020-3122 | Displays | ST3.2

Thermospheric composition response to Sudden Stratospheric Warmings observed by the Global-Scale Observations of the Limb and Disk (GOLD) instrument

Jens Oberheide, Nicholas Pedatella, Quan Gan, Komal Kumari, Alan Burns, and Richard Eastes

EGU2020-12350 | Displays | ST3.2

The upper atmospheric responses to tidal and planetary waves

Sheng-Yang Gu

Tidal and planetary waves (PWs) in the mesosphere and lower thermosphere region could have significant impact on the upper thermosphere/ionosphere system through direct propagations, E region wind dynamo, and the change of residual circulations. We would like to show some results from BeiDou and COSMIC observations, as well as TIME-GCM simulations, to illustrate the lower/upper atmospheric couplings through different mechanisms. Generally, the spatial structures of the ionospheric responses to planetary waves agree with the ionospheric fountain effect, which indicates the important roles of equatorial wind dynamos in transmitting planetary wave signals to the ionosphere. The TIME-GCM simulations show that the zonal and meridional components of the planetary waves could result in evident vertical ion drift perturbations, while the net ionospheric effect is related to both their latitudinal structures and phases. The simulations also show that the change of tidal amplitudes and secondary PWs generated by PW-tide interaction are also important to the ionospheric variabilities. Besides, the couplings through PW-induced residual circulations are exhibited by both model simulations and TEC observations from BeiDou satellite system.

How to cite: Gu, S.-Y.: The upper atmospheric responses to tidal and planetary waves, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-12350, https://doi.org/10.5194/egusphere-egu2020-12350, 2020.

EGU2020-18642 | Displays | ST3.2

Comparing the ionospheric response to the 2008/2009 and 2018/2019 SSW events

Tarique Adnan Siddiqui, Yosuke Yamazaki, and Claudia Stolle

It is now well accepted that the ionosphere and thermosphere are sensitive to forcing from the lower atmosphere (troposphere-stratosphere) owing mainly to the progress that have been made in the last decade in understanding the vertical coupling mechanisms connecting these two distinct atmospheric regions. In this regard, the studies linking the upper atmosphere (mesosphere-lower thermosphere-ionosphere) variability due to sudden stratospheric warming (SSW) events have been particularly important. The change of stratospheric circulation due to SSW events modulate the spectrum of vertically upward propagating atmospheric waves (gravity waves, tides, and planetary waves) resulting in numerous changes in the state of the upper atmosphere. Much of our understanding about the upper atmospheric variability associated due to the SSWs events have been gained by studying the 2008/2009 SSW event, which occurred under extremely low solar flux conditions. Recently another SSW event in 2018/2019 occurred under similar low solar flux conditions. In this study we simulate both these SSW events using Whole Atmosphere Community Climate Model with thermosphere and ionosphere extension (WACCM-X) and present the findings by comparing the ionospheric and thermospheric response to both these SSW events. The tidal characteristics of the semidiurnal solar and lunar tides and the thermospheric composition for both these SSW events are compared and the causes of varying responses are investigated.

How to cite: Siddiqui, T. A., Yamazaki, Y., and Stolle, C.: Comparing the ionospheric response to the 2008/2009 and 2018/2019 SSW events, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18642, https://doi.org/10.5194/egusphere-egu2020-18642, 2020.

EGU2020-2631 | Displays | ST3.2

Statistical investigation of gravity wave propagation in the Czech Republic and above

Jaroslav Chum, Katerina Podolska, Jan Rusz, and Jiri Base

Propagation of gravity waves (GWs) is studied in the troposphere and thermosphere/ionosphere. The investigation of GW propagation in the troposphere is based on measurements by large scale array of absolute microbarometers with high resolution that is located in the westernmost part of the Czech Republic. On the other hand, the propagation of GWs in the thermosphere/ionosphere is observed remotely, using multi-frequency and multi-point continuous HF Doppler sounding system operating in the western part of the Czech Republic. The reflection heights of sounding radio waves of different frequencies are determined from ionospheric sounder, located in Pruhonice in the vicinity of Prague. Propagation velocities and directions are in both cases calculated from time/phase delays between signals recorded at different locations. The investigation of propagation of GWs in the ionosphere is performed in three dimensions as the observation points (reflection points of radio signals) are separated both horizontally and vertically. It is shown that GWs in the ionosphere usually propagate with wave vectors directed obliquely downward, which means upward propagation of energy. In addition, seasonal and diurnal changes of propagation directions were found. Typical propagation velocities of GWs observed at ionospheric heights are much higher (~100 to 200 m/s) than those observed on the ground (several tens of m/s).        

How to cite: Chum, J., Podolska, K., Rusz, J., and Base, J.: Statistical investigation of gravity wave propagation in the Czech Republic and above , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2631, https://doi.org/10.5194/egusphere-egu2020-2631, 2020.

This paper studies the daytime medium scale traveling ionospheric disturbances (MSTIDs) in the mid- and low-latitude ionosphere for a period of nearly half a solar cycle (2014-2019) using SWARM observations. We specifically focus on daytime MSTIDs to rule out any contribution from nighttime plasma irregularities. Fluctuations in electron density are primarily used to identify the MSTIDs. These wave like structures are independently observed in both electron density and magnetic fluctuations, although they do not always show one to one correlation. In most cases, the structures are observed by both satellite ‘A’ and ‘C’, suggesting that their zonal extent is more than 140 km. The study makes an attempt to understand and explain the magnetic conjugate nature of the MSTIDs. To have a better understanding of the dynamics of the MSTIDs, ground based GPS-TEC and ionosonde data has been used on case to case basis, wherever available. Additionally, spatio-temporal statistics of MSTID distribution is presented.

How to cite: Nayak, C. and Buchert, S.: Characteristics of daytime medium scale traveling ionospheric disturbances (MSTIDs) as observed by SWARM, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-8844, https://doi.org/10.5194/egusphere-egu2020-8844, 2020.

EGU2020-7390 | Displays | ST3.2

Monitoring Perturbations in the Lower-Ionosphere Using GNSS Radio Occultation Observed from Spire's Cubesat Constellation

Giorgio Savastano, Karl Nordström, Matthew Angling, Vu Nguyen, Timothy Duly, Takayuki Yuasa, and Dallas Masters

The lower altitude region of the ionosphere (60-150 km) is characterized by a strong coupling between the neutral atmosphere and ionospheric plasma. Due to the high ion-neutral collision rate the plasma at these altitudes is less constrained to follow the magnetic field lines compared to plasma at higher altitudes in the ionosphere. This both permits the development of the windshear mechanism responsible for the formation of sporadic E (Es) layers and affects the coupling between atmospheric gravity waves (AGWs) and the ionospheric plasma. 

AGWs transport energy from the lower atmosphere upward to higher altitudes. The wave amplitudes increase with altitude and eventually couple to the ionospheric plasma generating electron density perturbations or travelling ionospheric disturbances (TIDs). 

Es layers are high-density, narrow-altitude layers of enhanced electron density in the ionosphere’s E region. Contrary to what the name would suggest, Es occurs relatively frequently and its climatology has been characterised through ionosonde studies. Furthermore, the vertical structure of Es has been studied using sounding rockets. However, such measurements are very sparse and cannot be used to routine monitoring or for detecting the Es occurrence at a particular time and location. 

Monitoring AGW and Es layers is of great interest to many terrestrial applications, such as natural hazard warning systems, radio communications, and global navigation satellite system (GNSS) users. Recently, the coupling between Es layers and AGWs has also seen increased research attention. 

Spire operates a large constellation of 3U cubesats which carry a radio occultation (RO) GNSS receiver. For ionospheric studies, the satellites measure Total Electron Content (TEC) data in both zenith-looking and RO geometries using dual frequency observations. Furthermore, the high rate (50Hz) phase measurements that are generally used for neutral atmosphere RO can also be used to produce relative TEC profiles of the lower ionosphere with high vertical resolution (approximately 100m at E region altitudes). In this talk, we review recent results describing the coverage and quality of E region ionospheric measurements collected by Spire. Furthermore, we describe Spire's Es and AGW automated detection algorithm that is based on a Hilbert–Huang transform (HHT) of the relative TEC profiles and we compare our results with time coincident and co-located ionosonde data. We also look toward the future and describe how low cost cubesat constellations can be used for global monitoring of AGWs and Es layers. These first results also open the way to near real-time monitoring and classification of more general ionospheric anomalies

How to cite: Savastano, G., Nordström, K., Angling, M., Nguyen, V., Duly, T., Yuasa, T., and Masters, D.: Monitoring Perturbations in the Lower-Ionosphere Using GNSS Radio Occultation Observed from Spire's Cubesat Constellation, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7390, https://doi.org/10.5194/egusphere-egu2020-7390, 2020.

EGU2020-6009 | Displays | ST3.2

Perturbations of Global Wave Dynamics During Stratospheric Warming Events of the Solar Cycle 24

Valery Yudin, Larisa Goncharenko, Svetlana Karol, and Lynn Harvey

The paper presents analysis and interpretation of observed perturbations of global wave dynamics in the Ionosphere-Thermosphere-Mesosphere (ITM) during the recent mid-winter Arctic Sudden Stratospheric Warming (SSW) events under solar minimum (2009, 2010, 2018, and 2019), transition to solar maximum (2012) and solar maximum (2013) conditions of the Solar Cycle 24. Employing the 116-level configuration of the thermosphere extension of Whole Atmosphere Community Climate Model (WACCMX-116L), constrained by the meteorological troposphere-stratosphere analyses of Goddard Earth Observing System, version 5 (GEOS-5) of Global Modeling and Data Assimilation Office, we study and characterize the striking amplifications of the solar thermal semidiurnal tide, as one of the main drivers of the ITM variability, after onsets of major and minor SSW events. The dominance and growth of the semidiurnal tide over the diurnal and terdiurnal modes in the lower thermosphere above ~100 km are typical features of the tidal dynamics during major SSW events of the Solar Cycle 24 as suggested by model predictions. The growth of the semidiurnal tidal mode during SSW events is also supported by observational analysis of diurnal cycles from temperature space-borne observations (SABER/TIMED). In the vertical domain of the meteor radar observations at the Southern extra-tropics and low latitudes the model and data revealed the systematic presence of the strong quasi two-day wave wind oscillations that prevail over the tidal winds between 80 and 100 km during mid-January SSW events. In the high and middle latitudes of the Northern Hemisphere model simulations are capable to reproduce the day-to-day variability of tidal and PW oscillations deduced from satellite temperature data. The self-consistent whole atmosphere predictions of global-scale components of neutral dynamics (prevailing winds, planetary waves and tides) become important factor to reproduce and forecast the perturbed state of the ITM as observed from the ground and the space during SSW events of the Solar Cycle 24. The SSW-driven global perturbations of tides can significantly change diurnal cycles of the plasma in the low-latitude and extra-tropical E-region of the ionosphere as will be briefly illustrated by day-day variations of observed and simulated total electron content and plasma drifts.

How to cite: Yudin, V., Goncharenko, L., Karol, S., and Harvey, L.: Perturbations of Global Wave Dynamics During Stratospheric Warming Events of the Solar Cycle 24, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6009, https://doi.org/10.5194/egusphere-egu2020-6009, 2020.

The hemispheric asymmetry of the ionospheric variation in the American sector (45°N~45°S, MLAT; 80°~60°W) is studied with total electron content (TEC) data during major sudden stratospheric warming events. The amplitude (AM2) and relative strength (RSM2) of the semi-diurnal lunar tidal component (M2) of TEC are analyzed. RSM2 is the ratio between the energy of M2 and the energy of all the studied tidal components. The magnitudes of AM2 and RSM2 exhibit clear hemispheric and latitudinal variations. The AM2 in the north of the magnetic equator tends to occur at lower magnetic latitudes than the AM2 in the south of the magnetic equator. The RSM2 exhibits similar features as the AM2 but the difference is more distinct. We suggest that such hemispheric asymmetry of M2 parameters is related to the hemispheric asymmetry of the EIA and the latitudinal variation of the amplitude of the solar tidal components in winter.

How to cite: Zhang, D. and Liu, J.: Hemispheric asymmetry of the ionospheric variation during major sudden stratospheric warming events, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-20247, https://doi.org/10.5194/egusphere-egu2020-20247, 2020.

EGU2020-4062 | Displays | ST3.2

Variations of upper atmospheric high-order solar tidal harmonics during sudden stratospheric warming 2018

Maosheng He, Jeffrey Forbes, Jorge Chau, Guozhu Li, Weixing Wan, and Dmitry Korotyshkin

Solar tides are the most predictably-occurring waves in the upper atmosphere. Although the dynamical theory can be dated back to Laplace in the 16th century, in the upper atmosphere tides  were rarely studied observationally until satellites and ground-based radars became common. To date, studies have mainly focused on low-order harmonics. Here, we combine mesospheric wind observations from three longitudinal sectors to investigate high-order harmonics. Results illustrate that the first six harmonics appear in early 2018, all of which are dominated by sum-synchronous components. Among these harmonics, the 6hr, 4.8hr, and 4hr components weaken at the sudden stratospheric warming (SSW) onset. The weakening could be explained in terms of variations in the background zonal wind.

How to cite: He, M., Forbes, J., Chau, J., Li, G., Wan, W., and Korotyshkin, D.: Variations of upper atmospheric high-order solar tidal harmonics during sudden stratospheric warming 2018, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4062, https://doi.org/10.5194/egusphere-egu2020-4062, 2020.

EGU2020-11224 | Displays | ST3.2

Vertical Atmospheric Coupling during the September 2019 Antarctic Sudden Stratospheric Warming

Yosuke Yamazaki, Vivien Matthias, Yasunobu Miyoshi, Claudia Stolle, Tarique Siddiqui, Guram Kervalishvili, Jan Laštovička, Michal Kozubek, William Ward, David Themens, Samuel Kristoffersen, and Patrick Alken

A sudden stratospheric warming (SSW) is an extreme wintertime meteorological phenomenon occurring mostly over the Arctic region. Studies have shown that an Arctic SSW can influence the whole atmosphere including the ionosphere. In September 2019, a rare SSW event occurred in the Antarctic region, following strong wave-1 planetary wave activity. The event provides an opportunity to investigate its broader impact on the upper atmosphere, which has been largely unexplored in previous studies. Ionospheric data from ESA's Swarm satellite constellation mission show prominent 6-day variations in the dayside low-latitude region during the SSW, including 20-70% variations in the equatorial zonal electric field, 20-40% variations in the electron density, and 5-10% variations in the top-side total electron content. These ionospheric variations have characteristics of a westward-propagating wave with zonal wavenumber 1, and can be attributed to forcing from the middle atmosphere by the Rossby normal mode “quasi-6-day wave” (Q6DW). Geopotential height measurements by the Microwave Limb Sounder aboard NASA's Aura satellite reveal a burst of global Q6DW activity in the mesosphere and lower thermosphere at this time, which is one of the strongest in the record. These results suggest that an Antarctic SSW can lead to ionospheric variability by altering middle atmosphere dynamics and propagation characteristics of large-scale waves from the middle atmosphere to the upper atmosphere.

How to cite: Yamazaki, Y., Matthias, V., Miyoshi, Y., Stolle, C., Siddiqui, T., Kervalishvili, G., Laštovička, J., Kozubek, M., Ward, W., Themens, D., Kristoffersen, S., and Alken, P.: Vertical Atmospheric Coupling during the September 2019 Antarctic Sudden Stratospheric Warming, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11224, https://doi.org/10.5194/egusphere-egu2020-11224, 2020.

The energy input from the solar wind and magnetosphere is thought to dominate the ionospheric response during geomagnetic storms. However, at the storm recovery phase, the role of forces from lower atmosphere could be as important as that from above. In this study, we focused on the geomagnetic storm happened on 6–11 September 2017. The ground-based total electron content (TEC) data as well as the F region in situ electron density measured by the Swarm satellites reveals that at low and equatorial latitudes the dayside ionosphere shows as prominent positive and negative responses at the Asian and American longitudinal sectors, respectively. The global distribution of thermospheric O/N2 ratio measured by global ultraviolet imager on board the TIMED satellite cannot well explain such longitudinally opposite response of the ionosphere. Comparison between the equatorial electrojet variations from stations at Huancayo in Peru and Davao in the Philippines suggests that the longitudinally opposite ionospheric response should be closely associated with the interplay of E region electrodynamics. By further applying nonmigrating tidal analysis to the ground‐based TEC data, we find that the diurnal tidal components, D0 and DW2, as well as the semidiurnal component SW1, are clearly enhanced over prestorm days and persist into the early recovery phase, indicating the possibility of lower atmospheric forcing contributing to the longitudinally opposite response of the ionosphere on 9–11 September 2017.

How to cite: Xiong, C., Luehr, H., and Yamazaki, Y.: An opposite response of the low-latitude ionosphere at Asian and American sectors during storm recovery phase: drivers from below and above, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5401, https://doi.org/10.5194/egusphere-egu2020-5401, 2020.

Beginning with 1959 that means over more than 60 years, field strength measurements of the broadcasting station, Allouis (Central France), have been carried out at Kühlungsborn (54° N, 12° E, Mecklenburg, Northern Germany. These so-called indirect phase-height measurements of low frequency radio waves (here with a frequency of 162 kHz) are used to examine the long-term evolution and trends of the mesosphere over Europe. The advantages of the method are the low costs and the simplicity of operation. The extended reanalyzed fifth release of standard-phase height (SPH) are presented.

The SPH-series are anti-correlated to the solar cycle as known because stronger photo-ionization is linked with higher number of electrons, which reduces the SPH. The anti-correlation between SPH and proxies of solar cycle are well established. Furthermore the statistical analysis of the SPH-series shows a significant overall trend in the order of hundred meters per decade induced by a shrinking stratosphere due to global warming. Strong intra-decadal variability is related to QBO like and ENSO like variability. The derived thickness temperature of the mesosphere decreased statistically significant over the period 1959-2019 after pre-whitening with summer means of solar sun spot numbers. The trend value is in the order of about -1 K/ decade if the stratopause trend is excluded. The amount of linear regression is weaker, -0.8 K/ decade for the period of 1963-1985 (2 SCs), but stronger, about -1.6 K/ decade during 1995-2016 (last 2 SCs).

How to cite: Peters, D. H. W. and Entzian, G.: Standard-Phase-height measurements over Europe during 60 years of measurements – Long-term variability and trends of the mesosphere, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-9551, https://doi.org/10.5194/egusphere-egu2020-9551, 2020.

