色散浅水波浪模拟。第四部分:全局球面几何的数值模拟

G. Khakimzyanov, D. Dutykh, O. Gusev
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引用次数: 12

摘要

在本文中,我们考虑了一个旋转全局球面几何上的色散波模拟问题。在第四部分中,我们将重点放在数值方面,而模型推导在第三部分中进行了描述。我们提出的算法是基于分裂方法。即,将方程分解为色散压力分量的均匀椭圆方程和带源项的浅水方程(球面上)的双曲部分。该算法采用两步预测校正方案实现。在每一步中,我们分别求解椭圆型和双曲型问题。然后,在具有均匀底部的模型理想化情况下说明了该算法的性能,并估计了球度和旋转效应对色散波传播的影响。色散效应根据在球上的传播距离和产生区域的线性程度来量化。最后,将数值方法应用于几个实际事件。也就是说,我们进行了2007年保加利亚和2010年智利海啸的模拟。只要有数据,我们的计算结果就会与实际测量结果相冲突。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Dispersive shallow water wave modelling. Part IV: Numerical simulation on a globally spherical geometry
In the present manuscript, we consider the problem of dispersive wave simulation on a rotating globally spherical geometry. In this Part IV, we focus on numerical aspects while the model derivation was described in Part III. The algorithm we propose is based on the splitting approach. Namely, equations are decomposed on a uniformly elliptic equation for the dispersive pressure component and a hyperbolic part of shallow water equations (on a sphere) with source terms. This algorithm is implemented as a two-step predictor-corrector scheme. On every step, we solve separately elliptic and hyperbolic problems. Then, the performance of this algorithm is illustrated on model idealised situations with an even bottom, where we estimate the influence of sphericity and rotation effects on dispersive wave propagation. The dispersive effects are quantified depending on the propagation distance over the sphere and on the linear extent of generation region. Finally, the numerical method is applied to a couple of real-world events. Namely, we undertake simulations of the Bulgarian 2007 and Chilean 2010 tsunamis. Whenever the data is available, our computational results are confronted with real measurements.
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