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Modeling seismic wave propagation in heterogeneous medium using overlap domain pseudospectral method

机译:使用重叠域伪谱方法对地震波在非均质介质中的建模

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Pseudospectral method is an efficient and high accuracy numerical method for simulating seismic wave propagation in heterogeneous earth medium. Since its derivative operator is global, this method is commonly considered not suitable for parallel computation. In this paper, we introduce the parallel overlap domain decomposition scheme and give a parallel pseudospectral method implemented on distributed memory PC cluster system for modeling seismic wave propagation in heterogeneous medium. In this parallel method, the medium is decomposed into several subdomains and the wave equations are solved in each subdomain simultaneously. The solutions in each subdomain are connected through the transferring at the overlapped region. Using 2D models, we compared the parallel and traditional pseudospectral method, analyzed the accuracy of the parallel method. The results show that the parallel method can efficiently reduce computation time for the same accuracy as the traditional method. This method could be applied to large scale modeling of seismic wave propagation in 3D heterogeneous medium.
机译:伪谱法是一种模拟地震波在非均质土介质中传播的高效,高精度数值方法。由于其导数运算符是全局运算符,因此通常认为此方法不适用于并行计算。在本文中,我们介绍了并行重叠域分解方案,并给出了一种在分布式存储PC集群系统上实现的并行伪谱方法,用于对非均质介质中的地震波传播进行建模。在这种并行方法中,将介质分解为几个子域,并在每个子域中同时求解波动方程。每个子域中的解通过重叠区域的传递而连接。使用2D模型,我们比较了并行和传统的伪光谱方法,分析了并行方法的准确性。结果表明,并行方法可以有效地减少计算时间,且精度与传统方法相同。该方法可以应用于3D非均质介质中地震波传播的大规模建模。

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