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The 2018 update of the US National Seismic Hazard Model: Where, why, and how much probabilistic ground motion maps changed

机译:2018年的美国国家地震危险模型的更新:在哪里,为什么和多少概率地面运动地图改变了

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The 2018 US Geological Survey National Seismic Hazard Model (NSHM) incorporates new data and updated science to improve the underlying earthquake and ground motion forecasts for the conterminous United States. The NSHM considers many new data and component input models: (1) new earthquakes between 2013 and 2017 and updated earthquake magnitudes for some earlier earthquakes; (2) two updated smoothed seismicity models to forecast earthquake rates; (3) two suites of new central and eastern US (CEUS) ground motion models (GMMs) to translate ground shaking for various earthquake sizes and source-to-site distances considered in the model; (4) two CEUS GMMs for aleatory variability; (5) two CEUS site-effect models that modify ground shaking based on alternative shallow site conditions; (6) more advanced western US (WUS) lithologic and structural information to assess basin site effects for selected urban regions; and (7) a more comprehensive range of outputs (22 periods and 8 site classes) than in previous versions of the NSHMs. Each of these new datasets and models produces changes in the probabilistic ground shaking levels that are spatially and statistically analyzed. Recent earthquakes or changes to some older earthquake magnitudes and locations mostly result in probabilistic ground shaking levels that are similar to previous models, but local changes can reach up to +80% and -60% compared to the 2014 model. Newly developed CEUS models for GMMs, aleatory variability, and site effects cause overall changes up to +/- 64%. The addition of the WUS basin amplifications causes changes of up to +60% at longer periods for sites overlying deep soft soils. Across the conterminous United States, the hazard changes in the model are mainly caused by new GMMs in the CEUS, by sedimentary basin effects for long periods (= 1 s) in the WUS, and by seismicity changes for short (0.2 s) and long (1 s) periods for both areas.
机译:2018年美国地质调查国家地震危险模型(NSHM)纳入了新的数据和更新的科学,以改善潜在的美国潜在地震和地面运动预测。 NSHM考虑了许多新数据和组件输入模型:(1)2013年和2017年之间的新地震,并更新了一些早期地震的地震大小; (2)两个更新的平滑地震模型,以预测地震率; (3)两套新的中央和东部和东方地区(CEUS)地面运动模型(GMMS)为各种地震尺寸和模型中考虑的源地距离的地面震动; (4)两个CEUS GMMS,用于溶液变异性; (5)两个CEUS现场效果模型,可根据替代浅地点条件修改地面震动; (6)更先进的美国(WUS)岩性和结构信息,评估选定城市地区的盆地现场效应; (7)比以前的NSHMS版本更全面的输出(22个时段和8个网站类)。这些新数据集和模型中的每一个都会产生在空间和统计学上分析的概率地面摇动水平的变化。最近的地震或对某些较旧地震大小和位置的变化主要导致概率的地面摇动水平与以前的模型相似,但与2014型号相比,局部变化可以达到高达+ 80%和-60%。新开发的GMMS的CEUS模型,综合体变异性和现场效果导致总体变化高达+/- 64%。添加WUS盆地扩增导致覆盖深软土壤的距离更长+ 60%的变化。在孔雀石美国,模型的危险变化主要是由CEU中的新GMMS引起的,通过沉积盆地在WUS中长时间(& = 1s),以及短(0.2秒)的地震性变化和两个领域的长(1秒)。

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