日本地球惑星科学連合2016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 M (領域外・複数領域) » M-IS ジョイント

[M-IS03] Interdisciplinary studies on pre-earthquake processes

2016年5月25日(水) 09:00 〜 10:30 304 (3F)

コンビーナ:*服部 克巳(千葉大学大学院理学研究科)、Ouzounov Dimitar(Center of Excellence in Earth Systems Modeling & Observations (CEESMO) , Schmid College of Science & Technology Chapman University, Orange, California, USA)、劉 正彦(国立中央大学太空科学研究所)、Huang Qinghua(Department of Geophysics, Peking University)、座長:劉 正彦(国立中央大学太空科学研究所)、Huang Qinghua(Department of Geophysics, Peking University)

10:15 〜 10:30

[MIS03-06] Spatiotemporal characteristics of the geomagnetic diurnal variation anomalies prior to the 2011 Tohoku earthquake (Mw9.0)

★招待講演

*Han Peng1,3Hattori Katsumi1Huang Qinghua2 (1.Department of Earth Sciences, Graduate School of Science, Chiba University、2.Department of Geophysics, School of Earth and Space Sciences, Peking University, Beijing, China、3.Institute of Statistical Mathematics, Tokyo, Japan)

キーワード:seismo-magnetic phenomena, anomalous geomagnetic diurnal variation, coupling of multiple pre-earthquake phenomena, the Tohoku earthquake

Xu et al., 2013 and Han et al., 2015 have reported unusual behaviors of geomagnetic diurnal variation (GDV) in the vertical component prior to the 2011 off the Pacific coast of Tohoku earthquake (Mw 9.0). To make a better understanding of this phenomenon, temporal-spatial analyses of GDV have been applied in this study. Geomagnetic data of long-term observations at 17 stations in Japan have been analyzed using the same method in Han et al. 2015. Ratios of diurnal variation range between the reference station KAK and the target stations have been computed. After removing seasonal variations, the 15-day mean values of the ratios in the vertical component shows a clear anomaly exceeding the statistical threshold about 2 months before the mega event at both ESA and MIZ stations in the Tohoku Region. Locations of anomalies in spatial distribution show a good correlation with the epicenter of the Mw 9.0 earthquake. These spatiotemporal results are consistent with those obtained from other independent observations such as groundwater level and GPS displacements. The coupling of multiple pre-earthquake phenomena may help to understand the preparation process of a mega earthquake in the subduction zone.