首页> 外文期刊>Bulletin of the Seismological Society of America >Evaluation of Ground-Motion Models for USGS Seismic Hazard Models Using Near-Source Instrumental Ground-Motion Recordings of the Ridgecrest, California, Earthquake Sequence
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Evaluation of Ground-Motion Models for USGS Seismic Hazard Models Using Near-Source Instrumental Ground-Motion Recordings of the Ridgecrest, California, Earthquake Sequence

机译:利用RidGecrest,加利福尼亚州,地震序列的近源工具地面运动录制评估USGS地震危险模型的地面运动模型

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摘要

We evaluated the performance of 12 ground-motion models (GMMs) for earthquakes in the tectonically active shallow crustal region of southern California using instrumental ground-motion observations from the 2019 Ridgecrest, California, earthquake sequence (M-w 4.0-7.1). The sequence was well recorded by the Southern California Seismic Network and rapid response portable aftershock monitoring stations. Ground-motion recordings of this size and proximity are rare, valuable, and independent of GMM development, allowing us to evaluate the predictive powers of GM Ms. We first compute total residuals and compare the probability density functions, means, and standard deviations of the observed and predicted ground motions. Next we use the total residuals as inputs to the probabilistic scoring method (log-likelihood [LLH]). The LLH method provides a single score that can be used to weight GMMs in the U.S. Geological Survey (USGS) National Seismic Hazard Model (NSHM) logic trees. We also explore GMM performance for a range of earthquake magnitudes, wave propagation distances, and site characteristics. We find that the Next Generation Attenuation West-2 (NGAW2) active crust GMMs perform well for the 2019 Ridgecrest, California, earthquake sequence and thus validate their use in the 2018 USGS NSHM. However, significant ground-motion residual scatter remains unmodeled by NGAW2 GMMs due to complexities such as local site amplification and source directivity. Results from this study will inform logic-tree weights for updates to the USGS National NSHM. Results from this study support the use of nonergodic GMMs that can account for regional attenuation and site variations to minimize epistemic uncertainty in USGS NSHMs.
机译:我们利用2019年加利福尼亚Ridgecrest地震序列(M-w 4.0-7.1)的仪器地震动观测,评估了南加州构造活动浅地壳区12个地震地震动模型(GMM)的性能。南加州地震台网和快速反应便携式余震监测站对该序列进行了良好记录。这种大小和接近度的地震动记录是罕见的、有价值的,并且独立于GMM开发,使我们能够评估GM Ms的预测能力。我们首先计算总残差,并比较观测和预测地震动的概率密度函数、平均值和标准差。接下来,我们使用总残差作为概率评分方法(对数似然[LLH])的输入。LLH方法提供了一个分数,可用于在美国地质调查局(USGS)国家地震灾害模型(NSHM)逻辑树中对GMM进行加权。我们还探讨了一系列地震震级、波传播距离和场地特征的GMM性能。我们发现,下一代衰减West-2(NGAW2)活动地壳GMM在2019年加利福尼亚Ridgecrest地震序列中表现良好,因此验证了其在2018年美国地质勘探局NSHM中的使用。然而,由于局部场地放大和震源方向性等复杂性,NGAW2 GMMs仍未对显著的地震动剩余散射进行建模。这项研究的结果将为美国地质勘探局国家NSHM的更新提供逻辑树权重。本研究的结果支持使用非RGODIC GMM,该GMM可以解释区域衰减和场地变化,以最小化美国地质调查局NSHM中的认知不确定性。

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