Visualization of Seismic Wave Propagation from Recent Damaging Earthquakes in Japan: Dense Array Observations and Parallel Simulations Using the Earth Simulator

T. Furumura, Li Chen
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Abstract

This paper presents recent developments of large-scale parallel simulation of seismic wave propagation and concurrent visualization of 3D seismic wavefield using the Earth Simulator supercomputer. The developments of high-performance computing facilities and dense networks of strong ground motion instruments in Japan (K-NET and KiK-net) have now made it possible to directly visualize regional seismic wave propagation during large earthquakes. Our group has developed efficient parallel finite difference method (FDM) code for modeling the seismic wavefield, and a 3D visualization technique, both suitable for implementation on the Earth Simulator. Large-scale 3D simulations of seismic wave propagation have been conducted using these techniques to recast strong ground motions during recent damaging earthquakes such as the 2000 Tottori-ken Seibu (MJ7.3) earthquake, the 1923 great Kanto earthquake (MJ 7.9), and the 1855 Ansei Edo (M7) earthquake. Comparison of the simulation results with the dense array observations provides insights into the nature of complex seismic wave propagation through the heterogeneous subsurface structure in Japan. The simulation results are in very good agreement with the observations in terms of the features of the waveform and the regional intensity pattern, indicating that the simulation is already at a suitable level for use in investigating the expected pattern of ground motions for future earthquake scenarios.
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日本近期破坏性地震地震波传播的可视化:密集阵列观测和地球模拟器并行模拟
本文介绍了地球模拟器超级计算机在地震波传播大规模并行模拟和三维地震波场并行可视化方面的最新进展。日本的高性能计算设施和密集的强地震动仪器网络(K-NET和KiK-net)的发展,现在已经可以直接看到大地震期间区域地震波的传播。我们的团队开发了高效的并行有限差分法(FDM)代码来模拟地震波场,以及一种三维可视化技术,两者都适合在地球模拟器上实现。在最近的破坏性地震中,如2000年的鸟鸟健西武(MJ7.3)地震、1923年的关东大地震(MJ 7.9)和1855年的安sei江户(M7)地震,已经使用这些技术进行了大规模的地震波传播的三维模拟,以重新模拟强烈的地面运动。将模拟结果与密集阵列观测结果进行比较,有助于深入了解日本非均匀地下结构中复杂地震波传播的性质。在波形特征和区域烈度分布方面,模拟结果与观测结果非常吻合,表明模拟已经达到了研究未来地震情景的预期地震动模式的适当水平。
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