JpGU-AGU Joint Meeting 2020

Presentation information

[E] Oral

M (Multidisciplinary and Interdisciplinary) » M-IS Intersection

[M-IS09] Interdisciplinary studies on pre-earthquake processes

convener:Katsumi Hattori(Department of Earth Sciences, Graduate School of Science, Chiba University), Dimitar Ouzounov(Center of Excellence in Earth Systems Modeling & Observations (CEESMO) , Schmid College of Science & Technology Chapman University, Orange, California, USA), Jann-Yenq LIU(Department of Space Science and Engineering, National Central University, Taiwan), Qinghua Huang(Peking University)

[MIS09-12] Statistical Test of Spatio-Temporal Variation of b Value in Japan

*weiyun xie1, Peng Han2, Katsumi Hattori1 (1.chiba university, 2.Southern University of Science and Technology )

Keywords:b value, Mc, AIC

The Gutenberg-Richter (GR) law: log10NM=a-bM denotes the relationship between the frequency-magnitude distribution (FMD), in which N is the cumulative number of earthquakes with magnitude equal to or larger than M. Constant b measures difference in the relative proportion of small and large earthquakes and shows the variation of seismicity activity and stress evolution before earthquake. Many studies show that b-value decreased prior to great earthquakes. Since the b value depends very much on the magnitude of completeness (Mc), we investigated the spatial variation of Mc in Japan, combining the maximum curvature (MAXC) technique and the bootstrap approaches. Then, for the area that has approximately equal Mc value, we check the temporal variation of Mc and apply its maximum to calculate b values. This process helps the computation of b value in this area and its uncertainty can be computed more properly.

We used the bootstrap approach to generate reference b values and applied the Akaike Information Criterion (AIC) to assess the spatial variation of b values of the area statistically. Here, we define the P(ΔAIC≧2) value, where P(ΔAIC≧2) means that the percentage of ΔAIC between the b value at the target space and time and that of the reference is larger or equals to 2. This gives the significance level of difference between target and the reference periods. In the area, we narrowed a target area depending on P(ΔAIC≧2), after that we quantified the temporal variation of the target area and discuss the precursor of the large earthquake occurred in this area. Also, the spatial distribution of ΔAIC between reference and the period prior to the main shock will also be investigated. In this paper, we will demonstrate capability of the proposed method. A case study of the 2016 Kumamoto Earthquake (M7.3) shows a statistically clear decrease in b value and large increase of P(ΔAIC≧2) value few months before the main shock. It indicates that the b value with statistical assessment may emerge positive impact for forecasting a future large earthquake.