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An improved depth-averaged nonhydrostatic shallow water model with quadratic pressure approximation

机译:具有二次压力近似的改进的深度平均无水性浅水模型

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摘要

Phase-resolved information is necessary for many coastal wave problems, for example, for the wave conditions in the vicinity of harbor structures. Two-dimensional (2D) depth-averaging shallow water models are commonly used to obtain a phase-resolved solution near the coast. These models are in general more computationally effective compared with computational fluid dynamics software and will be even more capable if equipped with a parallelized code. In the current article, a 2D wave model solving the depth-averaged continuity equation and the Euler equations is implemented in the open-source hydrodynamic code REEF3D. The model is based on a nonhydrostatic extension and a quadratic vertical pressure profile assumption, which provides a better approximation of the frequency dispersion. It is the first model of its kind to employ high-order discretization schemes and to be fully parallelized following the domain decomposition strategy. Wave generation and absorption are achieved with a relaxation method. The simulations of nonlinear long wave propagations and transformations over nonconstant bathymetries are presented. The results are compared with benchmark wave propagation cases. A large-scale wave propagation simulation over realistic irregular topography is shown to demonstrate the model's capability of solving operational large-scale problems.
机译:例如,对于许多沿海波问题,例如,对于港口结构附近的波条件是必要的。二维(2D)深度平均浅水模型通常用于在海岸附近获得相位分辨的溶液。与计算流体动力学软件相比,这些模型通常更加计算地有效,并且如果配备有并行化代码,则将更有能力。在当前文章中,求解深度平均连续性方程和欧拉方程的2D波模型在开源流体动力学代码ref3d中实现。该模型基于非水压延伸和二次垂直压力曲线假设,其提供了频率分散的更好近似。它是本类型采用高阶离散化方案的第一模型,并在域分解策略之后完全并行化。通过弛豫方法实现波浪产生和吸收。介绍了非线性长波传播的模拟和非合作浴形式的转化。将结果与基准波传播案例进行比较。展示了逼真的不规则形貌的大规模波传播仿真,以展示模型解决操作大规模问题的能力。

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