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_1AM2] 惑星大気圏・電磁圏

2014年5月1日(木) 11:00 〜 12:45 423 (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:今村 剛(宇宙航空研究開発機構 宇宙科学研究本部)

12:30 〜 12:45

[PCG38-14] ひさき衛星とハッブル宇宙望遠鏡の協調観測で明らかになった木星の自励的オーロラ加速

*木村 智樹1垰 千尋2Badman Sarah3吉岡 和夫1村上 豪1山崎 敦1土屋 史紀4藤本 正樹1 (1.宇宙航空研究開発機構宇宙科学研究所、2.IRAP, Fance、3.Lancaster University、4.東北大学)

キーワード:ひさき衛星, ハッブル宇宙望遠鏡, 木星, オーロラ

Two possible drivers have been proposed for planetary auroral acceleration processes: magnetosphere-solar wind interaction referred to as an 'external driver' and shear flow of magnetospheric plasma around a planet referred to as an 'internal driver'. Recent observations of Jupiter's aurora indicated significant responses of auroral intensity and morphology to the solar wind. These results are suggestive of the 'external driver' for Jupiter. On the other hand, there have not been reported dynamics of the 'internal driver' for Jupiter yet which should be essential because of Jupiter's fast rotation and internal plasma source Io. Here we firstly report dynamics of the 'internal driver' based on long-term continuous observation of extreme ultraviolet (EUV) aurora by Hisaki satellite. The long-term variations in EUV aurora are compared with solar wind extrapolated from Earth's orbit by numerical simulation. We found dramatical brightening and decay of EUV aurora during the solar wind quiet period. The brightening occurs once every a few days followed by sudden decay with a timescale less than a half of rotation (~5 hours), which is significantly faster than the solar wind daily variations. Highly-resolved auroral imaging by Hubble Space Telescope captured expansion of diffuse aurora down to latitudes of Io's footprint aurora during the brightening. These observations are indicative of hot plasma deeply injected into the inner magnetosphere around Io's orbit independently from the solar wind, followed by rapid energy dissipation through auroral emissions and possibly other radiation and/or chemical processes.