Improvements to seismicity forecasting based on a Bayesian spatio-temporal ETAS model

被引:5
|
作者
Ebrahimian, Hossein [1 ]
Jalayer, Fatemeh [1 ,2 ]
Asayesh, Behnam Maleki [3 ,4 ,5 ]
Hainzl, Sebastian [4 ]
Zafarani, Hamid [5 ]
机构
[1] Univ Naples Federico II, Dept Struct Engn & Architecture, Naples, Italy
[2] UCL, Inst Risk & Disaster Reduct IRDR, London, England
[3] Univ Potsdam, Inst Geosci, Potsdam, Germany
[4] GFZ German Res Ctr Geosci, Potsdam, Germany
[5] Int Inst Earthquake Engn & Seismol IIEES, Tehran, Iran
基金
美国国家科学基金会;
关键词
REAL-TIME FORECASTS; EARTHQUAKE FORECASTS; SHORT-TERM; CLUSTERING MODEL; HAZARD ANALYSIS; RISK-ASSESSMENT; AFTERSHOCKS; MAGNITUDE; STATE; UCERF3-ETAS;
D O I
10.1038/s41598-022-24080-1
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The epidemic-type aftershock sequence (ETAS) model provides an effective tool for predicting the spatio-temporal evolution of aftershock clustering in short-term. Based on this model, a fully probabilistic procedure was previously proposed by the first two authors for providing spatio-temporal predictions of aftershock occurrence in a prescribed forecasting time interval. This procedure exploited the versatility of the Bayesian inference to adaptively update the forecasts based on the incoming information provided by the ongoing seismic sequence. In this work, this Bayesian procedure is improved: (1) the likelihood function for the sequence has been modified to properly consider the piecewise stationary integration of the seismicity rate; (2) the spatial integral of seismicity rate over the whole aftershock zone is calculated analytically; (3) background seismicity is explicitly considered within the forecasting procedure; (4) an adaptive Markov Chain Monte Carlo simulation procedure is adopted; (5) leveraging the stochastic sequences generated by the procedure in the forecasting interval, the N-test and the S-test are adopted to verify the forecasts. This framework is demonstrated and verified through retrospective early forecasting of seismicity associated with the 2017-2019 Kermanshah seismic sequence activities in western Iran in two distinct phases following the main events with Mw7.3 and Mw6.3, respectively.
引用
收藏
页数:27
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