日本地球惑星科学連合2023年大会

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[E] 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-IS04] Interdisciplinary studies on pre-earthquake processes

2023年5月21日(日) 10:45 〜 12:00 104 (幕張メッセ国際会議場)

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

11:45 〜 12:00

[MIS04-10] The 3-D ionospheric Ne disturbances prior to Tohoku-Oki Earthquake occurred on March 11, 2011

★Invited Papers

*Song Rui1服部 克巳1张 学民2劉 正彦3 (1.千葉大学理学部、2.Institute of Earthquake Forecasting, China Earthquake Administration, China、3.Institute of Space Science, National Central University, Taiwan)

キーワード:Seismo-ionospheric effect、Computerized ionospheric tomography、Electron density pertubation

We detailly studied the three-dimensional (3-D) ionospheric electron density (Ne) disturbances prior to the 2011 M9.0 Tohoku Oki Earthquake in Japan by the ground-based total electron content data sets provided by the global positioning system (GPS) Earth Observation Network (GEONET). To retrieve the 3-D ionospheric Ne distributions, we developed an initial input-free algorithm, termed the improved constraint least square fitting (ICLSF) algorithm based on the computerized ionospheric tomography (CIT) technique. It has an excellent performance in visualizing ionospheric disturbances, owing to its independence of any initial guesses with only vertical direction constraints. Two kinds of ionospheric Ne anomalies were detected in our study. First, by calculating the percent Ne variations, we found remarkable negative Ne anomalies ranging from -20% to -60% around the epicenter on March 8, 2011, which is three days prior to the mainshock. They lasted for more than ~20 hours in the lower altitudes of F2 layer in 190 - 250 km. Second, prominent continuous downward drift of Ne in the F2 layer with displacement of ~ 60 km was recognized immediately before the mainshock during 04:52 - 05:30 UT west of epicenter. Finally, we discussed the possible triggering mechanism based on the 3-D CIT results.