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High Order Accurate Finite Difference Modeling of Seismo-Acoustic Wave Propagation in a Moving Atmosphere and a Heterogeneous Earth Model Coupled Across a Realistic Topography

机译:运动大气中声波传播的高阶精确有限差分建模和跨真实地形耦合的非均质地球模型

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We develop a numerical method for simultaneously simulating acoustic waves in a realistic moving atmosphere and seismic waves in a heterogeneous earth model, where the motions are coupled across a realistic topography. We model acoustic wave propagation by solving the linearized Euler equations of compressible fluid mechanics. The seismic waves are modeled by the elastic wave equation in a heterogeneous anisotropic material. The motion is coupled by imposing continuity of normal velocity and normal stresses across the topographic interface. Realistic topography is resolved on a curvilinear grid that follows the interface. The governing equations are discretized using high order accurate finite difference methods that satisfy the principle of summation by parts. We apply the energy method to derive the discrete interface conditions and to show that the coupled discretization is stable. The implementation is verified by numerical experiments, and we demonstrate a simulation of coupled wave propagation in a windy atmosphere and a realistic earth model with non-planar topography.
机译:我们开发了一种数值方法,用于同时模拟真实移动的气氛中的声波和异质地球模型中的地震波,在异质地球模型中,运动在真实地形中耦合。我们通过求解可压缩流体力学的线性Euler方程对声波传播进行建模。在非均质各向异性材料中,通过弹性波方程对地震波进行建模。通过在地形界面上施加法向速度和法向应力的连续性来耦合运动。逼真的地形在遵循界面的曲线网格上解析。控制方程使用满足零件求和原理的高阶精确有限差分法离散化。我们应用能量方法得出离散的界面条件,并证明耦合离散化是稳定的。通过数值实验验证了该实现,并且我们演示了在有风的大气中耦合波传播的仿真以及具有非平面地形的真实地球模型。

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