Energy dependence of relativistic electron variations in the outer radiation belt during the recovery phase of magnetic storms: Arase/XEP observations

Tuesday, 6 March 2018
Lakehouse (Hotel Quinta da Marinha)
Nana Higashio1, Kanako Seki2, Yoshizumi Miyoshi3, Mariko Teramoto3, Tomoaki Hori3, Satoshi Kurita3 and Ayako Matsuoka4, (1)JAXA, Tukuba, Japan, (2)The University of Tokyo, Tokyo, Japan, (3)Nagoya University, Nagoya, Japan, (4)ISAS/JAXA, Sagamihara, Japan
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Abstract:
The Arase satellite was launched in December 2016. The extremely high-energy electron experiments(XEP) onboard Arase measures electrons in the energy range of 400 keV - 20 MeV. After the launch, the XEP has observed variations of the relativistic electrons successfully in the inner magnetosphere. There are roughly two candidate processes of electron acceleration. The first one is the adiabatic acceleration due to the radial transport of electrons from the plasma sheet to the inner magnetosphere. Interaction with ultra-low frequency (ULF) waves are a plausible candidate to drive the radial transport. Another acceleration process is the non-adiabatic acceleration of sub-relativistic electrons to the relativistic energies in the heart of the radiation belt. The interaction with very-low frequency (VLF) waves is considered to play an important role in the internal acceleration. One of the science goals of the XEP instrument is to understand the acceleration mechanisms of the relativistic electrons.

In order to investigate the electron acceleration processes, we here focus on three geomagnetic storms occurred on March 27, April 4, May 28, and September 7, 2017, respectively. In these events, relativistic electrons in the outer belt showed a typical time variation, i.e., decrease in the main phase and then increase in the recovery phase. On one hand, the increase rates of the electrons are different between the storms. The March 27 storm, which is caused by the arrival of the high-speed coronal hole stream, accompanies a large increase of the relativistic electrons. The April 4 storm, which has a rapid Dst development and recovery, shows less acceleration and does not recover to the pre-storm level. The May 28 storm is caused by a CME and with moderate increase of the relativistic electrons especially in the small L region (L=[3,4]) . We will report on energy dependence of the increase rate and location of the relativistic electrons during the recovery phase, and their comparison between the three geomagnetic storms. The September 7 storm is a CME and this event is similar to the event on May 28.