EGU2020-381 | Displays | ST3.2

The nighttime poleward wind responses to SAPS simulated by TIEGCM: a universal time effect

Kedeng Zhang, Hui Wang, Wenbin Wang, Jing Liu, Shunrong Zhang, and Cheng Sheng

The present work investigates the nighttime meridional wind (30º-50º magnetic latitude and 19-22 magnetic local time) in response to subauroral polarization streams (SAPS) that commence at different universal time (UT) by using Thermosphere Ionosphere Electrodynamics General Circulation Model (TIEGCM) under geomagnetically disturbed conditions that are closely related to the southward interplanetary magnetic field (IMF) carried by the solar wind. The SAPS effects on the meridional winds show a remarkable UT variation, with larger magnitudes at 00 and 12 UT than at 06 and 18 UT. The strongest poleward wind emerges when SAPS commence at 06 UT, and the weakest poleward wind develops when SAPS occur at 00 UT. A diagnostic analysis of model results shows that the pressure gradient is more prominent for the developing of the poleward wind at 00 and 12 UT. Meanwhile, the effect of the ion drag is important in the modulation of the poleward wind velocity at 06 and 18 UT. This is caused by the misalignment of the geomagnetic and geographic coordinate systems, resulting to a large component of ion drag in geographically northward (southward) direction due to the SAPS channel orientation at 06 and 18 UT (00 and 12 UT). The Coriolis force effect induced by westward winds maximizes (minimizes) when SAPS commence at 12 UT (00 UT). The centrifugal force due to the accelerated westward winds shows similar UT variations as the Coriolis force, but with an opposite effect.

How to cite: Zhang, K., Wang, H., Wang, W., Liu, J., Zhang, S., and Sheng, C.: The nighttime poleward wind responses to SAPS simulated by TIEGCM: a universal time effect, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-381, https://doi.org/10.5194/egusphere-egu2020-381, 2020.

EGU2020-1309 | Displays | ST3.2

Geomagnetic field variations due to Solar and Lunar tides in the Brazilian Sector

Vera Yesutor Tsali-Brown, Paulo Roberto Fagundes, Ana Roberta Paulino, Valdir Gil Pillat, and Maurício José Alves Bolzam

Abstract

Geomagnetic field variations in 2018 due to solar and lunar tides in the Brazilian sector were studied using data provided by magnetometers installed at São José dos Campos (23.21oS, 0345.97oW; Dip latitude 20.9oS), Eusébio, Ceará (3.89° S, 38.46° W) and São Luís, Maranhão (2.53° S, 44.30° W). Variations associated with these tides were identified using the horizontal component of the geomagnetic field, H(nT). Least square fit method was employed in determining the monthly amplitudes and phases of the diurnal, semidiurnal and ter-diurnal solar tides. The monthly amplitudes and phases of the lunar tide were then calculated using the residual measurements (obtained after subtracting the solar tidal components from each day), converting the solar local time to lunar time and subjecting the residuals to harmonic analysis. The maximum solar tide amplitude recorded was 23.96nT(diurnal) in March, at Eusébio whereas the minimum amplitude was 0.45nT(terdiurnal) recorded in December at São José dos Campos. The lunar tide recorded a maximum amplitude of 4.33nT(semidiurnal) in February, at São Luís and a minimum amplitude of 0.13nT(diurnal) in August, at Eusébio.

 

 

Keywords: Solar tides, Lunar tides, Geomagnetic field, Magnetometer.

 

How to cite: Tsali-Brown, V. Y., Fagundes, P. R., Paulino, A. R., Pillat, V. G., and Bolzam, M. J. A.: Geomagnetic field variations due to Solar and Lunar tides in the Brazilian Sector, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1309, https://doi.org/10.5194/egusphere-egu2020-1309, 2020.

Based on Swarm satellite data from 2015 through 2018, we present the mean characteristics of
magnetic fifield flfluctuations at midlatitudes and low latitudes. It is the fifirst comprehensive study focusing on
small‐scale variations (<10 km). Events are observed on about 35% of the orbits. The highest occurrence
rates are detected after sunset, in the East Asian/Australian sector, and during months around June solstice.
Low occurrence rates are found at low magnetic latitudes (below ±10° quasi‐dipole latitude), in the region
of the South Atlantic Anomaly, and during equinox seasons. All these occurrence features compare well
with those of medium‐scale traveling ionospheric disturbances. We therefore term our small‐scale events
small‐scale traveling ionospheric disturbances (SSTIDs). SSTIDs exhibit high fifield‐aligned current (FAC)
densities connected to narrow current sheets with meridional width of typically 4 km. The intense FACs of
several μA/m2 flflow typically between the hemispheres. Return currents are distributed over larger scales
and thus have smaller amplitudes. Peak current densities get larger toward lower latitudes. There are two
groups of events, around morning‐noontime and evening‐night, which are separated by demarcation lines
near 04 and 15 magnetic local time. The magnetic amplitudes of the small‐scale flfluctuations are larger in
sunlight than in darkness, indicating larger total currents in the loops. But the FAC peak current densities
are larger in darkness, inferring a stronger squeezing of the current sheet under low‐conductivity conditions.
We suggest that our SSTIDs are an evolutional state of medium‐scale traveling ionospheric disturbances.

How to cite: Yin, F., Lühr, H., Park, J., and Wang, L.: Comprehensive Analysis of the Magnetic Signatures of Small‐Scale Traveling Ionospheric Disturbances, as Observed by Swarm, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7175, https://doi.org/10.5194/egusphere-egu2020-7175, 2020.

EGU2020-6863 | Displays | ST3.2

Correlation between wave activities in different layers of the atmosphere

Konstantin Ratovsky, Irina Medvedeva, Anna Yasyukevich, Boris Shpynev, and Denis Khabituev

We study the correlation between wave activities in different layers of the atmosphere. The variability of the measured characteristic in the range of internal gravity wave periods is used as a proxy of wave activity. In the case of ground-based measurements, we consider temporal variations with periods less than ~ 6 hours; while in the case of satellite measurements we take into account spatial variations with periods less than ~ 1000 km. The wave activity is calculated as the standard deviation of variations in the indicated period range with averaging over one day. The aim of the study is to detect a correlation between day-to-day variations of wave activity in different layers of the atmosphere. Correlation coefficients are calculated for various intervals from one month to one year. Correlation analysis reveals the potential relationship between wave phenomena in the stratosphere, mesosphere and ionosphere. The study uses the following characteristics. The ionospheric characteristics are the peak electron density from the Irkutsk ionosonde (52.3 N, 104.3 E) and the total electron content from the Irkutsk GPS receiver. The characteristic of the mesosphere is the mesopause temperature from spectrometric measurements of the OH emission (834.0 nm, band (6-2)) near Irkutsk (51.8 N, 103.1 E, Tory). The stratospheric characteristic is the vertical gas velocity at 1 hPa from the ERA-Interim reanalysis (apps.ecmwf.int/datasets/data/).

This study was supported by the Grant of the Russian Science Foundation (Project N 18-17-00042). The observational results were obtained using the equipment of Center for Common Use «Angara» http: //ckp-rf.ru/ckp/3056/ within budgetary funding of Basic Research program II.12.

How to cite: Ratovsky, K., Medvedeva, I., Yasyukevich, A., Shpynev, B., and Khabituev, D.: Correlation between wave activities in different layers of the atmosphere, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6863, https://doi.org/10.5194/egusphere-egu2020-6863, 2020.

EGU2020-12283 | Displays | ST3.2

Observations of ionospheric TEC peaked structures from Global Ionosphere Maps

Tsung-Che Tsai, Hau-Kun Jhuang, Lou-Chuang Lee, and Yi-Ying Ho

The total electron content (TEC) data from Global Ionosphere Maps provide a global TEC map in the region between latitude 87.5°S to 87.5°N, and longitude 180°W to 180°E. The TEC data in geographic coordinates are first transformed into geomagnetic coordinates through Altitude-Adjusted Corrected Geomagnetic Model (AACGM). We then use 2-dimensional (longitudinal, 180°W-180°E and time, 10 days) Fourier transform (FT) of TEC variations along different geomagnetic latitude to obtain all wave modes in both UT (universal time) and LT (local time) frames for the period from November 18, 2002 to October 15, 2014. The summation of contributing wave modes at a given local time provides the longitudinal variation of the associated zonal waves. The phases of wave modes lead to a constructive or destructive interference of contributing zonal wave, which gives different structures at different local time. These local time structures include Weddell Sea Anomaly (WSA), Southern Atlantic Anomaly (SAA), and Four-peaked structure. The dependence of the peaked structures on latitudinal, seasonal, and solar activity is studied.

How to cite: Tsai, T.-C., Jhuang, H.-K., Lee, L.-C., and Ho, Y.-Y.: Observations of ionospheric TEC peaked structures from Global Ionosphere Maps, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-12283, https://doi.org/10.5194/egusphere-egu2020-12283, 2020.

EGU2020-5541 | Displays | ST3.2

Tropical cyclone induced gravity wave perturbations in the upper atmosphere: GITM-R simulations

Yuxin Zhao, Cissi-Y. Lin, Yue Deng, Jing-Song Wang, Shun-Rong Zhang, and Tian Mao

The tropical cyclone induced concentric gravity waves (CGWs) are capable of propagating upward from convective sources in the troposphere to the upper atmosphere and creating concentric traveling ionosphere disturbances (CTIDs). To examine the CGWs propagation, we implement tropical cyclone induced CGWs into the lower boundary of Global Ionosphere–Thermosphere Model with local-grid refinement (GITM-R). GITM-R is a three-dimensional non-hydrostatic general circulation model for the upper atmosphere with the local-grid refinement module to enhance the resolution at the location of interest. In this study, we simulate CGWs induced by typhoon Meranti in 2016. Information of the TC shape and moving trails is obtained from the TC best-track dataset and the gravity wave patterns are specified at the lower boundary of GITM-R (100 km altitude). The horizontal wavelength and phase speed of wave perturbation at the lower boundary are specified to be consistent with the TEC observations. The simulation results reveal a clear evolution of CTIDs, which shows reasonable agreement with the GPS-TEC observations. To further examine the dependence of the CTIDs on the wavelength and frequency of the gravity wave perturbation at the lower boundary, different waveforms have been tested as well. The magnitude of CTIDs has a negative correlation with the period, but a positive correlation with the wavelength when the horizontal phase velocities are sufficiently fast against the critical- level absorption.

How to cite: Zhao, Y., Lin, C.-Y., Deng, Y., Wang, J.-S., Zhang, S.-R., and Mao, T.: Tropical cyclone induced gravity wave perturbations in the upper atmosphere: GITM-R simulations, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5541, https://doi.org/10.5194/egusphere-egu2020-5541, 2020.

EGU2020-4805 | Displays | ST3.2

Graphical models method - implementation to coupling processes in the atmosphere

Kateřina Podolská, Petra Koucká Knížová, Jaroslav Chum, Michal Kozubek, and Dalia Burešová

Internal atmospheric waves interact with themselves and/or with the undisturbed atmospheric flow, creating very complicated dynamical system with long-range dependencies. We suspect that regional character of the atmosphere at tropospheric heights may be crucial for explanation of the three different dependencies of foF2 on F10.7cm. We employ multivariate statistic methods applied to daily observational data which were obtained using mid-latitude ionosondes for the investigation of these relationships.

We consider specific and characteristic atmospheric wave generation that correspond to particular climatology of each location “European”, “American” and “Far East”. Specific conditions of each region, involving meteorological phenomena of the location as spectrum of atmospheric wave generation and their propagation. We consider significant difference in low atmosphere climatology as a key explanation of the three classes of ionospheric response to the F10.7cm on long time-scales and suggest that climatology of the troposphere must be taken into account for modelling of the ionospheric response.

Our aim is also to demonstrate that conditional independence graph (CIG) models, representing a robust method of multivariet statistical analysis, are useful for finding a relation between the ionosphere and space weather. This method appears to be more appropriate than correlation analysis between foF2 and geomagnetic and solar indices, especially for longitudinal data for which the characteristics may change over time or time series is interrupted. This method seems more effective to us than correlation analysis or scale analysis.

The final results of our analysis by CIG show that the dependence time shifts were clearly identified, namely +0 day shift in all cases, and +3 / +4 / +5 day shift in the dependence on the solar cycle phase and geographical longitude. Here, we would like to point out that we have analyzed data from ionospheric stations in a rather short span of latitudes, all stations belong to midlatitudes (41.4° N – 54° N) and one would expect either practically same response/dependence of foF2 to F10.7 cm for longitudes and/or geomagnetic dependence as solar and geomagnetic forcing is considered as the most important. However, we have not identified any significant geomagnetically dependence with respect to selected stations and their geomagnetic location. Knowing that ionosphere is strongly coupled with lower-laying atmosphere, we come to the conclusion that climatology of the troposphere may come into play and be responsible for the difference in time-dependencies and time-lags in ionospheric response  to the external solar forcing.

How to cite: Podolská, K., Koucká Knížová, P., Chum, J., Kozubek, M., and Burešová, D.: Graphical models method - implementation to coupling processes in the atmosphere, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4805, https://doi.org/10.5194/egusphere-egu2020-4805, 2020.

EGU2020-16618 | Displays | ST3.2

Efficient global ionospheric modeling based on multi-source and massive observation data

Xulei Jin, Shuli Song, Wei Li, and Na Cheng

Abstract Ionosphere is an important error source of satellite navigation and a key component of space weather. With the rapid development of multiple Global Navigation Satellite System (GNSS) and other ionospheric research technologies, and the high precision and near real-time requirements for ionospheric products, it is necessary to carry out a research on multi-source data fusion, massive data processing and near-real-time solution of global ionosphere model (GIM); therefore, we modified the traditional ionospheric modeling technology and generate the GIM products (GIM/SHA). In view of the defect of ground-based GNSS data missing in the ocean regions, the method of adding virtual observation stations to the data missing regions in a large range was adopted, which not only enhanced the accuracy of the GIM in the ocean regions, but also avoided the weight determination among different data sources. In terms of near-real-time modeling, the multi-threaded parallel modeling strategy was adopted. Four GNSS (GPS, GLONASS, BEIDOU, Galileo) observation data, eight virtual observation stations and a server with a CPU frequency of 2.1 GHz and 16 threads were utilized. It took less than 30 minutes to construct the GIM by using parallel modeling strategy, which was 10.3 times faster than serial modeling strategy. The accuracy of the GIM/SHA was verified by using the ionospheric products of International GNSS Service (IGS) Ionosphere Associate Analysis Centers (IAACs) in the period of day of year (DOY) 200-365, 2019. Compared with the ionospheric products of CODE, ESA/ESOC, JPL, UPC, EMR, CAS and WHU, the vertical total electron content (VTEC) root mean squares (RMSs) were 1.09 TEC units (TECu), 1.51TECu, 2.32TECu, 1.88TECu, 2.24TECu, 1.25TECu and 1.38TECu, respectively. The result shows that the GIM/SHA have comparable accuracy with IGS ionospheric products. Satellite altimetry data was exploited to verify the accuracy of GIM/SHA in ocean regions, and it can be concluded that the accuracy of the GIM in ocean regions can be significantly reinforced by adding virtual observation stations in ocean regions. Multi-system and multi-frequency differential code bias (DCB) products (DCB/SHA) were simultaneously generated. Compared with IGS DCB products, the satellite DCB RMSs of DCB/SHA were 0.16ns for GPS, 0.08ns for GLONASS, 0.17ns for BEIDOU and 0.14ns for Galileo; the GNSS receiver DCB RMSs of DCB/SHA were 0.69ns for GPS, 1.06ns for GLONASS, 0.75 for BEIDOU and 1.03ns for Galileo. It can be proved that the accuracy of DCB/SHA are comparable to IGS DCB products.

Keywords Multi-GNSS; GIM; Virtual observation station; Near real-time; VTEC; DCB

How to cite: Jin, X., Song, S., Li, W., and Cheng, N.: Efficient global ionospheric modeling based on multi-source and massive observation data, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-16618, https://doi.org/10.5194/egusphere-egu2020-16618, 2020.

EGU2020-3044 | Displays | ST3.2

Influence of tides on the ionospheric annual anomalies

Zhipeng Ren, Weixing Wan, Jiangang Xiong, Libo Liu, and Xing Li

Through respectively adding June tides and December tides at the low boundary of GCITEM-IGGCAS model (Global Coupled Ionosphere-Thermosphere-Electrodynamics Model, Institute of Geology and Geophysics, Chinese Academy of Sciences), we simulate the influence of tides on the annual anomalies of the ionospheric electron density. The tides’ influence on the annual anomalies of the ionospheric electron density varies with latitude, altitude and solar activity level. Compared with the density driven by December tides, the June tides mainly increases the lower ionospheric electron density, and mainly decreases the electron density at higher ionosphere. In the low-latitude ionosphere, tide drives an additional equatorial ionization anomaly structure (EIA) at higher ionosphere in the relative difference of electron density, which suggests that tide affect the equatorial vertical E×B plasma drifts. Although the lower ionospheric annual anomalies driven by tides mainly increases with the increase of solar activity, the annual anomalies at higher ionosphere mainly decreases with solar activity.

How to cite: Ren, Z., Wan, W., Xiong, J., Liu, L., and Li, X.: Influence of tides on the ionospheric annual anomalies, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3044, https://doi.org/10.5194/egusphere-egu2020-3044, 2020.

ST4.1 – Space weather prediction of solar wind transients in the heliosphere

Coronal mass ejections (CMEs) typically cause the strongest geomagnetic storms so a major focus of space weather research has been predicting the arrival time of CMEs. Most arrival time models fall into two categories: (1) drag-based models that integrate the drag force between a simplified CME structure and the background solar wind and (2) full magnetohydrodynamic (MHD) models. Drag-based models typically are much more computationally efficient than MHD models, allowing for ensemble modeling. While arrival time predictions have improved since the earliest attempts,both types of models currently have difficulty achieving mean absolute errors below 10 hours. Here we use a drag-based model ANTEATR to explore the sensitivity of arrival times to various input parameters. We consider CMEs of different strengths from average to extreme size, speed, and mass (kinetic energies between 9x10^29 and 6x10^32 erg). For each scale CME we vary the input parameters to reflect the current observational uncertainty in each and determine how accurately each must be known to achieve predictions that are accurate within 5 hours. We find that different scale CMEs are the most sensitive to different parameters. The transit time of average strength CMEs depends most strongly on the CME speed whereas an extreme strength CME is the most sensitive to the angular width. A precise CME direction is critical for impacts near the flanks, but not near the CME nose. We also show that the Drag Based Model has similar sensitivities, suggesting that these results are representative for all drag-based models.

 

How to cite: Kay, C.: Identifying Critical Input Parameters for Improving Drag-Based CME Arrival Time Predictions, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-568, https://doi.org/10.5194/egusphere-egu2020-568, 2020.

Previous research has shown that the deflection of coronal mass ejections (CMEs) in interplanetary space, especially fast CMEs, is a common phenomenon. The deflection caused by the interaction with background solar wind is an important factor to determine whether CMEs could hit Earth or not. As the Sun rotates, there will be interactions between solar wind flows with different speeds. When faster solar wind runs into slower solar wind
ahead, it will form a compressive area corotating with the Sun, which is called a corotating interaction region (CIR). These compression regions always have a higher density than the common background solar wind. When interacting with CME, will this make a difference in the deflection process of CME? In this research, first, a three-dimensional (3D) flux-rope CME initialization model is established based on the graduated cylindrical shell (GCS)
model. Then this CME model is introduced into the background solar wind, which is obtained using a 3D IN (INterplanetary) -TVD-MHD model. The Carrington Rotation (CR) 2154 is selected as an example to simulate the propagation and deflection of fast CME when it interacts with background solar wind, especially with the CIR structure.

