日本地球惑星科学連合2014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-EM09_29PM2] VarSITI - Variability of the Sun and Its Terrestrial Impact

2014年4月29日(火) 16:15 〜 16:45 501 (5F)

コンビーナ:*塩川 和夫(名古屋大学太陽地球環境研究所)、坂尾 太郎(独立行政法人宇宙航空研究開発機構 宇宙科学研究所 太陽系科学研究系)、廣岡 俊彦(九州大学大学院理学研究院地球惑星科学部門)、座長:鈴木 臣(名古屋大学太陽地球環境研究所)、江尻 省(国立極地研究所)

16:15 〜 16:30

[PEM09-43] A Realistic Whole Atmosphere-Ionosphere Modeling and Collaboration with Observations

*陣 英克1三好 勉信2藤原 均3品川 裕之1松尾 朋子4 (1.情報通信研究機構、2.九州大学、3.成蹊大学、4.アメリカ海洋大気庁)

キーワード:電離圏, 熱圏, 大気上下結合, シミュレーション, データ同化, 宇宙天気

There has been an increasing number of collaboration between modeling and observation for the study of upper atmospheric variability and its relation to the lower atmosphere. Observations are used as the forcing inputs to models as well as for their validation. Outputs from models can be useful for the interpretation of observed phenomena owing to their sufficient spatial and temporal coverage, especially for the analysis of phenomena whose effects extend beyond the several atmospheric layers. Recently, we have examined the effects of a prominent stratospheric sudden warming (SSW) in January 2009 on the upper atmospheric variability, by using a whole atmosphere-ionosphere coupled model called GAIA. The model used the meteorological reanalysis data as realistic lower atmospheric forcing, and we compared the model outputs with the satellite observations of upper atmosphere [Jin et al., 2012; Liu et al., 2012]. The comparison suggests that the model can reproduce the overall major features of the observed perturbed variations in the upper atmosphere during the SSW period, which ensures the usage of model output for the detail analysis of vertical coupling mechanism during the event. In this study, we applied the same method for the inclusion of realistic lower atmospheric forcing and carried out a whole atmosphere-ionosphere simulation for longer period. We will show the relation of ionospheric variability to the climatological and irregular variations in the lower atmosphere including several SSW events. Initial results from data assimilation experiment will also be shown as an example of model-observation collaboration.