Forecasting aftershock activity: 1. Adaptive estimates based on the Omori and Gutenberg-Richter laws

被引:8
|
作者
Baranov, S. V. [1 ]
Shebalin, P. N. [2 ]
机构
[1] Russian Acad Sci, Kola Branch, Geophys Survey, Ul Fersmana 14, Apatity 184209, Russia
[2] Russian Acad Sci, Inst Earthquake Predict Theory & Math Geophys, Ul Profsoyuznaya 84-32, Moscow 117997, Russia
基金
俄罗斯基础研究基金会;
关键词
MODEL; COMPLETENESS; EARTHQUAKES; MAGNITUDE; STATE;
D O I
10.1134/S1069351316020038
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The method for forecasting the intensity of the aftershock processes after strong earthquakes in different magnitude intervals is considered. The method is based on the joint use of the time model of the aftershock process and the Gutenberg-Richter law. The time model serves for estimating the intensity of the aftershock flow with a magnitude larger than or equal to the magnitude of completeness. The Gutenberg-Richter law is used for magnitude scaling. The suggested approach implements successive refinement of the parameters of both components of the method, which is the main novelty distinguishing it from the previous ones. This approach, to a significant extent, takes into account the variations in the parameters of the frequency-magnitude distribution, which often show themselves by the decreasing fraction of stronger aftershocks with time. Testing the method on eight aftershock sequences in the regions with different patterns of seismicity demonstrates the high probability of successful forecasts. The suggested technique can be employed in seismological monitoring centers for forecasting the aftershock activity of a strong earthquake based on the results of operational processing.
引用
收藏
页码:413 / 431
页数:19
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