The simulation results show that: (1) the fast CME will deflect eastward when it propagates into the background solar wind without the CIR; (2) when the fast CME hits the CIR on its west side, it will also deflect eastward, and the deflection angle will increase compared with the situation without CIR.

How to cite: Shen, F., Liu, Y., and Yang, Y.: Numerical Simulation on the Propagation and Deflection of Fast Coronal Mass Ejections (CMEs) Interacting with a Corotating Interaction Region in Interplanetary Space, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1815, https://doi.org/10.5194/egusphere-egu2020-1815, 2020.

Near-Earth solar wind conditions, including disturbances generated by coronal mass ejections (CMEs), are routinely forecast using 3-dimensional, numerical magnetohydrodynamic (MHD) models of the heliosphere. The resulting forecast errors are largely the result of uncertainty in the near-Sun boundary conditions, rather than heliospheric model physics or numerics. Thus ensembles of heliospheric model runs with perturbed initial conditions are used to estimate forecast uncertainty. MHD heliospheric models are relatively cheap in computational terms, requiring tens of minutes to an hour to simulate CME propagation from the Sun to Earth. Thus such ensembles can be run operationally. However, ensemble size is typically limited to ~101-102, which may be inadequate to sample the relevant high-dimensional parameter space. Here, we describe a simplified solar wind model that can estimate CME arrival time in approximately 0.01 seconds on a modest desktop computer and thus enables significantly larger ensembles. It is a 1-dimensional, incompressible, hydrodynamic model, which has previously been used for the steady-state solar wind, but is here used in time-dependent form. This approach is shown to adequately emulate the MHD solutions to the same boundary conditions for both steady-state solar wind and CME-like disturbances. We suggest it could serve as a “surrogate” model for the full 3-dimensional MHD models. For example, ensembles of ~105-106 members can be used to identify regions of parameter space for more detailed investigation by the MHD models. Similarly, the simplicity of the model means it can be rewritten as an adjoint model, enabling variational data assimilation with MHD models without the need to alter their code. Model code is available as an Open Source download in the Python language.

How to cite: Owens, M.: Quantifying CME arrival time uncertainty with mega ensembles, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2648, https://doi.org/10.5194/egusphere-egu2020-2648, 2020.

EGU2020-20900 | Displays | ST4.1 | Highlight

A Comprehensive Study of Superstorms from 1957 to present

Xing Meng, Bruce Tsurutani, and Anthony Mannucci

We present a comprehensive study of all 39 superstorms (minimum Dst ≤ −250 nT) occurring from 1957 to present including analyzing their main phase developments, seasonal and solar cycle dependences, as well as their solar and interplanetary causes. We find that 87% of the superstorms have a multistep main phase development or are built upon preceding geomagnetic activities, and 90% of the superstorms occurred either near solar maximum or during the declining phase.  For the superstorm association with solar activities, 54% of the superstorms were associated with X‐class solar flares, 36% were associated with M‐class flares, and 5% with C‐class flares. All solar flares related to superstorms occurred in active regions, indicating the importance of active regions to superstorms. Most flares were located in the central meridian or slightly west of it as expected. For the interplanetary conditions leading to the development of the superstorm main phase, 95% of the 19 superstorms with available solar wind data are solely caused or partially caused by the sheath anti-sunward of an interplanetary coronal mass ejection (ICME), indicating the importance of the sheath structure in driving superstorms. For eight superstorms that have identifiable interplanetary shocks preceding the ICMEs, the shock normal angles were almost all quasi‐perpendicular. Larger shock normal angles statistically corresponded to greater superstorm intensities.

How to cite: Meng, X., Tsurutani, B., and Mannucci, A.: A Comprehensive Study of Superstorms from 1957 to present, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-20900, https://doi.org/10.5194/egusphere-egu2020-20900, 2020.

EGU2020-5224 | Displays | ST4.1

SOLSTICE: Space Weather Modeling Meets Machine Learning

Tamas Gombosi and the SOLSTICE Team

The last decade has truly witnessed the rise of the machine age. The enormous expansion of technology that can generate and manipulate massive amounts of information has transformed all aspects of society. Missions such as SDO and MMS, and numerical models such as the Space Weather Modeling Framework (SWMF) are now routinely generating terabytes of science data, far beyond what can be analyzed directly by humans. Fortunately, concurrent with this explosion in information has come the development of powerful capabilities, such as machine learning (ML) and artificial intelligence (AI), that can retrieve revolutionary new understanding and utility from the massive data sets. 

SOLSTICE (Solar Storms and Terrestrial Impacts Center) is a recently selected NASA/NSF DRIVE Center. It will serve as the vanguard for developing and applying ML methods, which will then raise the capabilities of the entire community. We will combine next generation ML technology with our world-leading numerical models and the exquisite data from the space missions to make breakthrough advances in Heliophysics understanding and space weather capabilities, and then transition our technology to the CCMC for the benefit of all.

We use ML to attack Grand Challenge Problems that cover the major aspects of space weather science: (i) use interpretable deep learning models, archived solar observations and high-performance physics-based simulations to identify the onset mechanism of solar flares and coronal mass ejections; and (ii) use high-cadence observations and physics-based feature learning to predict solar storms many hours before eruption, training time-to-event models to predict event times and flare magnitudes using innovative machine learning techniques.

How to cite: Gombosi, T. and the SOLSTICE Team: SOLSTICE: Space Weather Modeling Meets Machine Learning, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5224, https://doi.org/10.5194/egusphere-egu2020-5224, 2020.

EGU2020-15245 | Displays | ST4.1

Real time physics-based solar wind forecasts for SafeSpace

Rui Pinto, Rungployphan Kieokaew, Benoît Lavraud, Vincent Génot, Myriam Bouchemit, Alexis Rouillard, Stefaan Poedts, Sébastien Bourdarie, and Yannis Daglis

We present the solar wind forecast module to be implemented on the Sun – interplanetary space – Earth’s magnetosphere chain of the H2020 SafeSpace project. The wind modelling pipeline, developed at the IRAP, performs real-time robust simulations (forward modelling) of the physical processes that determine the state of the solar wind from the surface of the Sun up to the L1 point. The pipeline puts together different mature research models: determination of the background coronal magnetic field, computation of many individual solar wind acceleration profiles (1 to 90 solar radii), propagation across the heliosphere and formation of CIRs (up to 1 AU or more), estimation of synthetic diagnostics (white-light and EUV imaging, in-situ time-series) and comparison to observations and spacecraft measurements. Different magnotograms sources (WSO, SOLIS, GONG, ADAPT) can be combined, as well as coronal field reconstruction methods (PFSS, NLFFF), wind models (MULTI-VP), and heliospheric propagation models (CDPP/AMDA 1D MHD, ENLIL, EUHFORIA). We provide a web-based service that continuously supplies a full set of bulk physical parameters (wind speed, density, temperature, magnetic field, phase speeds) of the solar wind up to 6-7 days in advance, at a time cadence compatible with space weather applications.

How to cite: Pinto, R., Kieokaew, R., Lavraud, B., Génot, V., Bouchemit, M., Rouillard, A., Poedts, S., Bourdarie, S., and Daglis, Y.: Real time physics-based solar wind forecasts for SafeSpace, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-15245, https://doi.org/10.5194/egusphere-egu2020-15245, 2020.

EGU2020-1642 | Displays | ST4.1

Energetic Solar Particle Access to the Near-Equatorial Inner Magnetosphere

Rachael Filwett, Allison Jaynes, Daniel Baker, Shrikanth Kanekal, Bern Blake, and Brian Kress

Solar proton events are comprised of energetic protons of solar and interplanetary origin. Such energetic particles are able to access the magnetosphere at various locations according to their cutoff rigidity. The specific properties of solar proton access are of great interest for space weather prediction purposes. Using Van Allen Probes/Relativistic Electron-Proton Telescope (REPT) 20-200 MeV proton data we examine four of the strongest solar proton events over the lifetime of the mission. We present evidence of the direct magnetospheric access of these energetic solar protons and find strong flux increases at L<4. Results indicate that small and sudden flux changes measured by ACE spacecraft sensors upstream of Earth are also seen in the near-equatorial inner magnetosphere. Using the East-West asymmetry of solar protons as a proxy for cutoffs we examine the highly dynamic cutoff rigidity. We find there is evidence for: (1) cutoff rigidity dependence on MLT; (2) suppressed cutoffs with rapid Dst changes; and (3) rapid evolution of cutoffs even during quiet magnetospheric conditions.

How to cite: Filwett, R., Jaynes, A., Baker, D., Kanekal, S., Blake, B., and Kress, B.: Energetic Solar Particle Access to the Near-Equatorial Inner Magnetosphere, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1642, https://doi.org/10.5194/egusphere-egu2020-1642, 2020.

A hyperbolic cell-centered finite volume solver (HCCFVS) is first proposed to obtain the potential magnetic field solutions prescribed by the solar observed magnetograms. By introducing solution gradients as additional unknowns and adding a pseudo-time derivative, HCCFVS transforms second-order Poisson equation into an equivalent first-order as well as pseudo-time-dependent hyperbolic system. Thus, instead of directly solving the second-order Poisson equation, HCCFVS obtains the solution to the Poisson equation by achieving the steady-state solution to this first-order hyperbolic system. The code is established in Fortran 90 with Message Passing Interface parallelization. To preliminarily demonstrate the effectiveness and accuracy of the code, two test cases with exact solutions are first performed. The numerical results show its second-order convergence. Then, we apply the code to the solar potential magnetic field problem that is often approximated analytically as an expansion of spherical harmonics. A comparison between the potential magnetic field solutions demonstrates the capability of our new HCCFVS to adequately handle the solar potential magnetic field problem, and thus it can be used as an alternative to the spherical harmonics approach. Furthermore, HCCFVS, like the spherical harmonics approach, can be used to provide the initial magnetic field for solar corona or solar wind magnetohydrodynamic (MHD) models. Using the potential magnetic field obtained by HCCFVS as input, the large-scale solar coronal structures during Carrington rotation (CR) 2098 have been studied. Meanwhile, HCCFVS automatically deals with the Poisson projection method to keep the magnetic field divergence-free constraint during the time-relaxation process of achieving the steady state. The numerical results show that the simulated corona captures main solar coronal features and the average relative magnetic field divergence error is maintained to be an acceptable level, which again displays the performance of HCCFVS.

How to cite: Feng, X.: Finite volume method for obtaining potential magnetic field solutions, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4301, https://doi.org/10.5194/egusphere-egu2020-4301, 2020.

EGU2020-5202 | Displays | ST4.1

Helio4Cast - a real time test environment to enhance space weather prediction at Earth

Christian Möstl, Rachel L. Bailey, Ute V. Amerstorfer, Tanja Amerstorfer, Andreas J. Weiss, Martin A. Reiss, Jürgen Hinterreiter, and Maike Bauer

We introduce Helio4cast, an open source python package to provide real time solar wind predictions at the Sun-Earth L1 point, and to directly couple them to forecasts of the aurora oval, geomagnetically induced currents and further geomagnetic indices. We present its current status, using a combination of our PREDSTORM solar wind forecast and the real time modeling of the aurora with the OVATION model. The solar wind prediction is driven by data from either STEREO-A, a recurrence model, an empirical background solar wind model or a future L5 mission. For coronal mass ejections (CMEs), we plan to use our semi-empirical 3DCORE model to produce in situ magnetic flux rope signatures constrained by real-time solar observations, or a machine learning approach based on many previous observations of in situ CMEs. We are particularly interested in how the errors in the solar wind prediction propagate to ground-based observations. Challenges and future plans of the real-time implementation are discussed.

How to cite: Möstl, C., Bailey, R. L., Amerstorfer, U. V., Amerstorfer, T., Weiss, A. J., Reiss, M. A., Hinterreiter, J., and Bauer, M.: Helio4Cast - a real time test environment to enhance space weather prediction at Earth, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5202, https://doi.org/10.5194/egusphere-egu2020-5202, 2020.

EGU2020-5247 | Displays | ST4.1

Using STEREO-HI beacon data to predict CME arrival time and speed with the ELEvoHI model

Maike Bauer, Tanja Amerstorfer, Jürgen Hinterreiter, Christian Möstl, Jackie A. Davies, Ute V. Amerstorfer, Rachel L. Bailey, Martin A. Reiss, and Andreas J. Weiss

Coronal mass ejections (CMEs) may induce strong geomagnetic storms which have a significant impact on satellites in orbit as well as electrical devices on Earth’s surface. If we want to be able to mitigate the potentially devastating consequences which strong CMEs might have on Earth, developing models which accurately predict their arrival time is an integral step. The Ellipse Evolution model based on Heliospheric Imager observations (ELEvoHl) predicts the arrival of coronal mass ejections using data from STEREO’s HI instruments. HI data is available as high-resolution science data, which is downlinked every few days and low-resolution beacon data, which is downlinked in near real-time. Therefore, to allow for real time predictions of CME arrivals, beacon data must be used. We study different data reduction procedures to improve the quality of the measurements and compile the resulting images into time-elongation plots (J-plots). We track the leading edge of each selected CME event by hand, resulting in a series of time-elongation points which function as input for the ELEvoHI model. We compare the resulting predictions to those obtained using science data in terms of accuracy and errors of the predicted arrival time and speed.

How to cite: Bauer, M., Amerstorfer, T., Hinterreiter, J., Möstl, C., Davies, J. A., Amerstorfer, U. V., Bailey, R. L., Reiss, M. A., and Weiss, A. J.: Using STEREO-HI beacon data to predict CME arrival time and speed with the ELEvoHI model, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5247, https://doi.org/10.5194/egusphere-egu2020-5247, 2020.

EGU2020-6921 | Displays | ST4.1

Predicting the magnetic flux rope fields at the Sun-Earth L1 point

Ute Amerstorfer, Christian Möstl, Rachel Bailey, Andreas Weiss, Martin Reiss, Tanja Amerstorfer, Jürgen Hinterreiter, and Maike Bauer

Forecasting of coronal mass ejection magnetic flux rope fields at L1 is a long-standing challenge and one of the major problems in space weather forecasting. We attempt to make progress by using two approaches: 1) machine learning approaches (e.g., linear regression, lars lasso, RANSAC, or random forest), and 2) analogue ensemble methods. For our study, we take events observed at the Wind, Stereo-A and Stereo-B satellites from the ICME list created within the EU-project HELCATS. We analyse different scores (e.g., RMSE, or the skill of the model) of the presented methods. Further, we investigate how well the flux rope field can be anticipated when the first few hours of the flux rope have already been observed at L1.

How to cite: Amerstorfer, U., Möstl, C., Bailey, R., Weiss, A., Reiss, M., Amerstorfer, T., Hinterreiter, J., and Bauer, M.: Predicting the magnetic flux rope fields at the Sun-Earth L1 point, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6921, https://doi.org/10.5194/egusphere-egu2020-6921, 2020.

EGU2020-10446 | Displays | ST4.1

CME evolution and the corresponding Forbush decrease: modelling vs multi-spacecraft observation

Mateja Dumbovic, Bojan Vrsnak, Jingnan Guo, Bernd Heber, Karin Dissauer, Fernando Carcaboso-Morales, Manuela Temmer, Astrid Veronig, Tatiana Podladchikova, Christian Möstl, Tanja Amerstorfer, and Anamarija Kirin

One of the very common in-situ signatures of ICMEs, as well as other interplanetary transients are Forbush decreases (FDs), i.e. short-term reductions in the galactic cosmic ray (GCR) flux. A two-step FD is often regarded as a textbook example, which presumably owns its specific morphology to the fact that the measuring instrument passed through the ICME head-on, encountering first the shock front (if developed), then the sheath and finally the magnetic structure. The interaction of GCRs and the shock/sheath region as well as CME magnetic structure occurs all the way from Sun to Earth, therefore, FDs are expected to reflect the evolutionary properties of CMEs and their sheaths. We apply modelling to different ICME regions in order to obtain a generic two-step FD profile, which qualitatively agrees with our current observation-based understanding of FDs. We next adapt the models for energy dependence to enable comparison with different GCR measurement instruments (as they measure in different particle energy ranges). We test these modelling efforts against a set of multi-spacecraft observations of the same event.

How to cite: Dumbovic, M., Vrsnak, B., Guo, J., Heber, B., Dissauer, K., Carcaboso-Morales, F., Temmer, M., Veronig, A., Podladchikova, T., Möstl, C., Amerstorfer, T., and Kirin, A.: CME evolution and the corresponding Forbush decrease: modelling vs multi-spacecraft observation, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-10446, https://doi.org/10.5194/egusphere-egu2020-10446, 2020.

EGU2020-12647 | Displays | ST4.1

A new model describing Forbush Decreases at Mars: combining the heliospheric modulation and the atmospheric influence

Jingnan Guo, Robert Wimmer-Schweingruber, Mateja Dumbovic, Bernd Heber, and Yuming Wang

Forbush decreases are depressions in the galactic cosmic rays (GCRs) which are mostly caused by the modulations of interplanetary coronal mass ejections (ICMEs) and also sometimes by stream/corotating interaction regions (SIRs/CIRs). Forbush decreases have been studied extensively using neutron monitors at Earth and have been recently, for the first time, measured on the surface of another planet - Mars by the Radiation Assessment Detector (RAD), on board Mars Science Laboratory’s (MSL) rover Curiosity. The modulation of the GCR particles by heliospheric transients in space is energy-dependent and afterwards these particles are also interacting with the Martian atmosphere with the interaction process depending on the particle type and energy. In order to study the space weather environment near Mars using the ground-measured Forbush decreases, it is important to understand and quantify the energy-dependent modulation of the GCR particles by not only the pass-by heliospheric disturbances but also the Martian atmosphere. In this study, we develop a model which combines the heliospheric modulation of GCRs and the atmospheric modification of such modulated GCR spectra to quantify the amplitudes of the Forbush decreases at Mars: both on ground and in the interplanetary space near Mars during the pass-by of an ICME/SIR. The modeled results are in good agreement when compared to studies of Forbush decreases caused by ICMEs/SIRs measured by MSL on the surface of Mars and by the Mars Atmosphere and Volatile EvolutioN (MAVEN) spacecraft in orbit.  This supports the validity of both the Forbush decrease description and the Martian atmospheric transport models.  Our model can be potentially used to understand the property of ICMEs and SIRs passing Mars.

How to cite: Guo, J., Wimmer-Schweingruber, R., Dumbovic, M., Heber, B., and Wang, Y.: A new model describing Forbush Decreases at Mars: combining the heliospheric modulation and the atmospheric influence, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-12647, https://doi.org/10.5194/egusphere-egu2020-12647, 2020.

