Mapping Seismic Hazard for Canadian Sites Using Spatially Smoothed Seismicity Model

被引:1
作者
Feng, Chao [1 ]
Hong, Han-Ping [2 ,3 ]
机构
[1] Changan Univ, Sch Civil Engn, Xian 710061, Peoples R China
[2] Harbin Inst Technol, Sch Civil & Environm Engn, Shenzhen 518055, Peoples R China
[3] Univ Western Ontario, Dept Civil & Environm Engn, London, ON N6A 5B9, Canada
关键词
Adaptive kernel smoothing; Fixed kernel smoothing; Ground motion model; Probabilistic seismic hazard analysis; Seismic hazard map; Uniform hazard spectra; MOTION PREDICTION EQUATIONS; EASTERN NORTH-AMERICA; PEAK GROUND-MOTION; KERNEL ESTIMATION; INTERFACE EARTHQUAKES; PARAMETERS; CASCADIA; DESIGN; AREA; PGV;
D O I
10.1007/s13753-023-00521-x
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The estimated seismic hazard based on the delineated seismic source model is used as the basis to assign the seismic design loads in Canadian structural design codes. An alternative for the estimation is based on a spatially smoothed source model. However, a quantification of differences in the Canadian seismic hazard maps (CanSHMs) obtained based on the delineated seismic source model and spatially smoothed model is unavailable. The quantification is valuable to identify epistemic uncertainty in the estimated seismic hazard and the degree of uncertainty in the CanSHMs. In the present study, we developed seismic source models using spatial smoothing and historical earthquake catalogue. We quantified the differences in the estimated Canadian seismic hazard by considering the delineated source model and spatially smoothed source models. For the development of the spatially smoothed seismic source models, we considered spatial kernel smoothing techniques with or without adaptive bandwidth. The results indicate that the use of the delineated seismic source model could lead to under or over-estimation of the seismic hazard as compared to those estimated based on spatially smoothed seismic source models. This suggests that an epistemic uncertainty caused by the seismic source models should be considered to map the seismic hazard.
引用
收藏
页码:898 / 918
页数:21
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