日本地球惑星科学連合2024年大会

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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-EM17] 宇宙プラズマ科学

2024年5月30日(木) 13:45 〜 15:15 101 (幕張メッセ国際会議場)

コンビーナ:天野 孝伸(東京大学 地球惑星科学専攻)、三宅 洋平(神戸大学大学院システム情報学研究科)、諌山 翔伍(九州大学総合理工学研究院)、梅田 隆行(北海道大学 情報基盤センター)、座長:天野 孝伸(東京大学 地球惑星科学専攻)、松清 修一(九州大学大学院総合理工学研究院)

14:15 〜 14:30

[PEM17-03] Insights into the Structure of Quasiparallel Shocks from VEX Data.

*Michael A Balikhin1、Michael Gedalin2、Simon N. Walker1 (1.University of Sheffield、2.Ben Gurion University)

キーワード:Collisionless Shock, Venus

Venus does not possess an intrinsic magnetic field. The Venusian ionosphere forms the obstacle within the solar wind flow, resulting in the formation of the Venusian bow shock. The subsolar standoff distance of the Venusian bow shock is much smaller in comparison with the terrestrial bow shock, that results from the interaction between the solar wind and the intrinsic magnetic field of the Earth. This translates into much smaller spatial size of Venusian shock and foreshock. This limits the time for wave growth in the unstable foreshock region. Therefore the Venusian environment is more favourable for observations of the quasiparallel shock front structure that are not masked by high amplitude waves and nonlinear structures such as SLAMS. Here, observations of quasiparallel shock crossings by Venus Express are presented and compared with a two-fluid analytic model of the shock front.