EGU2020-4703 | Displays | ST4.1

CME arrival prediction and its dependency on input data and model parameters

Tanja Amerstorfer, Jürgen Hinterreiter, Martin A. Reiss, Maike Bauer, Christian Möstl, Rachel L. Bailey, Andreas J. Weiss, Ute V. Amerstorfer, Jackie A. Davies, and Richard Harrison

During the last years, we focused on developing a prediction tool that utilizes the wide-angle observations of STEREO's heliospheric imagers. The unsurpassable advantage of these imagers is the possibility to observe the evolution and propagation of a coronal mass ejection (CME) from close to the Sun up to 1 AU and beyond. We believe that using this advantage instead of relying on coronagraph observations that are limited to observe only 14% of the Sun-Earth line, it is possible to improve today's CME arrival time predictions.
The ELlipse Evolution model based on HI observations (ELEvoHI) assumes an elliptic frontal shape within the ecliptic plane and allows the CME to adjust to the ambient solar wind speed, i.e. it is drag-based. ELEvoHI is used as an ensemble simulation by varying the CME frontal shape within given boundary values. The results include a frequency distrubution of predicted arrival time and arrival speed and an estimation of the arrival probability. ELEvoHI can be operated using several kinds of inputs. In this study we investigate 15 well-defined single CMEs when STEREO was around L4/5 between the end of 2009 and the beginning of 2011. Three different sources of input propagation directions (and shapes) are used together with three different sources of ambient solar wind speed and two different ways of defining the most appropriate fit to the HI data. The combination of these different approaches and inputs leads to 18 different model set-ups used to predict each of the 15 events in our list leading to 270 ELEvoHI ensemble predictions and all in all to almost 60000 runs. To identify the most suitable and most accurate model set-up to run ELEvoHI, we compare the predictions to the actual in situ arrival of the CMEs.
This model is specified for using data from future space weather missions carrying HIs located at L5 or L1 and can also directly be used together with STEREO-A near real-time HI beacon data to provide real-time CME arrival predictions during the next 7 years when STEREO-A is observing the Sun-Earth space.

How to cite: Amerstorfer, T., Hinterreiter, J., Reiss, M. A., Bauer, M., Möstl, C., Bailey, R. L., Weiss, A. J., Amerstorfer, U. V., Davies, J. A., and Harrison, R.: CME arrival prediction and its dependency on input data and model parameters, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-4703, https://doi.org/10.5194/egusphere-egu2020-4703, 2020.

EGU2020-9847 | Displays | ST4.1

Predicting heliospheric propagation of CMEs with probabilistic Drag-Based Ensemble Model (DBEM)

Jaša Čalogović, Mateja Dumbović, Bojan Vršnak, Davor Sudar, Manuela Temmer, and Astrid Veronig

Understanding space weather driven by the solar activity is crucial as it can affect various human technologies, health as well as it can have important implications for the space environment near the Earth and the Earth’s atmosphere. In order to better asses space weather forecasts various empirical, drag-based and MHD models have been developed to predict the arrival time of CMEs. One of them is the analytical Drag-based Model (DBM) applying the equation of CME motion which is determined by the drag force from the background solar wind acting on the CME. DBM predictions depend on various initial parameters such as CME launch speed, background solar wind speed and empirically derived drag parameter as well CME’s angular half-width and longitude of CME source region for a DBM CME cone geometry. Since many of input parameters may be inaccurate or unreliable due to limited observations, the Drag-Based Ensemble Model (DBEM) was developed that considers the variability of model input parameters by making an ensemble of a number of different input parameters to calculate a distribution and significance of DBM results. DBM has the advantage of having very short computational time (< 0.01s) and DBEM ensemble runs with many thousand members can be performed within few seconds on a normal computer. Using such approach, DBEM can determine the most likely CME arrival times and speeds, quantify the prediction uncertainties and calculate the forecast confidence intervals. Recently, DBEM web interface was also integrated as one of the ESA Space Situational Awareness web portal space weather services (http://swe.ssa.esa.int/heliospheric-weather). We’ll present the recent DBEM developments together with the validation of its predictions using observations and other models as well as the input parameter sensitivity tests.

How to cite: Čalogović, J., Dumbović, M., Vršnak, B., Sudar, D., Temmer, M., and Veronig, A.: Predicting heliospheric propagation of CMEs with probabilistic Drag-Based Ensemble Model (DBEM), EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-9847, https://doi.org/10.5194/egusphere-egu2020-9847, 2020.

We present the project SPREAdFAST – Solar Particle Radiation Environment Analysis and Forecasting - Acceleration and Scattering Transport. This investigation fulfills a vital component of the space weather requirements of ESA’s Space Situational Awareness program by contributing to the capability to protect space assets from solar activity space radiation. It will allow for producing predictions of SEP fluxes at multiple locations in the inner heliosphere, by modelling their acceleration at Coronal Mass Ejections (CMEs) near the Sun, and their subsequent interplanetary transport using a physics-based, data-driven approach. The system prototype will incorporate results from our scientific investigations, the modification and linking of existing open source scientific software, and its adaptation to the goals of the proposed work. It will incorporate a chain of data-driven analytic and numerical models, for estimating: coronal magnetic fields; dynamics of large-scale coronal (CME-driven) shock waves; energetic particle acceleration; scatter-based (not simple ballistic), time-dependent SEP propagation in the heliosphere to specific time-dependent locations.

How to cite: Kozarev, K., Miteva, R., Dechev, M., and Zucca, P.: Development of a Physics-Based Prototype Model Chain for Solar Energetic Particle Acceleration and Transport Forecasting for the Inner Heliosphere, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-17156, https://doi.org/10.5194/egusphere-egu2020-17156, 2020.

EGU2020-16131 | Displays | ST4.1

Estimating the SEP Flux for the Upcoming Solar Cycle 25 Using LSTM Network

Mohamed Nedal and Kamen Kozarev

Estimating space weather parameters for the solar cycle 25, which has already started, is essential to anticipate the behavior of the near-Earth space environment. Artificial Neural Networks have in recent years become very widely used in several scientific fields owing to the advancement in computational power and the availability of big data. In this work, we take advantage of utilizing Recurrent Neural Network models in time-series analysis. We have developed and trained a Long-Short Term Memory (LSTM) model, in order to make long-term predictions of the hourly-averaged energetic proton fluxes at 1AU. We have used as input a combination of solar and interplanetary magnetic field indices (from the OMNI database) from the past four solar cycles and generated predictions of the solar energetic proton fluxes at three energies. So far, we found that the root-mean-square errors for the predictions over a three-month period were 0.0240, 0.0173, and 0.0309, respectively. We also found that the model underestimates the prediction at the highest energy band. We will extend the model architecture in order to estimate the future SEP fluxes over the whole solar cycle.

How to cite: Nedal, M. and Kozarev, K.: Estimating the SEP Flux for the Upcoming Solar Cycle 25 Using LSTM Network, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-16131, https://doi.org/10.5194/egusphere-egu2020-16131, 2020.

EGU2020-16522 | Displays | ST4.1

Long-term relationship of coronal holes and solar wind at Earth

Amr Hamada, Timo Asikainen, and Kalevi Mursula

EGU2020-21007 | Displays | ST4.1

On the Drag parameter of ICME propagation models

Gianluca Napoletano, Raffaello Foldes, Dario Del Moro, Francesco Berrilli, Luca Giovannelli, and Ermanno Pietropaolo

ICME (Interplanetary Coronal Mass Ejection) are violent phenomena of solar activity that affect the whole heliosphere and the prediction of their impact on different solar system bodies is one of the primary goals of the planetary space weather forecasting. The travel time of an ICME from the Sun to the Earth can be computed through the Drag-Based Model (DBM), which is based on a simple equation of motion for the ICME defining its acceleration as a=-Γ(v-w)v-w, where a and v are the CME acceleration and speed, w is the ambient solar-wind speed and Γ is the so-called drag parameter (Vršnak et al., 2013).
In this framework, Γ depends on the ICME mass and cross-section, on the solar-wind density and, to a lesser degree, on other parameters. The typical working hypothesis for DBM implies that both Γ and w are constant far from the Sun. To run the codes, forecasters use empirical
input values for Γ and w, derived by pre-existent knowledge of solar-wind condition and by solving the “inverted problem” (where the ICME travel time is known and the unknowns are Γ and/or w). In
the 'Ensemble' approaches (Dumbovich et al., 2018; Napoletano et al. 2018), the uncertainty about the actual values of such inputs are rendered by Probability Distribution Functions (PDFs), accounting for the values variability and our lack of knowledge. Among those PDFs, that of Γ is poorly defined due to the relatively scarce statistics of recorded values. 

Employing a list of past ICME events, for which initial conditions when leaving the Sun and arrival conditions at the Earth are known, we employ a statistical approach to the Drag-Based Model to determine a measure of Γ and w for each case. This allows to obtain distributions for the model parameters on experimental basis and, more importantly, to test whether different conditions of relative velocity to the solar wind influence the value of the drag efficiency, as it must be expected for solid objects moving into an external fluid. In addition, we perform numerical simulations of a solid ICME-shaped structure moving into the solar-wind modelled as an external fluid. Outcomes from these simulations are compared with our experimental results, and thus employed to interpret them on physical basis.

How to cite: Napoletano, G., Foldes, R., Del Moro, D., Berrilli, F., Giovannelli, L., and Pietropaolo, E.: On the Drag parameter of ICME propagation models, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21007, https://doi.org/10.5194/egusphere-egu2020-21007, 2020.

ST4.2 – Nowcasting, forecasting, operational monitoring and post-event analysis of the space weather and space climate in the Sun-Earth system

EGU2020-7386 | Displays | ST4.2 | Highlight

Visualizing models and observations of the thermosphere-ionosphere in support of the ESA EE10 candidate mission Daedalus

Eelco Doornbos, Theodoros Sarris, Stylianos Tourgaidis, Panagiotis Pirnaris, Stephan Buchert, Hanli Liu, Gang Lu, and Federico Gasperini

Daedalus is a new satellite mission concept for studying the lower thermosphere-ionosphere (LTI). The mission is currently undergoing Phase 0 studies, funded by ESA as one of three missions that are candidates for becoming its Earth Explorer 10 mission (EE10).

Using an elliptical orbit with a very low perigee (140 km and lower), the mission will make comprehensive in-situ measurements, including local density, composition, temperature and velocities of both the neutral and charged particles. An option of having two Daedalus satellites is being studied to allow better separation of temporal and spatial variability, and to better measure the strong vertical gradients and wave activity that occur in the LTI. The complete suite of instruments on Daedalus will allow the computation of higher level products such as local collision frequencies, conductivities and heating rates, along the orbit. The unique complementarity of instrumentation and orbit sampling over a large range of altitudes will be extremely valuable in advancing the science of the LTI region, which is a key region for many space weather phenomena.


High quality visualizations of models and data are very important during the definition of the mission. They allow both experts and newcomers to the field to better comprehend the physics of the LTI region, how it couples with other regions and systems, as well as how Daedalus will be able to sample this region from its unconventional orbit. The presentation will showcase 2D and 3D visuals that were developed during the phase 0 studies, and that make use of empirical and physics-based models of the thermosphere-ionosphere, Earth's magnetic field and simulated satellite orbits.

How to cite: Doornbos, E., Sarris, T., Tourgaidis, S., Pirnaris, P., Buchert, S., Liu, H., Lu, G., and Gasperini, F.: Visualizing models and observations of the thermosphere-ionosphere in support of the ESA EE10 candidate mission Daedalus, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7386, https://doi.org/10.5194/egusphere-egu2020-7386, 2020.

EGU2020-6646 | Displays | ST4.2 | Highlight

Open-ended, high cadence, Kp-like geomagnetic index Hp

Jürgen Matzka, Guram Kervalishvili, Jan Rauberg, Claudia Stolle, and Yosuke Yamazaki

An open-ended, high cadence, Kp-like geomagnetic index, called Hp index, is developed within the H2020 project SWAMI (Space Weather Atmosphere Models and Indices). The traditional Kp index is an excellent measure for energy input by the solar wind and is widely used in space weather science and applications. The new planetary index Hp resembles the Kp index by having a similar derivation scheme and a nearly identical frequency distribution of index values. Hp is available from 1995 onward with different time resolutions, e.g., 30 minutes and 60 minutes, and thus provides a higher temporal resolution than the 3-hourly Kp index. Additionally, events with Hp > 9- were further subdivided using an open-ended scale (9o, 9+, 10-, 10o, 10+, 11-, ...) to represent the highest levels of geomagnetic activity with higher resolution.

How to cite: Matzka, J., Kervalishvili, G., Rauberg, J., Stolle, C., and Yamazaki, Y.: Open-ended, high cadence, Kp-like geomagnetic index Hp, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6646, https://doi.org/10.5194/egusphere-egu2020-6646, 2020.

An intriguing aspect of the 2 September 1859 geomagnetic disturbance (or Carrington event) is the horizontal magnetic dataset measured in Colaba, India (magnetic latitude approximately 20 degrees N). This dataset exhibits a sharp decrease of over 1600 nT and a quick recovery of about 1300 nT, all within a few hours during the solar daytime. The mechanism behind this has previously been attributed to magnetospheric processes, ionospheric processes or a combination of both. In this talk, we outline our efforts to recreate this low-latitude magnetic dataset using the Space Weather Modelling Framework (SWMF). By simulating an array of extremely high pressure solar wind scenarios, we can recreate the low-latitude surface magnetic signal at Colaba. We find that the position of the magnetopause is an important factor for such quick deviations and recoveries in dayside surface magnetic measurements. In addition, we find that scenarios which accurately recreated surface magnetic field observations during the Carrington event had minimum Dst values of only -610 nT.

How to cite: Blake, S., Pulkkinen, A., Schuck, P., and Glocer, A.: Recreating the Carrington Event Magnetic Field Measurements using Extremely High Pressure Solar Wind Scenarios and the Space Weather Modelling Framework, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-22086, https://doi.org/10.5194/egusphere-egu2020-22086, 2020.

EGU2020-12209 | Displays | ST4.2

Low-Earth-Orbit observations for space weather and space climate

Irina Zakharenkova, Iurii Cherniak, Sergey Sokolovskiy, William Schreiner, Qian Wu, and John Braun

Many of the modern Low-Earth-Orbiting satellites are now equipped with dual-frequency GPS receivers for Radio Occultation (RO) and Precise Orbit Determination (POD). The space-borne GPS measurements can be successfully utilized for ionospheric climatology and space weather monitoring. The combination of GPS measurements, which include RO observations and POD measurements from the upward-looking GPS antenna, provides information about electron density distribution (profile) below the satellite orbit and an integrated Total Electron Content (TEC) above the satellite representing an important data source for electron density climatology above the F2 layer peak on a global scale. We demonstrate the advantages of using space-borne LEO GPS measurements, both RO and upward-looking, for Space Weather activity monitoring including specification of ionospheric plasma density structures at different altitudinal domains of the ionosphere in quiet and disturbed conditions. After the great success of the COSMIC-1 (Constellation Observing System for Meteorology, Ionosphere, and Climate) mission operating since 2006, the six COSMIC-2 satellites were launched into a 24 deg inclination orbit in June 2019. The COSMIC-2 scientific payloads with the advanced Tri-GNSS Radio-Occultation Receiver System provide multiple observation types including multi-GNSS TEC (limb and overhead), RO electron density profiles, amplitude/phase scintillation indices, in-situ ion densities and velocities. The COSMIC-2 advanced instruments allow detection of ionospheric plasma density structures of various scales, and the monitoring of high-rate amplitude and phase scintillations both above and below a satellite orbit. The COSMIC-2 multi-instrumental observations will contribute to a better understanding of the equatorial ionosphere morphology and future forecasting of ionospheric irregularities and radio wave scintillations that harmfully affect satellite-to-Earth communication and navigation systems. We present results of post-event analyses for severe space weather events demonstrating a great potential and contribution of the COSMIC-1/2 missions in combination with the ground-based GNSS receivers and other LEO missions like C/NOFS, DMSP, MetOp, TerraSAR-X, and Swarm for monitoring the space weather effects in the Earth’s ionosphere.

How to cite: Zakharenkova, I., Cherniak, I., Sokolovskiy, S., Schreiner, W., Wu, Q., and Braun, J.: Low-Earth-Orbit observations for space weather and space climate, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-12209, https://doi.org/10.5194/egusphere-egu2020-12209, 2020.

Nowcast and forecast of ring current electron dynamics are crucial for space weather applications since the elevated fluxes of the ring current electrons may lead to surface charging of satellites that operate in the inner magnetosphere. Physics-based models of ring current electron dynamics contain uncertainties in boundary conditions, electric and magnetic fields, electron scattering rates, and plasmapause and magnetopause locations. The accuracy of the models can be improved by correcting the model predictions given the information obtained from in-situ satellite measurements by means of data assimilation techniques.

 

The scarcity of in-situ measurements may complicate the application of data assimilation methods for ring current electrons. The effect of data assimilation methods can be localized in time in space due to the multidimensionality of the ring current models and spatial and temporal limitations of spacecraft measurements. In this work, we investigate whether the Kalman filter can be used to improve ring current model predictions given only sparse satellite measurements. We blend the convection part of the four-dimensional Versatile Electron Radiation Belt code with the Van Allen Probe data, using the log-normal Kalman filter. By using synthetic data, we show that the Kalman filter is capable of correcting errors in model predictions associated with uncertainties in electron lifetimes, boundary conditions, and convection electric fields. We demonstrate that reanalysis retains features that cannot be fully reproduced by the convection model such as storm-time earthward propagation of the electrons down to 2.5 Earth’s radii. The Kalman filter can adjust model predictions to satellite measurements even in regions where data are not available. Our results demonstrate that data assimilation can improve the performance of ring current models, better quantify model uncertainties, and help us to improve the nowcast and forecast of the dynamics of the particles in the inner magnetosphere.

How to cite: Aseev, N. and Shprits, Y.: Reanalysis of ring current electron phase space densities using Van Allen Probe observations, convection model, and log-normal Kalman filter, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-17747, https://doi.org/10.5194/egusphere-egu2020-17747, 2020.

EGU2020-9196 | Displays | ST4.2

On Space Weather Data Assimilation

Mihail Codrescu, Stefan Codrescu, Mariangel Fedrizzi, and Claudia Borries

Most if not all terrestrial weather prediction services today are based on data assimilation and numerical weather prediction models. Space Weather services are expected to follow a similar path towards data assimilation. However, the application of data assimilation in Space Weather requires a different implementation compared to terrestrial weather because space systems tend to be strongly forced and because the amount of data available for assimilation is critically small. In this paper we review the implementation of an ensemble Kalman filter data assimilation system based on the Space Weather Prediction Center operational Coupled Thermosphere Ionosphere Plasmasphere Electrodynamics (CTIPe) model. We present assimilation results for neutral mass density during geomagnetically quiet and disturbed conditions and discuss the future use of data assimilation for the thermosphere ionosphere system. 

How to cite: Codrescu, M., Codrescu, S., Fedrizzi, M., and Borries, C.: On Space Weather Data Assimilation, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-9196, https://doi.org/10.5194/egusphere-egu2020-9196, 2020.

EGU2020-7702 | Displays | ST4.2

Comparing three approaches to the ground geoelectric field modelling due to space weather events

Elena Marshalko, Mikhail Kruglyakov, Alexey Kuvshinov, Elena Sokolova, Viacheslav Pilipenko, and Olga Kozyreva

In order to estimate the potential hazard to technological systems from space weather, it is necessary to understand the spatiotemporal evolution of the geoelectric field during geomagnetic disturbances. Once the geoelectric field is quantitively estimated, geomagnetically induced currents can be calculated from the geometry of transmission lines and system design parameters. To address the complex problem of the ground electromagnetic (EM) field modelling due to space weather events, it is necessary to consider the spatiotemporal structure of the source of the EM induction in a realistic way and take into account a realistic three‐dimensional (3‐D) distribution of the Earth's electrical conductivity.

