日本地球惑星科学連合2015年大会

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インターナショナルセッション(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-EM07] Space Weather, Space Climate, and VarSITI

2015年5月24日(日) 16:15 〜 18:00 302 (3F)

コンビーナ:*片岡 龍峰(国立極地研究所)、海老原 祐輔(京都大学生存圏研究所)、三好 由純(名古屋大学太陽地球環境研究所)、清水 敏文(宇宙航空研究開発機構宇宙科学研究所)、浅井 歩(京都大学宇宙総合学研究ユニット)、陣 英克(情報通信研究機構)、佐藤 達彦(日本原子力研究開発機構)、草野 完也(名古屋大学太陽地球環境研究所)、宮原 ひろ子(武蔵野美術大学造形学部)、中村 卓司(国立極地研究所)、塩川 和夫(名古屋大学太陽地球環境研究所)、伊藤 公紀(横浜国立大学大学院工学研究院)、座長:海老原 祐輔(京都大学生存圏研究所)

17:45 〜 18:00

[PEM07-06] Statistical analyses on the thermal plasma density of the plasmasphere from the Akebono PWS observation

長谷川 周平1、*三好 由純1北村 成寿1桂華 邦裕1小路 真史1熊本 篤志2町田 忍1 (1.名古屋大学太陽地球環境研究所、2.東北大学大学院理学研究科地球物理学専攻)

The plasmasphere is a region of cold and dense plasma surrounding the Earth. The thermal plasma density of the plasmasphere is an important parameter for understanding the dynamics of the radiation belts as well as the inner magnetosphere, because the thermal plasma density controls the wave-dispersion relation, resonance conditions, etc. In this study, we conduct statistical analyses on the variations of the plasmasphere and plasmatrough, using electron density data derived from long-term plasma wave observations by the PWS experiments on board the Akebono satellite. We investigate the solar cycle variations of the thermal plasma density distribution. In deep plasmasphere, the thermal plasma density distributions along the field line do not significantly change during the solar cycle, and their distributions are well modeled as the diffusive equilibrium. On the other hand, the thermal plasma density distributions drastically change during the solar cycle in the outer portion of the plasmasphere. The thermal plasma density distributions are similar to the collisionless model during the solar active periods, while those are similar to the diffusive equilibrium model during the solar quiet periods. We also investigate time variations of the plasmaspheric density distribution during geomagnetic storms driven by CMEs and CIRs with superposed epoch analyses. The zero time corresponds to the minimum of the Dst index. The plasmaspheric density shrinkage depends on the storm amplitudes. The recovery time of the thermal plasma density is significantly different between CME- and CIR-storms. During the recovery phase of CIR-storms, the plamapause does not recover quickly because of prolonged substorm activities during the high-speed steams. The recovery rates of the thermal plasma density depend on the L-shell, which is consistent with the previous studies. We find that the recovery rates of CME-storms are larger than that of CIR-storms.