*Yoshizumi Miyoshi1, Sandeep Kumar2, Satoshi Kurita3, Shinji Saito4, Shoya Matsuda5, Yuto Katoh6, Ryuho Kataoka7, Rui Chen8, Shreedevi Porunakatu Radhakrishna1, Iku Shinohara9, Kazushi Asamura9, Yoichi Kazama10, Shiang-Yu Wang10, Chae-Woo Jun1, Tomoaki Hori1, Satoshi Kasahara11, Shoichiro Yokota12, Kunihiro Keika11, Takefumi Mitani9, Takeshi Takashima9, Nana Higashio9, Yoshiya Kasahara5, Fuminori Tsuchiya13, Atsushi Kumamoto13, Atsuki Shinbori1, Naritoshi Kitamura1, Ayako Matsuoka3, Kazuhiro Yamamoto1, Mariko Teramoto13
(1.Institute for Space-Earth Environmental Research, Nagoya University, 2.NASA/GSFC, 3.Kyoto University, 4.NICT, 5.Kanazawa University, 6.Tohoku University, 7.NIPR, 8.Auburn University, 9.JAXA, 10.ASIAA, 11.University of Tokyo, 12.Osaka University, 13.Kyushu Instituite for Technology)
Keywords:Arase satellite, inner magnetosphere, radiation belts, wave-particle interactions
The Arase satellite has successfully observed the inner magnetosphere for over eight years, providing continuous data on a wide range of electron energy and various plasma waves. We conducted a superposed epoch analysis of electrons at different energies, including source and seed populations, as well as plasma density and plasma waves. The result was sorted as a function of L-shell, magnetic local time (MLT), and storm phase to identify the average variations in these key parameters that contribute to the acceleration of relativistic electrons in the outer radiation belt. The results are consistent with the concept of cross-energy coupling, in which wave-particle interactions play a crucial role. In particular, prolonged substorm activities that drive continuous chorus waves through hot electron flux enhancements are essential for the buildup of relativistic electrons via wave-particle interactions. We also compare these findings with data-driven simulations of the evolution of the electron energy spectrum to discuss potential acceleration mechanisms.