In this work we compare three approaches to the geoelectric field modelling. All approaches are based on the numerical solution of Maxwell's equations in Earth's models with 3-D conductivity distribution. The difference between them lies in different setting of the EM induction source. In the first two methods the source is represented by a laterally varying sheet current flowing above the Earth. The current in the first approach is computed on the base of 3-D magnetohydrodynamic simulation of near-Earth space. In the second one the source is constructed using ground-based magnetometers' data. In the third approach the geoelectric field is calculated using plane wave excitation. We carry out geoelectric field modellings for Kola Peninsula and Karelia using these three approaches. In our simulations we utilise the 3-D conductivity model of Fennoscandia (SMAP). The geoelectric field is computed using 3-D EM forward modelling code extrEMe based on a contracting integral equation method. We compare modelling results to EM field observations and discuss advantages and disadvantages of the considered approaches.

How to cite: Marshalko, E., Kruglyakov, M., Kuvshinov, A., Sokolova, E., Pilipenko, V., and Kozyreva, O.: Comparing three approaches to the ground geoelectric field modelling due to space weather events, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7702, https://doi.org/10.5194/egusphere-egu2020-7702, 2020.

EGU2020-2696 | Displays | ST4.2

Dispersionless and Weakly Dispersed Injections in the Dayside Magnetosphere with Evidence of Mirror Wave Signatures

Matthew Cooper, Andrew Gerrard, Louis Lanzerotti, Gareth Perry, and Rualdo Soto-Chavez

We present observational evidence of mirror waves in the dayside inner magnetosphere as measured with instrumentation on the dual NASA Van Allen Probes spacecraft.  While mirror waves near the dayside bow shock have been reported from several spacecraft missions (e.g. Cluster, THEMIS, MMS), their presence in the dayside inner magnetosphere has not been reported.  We speculate that the mirror modes are associated with direct dayside injections under negative Bz conditions, and drift to lower L-shells.  The analyzed event coincides with the main phase of a CME shock-induced space weather storm, with high solar wind speeds in excess of 700 km/s and a sudden drop in Dst occurring approximately eight hours prior to the event.  The highest plasma beta values were measured by spacecraft B at 12:24 at magnetic noon at L ~ 4.5-5.5.  Spacecraft A later measured a similar feature at 13:00 local magnetic time.  The potential presence of such mirror waves would indicate dayside sources of anisotropy inside the magnetopause, or the penetration of bow shock particles into the dayside inner L-shells.  To our knowledge, this is the first time such waves have been reported in the inner magnetosphere.

How to cite: Cooper, M., Gerrard, A., Lanzerotti, L., Perry, G., and Soto-Chavez, R.: Dispersionless and Weakly Dispersed Injections in the Dayside Magnetosphere with Evidence of Mirror Wave Signatures, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-2696, https://doi.org/10.5194/egusphere-egu2020-2696, 2020.

It is an important method to study solar wind speed through observation of Interplanetary Scintillation (IPS). There are two big antenna with multi- frequency channels simultaneous observing interplanetary scintillation in Miyun Observatories NAOC. The aperture of the antenna is 40 meters and 50 meters respectively. There are two dual-frequency channels available in these systems: 327/611 MHz and 2300/8400 MHz. We will carriy out a comparison of these method using the normalized cross-spectrum and dual- frequency IPS measurement to observing the solar wind speed. Dual-Antenna Interference system have better sensitivity and time resolution. It can observe more weak radio sources one by one around the Sun. We can obtain more solar wind information on the Solar-Terrestrial distribution. 

How to cite: Liu, D.: Observing Interplanetary Scintillation with Dual-Antenna Interference , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6373, https://doi.org/10.5194/egusphere-egu2020-6373, 2020.

EGU2020-7474 | Displays | ST4.2

Evaluation of Aurora Activity Obtained from Abisko and Kiruna Ground Based Observation

Kiyonobu Sugihara, Masatoshi Yamauchi, Makoto Kobayashi, Shin Koichi, and Masahiro Nishi

Available space weather forecasts mainly use data from the Sun and upstream interplanetary monitoring, to provide the early warning. Although the accuracy is improving, it cannot provide onset timing and actual strength of the substorm and its propagations better than 1 hour. A higher-accuracy forecast requires monitoring of the ionosphere (e.g., aurora and geomagnetic field). In this sense, it is also necessary to develop a value-based nowcast based on such monitoring. In EGU 2018, Yamauchi et al. has proposed simple index showing aurora and geomagnetic conditions using 1-minute resolution values from Kiruna. This study improved in the following directions:

(1) We used 1-sec resolution data and optimized the indices above: By using 1-sec values, the products representing variation (standard deviation and peak-to-peak variation) can be obtained every minute and improved, whereas combination of ∑L3 (or ∑L*exp(L)) and area of aurora found to be the best in representing the aurora activity, where L is luminosity of each pixel defined by HLS color code. Using these values, we confirmed that the intensity of the aurora was different for the same magnetic variation between before and after the strongest aurora (substorm onset). Therefore, it is necessary to add a condition of "increasing trend" of both aurora and magnetic variation from the viewpoint of forecasting.

(2) We compared the results from two different places (Abisko and Kiruna in Sweden) that are 89 km apart in linear distance. Our Abisko camera system (DASC, Digital All Sky Camera) is in operation since March 2014. When the aurora was observed at both sites, the shapes of the aurora at both sites are sometimes quite different at the same time. In addition, the timing of the brightest aurora (∑L3 or ∑L*exp(L) is maximum) was different between both sites. These results confirm that the aurora had a three-dimensional structure, which has been known for many years.

(3) Using superposed epoch analysis, we also took statistics of last 10 minutes before the largest aurora (in the index mentioned above) occurred.

How to cite: Sugihara, K., Yamauchi, M., Kobayashi, M., Koichi, S., and Nishi, M.: Evaluation of Aurora Activity Obtained from Abisko and Kiruna Ground Based Observation, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7474, https://doi.org/10.5194/egusphere-egu2020-7474, 2020.

EGU2020-7650 | Displays | ST4.2

PECASUS - ICAO Designated Space Weather Service Network for Aviation

Harri Haukka, Ari-Matti Harri, Kirsti Kauristie, Jesse Andries, Mark Gibbs, Peter Beck, Jens Berdermann, Loredana Perrone, Bert van den Oord, David Berghmans, Nicolas Bergeot, Erwin De Donder, Martin Latocha, Mark Dierckxsens, Haris Haralambous, Iwona M Stanislawska, Volker Wilken, Vincenzo Romano, Martin Kriegel, and Kari Österberg

The PECASUS Consortium (European Consortium for Aviation Space weather User Services) provides targeted space weather services focusing on the dissemination of warning messages, called 'advisories', towards aviation actors. PECASUS services corresponds to extreme space weather events with impact on aviation GNSS systems, HF communication and radiation levels at flight altitudes. In November 2018 ICAO (International Civil Aviation Organization) designated three global space weather service centers. These centers acre operated by the European PECASUS consortium, by United States and by the consortium of Australia, Canada, France and Japan.

PECASUS was set-up as a consortium bringing together a number of European partners with proven space weather service capabilities. The PECASUS consortium is coordinated by FMI (Finland) who is also the ultimate responsible for communications towards the aviation sector. The Advisory Messages are produced by STCE (Belgium) on the basis of expert interpretation and data streams produced by DLR (Germany), INGV (Italy), Seibersdorf Laboratories (Austria), STCE (Belgium), SRC (Poland) and FU (Cyprus). In addition, the MetOffice (UK) will act as a resilience node in case of a major failure in the network, while the KNMI (The Netherlands) will take care of user liaison and monitor the PECASUS performance.

The PECASUS Consortium was audited in February 2018 by space weather and operational management experts, nominated by the World Meteorological Organisation (WMO). The audit addressed a broad spectrum of criteria under Institutional, Operational, Technical and Communication/ Dissemination categories. PECASUS was declared fully compliant in all ICAO/WMO criteria with no areas for improvement identified.

Our presentation we will describe the coordinated actions of three ICAO Space Weather Centers, PECASUS network and its operations, and the vision of the PECASUS team to move forward. User interactions such as education and training, user feedback at ESWW, product and performance verification are part of PECASUS operations.

How to cite: Haukka, H., Harri, A.-M., Kauristie, K., Andries, J., Gibbs, M., Beck, P., Berdermann, J., Perrone, L., van den Oord, B., Berghmans, D., Bergeot, N., De Donder, E., Latocha, M., Dierckxsens, M., Haralambous, H., Stanislawska, I. M., Wilken, V., Romano, V., Kriegel, M., and Österberg, K.: PECASUS - ICAO Designated Space Weather Service Network for Aviation, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7650, https://doi.org/10.5194/egusphere-egu2020-7650, 2020.

EGU2020-7933 | Displays | ST4.2

Effect of selecting different simulation configurations on the prediction performance of the Space Weather Modeling Framework regarding ground magnetic perturbations

Norah Kaggwa Kwagala, Michael Hesse, Therese M. Jorgensen, Paul Tenfjord, Cecilia Norgren, Gabor Toth, Tamas Gombosi, Håkon M. Kolstø, and Susanne F. Spinnangr

This study investigates the effect of selecting different simulation configurations of the Space Weather Modeling Framework (SWMF) on the predictions of ground magnetic perturbations. A historic geomagnetic storm, the St. Patrick Storm 2015, is simulated with several different model configurations. The objective is to investigate how the different configurations affect the prediction performance regarding ground magnetic perturbations. For each simulation, the modeled ground magnetic perturbations are compared to the measured perturbations from several ground magnetometer stations located at sub-auroral, auroral and polar cap latitudes. Among the magnetometer stations are the Norwegian and Greenland magnetometer chains. The comparison is based on metrics for both ΔB and dB/dt. The SWMF configurations investigated include variations in grid resolution and integration schemes for the MHD equations, and different settings for the inner magnetosphere, the ionosphere electrodynamics, and the magnetosphere-ionosphere coupling.

How to cite: Kwagala, N. K., Hesse, M., M. Jorgensen, T., Tenfjord, P., Norgren, C., Toth, G., Gombosi, T., M. Kolstø, H., and F. Spinnangr, S.: Effect of selecting different simulation configurations on the prediction performance of the Space Weather Modeling Framework regarding ground magnetic perturbations , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-7933, https://doi.org/10.5194/egusphere-egu2020-7933, 2020.

EGU2020-11371 | Displays | ST4.2

Development of a local nowcast magnetospheric ring current index based on geomagnetic observatory data

Guram Kervalishvili, Claudia Stolle, and Jürgen Matzka

The Disturbance storm time (Dst) index is derived using the H-component perturbation on magnetometers from four observatories (Hermanus, Kakioka, Honolulu, and San Juan) near the Sq focus. The Dst index is a quantitative measure of geomagnetic activity (major disturbances are negative) that monitors the intensity of the magnetospheric ring current and it is derived and maintained by WDC Kyoto. The local nowcast index presented here is a geomagnetic index that is derived similarily to the Dst index for the each of the following low and mid-latitude observatories: Tristan da Cunha (South Atlantic, TDC), St. Helena (South Atlantic, SHE), Keetmanshoop (Namibia, KMH), Vassouras (Brazilian, VSS), Gan (Maldives, GAN) and Panagjurishte (Bulgaria, PAG). This local index is developed within the ESA’s SSA SWE G-ESC activity. Here, we assess the influence of the quiet-time Sq estimation on the local ring current index and the correlation of the index with other solar and geophysical parameters.

How to cite: Kervalishvili, G., Stolle, C., and Matzka, J.: Development of a local nowcast magnetospheric ring current index based on geomagnetic observatory data, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-11371, https://doi.org/10.5194/egusphere-egu2020-11371, 2020.

The Polar Cap (PC) indices are derived from the magnetic variations generated by the transpolar convection of magnetospheric plasma and embedded magnetic fields driven by the interaction with the solar wind. The PC indices are potentially very useful for Space Weather monitoring and forecasts and for related research. However, the PC index series in the near-real time and final versions endorsed by the International Association for Geomagnetism and Aeronomy (IAGA) have been proven unreliable (Stauning, 2013, 2015, 2018a,b,c, 2020). Both versions include solar wind sector (SWS) effects in the calculation of the reference levels from which magnetic disturbances are measured. The SWS effects are caused by current systems in the dayside Cusp region related to the Y-component, BY, of the Interplanetary Magnetic Field (IMF). However, the IAGA-endorsed handling of SWS effects may generate unfounded PC index changes of up to 3 mV/m at the nightside away from the Cusp. For the real-time PCN and PCS indices, their cubic spline-based reference level construction may cause additional unjustified index excursions of more than 3 mV/m with respect to the corresponding final index values. Noting that PC index values above 2 mV/m indicate geomagnetic storm conditions, such unjustified contributions are considered to invalidate the IAGA-endorsed PC index series. The presentation shall include a description of alternative derivation methods shown to provide more consistent index reference levels for both final and real-time PC indices, to reduce their unfounded excursions, and to significantly increase their reliability (Stauning, 2016, 2018b,c).

References. Stauning, P. (2020): The Polar Cap (PC) index: invalid index series and a different approach. Space Weather, 2020SW002442 (submitted).

Stauning, P. (2013). Comments on quiet daily variation derivation in “Identification of the IMF sector structure in near-real time by ground magnetic data” by Janzhura and Troshichev (2011). Annales Geophysicae, 31, 1221-1225. https://doi.org/10.5194/angeo-31-1221-2013 .

Stauning, P. (2015). A critical note on the IAGA-endorsed Polar Cap index procedure: effects of solar wind sector structure and reverse polar convection. Annales Geophysicae, 33, 1443-1455. https://doi.org/10.5194/angeo-33-1443-2015 .

Stauning, P. (2016). The Polar Cap (PC) Index.: Derivation Procedures and Quality Control. DMI Scientific Report SR-16-22. Available at: https://www.dmi.dk/fileadmin/user_upload/Rapporter/TR/2016/SR-16-22-PCindex.pdf .

Stauning, P. (2018a). A critical note on the IAGA-endorsed Polar Cap (PC) indices: excessive excursions in the real-time index values. Annales Geophysicae, 36, 621–631. https://doi.org/10.5194/angeo-36-621-2018 .

Stauning, P. (2018b): Multi-station basis for Polar Cap (PC) indices: ensuring credibility and operational reliability. Journal of Space Weather and Space Climate, 8, A07. https://doi.org/10.1051/swsc/2017036 .

Stauning, P. (2018c). Reliable Polar Cap (PC) indices for space weather monitoring and forecast

How to cite: Stauning, P.: Unreliable IAGA-endorsed Polar Cap (PC) index series and a different approach, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-10195, https://doi.org/10.5194/egusphere-egu2020-10195, 2020.

EGU2020-22188 | Displays | ST4.2

SWx TREC: Further Developments on an Integrative Space Weather (SWx) Data Portal

Tom Baltzer, Greg Lucas, Chris Pankratz, Jennifer Knuth, and Doug Lindholm

Working under the Space Weather Technology, Research and Education Center (SWx-TREC https://www.colorado.edu/spaceweather/).  The Laboratory for Atmospheric and Space Physics (LASP) is developing a Space Weather (SWx) Data Portal to provide unified access to disparate datasets to help close the Research to Operations (R2O) and Operations to Research (O2R) gap. 

LASP is building the SWx Portal leveraging technologies developed in support of spacecraft operations (WEBTCAD), Irradiance Dataset viewing and downloading (LISIRD: http://lasp.colorado.edu/lisird/ ) and the MAVEN and MMS Science Data Portals.  The primary technologies include a data model and software library that enables data interoperability known as LaTiS (https://github.com/latis-data) and the LASP Extended Metadata Repository (LEMR) which is developed as ontologies that not only represent the datasets, but also the front-end elements which are used to display them.  Additionally, we have developed a JavaScript science data display technology that leverages off LaTiS server instances to allow for consistent and straightforward display of datasets.  These technologies together facilitate a common interface to myriad datasets and formats which will enable us to expand the offerings quickly and provide consistent visualization, access to metadata, and download capabilities across them.

This presentation will discuss advancements in the portal development in the last year to both in terms of available datasets and in terms of new functionality.  We will also provide a demonstration of the released system that will include datasets demonstrating a solar event, its progression toward Earth and its Earth affect perspective of Space Weather Data centering on the 2015 St. Patrick’s day storm.

How to cite: Baltzer, T., Lucas, G., Pankratz, C., Knuth, J., and Lindholm, D.: SWx TREC: Further Developments on an Integrative Space Weather (SWx) Data Portal, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-22188, https://doi.org/10.5194/egusphere-egu2020-22188, 2020.

EGU2020-22144 | Displays | ST4.2

The SWx TREC Integrative Space Weather Data Portal and Model/Algorithm Testbed Environment

Chris Pankratz, Thomas Baltzer, Greg Lucas, James Craft, Thomas Berger, Daniel Baker, Jennifer Knuth, and Allison Jaynes

The Space Weather Technology, Research and Education Center (SWx TREC) is a center of excellence in cross-disciplinary research, technology, innovation, and education, intended to facilitate evolving space weather research and forecasting needs.  SWx TREC facilitates research advances, innovative missions, and data and computing technologies that directly support the needs of the SWx community to advance understanding and support closure of the Research to Operations (R2O) and Operations to Research (O2R) loop. Improving our understanding and prediction of space weather requires coupled Research and Operations. SWx-TREC is working to provide new research models, applications and data for use in operational environments, improving the Research-to-Operations (R2O) pipeline.  Advancement in the fundamental scientific understanding of space weather processes is also vital, requiring that researchers have convenient and effective access to a wide variety of data sets and models from multiple sources. The space weather research community, as with many scientific communities, must access data from dispersed and often uncoordinated data repositories to acquire the data necessary for the analysis and modeling efforts that advance our understanding of solar influences and space physics in the Earth’s environment. The University of Colorado (CU) is a leading institution in both producing data products and advancing the state of scientific understanding of space weather processes, and we are now hosting both an interoperable data portal providing streamlined, centralized, and event-based access to a wide variety of disparate data sets and also a community-accessible, Cloud-based testbed environment to support development, testing, transition, and use of new models, visualizations, algorithms, and forecast products.  In this presentation, we will describe our community-accessible testbed environment and demonstrate the Space Weather Data Portal.

How to cite: Pankratz, C., Baltzer, T., Lucas, G., Craft, J., Berger, T., Baker, D., Knuth, J., and Jaynes, A.: The SWx TREC Integrative Space Weather Data Portal and Model/Algorithm Testbed Environment, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-22144, https://doi.org/10.5194/egusphere-egu2020-22144, 2020.

