日本地球惑星科学連合2023年大会

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[E] オンラインポスター発表

セッション記号 P (宇宙惑星科学) » P-EM 太陽地球系科学・宇宙電磁気学・宇宙環境

[P-EM13] Dynamics of the Inner Magnetospheric System

2023年5月23日(火) 09:00 〜 10:30 オンラインポスターZoom会場 (1) (オンラインポスター)

コンビーナ:桂華 邦裕(東京大学大学院理学系研究科地球惑星科学専攻)、三好 由純(名古屋大学宇宙地球環境研究所)、Theodore E Sarris(Democritus University of Thrace)、Evan G Thomas(Dartmouth College)

現地ポスター発表開催日時 (2023/5/23 17:15-18:45)

09:00 〜 10:30

[PEM13-P17] Distribution of electron temperature anisotropy in the inner magnetosphere observed by Arase (ERG)

*篠原 育1楊 敬軒、風間 洋一2、Wang Shiang-Yu2笠原 慧3三谷 烈史1浅村 和史1 (1.宇宙航空研究開発機構/宇宙科学研究所、2.Institute of Astronomy and Astrophysics, Academia Sinica、3.東京大学大学院理学系研究科)

キーワード:電子温度異方性、内部磁気圏

Recently, it is becoming apparent that cyclotron acceleration by whistler chorus waves plays an important role in generating relativistic high-energy electrons in the outer radiation belt. Numerical simulations have shown that electrons are accelerated by wave-particle interactions associated with the nonlinear evolution of chorus waves excited near the magnetic equator. It is believed that electron temperature anisotropy is the free energy of chorus wave excitation and is provided by injections from the magnetotail. However, since there are fewer plasma observations in the inner magnetospheric region, the reality of the distribution of the electron temperature anisotropy is not well understood. In this study, we statistically investigate the distribution of temperature anisotropy in the inner magnetospheric region using data obtained from low-energy and medium-energy electron instruments (LEP-e and MEP-e) for a period from March 2017 to December 2019 and compare the results with the stability condition of the temperature anisotropy instability. As a result, we found that the boundary of the temperature anisotropy distribution is consistent with the marginal condition of the instability from the data obtained near the magnetic equator as in the previous study of the RBSP satellite (An et al., 2017) and that the temperature anisotropy tends to be stronger at high latitudes. Furthermore, we also examined the contribution of injections to temperature anisotropy by focusing on data obtained during injection events. However, we could not find a trend of strong temperature anisotropy during the injection events. In this presentation, we will discuss the statistical properties of the distribution of temperature anisotropy in the inner magnetosphere, including these results.