Broadband (0-5 Hz) Fully Deterministic 3D Ground-Motion Simulations of a Magnitude 7.0 Hayward Fault Earthquake: Comparison with Empirical Ground-Motion Models and 3D Path and Site Effects from Source Normalized Intensities

被引:49
|
作者
Rodgers, Arthur J. [1 ,5 ,6 ]
Petersson, N. Anders [2 ]
Pitarka, Arben [1 ]
McCallen, David B. [3 ,5 ]
Sjogreen, Bjorn [2 ]
Abrahamson, Norman [4 ]
机构
[1] Lawrence Livermore Natl Lab, Atmospher Earth & Energy Div & Geophys Monitoring, 7000 East Ave,L-046, Livermore, CA 94551 USA
[2] Lawrence Livermore Natl Lab, Ctr Appl Sci Comp, 7000 East Ave,L-561, Livermore, CA 94551 USA
[3] Univ Nevada, 1644 North Virginia St,Reno MS 0258, Reno, NV 89577 USA
[4] Univ Calif Berkeley, Dept Civil & Enviornm Engn, 455 Davis Hall, Berkeley, CA 94720 USA
[5] Lawrence Berkeley Natl Lab, Earth & Environm Sci Area, 1 Cyclotron Rd,MS74R316C, Berkeley, CA 94720 USA
[6] Univ Calif Berkeley, Berkeley Seismol Lab, 307 McCone Hall 4760, Berkeley, CA 94720 USA
关键词
DISCONTINUOUS GALERKIN METHOD; SEISMIC-WAVE PROPAGATION; FINITE-DIFFERENCE; HORIZONTAL COMPONENTS; HETEROGENEOUS MEDIA; UNSTRUCTURED MESHES; ELEMENT-METHOD; ELASTIC-WAVES; LONG-PERIOD; PART II;
D O I
10.1785/0220180261
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
We report on high-performance computing (HPC) fully deterministic simulation of ground motions for a moment magnitude (Mw) 7.0 scenario earthquake on the Hayward fault resolved to 5 Hz using the SW4 finite-difference code. We computed motions obeying physics-based 3D wave propagation at a regional scale with an Mw 7.0 kinematic rupture model generated following Graves and Pitarka (2016). Both plane-layered (1D) and 3D Earth models were considered, with 3D subsurface material properties and topography interpolated from a model of the U. S. Geological Survey (USGS). The resulting ground-motion intensities cover a broader frequency range than typically considered in regional-scale simulations, including higher frequencies relevant for engineering analysis of structures. Median intensities for sites across the domain are within the reported between-event uncertainties (t) of groundmotion models (GMMs) across spectral periods 0.2-10 s (frequencies 0.1-5 Hz). The within-event standard deviation. of ground-motion intensity measurement residuals range 0.2-0.5 natural log units with values consistently larger for the 3D model. Source-normalized ratios of intensities (3D/1D) reveal patterns of path and site effects that are correlated with known geologic structure. These results demonstrate that earthquake simulations with fully deterministic wave propagation in 3D Earth models on HPC platforms produce broadband ground motions with median and within-event aleatory variability consistent with empirical models. Systematic intensity variations for the 3D model caused by path and site effects suggest that these epistemic effects can be estimated and removed to reduce variation in site-specific hazard estimates. This study motivates future work to evaluate the validity of the USGS 3D model and investigate the development of path and site corrections by running more scenarios. Supplemental Content: Animation of ground motions from the 3D subsurface model with topography.
引用
收藏
页码:1268 / 1284
页数:17
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