EGU2020-20318 | Displays | ST4.2

Variability of ionospheric parameters by the Swarm satellites for different solar activity

Daria Kotova, Yaqi Jin, and Wojciech Miloch

The use of satellite data allows us to study the variability of ionospheric plasma parameters globally without references to ground stations or receivers in different regions of the Earth. The Swarm mission, which was launched in 2014 and is still operational, allows us to investigate the effects of decreasing solar activity on the ionospheric variability. In our study we use the Swarm in-situ measurements of the electron density and derived parameters. This dataset provides characteristics of the plasma variability along the orbit and gives information on plasma density structures in the ionosphere in terms of their amplitudes, gradients and spatial scales. We analyze the variability of these parameters in the contexts of the northern and southern hemispheres, specific latitudinal regions, and the solar activity level. Understanding of the distribution of such parameters in the context of the solar activity level and selected ionospheric regions can have implications for the development of new satellite instruments and for the accuracy of GNSS precise positioning.

How to cite: Kotova, D., Jin, Y., and Miloch, W.: Variability of ionospheric parameters by the Swarm satellites for different solar activity, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-20318, https://doi.org/10.5194/egusphere-egu2020-20318, 2020.

EGU2020-1692 | Displays | ST4.2

A scheme for forecasting severe space weather

Balan Nanan

We have developed and tested a scheme for forecasting severe space weather (SvSW) that caused all known electric power outages and telecommunication system failures since 1957 and the Carrington event of 1859. The SvSW events of 04 August 1972 has puzzled the scientific community as it occurred during a moderate storm (DstMin = -124 nT) while all other SvSW events occurred during super storms (DstMin ≤ -250 nT). The solar wind velocity V and IMF Bz measured by ACE satellite at the L1 point since 1998 are used. For the earlier SvSW events such as the Carrington event of 1859, Quebec event of 1989, and the events in February 1958 and August 1972 we used the information from the literature. The coincidence of high ICME front (or shock) velocity ΔV (sudden increase in V over the background by over 275 km/s) and sufficiently large Bz southward at the time of the ΔV increase is associated with SvSW; and their product (ΔV×Bz) is found to exhibit a large negative spike at the speed increase. Such a product (ΔV×Bz) exceeding a threshold seems suitable for forecasting SvSW, with a maximum forecasting time of 35 minutes using ACE data. However, the coincidence of high V (not containing ΔV) and large Bz southward does not correspond to SvSW, indicating the importance of the impulsive action of high ΔV and large Bz southward coming through when they coincide. The need for the coincidence is verified using the CRCM.

How to cite: Nanan, B.: A scheme for forecasting severe space weather, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1692, https://doi.org/10.5194/egusphere-egu2020-1692, 2020.

EGU2020-15904 | Displays | ST4.2

Solar radio burst interference index dedicated to GNSS single and double frequency users

Jean-Marie Chevalier, Nicolas Bergeot, Pascale Defraigne, Christophe Marque, and Elisa Pinat

Intense solar radio bursts (SRBs) emitted at L-band frequencies are a source of radio frequency interference for Global Navigation Satellite Systems (GNSS) by inducing a noise increase in GNSS measurements, and hence degrading the carrier-to-noise density (C/N0). Such space weather events are critical for GNSS-based applications requiring real-time high-precision positioning.

Since 2015, the Royal Observatory of Belgium (ROB) monitors in near real-time the C/N0 observations from the European Permanent Network (EPN). The monitoring allows to detect accurately the general fades of C/N0 due to SRBs over Europe as from 1 dB-Hz. It provides in near real-time a quantification of the GNSS signal reception fade for the L1 C/A and L2 P(Y) signals and notifies civilian single and double frequency users with a 4-level index corresponding to the potential impact on their applications. This service is part of the real-time monitoring service of the PECASUS project of the International Civil Aviation Organization (ICAO) which started end of 2019.

Results of this 5-year monitoring will be discussed, including the 3 SRBs of 2015 and 2017, together with the new developments toward a global index using the International GNSS Service (IGS) network. In addition, we will show how the SRB monitoring is sometimes interfered by GPS flex power campaigns on the satellites from blocks IIR-M and IIF, and how it is mitigated . The routine and transient GPS flex power campaigns will be presented in terms of C/N0 variations for the EPN and IGS networks.

How to cite: Chevalier, J.-M., Bergeot, N., Defraigne, P., Marque, C., and Pinat, E.: Solar radio burst interference index dedicated to GNSS single and double frequency users, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-15904, https://doi.org/10.5194/egusphere-egu2020-15904, 2020.

EGU2020-12084 | Displays | ST4.2

An Empirical Model of Electron Flux from the Seven-Year Van Allen Probe Mission

Christine Gabrielse, James Roeder, Justin Lee, Seth Claudepierre, Drew L. Turner, T. Paul O'Brien, Joseph Fennell, and J. Bern Blake

The near-Earth radiation environment is a force to contend with when designing satellites and their instruments. Solar storms can accelerate and transport energetic particles closer to Earth, populating Earth’s radiation belts and increasing a satellite’s radiation dosage. A major application to the field of space weather is therefore knowing and understanding the near-Earth radiation environment. We use Van Allen Probe data throughout mission lifetime to look at electron fluxes at different energies, pitch angles, and L shells, creating a daily average flux model that can be used to deduce what fluences were observed by any satellite that flew within Van Allen Probe’s seven-year mission. We supplement Van Allen Probe fluxes with THEMIS statistical fluxes at higher L shells. This model can be applied to better understand satellite degradation issues related to the radiation environment. It is an improvement from previous empirical models in this regard by virtue of the fact that actual fluxes from a specific storm (or storms) can be deduced and compared to real satellite degradation data.

How to cite: Gabrielse, C., Roeder, J., Lee, J., Claudepierre, S., Turner, D. L., O'Brien, T. P., Fennell, J., and Blake, J. B.: An Empirical Model of Electron Flux from the Seven-Year Van Allen Probe Mission, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-12084, https://doi.org/10.5194/egusphere-egu2020-12084, 2020.

The Global Navigation Satellite System (GNSS) radio occultation and topside sounder provide materials for the validation of a mathematical description of the topside ionosphere up to satellite altitude. An attempt to represent the topside electron density profile is using α-Chapman function with a continuously varying scale height. In this study, the Vary-Chap scale height profiles are obtained based on Constellation Observing System for Meteorology, Ionosphere, and Climate (COSMIC) electron density profiles from 1 January 2008 to 31 December 2013 and fitted by a shape function composed of two weighted patterns representing the ion and electron contributions of lower and higher altitudes. The topside profiles of ISIS-1 data are used to define the transition height of different ions. The associated fitting parameters are analyzed to reveal their temporal and spatial features and variations along with enhancement of solar activity. Their prominent dependence on latitudes, longitudes, the local time, the season, and the solar cycle facilitates modeling of the Vary-Chap scale height in constructing empirical topside ionospheric models.

How to cite: Wu, M.: New topside ionosphere model based on Vary-Chap function using radio occultation and topside sounder data, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-12822, https://doi.org/10.5194/egusphere-egu2020-12822, 2020.

EGU2020-18174 | Displays | ST4.2

Realtime geomagnetic indices for mid-latitudes. MID-R, MID-E, MID-U and MID-L

Antonio Guerrero, Elena Saiz, and Consuelo Cid

Mid latitudes around 40 degree are influenced by effects typically found at both high and low latitudes. Moreover, the focus of the Solar Quiet ionospheric current system, drifts around these mid-latitudes. Consequently they have been considered as a complicated place to infer the geospace state from the ground and also complicated for practical procedures to generate geomagnetic indices. 
The procedure designed at the University of Alcala specially focused on removing solar regular variations at mid-latitudes is delivering a geomagnetic Local Disturbance index (LDi) in realtime. The same procedure can be used to produce global geomagnetic indices when applied to several geomagnetic stations at these latitudes. 
We present in this work the high-resolution (one minute) realtime production of ring current and auroral indices (MID-R, MID-E, MID-U and MID-L) similar to the well known Dst and AE indices for mid-latitudes which will help in the understanding of the complex physical processes that emerge at these latitudes. At the same time they fill a gap in the current operational space weather products available for these latitudes.

How to cite: Guerrero, A., Saiz, E., and Cid, C.: Realtime geomagnetic indices for mid-latitudes. MID-R, MID-E, MID-U and MID-L, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18174, https://doi.org/10.5194/egusphere-egu2020-18174, 2020.

This study presents experiments of driving a physics-based thermosphere model (TIE-GCM) by assimilating radio occultation electron density (Ne) profiles from the COSMIC (Constellation Observing System for Meteorology, Ionosphere and Climate) mission using an ensemble Kalman filter. This study not only helps to gauge the accuracy of the assimilation, to explain the inherent model bias, and to understand the limitations of the framework, but it also demonstrates the capability of the assimilation technique to forecast the highly dynamical thermosphere in the presence of realistic data assimilation scenarios.

Experiments cover both solar minimum (March 2008) and solar maximum (June 2014) periods. The results show that data assimilation improves the model state. Here the improvement is shown with comparisons to Ne and neutral density data from Swarm-A, Swarm-C, CHAMP, and GRACE-A satellite missions. The root mean squared error (RMSE) of Ne is reduced in the Ne-guided lower thermosphere more than that of the higher altitudes (e.g. 1.7×104 electrons/cm3 at 200 km vs 2.9×104 electrons/cm3 at 400 km). The average RMSE in the forecasted Ne is approximately 1.3×105 electrons/cm3 at altitudes between 200 and 400 km, and  drops to 0.7×105 electrons/cm3 at 500 km. The study also reveals that only a limited number of bonafide Ne profiles are available for assimilation tasks in the experiments. These results also provide insights into the biases inherent in the physics-based model. The systematic biases that this study highlight could be an indication that the specification of plasma-neutral interactions in the model needs further adjustments.

How to cite: Kodikara, T.: Forecasting of the Upper Atmosphere via Assimilation of Electron Density Data, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-13024, https://doi.org/10.5194/egusphere-egu2020-13024, 2020.

Space weather can be the source of severe disturbances in the ionosphere, which can influence the performance and reliability of GNSS (Global Navigation Satellite Systems) technology and applications. In order to forecast and minimize these effects, accurate corrections need to be provided. This goal can be achieved by employing a precise model to describe the complex chain of space weather processes and the non-linear spatial and temporal variability of the Vertical Total Electron Content (VTEC) within the ionosphere, as well as, to include a forecast component considering space weather events in order to provide an early warning system. This is a challenging but important task of high interest for the GNSS community.

Artificial intelligence applications, such as Machine Learning (ML), are able to find and learn patterns from historical data to solve problems, which are too complex and/or too vast for humans. To develop an effective and high performance ML algorithm special consideration needs to be given to the selection of the input data. Data need to be selected in order to have sufficient information to describe and predict ionosphere VTEC variability accurately. Therefore, the study of space weather impacts for the integration of space weather information in forecast ionosphere models is of crucial importance.

In this study, the relationship between various indices, describing space weather and space climate, and ionosphere VTEC variability in different latitudes during longer time periods within the solar cycle 24 is examined. Conditions in space weather are described by solar wind, the magnetic field and plasma data, energetic proton fluxes, geomagnetic and solar activity indices provided by worldwide distributed observatories. VTEC data are derived from GNSS measurement from permanent stations, belonging to the EPN (EUREF Permanent Network) and the IGS (International GNSS Service) networks and selected in latitudinal range from 0° to 60°N. The period from year 2014 to year 2017 is used to relate space weather indices to VTEC variability, as well as, to train the ML model. In addition, periods of intense geomagnetic storms caused by different sources (coronal mass ejections and high-speed streams of solar wind from coronal holes), occurred during different seasons in this period are analyzed. The evolution and severity of storms are investigated in relation to the conditions in the solar activity, solar wind speed, interplanetary magnetic field and geomagnetic field together with their impact on the ionosphere VTEC. Obtained results of this investigation will be presented, as well as the methodology, goals and challenges for ML model development including preliminary results of an initial ML model.

How to cite: Natras, R. and Schmidt, M.: Relationship Between Ionosphere VTEC and Space Weather Indices for Machine Learning-based Model Development, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18978, https://doi.org/10.5194/egusphere-egu2020-18978, 2020.

EGU2020-1002 | Displays | ST4.2

MAG-GIC: Geomagnetically Induced Currents risk hazard in the Portuguese power network

Joana Alves Ribeiro, Maria Alexandra Pais, Fernando J. G. Pinheiro, Fernando A. Monteiro Santos, and Pedro Soares

The MAG-GIC project has as a main goal to produce the chart of Geomagnetically Induced Currents (GIC) risk hazard in the distribution power network of Portugal mainland.

The study of GICs is important as they represent a threat for infrastructures such as power grids, pipelines, telecommunication cables, and railway systems. A deeper insight into GICs hazard may help in planning and designing more resilient transmission systems and help with criteria for equipment selection.

GICs are a result of variations in the ionospheric and magnetospheric electric currents, that cause changes in the Earth's magnetic field. The Coimbra magnetic observatory (COI) is one of the oldest observatories in operation in the world and the only one in Portugal mainland. It has been (almost) continuously monitoring the geomagnetic field variations since 1866, and in particular, it has registered the imprint of geomagnetic storms during solar cycle 24. Besides the geomagnetic storm signal, which represents the GICs driver, the crust and upper mantle electrical conductivities determine the amplitude and geometry of the induced electric fields.

To present a better approximation of the Earth's conductivity structure below the Portuguese power network, we initiated a campaign to acquire magnetotelluric (MT) data in a grid of 50x50 km all over the territory. Nonetheless, there already exist enough MT data to create a realistic 3D conductivity model in the south of Portugal.

The other important input is the electric circuit for the network grid. We benefit from the collaboration of the Portuguese high voltage power network (REN) company, in providing the grid parameters as resistances and transformer locations, thus allowing us to construct a more precise model. In particular, we implement in our model the effect of shield wires and shunt reactors resistances.

In this study, we present the results of GIC calculations for the south of Portugal for some of the strongest geomagnetic storms in the 20015-17 period recorded at COI during solar cycle 24. We will focus on the sensitivity of results concerning two different conductivity models and different values of the shielding circuit parameters and shunt reactors devices.

How to cite: Alves Ribeiro, J., Pais, M. A., J. G. Pinheiro, F., Monteiro Santos, F. A., and Soares, P.: MAG-GIC: Geomagnetically Induced Currents risk hazard in the Portuguese power network, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1002, https://doi.org/10.5194/egusphere-egu2020-1002, 2020.

EGU2020-10909 | Displays | ST4.2

Improving solar wind forecasts using data assimilation

Matthew Lang, Mathew Owens, and Amos Lawless

Data assimilation has been used in Numerical Weather Prediction models with great success, and it can be seen that the improvement of data assimilation methods has gone hand-in-hand with improvements in weather forecasting skill. The implementation of data assimilation for solar wind forecasting is still in its infancy and is still underused in the field. Hence, it is important to investigate the optimal implementation of these methods to improve our understanding of the solar wind.

To do this, we have generated a variational data assimilation scheme for use with a steady-state solar wind speed model based upon the Burger equation. This relatively simple scheme has the advantage of updating the inner-boundary conditions of the solar wind model allowing the updates to persist and improve the solar wind estimates throughout the whole domain.

To this effect, we present numerical experiments using our data assimilation scheme with STEREO and ACE data to improve estimates and forecasts of the solar wind in near-Earth space. Particular focus will be applied to assimilating data when the satellites are 60 degrees apart, such that they simulate Earth-L5 forecasting scenarios.

How to cite: Lang, M., Owens, M., and Lawless, A.: Improving solar wind forecasts using data assimilation, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-10909, https://doi.org/10.5194/egusphere-egu2020-10909, 2020.

ST4.3 – Space Weather and its Effects on Terrestrial and Geo-Space Environments: Science and Application

EGU2020-5667 | Displays | ST4.3

GIC drivers - the Characteristics of Storm-time Rapid Geomagnetic Variations

Hermann J. Opgenoorth, Audrey Schilling, and Maria Hamrin

Rapid storm-time geomagnetic disturbances, typically at sub-auroral latitudes, have been recognized as one of the most detrimental space weather phenomena, potentially leading to damage to and outage of critical power infrastructure. We can show that sub-auroral magnetic spikes in storms (of the order of 1000 nT/min) do resemble in their appearance and spatio-temporal behavior small but intense and very short-lived substorms, including three-dimensional current wedge and electrojet-enhancement formation. Statistically these spikes do occur at all local times, but preferably pre-midnight and around 0600 MLT in the morning sector, which is only partially in agreement with the substorm analogy, and indicate that there may indeed be several mechanisms at work. We will present results from event and statistical studies to clarify the physical characteristics and potential drivers for these potentially most damaging geomagnetic disturbances in the SWx realm.

 

How to cite: Opgenoorth, H. J., Schilling, A., and Hamrin, M.: GIC drivers - the Characteristics of Storm-time Rapid Geomagnetic Variations , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-5667, https://doi.org/10.5194/egusphere-egu2020-5667, 2020.

EGU2020-1416 | Displays | ST4.3

From the Sun to the Earth: August 25, 2018 geomagnetic storm effects

Mirko Piersanti, Paola De Michelis, Dario Del Moro, Roberta Tozzi, Michael Pezzopane, Giuseppe Consolini, Monica Laurenza, Simone Di Matteo, Alessio Pignalberi, Valerio Quattrociocchi, and Piero Diego

On August 25, 2018 the interplanetary counterpart of the August 20, 2018 Coronal Mass Ejection (CME) hit the Earth, giving rise to a strong geomagnetic storm. We present a description of the whole sequence of events from the Sun to the ground as well as a detailed analysis of the onserved effects on the Earth's environment by using a multi instrumental approach.
We studied the ICME propagation in the interplanetary space up to the analysis of its effects in the magnetosphere, ionosphere and at ground. To accomplish this task, we used ground and space collected data, including data from CSES (China Seismo Electric Satellite), launched on February 11, 2018. We found a direct connection between the ICME impact point onto the magnetopause and the pattern of the Earth's polar electrojects. Using the Tsyganenko TS04 model prevision, we were able to correctly identify the principal magnetospheric current system activating during the different phases of the geomagnetic storm. Moreover, we analyzed the space-weather effects associated with the August 25, 2018 solar event in terms of evaluation geomagnetically induced currents (GIC) and identification of possible GPS loss of lock. We found that, despite the strong geomagnetic storm, no loss of lock has been detected. On the contrary, the GIC hazard was found to be potentially more dangerous than other past, more powerful solar events, such as the St. Patrick geomagnetic storm, especially at latitudes higher than $60^\circ$ in the European sector.

How to cite: Piersanti, M., De Michelis, P., Del Moro, D., Tozzi, R., Pezzopane, M., Consolini, G., Laurenza, M., Di Matteo, S., Pignalberi, A., Quattrociocchi, V., and Diego, P.: From the Sun to the Earth: August 25, 2018 geomagnetic storm effects, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1416, https://doi.org/10.5194/egusphere-egu2020-1416, 2020.

