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Simulation of the Propagation of Tsunamis in Coastal Regions by a Two-Dimensional Non-Hydrostatic Shallow Water Solver

机译:二维非静水浅水求解器模拟海啸在沿海地区的传播

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Due to the enormous damages and losses of human lives in the inundated regions, the simulation of the propagation of tsunamis in coastal areas has received an increasing interest of the researchers. We present a 2D depth-integrated, non-hydrostatic shallow waters solver to simulate the propagation of tsunamis, solitary waves and surges in coastal regions. We write the governing continuity and momentum equations in conservative form and discretize the domain with unstructured triangular Generalized Delaunay meshes. We apply a fractional-time-step procedure, where two problems (steps) are consecutively solved. In the first and in the second step, we hypothesize a hydrostatic and a non-hydrostatic distribution of the pressure, respectively. Several literature models, which solve the same set of equations, are based on a fractional-time-step procedure. In the hydrostatic step of these literature solvers, the flow field does not satisfy the depth-integrated continuity equation, since the momentum equations are solved independently of the continuity equation. In both steps of the proposed numerical scheme, the computed flow field satisfies the depth-integrated continuity equation discretized in each computational cell. This is obtained by solving together the governing equations, according to the different numerical procedures adopted in the steps of the algorithm. Wet/dry problems are implicitly embedded in the proposed numerical solver. We present several model applications where analytical or measured reference solutions are available. The computational effort required by the proposed procedure is investigated.
机译:由于洪水泛滥地区造成了巨大的人类生命损失,模拟海啸在沿海地区传播的研究越来越引起研究人员的兴趣。我们提出了一种二维深度积分的非静水浅水求解器,以模拟海啸,孤波和海浪在沿海地区的传播。我们以保守的形式编写控制连续性和动量方程,并使用非结构化三角广义Delaunay网格离散化该域。我们应用分数时间步法,其中两个问题(步骤)被连续解决。在第一步和第二步中,我们分别假设压力的静液压分布和非静液压分布。解决分数方程组的几种文献模型均基于分数时间步长程序。在这些文献求解器的静液压步骤中,流场不满足深度积分的连续性方程,因为动量方程是独立于连续性方程求解的。在提出的数值方案的两个步骤中,计算的流场都满足在每个计算单元中离散化的深度积分连续性方程。这是根据算法步骤中采用的不同数值程序,通过将控制方程式一起求解而获得的。干/湿问题隐含地嵌入到提出的数值求解器中。我们介绍了几种模型应用程序,其中提供了分析或测量参考溶液。研究了所提出程序所需的计算量。

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