A One-Way Coupled Navier–Stokes-Serre Model for Simulating the Generation and Propagation of Tsunami Waves

IF 1.9 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS pure and applied geophysics Pub Date : 2024-04-20 DOI:10.1007/s00024-024-03485-1
Zhikang Xin, Yunfeng Shi, Yunxing Zhang, Yifan Zhang
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Abstract

In this paper, a two-dimensional numerical model for simulating the generation and propagation of tsunami waves caused by upthrust bed movement is developed. To consider the nonlinearity as well as save the computational cost, a Navier–Stokes equation solver is used for the generation zone, and a Serre equation solver is adopted for the downstream evolution of the tsunami waves. The solution of the Navier–Stokes equation solver is extracted and transferred as the initial solution of the Serre solver, which means a one-way coupling is achieved. In this way, a one-way coupled Navier–Stokes-Serre model is obtained. After a detailed validation of the individual solvers, the coupled model is utilized for simulating the generation and propagation of tsunami waves caused by the upthrust bed movement in shallow water of uniform depth. It is found that the coupled model is comparable to the traditional Boussinesq equation model. Finally, the capacity of the coupled model for simulating wave-breaking cases is demonstrated.

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模拟海啸波产生和传播的单向耦合纳维-斯托克斯-塞雷模型
本文建立了一个二维数值模型,用于模拟隆起床运动引起的海啸波的产生和传播。为了考虑非线性并节省计算成本,生成区采用 Navier-Stokes 方程求解器,海啸波的下游演变采用 Serre 方程求解器。纳维-斯托克斯方程求解器的解被提取并转移作为塞雷方程求解器的初始解,这意味着实现了单向耦合。这样,就得到了单向耦合的纳维-斯托克斯-塞雷模型。在对各个求解器进行详细验证后,利用该耦合模型模拟了在深度均匀的浅水中由隆起床运动引起的海啸波的产生和传播。结果发现,耦合模型与传统的布森斯克方程模型相当。最后,演示了耦合模型模拟破浪情况的能力。
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来源期刊
pure and applied geophysics
pure and applied geophysics 地学-地球化学与地球物理
CiteScore
4.20
自引率
5.00%
发文量
240
审稿时长
9.8 months
期刊介绍: pure and applied geophysics (pageoph), a continuation of the journal "Geofisica pura e applicata", publishes original scientific contributions in the fields of solid Earth, atmospheric and oceanic sciences. Regular and special issues feature thought-provoking reports on active areas of current research and state-of-the-art surveys. Long running journal, founded in 1939 as Geofisica pura e applicata Publishes peer-reviewed original scientific contributions and state-of-the-art surveys in solid earth and atmospheric sciences Features thought-provoking reports on active areas of current research and is a major source for publications on tsunami research Coverage extends to research topics in oceanic sciences See Instructions for Authors on the right hand side.
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