EGU2020-3367 | Displays | ST4.3 | ST Division Outstanding ECS Lecture

Explicit IMF By-dependence in geomagnetic activity

Lauri Holappa, Timo Asikainen, and Kalevi Mursula

The interaction of the solar wind with the Earth’s magnetic field produces geomagnetic activity, which is critically dependent on the orientation of the interplanetary magnetic field (IMF). Most solar wind coupling functions quantify this dependence on the IMF orientation with the so-called IMF clock angle in a way, which is symmetric with respect to the sign of the By component. However, recent studies have shown that IMF By is an additional, independent driver of high-latitude geomagnetic activity, leading to higher (weaker) geomagnetic activity in Northern Hemisphere (NH) winter for By > 0 (By < 0). For NH summer the dependence on the By sign is reversed. We quantify the size of this explicit By-effect with respect to the solar wind coupling function, both for northern and southern high-latitude geomagnetic activity. We show that for a given value of solar wind coupling function, geomagnetic activity is about 40% stronger for By > 0 than for By < 0 in NH winter. The physical mechanism of the By-effect is not yet fully understood. Here we show that IMF By modulates the flux of energetic electrons precipitating into the ionosphere which likely modulates the ionospheric conductivity and, thus, geomagnetic activity. Our results highlight the importance of the IMF By-component for space weather and must be taken into account in future space weather modeling.

How to cite: Holappa, L., Asikainen, T., and Mursula, K.: Explicit IMF By-dependence in geomagnetic activity, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3367, https://doi.org/10.5194/egusphere-egu2020-3367, 2020.

EGU2020-6925 | Displays | ST4.3

Unusually high thermospheric hydrogen density prior to severe storm of September 8, 2017 and its impact on the storm manifestations

Dmytro Kotov, Philip Richards, Oleksandr Bogomaz, Maryna Shulha, Naomi Maruyama, Mariangel Fedrizzi, Vladimír Truhlík, János Lichtenberger, Manuel Hernández-Pajares, Yoshizumi Miyoshi, Yoshiya Kasahara, Atsushi Kumamoto, Fuminori Tsuchiya, Masafumi Shoji, Ayako Matsuoka, Iku Shinohara, Taras Zhivolup, Leonid Emelyanov, Yakiv Chepurnyy, and Igor Domnin

Atomic hydrogen plays a key role for the plasmasphere, exosphere, and the nighttime ionosphere. It directly impacts the rate of plasmasphere refilling after strong magnetic storms as atomic hydrogen is the primary source of hydrogen ions. It is the source of the geocorona, which significantly affects ring current decay during the recovery phase of magnetic storms.

Our previous studies with the Kharkiv incoherent scatter radar (49.6 N, 36.3 E), Arase and DMSP satellite missions, and FLIP physical model showed that during magnetically quiet periods of 2016–2018 the hydrogen density was generally a factor of 2 higher than from the NRLMSIS00-E model (Kotov et al., 2018).

Even larger values of thermospheric hydrogen density were detected prior to the severe storm of September 8, 2017. With Kharkiv IS radar, AWDANet whistler receivers, Arase satellite, and TEC data we found that during the nights of September 5 to 6 and September 6 to 7, the thermospheric hydrogen density had to be at least a factor of 4 higher than the values from NRLMSIS00-E model i.e. ~100% higher than expected from our previous studies. We discuss the possible mechanisms that could lead to the increased hydrogen density.

Such high hydrogen densities may be the reason for very quick recovery of inner plasmasphere after the severe depletion by the storm of September 8, 2017 (Obana et al., 2019).

References:

1. Kotov, D. V., Richards, P. G., Truhlík, V., Bogomaz, O. V., Shulha, M. O., Maruyama, N., et al. ( 2018). Coincident observations by the Kharkiv IS radar and ionosonde, DMSP and Arase (ERG) satellites, and FLIP model simulations: Implications for the NRLMSISE‐00 hydrogen density, plasmasphere, and ionosphere. Geophysical Research Letters, 45, 8062– 8071. https://doi.org/10.1029/2018GL079206

2. Obana, Y., Maruyama, N., Shinbori, A., Hashimoto, K. K., Fedrizzi, M., Nosé, M., et al. (2019). Response of the ionosphere‐plasmasphere coupling to the September 2017 storm: What erodes the plasmasphere so severely? Space Weather, 17, 861–876. https://doi.org/10.1029/2019SW002168

How to cite: Kotov, D., Richards, P., Bogomaz, O., Shulha, M., Maruyama, N., Fedrizzi, M., Truhlík, V., Lichtenberger, J., Hernández-Pajares, M., Miyoshi, Y., Kasahara, Y., Kumamoto, A., Tsuchiya, F., Shoji, M., Matsuoka, A., Shinohara, I., Zhivolup, T., Emelyanov, L., Chepurnyy, Y., and Domnin, I.: Unusually high thermospheric hydrogen density prior to severe storm of September 8, 2017 and its impact on the storm manifestations, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-6925, https://doi.org/10.5194/egusphere-egu2020-6925, 2020.

EGU2020-10026 | Displays | ST4.3

Severe Space Weather: Simulations of Scaled-Up Storms

Joachim Raeder, Beket Tulegenov, William Douglas Cramer, Kai Germaschewswski, Banafsheh Ferdousi, Naomi Maruyama, and Timothy Fuller-Rowell

Extreme space weather events are extremely rare, but pose a significant threat to our infrastructure. The one known event of such kind was the Carrington storm of 1859, but it was not well documented; in particular the solar wind and IMF conditions that caused it remain guesses. On the other hand, the STEREO-A observations of July 23, 2012 showed solar wind and IMF parameters that are most likely comparable to those of the Carrington event, and remind us that such extreme events are very well possible even during times of a quiet sun. Here, we use OpenGGCM simulations of such events to assess the effects of such solar wind and IMF on the magnetosphere. Precious work has shown that during the much more benign Halloween storm the nose of the magnetopause was as close as 4.9 RE, with an accordingly large polar cap. We will present simulations of a sequence of scaled-up storms with increasingly larger driving and demonstrate the further expansion of the polar cap, intensity of plasma injections, and the eventual saturation. In addition, we will show how the ionosphere potential penetrates to lower latitudes and affects the ionosphere and thermosphere at mid latitudes when the solar wind drivers become extreme.

How to cite: Raeder, J., Tulegenov, B., Cramer, W. D., Germaschewswski, K., Ferdousi, B., Maruyama, N., and Fuller-Rowell, T.: Severe Space Weather: Simulations of Scaled-Up Storms, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-10026, https://doi.org/10.5194/egusphere-egu2020-10026, 2020.

EGU2020-21810 | Displays | ST4.3

Ionospheric Weather Observations of FORMOSAT-7/COSMIC-2

Fu-Yuan Chang, Jann-Yenq Liu, Chi-Yen Lin, Shih-Ping Chen, and Charles Lin

FORMOSAT-7/COSMIC-2 (F7/C2), with the mission orbit of 550 km altitude, 24-deg inclination, and a period of 97 minutes, was launched on June 25, 2019.  Tri-GNSS Radio occultation (RO) receiver System (TGRS), Ion Velocity Meter (IVM), and RF Beacon (RFB) onboard F7/C2 six small satellites allow scientists to three-dimensionally observe the plasma structure and dynamics in the mid-latitude, low-latitude, and equatorial ionosphere.  Measurements of F7/C2 RO as well as the IVM ion density, ion temperature, and ion velocity have a better understanding on mechanisms of the plasma depletion bays, non-migrating tides, and scintillations.  Moreover, observations of ionospheric F7/C2 RO electron density profiles and the total electron content derived from global ground-based GNSS receivers are used to carry out ionospheric weather monitoring, nowcast, and forecast for positioning, navigation, and communication application.

How to cite: Chang, F.-Y., Liu, J.-Y., Lin, C.-Y., Chen, S.-P., and Lin, C.: Ionospheric Weather Observations of FORMOSAT-7/COSMIC-2, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-21810, https://doi.org/10.5194/egusphere-egu2020-21810, 2020.

EGU2020-17905 | Displays | ST4.3 | Highlight

The next generation of IGS ROTI Maps: an extension toward global coverage

Andrzej Krankowski, Iurii Cherniak, Irina Zakharenkova, Adam Fron, and Kacper Kotulak

The International GNSS Service (IGS) has accepted for official release a new ionospheric product for specification of ionospheric irregularities occurrence and intensity over the Northern Hemisphere as derived from multi-site ground-based GPS observations. Initially, we focused on the Northern Hemisphere auroral and midlatitude regions because of the highest concentration of the GNSS users and user supporting permanent networks located within the American, European, and Asian sectors. The IGS ROTI maps product is routinely generated by multi-step processing of carrier phase delays in dual-frequency GPS signals and transferred to the IGS CDDIS database. Now, ROTI maps allow regular monitoring of ionospheric irregularities over the Northern Hemisphere and provide information about past events when strong ionospheric irregularities developed here.

Obviously, the plasma irregularities that occur at high, middle, and low latitudes have different physical mechanisms of their origin and development. For study of the climatological features of ionospheric irregularities occurrence, investigation of the ionospheric responses for Space Weather drivers, processes derived from below, this actual ROTI Map product is required to cover low latitudes and the Southern hemisphere polar and midlatitudes.

During last decade, numerous ground-based permanent receivers were deployed within the global and regional networks and these observations are publicly available. These data can support our activity toward extending the current IGS ROTI maps product for a global coverage. In this paper, we present initial results of ROTI maps product performance to characterize ionospheric irregularities exited by different types of geophysical processes and space weather events. The next generation of the IGS ROTI maps product can be a valuable tool for global ionospheric irregularities monitoring and retrospective analysis of plasma irregularities impact on the GNSS positioning in the “worst case scenario” domain.

The research is supported by the National Science Centre, Poland, through grants 2017/25/B/ST10/00479 and 2017/27/B/ST10/02190 and the National Centre for Research and Development, Poland, through grant DWM/PL-CHN/97/2019

 

Keywords: GPS, ionosphere, ionospheric irregularities, ROTI, IGS

How to cite: Krankowski, A., Cherniak, I., Zakharenkova, I., Fron, A., and Kotulak, K.: The next generation of IGS ROTI Maps: an extension toward global coverage, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-17905, https://doi.org/10.5194/egusphere-egu2020-17905, 2020.

In this study, we assess the hourly variations of the three-dimensional proton flux distribution inside the South Atlantic Anomaly (SAA) during a geomagnetic storm. We have developed a relativistic three-dimensional guiding center test particle simulation code in order to compute the proton trajectories in a time-varying magnetic field background provided by Tsyganenko model TS05 and the corresponding time-varying inductive electric field. The Dst index is the main input parameter to the simulation model, while the maximum proton flux, the area of the SAA calculated below a selected threshold, and the penetration depth of the protons are the main output variables investigated in this study were. Since the LEO spacecraft and human-related activities are already affected by space weather conditions, the South Atlantic Anomaly (SAA) is also believed to create an additional source of risk. As the radiation environment depends essentially on the particle flux, the objective of this study is to estimate quantitatively the proton flux variations inside the South Atlantic Anomaly (SAA) in quiet and in storm conditions. So far, it was found that after several drift periods, the protons in the South Atlantic Anomaly (SAA) could penetrate to lower altitudes during geomagnetic storm event, and that, the SAA maximum flux value and the corresponding area, varied differently with respect to altitudes. Numerical results were compared with observations by NOAA 17 and RD3R2 instrument mounted on International Space Station (ISS).

How to cite: Girgis, K., Hada, T., and Matsukiyo, S.: Space Weather Effects on Proton Flux Variations in the South Atlantic Anomaly: A Numerical Study performed by Test Particle Simulations, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1551, https://doi.org/10.5194/egusphere-egu2020-1551, 2020.

EGU2020-1562 | Displays | ST4.3

An unusual observation of a plasma structure in the mid-latitude ionosphere

Alan Wood, Gareth Dorrian, and Richard Fallows

The LOFAR (Low Frequency Array) is one of the world’s leading radio telescopes, operating across the frequency band 10-250 MHz. As radio waves from astronomical sources pass through the ionosphere, they can undergo refraction and/or diffraction. The variations in the intensity of the received signal are caused by irregularities with a spatial scale size ranging from the Fresnel dimension to an order of magnitude below this value. The received signal can therefore be used to infer information on plasma structures in the ionosphere. As the frequencies used are significantly lower than the 1.4 GHz typically associated with Global Navigation Satellite Systems (GNSS), the plasma structures that affect the signals received by LOFAR are significantly larger, typically of the order of kilometres.

On 14th July 2018 the Dutch stations of LOFAR observed the strong natural radio sources Cassiopeia A and Cygnus A between 17:00 UT and 18:05 UT at a frequency range of 20-80 MHz. During the observation, the signal intensity received by many of the stations underwent a substantial reduction across all frequencies, lasting approximately 10 minutes. Immediately before and after this, periodic enhancements in the signal strength were observed. These enhancements showed a noticeable frequency dependence, with longer period oscillations at lower frequencies. The feature was not observed simultaneously by the stations and evolved during the observations. Such a feature is most likely to be the result of a large-scale density structure in the ionosphere, which appears to move west and north over the northern Netherlands.

The deep fading of the received signal may be due to the presence of sporadic-E, which is a consequence of variations in the neutral wind speed with altitude in the presence of the geomagnetic field, resulting in plasma accumulating in a thin layer. This can cause incident radio waves to be strongly refracted, affecting the strength of the received signal. The wave-like structure immediately before and after the deep fade is a likely consequence of scattering of the observed signal.

How to cite: Wood, A., Dorrian, G., and Fallows, R.: An unusual observation of a plasma structure in the mid-latitude ionosphere, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-1562, https://doi.org/10.5194/egusphere-egu2020-1562, 2020.

Telluric currents are the natural phenomena especially pronounced in the high latitude areas (above 60 degrees). These currents, as any stray current, are able to interfere with pipeline cathodic protection systems, and came into wide consideration with construction of pipelines in northern areas, where the geomagnetic variations are more severe and last for prolonged times.

The paper will explain the approach developed for estimation of pipeline corrosion rates due to telluric activity, and results of its applications.

Statistical evaluation of the occurrence rates for the pipe-to-soil potential difference values based on modelling of the pipeline response to the geomagnetic activity in two different locations (high latitude and mid-latitude) will be combined with the method developed for calculation of corrosion rate (metal loss). The presented approach and results of its application to different types of pipelines located at different latitudes can be used as a practical guidance for the assessments of the space weather impacts on pipeline operations.

How to cite: Trichtchenko, L.: Evaluation of pipeline corrosion rates due to enhanced telluric activity associated with space weather , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-3747, https://doi.org/10.5194/egusphere-egu2020-3747, 2020.

EGU2020-8326 | Displays | ST4.3

Geoeffectiveness of the ‘Battle of Grunwald day’ in 2012

Agnieszka Gil, Renata Modzelewska, Szczepan Moskwa, Agnieszka Siluszyk, Marek Siluszyk, and Anna Wawrzynczak

During the solar activity cycle 24, which started at the end of 2008, Sun was behaving silently and there were not many spectacular geoeffective events. Here we analyze the geomagnetic storm which happened on July 15 of 2012 in the 602 anniversary of the famous Polish Battle of Grunwald. According to the NOAA scale, it was G3 geomagnetic storm with Bz heliospheric magnetic field component dropping up to -20 nT, Dst index below -130 nT, AE index greater than 1300 nT and ap index being above 130 nT. It was proceeded by the solar flare of X1.4 class on 12 of July. This geomagnetic storm was accompanied by the fast halo coronal mass ejection 16:48:05 on 12 of July-the first C2 appearance, with the apparent speed 885 km/s and space speed 1405 km/s. This geomagnetic storm was classified as the fourth of the strongest geomagnetic storms from SC 24. Around that time in Polish electric transmission lines infrastructure, there was observed a significant growth of the number of failures that might be of solar origin.

Acknowledgments: the Polish National Science Centre, grant number 2016/22/E/HS5/00406.

How to cite: Gil, A., Modzelewska, R., Moskwa, S., Siluszyk, A., Siluszyk, M., and Wawrzynczak, A.: Geoeffectiveness of the ‘Battle of Grunwald day’ in 2012, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-8326, https://doi.org/10.5194/egusphere-egu2020-8326, 2020.

EGU2020-8427 | Displays | ST4.3

Influence of seasonal changes on the mid-latitude trough properties

Barbara Matyjasiak, Dorota Przepiórka, and Hanna Rothkaehl

 

How to cite: Matyjasiak, B., Przepiórka, D., and Rothkaehl, H.: Influence of seasonal changes on the mid-latitude trough properties, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-8427, https://doi.org/10.5194/egusphere-egu2020-8427, 2020.

EGU2020-8604 | Displays | ST4.3

Sensing Ionospheric Turbulence Using GNSS

Giulio Tagliaferro, Andrea Gatti, and Eugenio Realini

Electron density in ionospheric plasma exhibits fluctuations and irregularities in time and space, at several scales. Plasma, being ionized gas, is subject to a turbulent behaviour similar to that observed in fluid dynamics, with two main distinctions: a) its dynamics are coupled with electromagnetic fields; b) collisions of particles are rare. These unique properties characterize the inertial range of ionospheric plasma turbulence, which represents the energy cascade from large-scale structures (e.g. travelling ionospheric disturbances) to small-scale ones (eddies) until energy dissipation occurs. 

Kolmogorov power law would predict a spectrum of 8/3 and equivalently a structure function with a power law of 5/3 for a phase signal crossing a 3D turbulent medium. However, the previous investigation of spatial structure characteristic of the ionosphere using LOFAR array observed a power law of around 1.9 in the spatial domain. In this study, we investigate the spatio-temporal and temporal structure of the ionosphere using structure function of GNSS phase geometry free signals from both medium earth orbit satellites and geostationary ones. We found two regimes, one compatible the 5/3 Kolmogorov theory and one obeying a 2 power law. We propose an interpretation for the two regimes, the first being a 3D turbulent flow driven by local instabilities, and the second one being driven by solar radiation-induced ionization and successive recombination. The second spectrum obeys a power law of 2, that is the power spectrum of a sinusoidal function like the local sun elevation. By using receivers at almost constant solar irradiance located in polar regions, we further observe the turbulent regimes also in spatio-temporal structure function.

How to cite: Tagliaferro, G., Gatti, A., and Realini, E.: Sensing Ionospheric Turbulence Using GNSS, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-8604, https://doi.org/10.5194/egusphere-egu2020-8604, 2020.

EGU2020-9763 | Displays | ST4.3

Long-term monitoring of neutron component of radiation background onboard International Space Station.

Maxim Litvak, Dmitry Golovin, Alexander Kozyrev, Igor Mitrofanov, and Anton Sanin

The Board Telescope of Neutrons (BTN) is a neutron spectrometer which was installed outside of the Russian “Zvezda” module of the International Space Station (ISS) in November 2006. The main goals of this experiment include measurement of neutron flux in broad energy band from low epithermal neutrons (>0.4 eV) up to fast neutrons (<15 MeV); investigation of its spatial variations at low and high geomagnetic latitudes above the South Atlantic anomaly (SAA) and at different orbital altitudes; observations of  GCR variations on different time scales from orbital fluctuations to variations affected by the 11-year solar cycle; estimation of the neutron component of radiation background outside ISS during various flight conditions in near-Earth orbit.

In this study we present measurements of neutron-flux spectral density in the vicinity of the International Space Station (ISS) based on BTN-Neutron space experimental data for the period 2007-2019. Neutron flux shows space and time variations. It varies by several orders of magnitude between equatorial latitudes and flybys across South Atlantic anomaly region. The time profile of neutron flux also demonstrates long-periodic variations produced by variations of GCRs and modulated by 11 year solar cycle. The observed amplitude of such variations is about two times. We have compared it with other space neutron monitors installed on Moon (NASA/LRO), Mars (NASA/Odyssey, ESA/ExoMars)and Mercury (ESA/BepiColombo) missions.   

