日本地球惑星科学連合2019年大会

講演情報

[E] 口頭発表

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] 内部磁気圏

2019年5月29日(水) 10:45 〜 12:15 A04 (東京ベイ幕張ホール)

コンビーナ:海老原 祐輔(京都大学生存圏研究所)、Danny Summers(Memorial University of Newfoundland)、三好 由純(名古屋大学宇宙地球環境研究所)、齊藤 慎司(名古屋大学 大学院理学研究科)、座長:海老原 祐輔(京都大学生存圏研究所)、Shinji Saito(ISEE, Nagoya University)

11:55 〜 12:10

[PEM13-21] Magnetic field disturbances associated with the magnetic dipolarization observed by Arase (ERG) in the inner magnetosphere

*松岡 彩子1能勢 正仁2三好 由純2篠原 育1寺本 万里子2野村 麗子3藤本 晶子4田中 良昌5篠原 学6笠原 禎也7笠羽 康正8石坂 圭吾9松田 昇也1小路 真史2中川 朋子10Kazama Yoichi11Wang Shiang-Yu11笠原 慧12横田 勝一郎13三谷 烈史1 (1.宇宙航空研究開発機構 宇宙科学研究所、2.名古屋大学 宇宙地球環境研究所、3.国立天文台 RISE月惑星探査検討室、4.九州工業大学 情報工学部、5.国立極地研究所、6.鹿児島工業高等専門学校、7.金沢大学 総合メディア基盤センター、8.東北大学 惑星プラズマ・大気研究センター、9.富山県立大学 工学部、10.東北工業大学 工学部、11.台湾中央研究院、12.東京大学 大学院理学系研究科、13.大阪大学 大学院理学研究科)

キーワード:あらせ、磁場、双極子化、アルフベン波

The magneto-hydrodynamic waves propagating in the plasma sheet are recognized to transport substantial energies in the magnetosphere. We investigated magnetic field disturbances of the Alfven waves observed by the Arase spacecraft at about 5 earth-radii distance in the midnight. In the inner plasma sheet Alfven waves were often accompanied by the magnetic dipolarization.
We examined the magnetic disturbances in the plane perpendicular to the ambient magnetic field. In the two events examined in our study, the magnetic field disturbances were linearly polarized and the polarization direction gradually rotated 180 degrees in 200 seconds. It is well interpreted that Arase traversed a magnetic flux tube where torsional Alfven waves propagated. The change of the polarization direction reflected the change of observation location in the flux tube. Torsional-mode is significantly common and natural as the parallel-propagating Alfven wave. It is known that large-scale energy transfer and dissipation of the torsional Alfven waves take place on the solar surface.
Meanwhile, in the boundary plasma sheet adjacent to the lobe, the magnetic field disturbances were linearly polarized again and confined to the dawn-dusk direction. They are interpreted as plane Alfven waves having uniformity in the dawn-dusk direction and propagating obliquely. The kinetic effect of the Alfven waves has been often discussed in previous works in association with the auroral emission at the ionospheric altitude.