日本地球惑星科学連合2014年大会

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セッション記号 P (宇宙惑星科学) » P-CG 宇宙惑星科学複合領域・一般

[P-CG38_1PM2] 惑星大気圏・電磁圏

2014年5月1日(木) 16:15 〜 18:00 423 (4F)

コンビーナ:*今村 剛(宇宙航空研究開発機構 宇宙科学研究本部)、関 華奈子(名古屋大学太陽地球環境研究所)、高橋 幸弘(北海道大学・大学院理学院・宇宙理学専攻)、高橋 芳幸(惑星科学研究センター)、深沢 圭一郎(九州大学情報基盤研究開発センター)、中川 広務(東北大学 大学院理学研究科 地球物理学専攻太陽惑星空間物理学講座 惑星大気物理学分野)、座長:中川 広務(東北大学 大学院理学研究科 地球物理学専攻太陽惑星空間物理学講座 惑星大気物理学分野)

16:30 〜 16:45

[PCG38-23] カッシーニ探査機の太陽風データを利用したMHDシミュレーションによる磁気圏対流、オーロラ発光の関係

*深沢 圭一郎1WALKER Raymond J.2ERIKSSON Stefan3 (1.九州大学情報基盤研究開発センター、2.UCLA, IGPP、3.Laboratory for Atmospheric and Space Physics, University of Colorado at Boulder)

In a series of our simulation studies we have reported that vortices formed at Saturn's dawn magnetopause in simulations when IMF was northward. We interpreted these vortices as resulting from the Kelvin Helmholtz (K-H) instability. In addition, thanks to the recent developments of computer performance, we have been able to perform the high resolution global MHD simulations of the Kronian magnetosphere. In these simulations we obtained the signature of the field-aligned currents from the K-H vortices in Saturn's auroral ionosphere and found small patchy regions of upward field-aligned current which may be related to auroral emissions. These patchy aurorae resembling our results have been reported from Cassini observations. In our previous simulations we used the constant and simple solar wind conditions to understand the basic behavior of Kronian magnetosphere. In this study we have used Cassini observations of the solar wind upstream of Saturn to drive a simulation. Using these solar wind data we simulated the Kronian magnetosphere from 2008-02-12/14:00:31 to 2008-02-13/01:59:31 when the Hubble Space Telescope (HST) observed the Kronian UV auroral emissions. In these solar wind conditions there are several enhancement of the solar wind dynamic pressure (shock) and polarity reversal in the IMF components. From these simulation the shape and convection of Kronian magnetosphere dynamically changed according to the variation of dynamic pressure and IMF directions. As the results, layered convection formed between the corotation region and magnetopause. Furthermore these convection interacted each other, then the large vortex configurations appeared. The calculated configuration of field aligned currents from the simulation also showed the layered and patchy distributions. In addition the upward field aligned current appeared in the dawn side mainly which resembles the configuration of auroral emission by HST.