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-EM 太陽地球系科学・宇宙電磁気学・宇宙環境

[P-EM08_2PM1] Space Weather and Space Climate

2014年5月2日(金) 14:15 〜 16:00 411 (4F)

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)、草野 完也(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)、三好 由純(名古屋大学太陽地球環境研究所)、浅井 歩(京都大学宇宙総合学研究ユニット)、佐藤 達彦(日本原子力研究開発機構)、陣 英克(情報通信研究機構)、伊藤 公紀(横浜国立大学大学院工学研究院)、宮原 ひろ子(武蔵野美術大学造形学部)、座長: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)

15:30 〜 15:45

[PEM08-26] MLT and seasonal dependence of auroral electrojets: IMAGE magnetometer network observations

*GUO Jianpeng1LIU Huixin2 (1.SIGMA Weather Group, State Key Laboratory of Space Weather, CSSAR, Chinese Academy of Sciences、2.Department of Earth and Planetary Sciences, Faculty of Sciences, Kyushu University)

Total eastward and westward electrojet currents (EEJ and WEJ) and their central latitudes derived from the IMAGE network magnetic measurements are analyzed for the combined MLT and seasonal dependence during the period 1995-2009. EEJ shows a strong MLT variation with significant dependence on season. During summer months the maxima occur around 1600-1800 MLT, whereas during winter months the maxima occur at a later local time sector around 1800-2000 MLT. Moreover, the summer maxima are much larger than the winter maxima, and appear at higher latitudes. The summer maxima are mainly associated with the solar EUV conductivity effect, while the winter maxima are mainly due to the contribution of northward convective electric field. EEJ exhibits a dominant annual variation with maximum in summer and minimum in winter. WEJ also exhibits a strong MLT variation with significant dependence on season. The maxima occur around 0200-0400 MLT during summer months, around 0000-0200 MLT during winter months, and around 0000-0400 MLT during equinoctial months. Moreover, the equinoctial maxima are much larger than the summer and winter maxima, and appear at relatively lower latitudes. The seasonal variations in WEJ are the combinations of annual variations and semiannual variations. Both annual and semiannual variations show significant dependence on MLT. These results increase our knowledge on what factors contribute to the auroral electrojets as well as their magnetic signatures, and hence help us better understand the limitations of global auroral electrojet indices, such as the AE and SME indices.