日本地球惑星科学連合2018年大会

講演情報

[EE] 口頭発表

セッション記号 S (固体地球科学) » S-SS 地震学

[S-SS06] CSEP, earthquake forecast testing, and the role of SSE in earthquake occurrence.

2018年5月21日(月) 10:45 〜 12:15 A01 (東京ベイ幕張ホール)

コンビーナ:Schorlemmer Danijel(GFZ German Research Centre for Geosciences)、平田 直(東京大学地震研究所)、Matt Gerstenberger(共同)、鶴岡 弘(東京大学地震研究所)、座長:鶴岡 弘(東京大学地震研究所)、Danijel Schorlemmer(GFZ German Research Centre for Geosciences)、Gerstenberger Matthew(GNS Science, New Zealand)

11:15 〜 11:30

[SSS06-03] Foreshock Discrimination and Short-Term Mainshock Forecast Based on Magnitude Differences and Spatio–Temporal Distances

*野村 俊一1尾形 良彦1 (1.統計数理研究所)

キーワード:前震識別、本震予測、ロジスティック回帰

Foreshocks are promising clues for short-term forecasting of large mainshocks. We propose a probabilistic discrimination model of foreshock activities to predict mainshocks. Using the single-link clustering method, the model updates the expanding seismic clusters and determines in real time the probabilities that larger subsequent events will occur. The foreshock clusters and other cluster types show different trends of certain feature statistics with respect to their magnitudes and spatio-temporal distances. Based on those features and the epicentral location, a non-linear logistic regression model is used to evaluate the probabilities that growing seismic clusters will be foreshocks triggering the mainshock within 30 days. The log of odds ratio is estimated between the foreshock clusters and other clusters for respective feature values as nonlinear spline functions from a Japanese hypocenter catalog of 1926 to 1999. From the estimated odds functions, foreshock clusters tend to have smaller differences in their two largest magnitudes, shorter time durations, and slightly longer epicentral distances within the individual clusters. Given a potential foreshock cluster, its mainshock magnitude can be predicted by the Gutenberg-Richter law over the largest foreshock magnitude. The predictive performance of our model is validated by a Japanese hypocenter catalog of 2000 to date and is not used in the parameter inference. The evaluated foreshock probabilities are roughly consistent with the actual portion of foreshocks in the validation catalog and may be used as an alert of large mainshocks.