EGU25-5458, updated on 14 Mar 2025
https://doi.org/10.5194/egusphere-egu25-5458
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Oral | Wednesday, 30 Apr, 08:35–08:45 (CEST)
 
Room 0.94/95
Arase Observations of the Radiation Belts During the May 2024 Geomagnetic Storm
Yoshizumi Miyoshi1, Iku Shinohara2, Takeshi Takashima2, Kazushi Asamura2, Takefumi Mitani2, Nana Higashio2, Satoshi Kasahara3, Shoichiro Yokota4, Ryuho Kataoka, Sandeep Kumar6, Tomoaki Hori1, Satoshi Kurita7, Shoya Matsuda8, Yuto Katoh9, Yoshiya Kasahara8, Fuminori Tsuchiya9, Atsushi Kumamoto9, Atsuki Shinbori1, Ayako Matsuoka7, Naritoshi Kitamura1, and the ERG Project Team*
Yoshizumi Miyoshi et al.
  • 1Nagoya University, Institute for Space-Earth Environmental Research, Nagoya, Japan (miyoshi@isee.nagoya-u.ac.jp)
  • 2JAXA, Japan
  • 3University of Tokyo, Japan
  • 4Osaka University, Japan
  • 6NASA, US
  • 7Kyoto University, Japan
  • 8Kanazawa University, Japan
  • 9Tohoku University, Japan
  • *A full list of authors appears at the end of the abstract

During the largest geomagnetic storm of Solar Cycle 25 that happened in May 2024, the Arase satellite has successfully operated all instruments and observed a number of remarkable phenomena in the inner magnetosphere and radiation belts. Due to significant compression of the magnetosphere caused by an interplanetary shock, the satellite's apogee was located outside the magnetosphere, indicating a substantial degree of compression. Following the main phase of the storm, a rapid flux increase of high-energy electrons with energies of several MeV was observed in the region of L < 3. This was the largest flux increase event recorded ever since the launch of the Arase satellite.

Additionally, the plasmasphere contracted inward more than usual, with the plasmapause reaching L ~ 2. The enhanced flux of high-energy electrons at L < 3 persisted for an extended period of 10 to 30 days or even more, significantly changing the radiation environment near the Earth. Analyzing observation data from the Arase satellite, we estimated the decay time constant of the electrons and compared it with the rates of pitch-angle scattering  caused by various plasma waves, such as hiss waves, VLF transmitters, and lightning whistlers. The results suggest that continuous scattering driven by plasmaspheric hiss primarily governs the decay of those high-energy electrons. In this presentation, we report on the variations in the radiation belts and inner magnetosphere observed by the Arase satellite during this historic geomagnetic storm.

 

ERG Project Team:

Kunihiro Keika, Yoichi Kazama, S.-W. Wang, C-W Jun, SHREEDEVI, P. R., Mariko Teramoto, Kazuhiro Yamamoto

How to cite: Miyoshi, Y., Shinohara, I., Takashima, T., Asamura, K., Mitani, T., Higashio, N., Kasahara, S., Yokota, S., Kataoka, R., Kumar, S., Hori, T., Kurita, S., Matsuda, S., Katoh, Y., Kasahara, Y., Tsuchiya, F., Kumamoto, A., Shinbori, A., Matsuoka, A., and Kitamura, N. and the ERG Project Team: Arase Observations of the Radiation Belts During the May 2024 Geomagnetic Storm, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-5458, https://doi.org/10.5194/egusphere-egu25-5458, 2025.