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Finite volume simulation of waves formed by sliding masses

机译:滑动质量形成的波浪的有限体积模拟

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We numerically study a relatively simple two-dimensional (2D) model for landslide-generated nonlinear surface water waves. The landslides are modeled as rigid and impervious bodies translating on a flat or an inclined bottom. The water motion is assumed to be properly modeled by the 2D nonlinear system of shallow water equations. The resulting 2D system is numerically solved by means of a conservative well-balanced high-resolution finite volume upwind scheme especially adapted to treat advancing wet/dry fronts over irregular topography. Numerical results for ID and 2D benchmark cases include comparisons with analytical or asymptotic solutions as well as comparisons with experimental data. The numerical investigation reveals that although the presented model has certain limitations, it appears to be able to model important aspects and the most significant characteristics of wave formation and propagation in their initial generation stage, namely, the waves moving toward the shore, the subsequent run-up and run-down, the waves propagating toward deep water, as well as the shape and arrival time of these waves.
机译:我们用数值方法研究了滑坡生成的非线性地表水波的一个相对简单的二维(2D)模型。滑坡被建模为在平坦或倾斜底部平移的刚性且不透水的物体。假设水运动由浅水方程的二维非线性系统正确建模。通过保守的平衡良好的高分辨率有限体积迎风方案,对所得的2D系统进行了数值求解,该方案特别适用于处理不规则地形上前进的湿/干锋面。 ID和2D基准案例的数值结果包括与解析解或渐近解的比较,以及与实验数据的比较。数值研究表明,尽管所提出的模型有一定的局限性,但它似乎能够对波的形成和传播的重要方面和最显着特征进行建模,即波的初始生成阶段,即波向海岸,随后的运行。上升和下降,海浪向深水传播,以及这些海浪的形状和到达时间。

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