日本地球惑星科学連合2024年大会

講演情報

[E] 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-EM10] Dynamics of Magnetosphere and Ionosphere

2024年5月27日(月) 17:15 〜 18:45 ポスター会場 (幕張メッセ国際展示場 6ホール)

コンビーナ:今城 峻(京都大学大学院理学研究科附属地磁気世界資料解析センター)、家田 章正(名古屋大学 宇宙地球環境研究所)、佐藤 由佳(日本工業大学)、藤本 晶子(九州工業大学)

17:15 〜 18:45

[PEM10-P01] Multi-spacecraft observations of the magnetosphere and ionosphere under low Alfvén Mach number solar wind

*Masaki N Nishino1Yukinaga Miyashita2,3Motoharu Nowada4Yoshifumi Saito1 (1.Japan Aerospace Exploration Agency, Institute of Space and Astronautical Science、2.Korean Astronomy and Space Science Institute、3.Korea National University of Science and Technology, Department of Astronomy and Space Science、4.Shandong Key Laboratory of Optical Astronomy and Solar-Terrestrial Environment, School of Space Science and Physics, Institute of Space Sciences)

キーワード:Solar wind Alfvén Mach number, Transpolar arc, Multi-satellite observations, Magnetosphere-Ionosphere coupling

The transpolar arcs (TPAs) appear in the auroral oval under the northward interplanetary magnetic field (IMF), sometimes accompanied by the change of the BY sign. Previous statistical studies showed that the solar wind magnetic field strength or the magnetic energy does not affect the occurrence of the TPAs. On the other hand, it has not been studied if the TPAs appear similarly when the solar wind density is very low, and thus, its Alfvén Mach number (MA) is very low (~2-3). Here, we show a case study of multiple TPAs during high MA solar wind observed by DMSP satellites, which was followed by TPA occurrence during very low MA solar wind. The TPA under low MA solar wind is typically single and faint, while multiple TPAs of complicated structures appeared in some cases. In this event, ARTEMIS P1 and P2 were in the mid-distant magnetotail in the same period, and their magnetopause crossings suggest a strong distortion of the magnetotail that might be related to the shape of the TPAs. We discuss the magnetosphere-ionosphere coupling under low MA solar wind and northward IMF based on multi-spacecraft observations.