We also used neutron measurements to evaluate biological impact contributed by neutrons and expressed in neutron equivalent dose rate.  

How to cite: Litvak, M., Golovin, D., Kozyrev, A., Mitrofanov, I., and Sanin, A.: Long-term monitoring of neutron component of radiation background onboard International Space Station., EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-9763, https://doi.org/10.5194/egusphere-egu2020-9763, 2020.

EGU2020-10821 | Displays | ST4.3 | Highlight

Solar induced earthquakes – review and new results

Sergey Pulinets and Galina Khachikyan

A lot of information has been accumulated recently demonstrating impacts of solar activity on the Earth’s seismicity. We observe the transition from correlation-driven papers to the more physical based works. The effects of solar influence could be separated by agents of energy transfer which could be electromagnetic emission of the Sun, particle fluxes of solar wind, solar proton events, modification of radiation belts and indirect impacts through the intermediate agent, such as atmosphere disturbances and modification of atmosphere circulation as effect of solar activity. Effects of the galactic cosmic rays should be taken into account including the Forbush decreases, which are result of geomagnetic storms. MHD electromagnetic sounding stimulating the earthquake activity could be considered as a physical model of the geomagnetic storms effect on the seismic activity.

The most intriguing effects discovered recently is the inducing the strong M>7 earthquakes by the precipitation from additional radiation belt at L-shell 1.5-1.8 formed after the strong geomagnetic storm. Precipitation of relativistic particles from this shell induces the strong earthquakes with delay nearly 2 months.

One very importing agent of geosphere coupling including the energy transfer int the lithosphere is the Global Electric Circuite.

It is difficult to explain the observed phenomena by simple transformation of solar energy into mechanical deformation, it seems that more plausible explanation is the pumping of energy into the Earth’s crust volume being in a metastable state.

This work was supported by the Ministry of Education and Science of the Russian Federation in accordance with Subsidy Agreement No. 05.585.21.0008. The unique identifier is RFMEFI58519X0008

How to cite: Pulinets, S. and Khachikyan, G.: Solar induced earthquakes – review and new results, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-10821, https://doi.org/10.5194/egusphere-egu2020-10821, 2020.

EGU2020-12964 | Displays | ST4.3

The effects of solar activity on the Global Atmospheric Electrical Circuit

Marzieh Khansari, Eija Tanskanen, and Shabnam Nikbakhsh

The global electric circuit (GEC) links the electric field and current flowing in the lower atmosphere, ionosphere and magnetosphere forming a giant spherical condenser, which is charged by the thunderstorms to a potential of several hundred thousand volts (Roble and Tzur, 1986) and drives vertical current through the atmosphere’s columnar resistance. Monitoring and researching the global electric circuit (GEC) are crucially important due to its links with climate change. Those two phenomena are connected by lightning activity, which itself is a measure of the GEC. It is known that space weather affects the Earth’s lightning activity, therefore the GEC might prove to be a critical tool in examining changing climate in terms of solar and lightning activity.

The possible relation between solar activity and lightning activity has been studied for a long period of time. The relation between sunspot number and lightning activity has been investigated, although the results still remain inconclusive across regions and time. At some regions a positive correlation is found, at others a negative one. Thus, it is important to explore other solar-geomagnetic variables possibly influencing lightning activity, such as geomagnetic index or fast solar wind streams, which were found to correlate well with lightning activity (Scott et al, 2014). Another increasingly important question is whether or not aerosols will contribute significantly to the Earth’s radiation budget, whether it be cooling or warming the climate. In a warming climate aerosol loading could alter and increase lightning activity, which in turn can lead to a positive feedback due to generation of NOx and thus O3 in the troposphere, a potent greenhouse gas.

In this project we will look at the connection between solar activity, aerosol loading, and thunderstorm activity in different types of regions such as coastal, boreal forest and urban area first in Finland and later on globally.

 

  1. Aniol, R., 1952. Schwankungen der Gewitterha

How to cite: Khansari, M., Tanskanen, E., and Nikbakhsh, S.: The effects of solar activity on the Global Atmospheric Electrical Circuit , EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-12964, https://doi.org/10.5194/egusphere-egu2020-12964, 2020.

EGU2020-12999 | Displays | ST4.3

Characterizing Ionospheric Disturbances for Space Weather Hazard Mitigation

Susan Skone, Maryam Najmafshar, and Gary Bust

The world relies increasingly on capabilities that are enabled or delivered by space-based systems, and there exists a need to continually refine our vulnerability assessment models and understanding of natural versus artificial threats. One area of growing global focus is monitoring and mitigating hazards for space-based systems that are highly dependent on the space atmospheric environment. For example, in 2018 the United States defined benchmarks for five space weather phenomena critical to vulnerability assessment for national infrastructure and services, and for stakeholder mitigation planning. We were invited to lead the next-phase national working group in benchmarking of ionospheric disturbances to capture physical properties of the medium and response to solar drivers; key parameters include ionospheric electron content, turbulence, and absorption that characterize the medium for radio propagation. All such values translate readily into impacts on existing and emerging technologies for users/operators.

In this context we present new methods of ionospheric characterization and parameterization to gain insight into the impact on ground- and space-based RF systems. Our approach exploits the University of Calgary Transition Region Explorer (TREx) network for geospace sensing – a federal investment in over 40 sophisticated optical, magnetic and radio instruments across Canada. Combined with our modeling tools, this is one of the world’s foremost high latitude facilities for remote sensing of the near-earth space environment. On track to be fully operational in 2020, our ground-based infrastructure includes new technologies in auroral cameras and imaging riometers. At distributed key locations within the target region, multi-constellation Global Navigation Satellite System (GNSS) total electron content (TEC)/scintillation receivers and commercial grade systems also provide multi-scale scientific observations.

We present space weather monitoring for ground-based and space-based RF systems. Our ionosphere modeling capabilities include a data driven approach to estimate the three-dimensional temporally evolving electron density distributions over regional spatial scales. Input observations can include integrated TEC for multi-constellation GNSS signals from ground-based receivers, topside over-satellite TEC from space-borne GNSS receivers (e.g. Swarm), and GNSS occulting link TEC from low-earth orbiters. We also exploit small-scale Swarm in situ plasma density observations to estimate ionospheric turbulence. We focus on two recent studies:

1) The assimilation of imaging riometer observations to provide D-region specification and estimation of key space weather parameters for HF applications.

2) Ionospheric scintillation modeling based on turbulence key parameters for transionospheric RF signal propagation and related applications such as GNSS.

Outcomes include new approaches in space situational awareness and monitoring of space environmental conditions with improved anomaly resolution (distinguishing artificial from natural hazards) and informed mitigation.

How to cite: Skone, S., Najmafshar, M., and Bust, G.: Characterizing Ionospheric Disturbances for Space Weather Hazard Mitigation, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-12999, https://doi.org/10.5194/egusphere-egu2020-12999, 2020.

EGU2020-14948 | Displays | ST4.3

LOFAR4SpaceWeather (LOFAR4SW) – Increasing European Space-Weather Capability with Europe’s Largest Radio Telescope: Beyond the Detailed Design Review (DDR)

Mario M. Bisi, Mark Ruiter, Richard A. Fallows, René Vermeulen, Stuart C. Robertson, Nicole Vilmer, Hanna Rothkaehl, Barbara Matyjasiak, Joris Verbiest, Peter T. Gallagher, Michael Olberg, Tobia Carozzi, Michael Lindqvist, Eoin Carley, Paulus Krüger, Maaijke Mevius, Carla Baldovin, and David Barnes

The Low Frequency Array (LOFAR) is an advanced phased-array radio-telescope system based across Europe.  It is capable of observing over a wide radio bandwidth of ~10-250 MHz at both high spatial and temporal resolutions.  LOFAR has capabilities that enable studies of many aspects of what we class as space weather (from the Sun to the Earth and afar) to be progressed beyond today’s state-of-the-art.   However, with the present setup and organisation behind the operations of the telescope, it can only be used for space-weather campaign studies with limited triggering availability.  This severely limits our ability to effectively use LOFAR to contribute to space-weather monitoring/forecast beyond its core strength of enabling world-leading scientific research.  LOFAR itself is made up of a dense core of 24 stations near Exloo in The Netherlands with an additional 14 stations spread across the northeast Netherlands.  In addition to those, there are a further 13 stations based internationally across Europe.  These international stations are, currently, six in Germany, three in northern Poland, and one each in France, Ireland, Latvia, Sweden, and the UK.  Further sites are under preparations (for example, in Italy).

 

We are undertaking a Horizon 2020 (H2020) INFRADEV design study to undertake investigations into upgrading LOFAR to allow for regular space-weather science/monitoring observations in parallel with normal radio-astronomy/scientific operations.  This project is called the LOFAR For Space Weather (LOFAR4SW) project (see: http://lofar4sw.eu/).  Our work involves all aspects of scientific and engineering work along with end-user and political engagements with various stakeholders.  This is with the full recognition that space weather is a worldwide threat with varying local, regional, continent-wide impacts, and also global impacts – and hence is a global concern.

 

Here, we summarise the most-recent key aspects of the LOFAR4SW progress including outputs/progress following the Detailed Design Review (DDR) that took place at ASTRON, The Netherlands, in March 2020, as well as the implementation of recommendations from the earlier Preliminary Design Review (PDR) with an outlook to the LOFAR4SW User Workshop the week following EGU 2020.  We also aim to briefly summarise a key set of the longer-term goals envisaged for LOFAR to become one of Europe’s most-comprehensive space-weather observing systems capable of shedding new light on several aspects of the space-weather system, from the Sun to the solar wind to Jupiter and Earth’s ionosphere.

How to cite: Bisi, M. M., Ruiter, M., Fallows, R. A., Vermeulen, R., Robertson, S. C., Vilmer, N., Rothkaehl, H., Matyjasiak, B., Verbiest, J., Gallagher, P. T., Olberg, M., Carozzi, T., Lindqvist, M., Carley, E., Krüger, P., Mevius, M., Baldovin, C., and Barnes, D.: LOFAR4SpaceWeather (LOFAR4SW) – Increasing European Space-Weather Capability with Europe’s Largest Radio Telescope: Beyond the Detailed Design Review (DDR), EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-14948, https://doi.org/10.5194/egusphere-egu2020-14948, 2020.

EGU2020-18228 | Displays | ST4.3

Solar activity and its impact on the mid-latitude trough during geomagnetic storms

Dorota Przepiórka, Barbara Matyjasiak, and Hanna Rothkaehl

How to cite: Przepiórka, D., Matyjasiak, B., and Rothkaehl, H.: Solar activity and its impact on the mid-latitude trough during geomagnetic storms, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18228, https://doi.org/10.5194/egusphere-egu2020-18228, 2020.

EGU2020-18287 | Displays | ST4.3

Ionospheric scintillation indexes for LOFAR single station observation mode

Mariusz Pożoga, Marcin Grzesiak, Barbara Matyjasiak, Hanna Rothkaehl, Roman Wronowski, Katarzyna Budzińska, and Łukasz Tomasik

How to cite: Pożoga, M., Grzesiak, M., Matyjasiak, B., Rothkaehl, H., Wronowski, R., Budzińska, K., and Tomasik, Ł.: Ionospheric scintillation indexes for LOFAR single station observation mode, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18287, https://doi.org/10.5194/egusphere-egu2020-18287, 2020.

EGU2020-18465 | Displays | ST4.3

High frequency radio emissions as a manifestation of physical processes in the auroral plasma

Hanna Rothkaehl, Barbara Matyjasiak, Agata Chuchra, Roman Schreiber, Michał Marek, and Dorota Przepiórka

The Earth’s auroral region and its close neighbourhood is the origin of strong radio emissions caused by complex physical plasma processes. Among them we can list auroral hiss, auroral roar, auroral medium frequency (MF) burst, and auroral kilometric radiation (AKR).  Analysis of such emissions can provide information about magnetospheric structure and dynamics. 

In this work we present selected cases of Earth’s AKR-like radio emissions observed by RELEC  and mission at the top side ionosphere leyers. The emissions are seen at frequencies of the order of hundreds of kHz in the ionosphere, just below the auroral oval and  can be observed not only in disturbed geomagnetic conditions, but also during quiet periods. The maximum occurrence is at ∼ 75 ◦ invariant latitude and can have extent up to ∼ 11 ◦ in invariant latitude.

 

How to cite: Rothkaehl, H., Matyjasiak, B., Chuchra, A., Schreiber, R., Marek, M., and Przepiórka, D.: High frequency radio emissions as a manifestation of physical processes in the auroral plasma, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18465, https://doi.org/10.5194/egusphere-egu2020-18465, 2020.

EGU2020-18481 | Displays | ST4.3

Problem ot the energy transfer for radio paths near single-hop limiting distance for low solar activity

Barbara Atamaniuk, Igor V. Krasheninnikov, Alexei Popov, and Barbara Matyjasiak

How to cite: Atamaniuk, B., Krasheninnikov, I. V., Popov, A., and Matyjasiak, B.: Problem ot the energy transfer for radio paths near single-hop limiting distance for low solar activity, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18481, https://doi.org/10.5194/egusphere-egu2020-18481, 2020.

EGU2020-18597 | Displays | ST4.3

Direction of ionospheric structures in LOFAR calibration data

Katarzyna Budzińska, Maaijke Mevius, Marcin Grzesiak, Mariusz Pożoga, Barbara Matyjasiak, and Hanna Rothkaehl

How to cite: Budzińska, K., Mevius, M., Grzesiak, M., Pożoga, M., Matyjasiak, B., and Rothkaehl, H.: Direction of ionospheric structures in LOFAR calibration data, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18597, https://doi.org/10.5194/egusphere-egu2020-18597, 2020.

EGU2020-18662 | Displays | ST4.3

Dome C North radar, a new radar of the SuperDARN network: the first year of observations.

Maria Federica Marcucci, Igino Coco, Stefano Massetti, Simona Longo, David Biondi, Enrico Simeoli, Alessandro Cirioni, Andrea Satta, Angelo De Simone, and Aurélie Marchaudon

In January 2019 the new Super Dual Auroral Radar Network (SuperDARN) radar installed at the Concordia Station in Antarctica and denominated Dome C North (DCN) saw the first light. SuperDARN is an international network of HF radars that observe the effects produced in the ionosphere by the chain of phenomena taking place in the Earth's space environment. DCN and its companion radar Dome C East (DCE) are positioned nearby the southern geomagnetic pole with their Field of View extending towards the auroral latitudes. Here we present the analysis of the first year of observations as a function of the interplanetary conditions.

How to cite: Marcucci, M. F., Coco, I., Massetti, S., Longo, S., Biondi, D., Simeoli, E., Cirioni, A., Satta, A., De Simone, A., and Marchaudon, A.: Dome C North radar, a new radar of the SuperDARN network: the first year of observations., EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-18662, https://doi.org/10.5194/egusphere-egu2020-18662, 2020.

EGU2020-19755 | Displays | ST4.3

Auroral omega bands are a significant cause of large geomagnetically induced currents

Sergey Apatenkov, Vyacheslav Pilipenko, Evgeniy Gordeev, Ari Viljanen, Liisa Juusola, Vladimir Belakhovsky, Yaroslav Sakharov, and Vasily Selivanov

The strongest event of geomagnetically induced currents (GIC) detected by the North-West Russian GIC network occurred during the main phase of the magnetic storm on June 28-29, 2013. Extremely high values, 120 A, were recorded in the 330 kV transformers on Kola Peninsula in the 04--07 magnetic local time (MLT) sector. The Defense Meteorological Satellite Program (DMSP) spacecraft took a sequence of ultraviolet (UV) auroral images in the southern hemisphere and observed multiple omega bands. The ionospheric equivalent electric currents based on the International Monitor for Auroral Geomagnetic Effects (IMAGE) magnetometer network reveal a sequence of current vortex pairs moving eastward with the speed of 0.5-2.5 km/s, that fits to the electrodynamics scheme of omega bands. Although the temporal variations of the associated current system are slow, the omega bands can be responsible for strong magnetic variations and GIC due to fast propagations of currents in the azimuthal direction.  The first steps towards the statistica study of the highest GIC recorded at Vykhodnoy transformer show that about 50% of events have properties similar to the comprehensively studied 29 June 2013 case.

How to cite: Apatenkov, S., Pilipenko, V., Gordeev, E., Viljanen, A., Juusola, L., Belakhovsky, V., Sakharov, Y., and Selivanov, V.: Auroral omega bands are a significant cause of large geomagnetically induced currents, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-19755, https://doi.org/10.5194/egusphere-egu2020-19755, 2020.

EGU2020-22231 | Displays | ST4.3 | Highlight

Space Weather in the UK: Updates on the UK Strategy, Investment, and International Engagements

Mario M. Bisi, Mark Gibbs, Mike A. Hapgood, Mike Willis, Richard A. Harrison, Simon Machin, and Ian W. McCrea

For the UK, the potential impacts from severe space weather (and everyday space weather) are considered of a high importance and hence the UK Government has included “Severe Space Weather” on its National Risk Register of Civil Emergencies since 2011.  This is not just considering direct impacts on UK infrastructures, but also impacts to key partner/trading/neighbouring nations.  This has led to a long series of national and international engagements and strategic developments both between UK agencies/entities and with international agencies/organisations (such as ESA, NOAA, NASA, COSPAR, ISES, ICAO, WMO, and UN COPUOS).  On top of this, the UK has undertaken a series of wide-ranging investigations to mitigate space-weather impacts at the national level including the ongoing development of a national Space Weather Strategy – where the UK looks to experts across all sectors to feed into its development.

 

An essential aspect of trying to mitigate space-weather impacts on the UK is the need for independent UK space-weather forecast capability in collaboration with the other 24/7 space-weather forecasting institutes around the World.  This UK capability allows for direct advice to government on all things space weather, particularly on what to do when an impending event is expected and throughout its duration and recovery.  Hence, he setting up of a UK staffed 24/7 space-weather forecasting centre at the Met Office alongside the formation of the Space Environment Impacts Expert Group (SEIEG) of experts were undertaken to provide the necessary advice to government.

 

The UK is currently committing a large amount of money both to dedicated UK-based and ESA-based space weather programmes as well as through traditional science research funding channels.  This includes the UKRI Strategic Priorities Fund (SPF) Space Weather Instrumentation, Measurement, Modelling and Risk (SWIMMR) programme and the ESA Space Safety Programme.  The UK has also taken a lead on several other space-/ground-based space-weather endeavours that are proving highly complementary to current UK and global capabilities.

 

In this presentation, we will provide an overview of the above along with any outline of the UK Space Weather Strategy open to the public at the time of the EGU 2020 Meeting.

How to cite: Bisi, M. M., Gibbs, M., Hapgood, M. A., Willis, M., Harrison, R. A., Machin, S., and McCrea, I. W.: Space Weather in the UK: Updates on the UK Strategy, Investment, and International Engagements, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-22231, https://doi.org/10.5194/egusphere-egu2020-22231, 2020.

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