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Application of an Element-free Galerkin Method to Water Wave Propagation Problems

机译:无元素Galerkin方法在水波传播问题中的应用

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The paper is concerned with the problem of gravitational wave propagation in water of variable depth. The problem is solved numerically by applying an element-free Galerkin method. First, the proposed model is validated by comparing its predictions with experimental data for the plane flow in water of uniform depth. Then, as illustrations, results of numerical simulations performed for plane gravity waves propagating through a region with a sloping bed are presented. These results show the evolution of the free-surface elevation, displaying progressive steepening of the wave over the sloping bed, followed by its attenuation in a region of uniform depth. In addition, some of the results of the present model are compared with those obtained earlier by using the conventional finite element method.
机译:本文关注的是重力波在变深度水中的传播问题。通过应用无元素Galerkin方法在数值上解决了该问题。首先,通过将模型的预测值与均匀深度水中平面流的实验数据进行比较,验证了所提出模型的有效性。然后,作为说明,给出了对通过倾斜床层的区域传播的平面重力波进行数值模拟的结果。这些结果显示了自由表面高程的演变,显示了倾斜床上的波浪逐渐变陡,然后在均匀深度的区域中逐渐衰减。另外,将本模型的某些结果与以前使用常规有限元方法获得的结果进行了比较。

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