日本地球惑星科学連合2015年大会

講演情報

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26日(火) 09:00 〜 10:45 302 (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:塩川 和夫(名古屋大学太陽地球環境研究所)

09:15 〜 09:30

[PEM07-33] ひので衛星とSDO衛星から迫る太陽表面における磁場輸送

*飯田 佑輔1堀田 英之2 (1.JAXA、2.HAO)

キーワード:太陽, 対流, 磁場, 拡散

Since magnetic field on the solar surface triggers various solar activities, it is very important to understand their structure in terms of the space weather. An important issue is transport mechanism of magnetic flux. It is thought that the flow dominates the magnetic field on the solar surface. Although the transport is treated as a pure diffusion process for long time, recent solar observations suggest the differences from the diffusion.

We reported the relationship between the travel distance of the magnetic flux concentration and the elapsed time from the birth of the concentrations. The sub-diffusion scaling was found in the time range longer than 2x104 seconds for the first time. The investigation is, however, limited because the analysis is done by using the magnetogram obtained by Solar Optical Telescope onboard the Hinode satellite (Hinode/SOT), which does NOT cover the whole Sun. Thus in this study we investigate the relationship with the Helioseismic and Magnetic Imager on board the Solar Dynamics Observatory (SDO/HMI), which covers the whole Sun. Since the spatial resolution of SDO/HMI is lower than that of Hinode/SOT, we use both telescopes in order to see the influence of the resolution on the analysis. We find the similar sub-diffusion scaling with the power law index of 0.7 ± 0.1. SDO/HMI shows a slightly larger magnitude. This difference may come from the difference of spatial resolution between the telescopes. In the presentation, we also plan to show the 3D MHD simulation of the magneto-convection if time permits.