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Physical and numerical modelling of irregular wave propagation in coastal waters.

机译:沿海水域不规则波传播的物理和数值模拟。

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摘要

The present research work concentrates on the development and verification of a numerical model capable of simulating wave transformation in coastal waters over uneven, two-dimensional bathymetry.Apart from monochromatic waves, irregular waves which are those actually encountered in nature are also taken into account. Furthermore, the processes of non-linear wave phase speed distortion due to amplitude dispersion as well as energy dissipation due to bottom friction, whose effects are intensified in shallow waters, are also incorporated in the model. Wave breaking inception is modelled using new regular and irregular wave breaking criteria which embody the spatial surface elevation slope as a parameter. These have been formulated based on laboratory experiments carried out on waves propagating in a basin over an elliptic shoal (2D bathymetry), and in a flume over a plane slope followed by a horizontal platform (1D bathymetry). Existing regular and irregular wave breaking criteria are reviewed and assessed with the aid of the collected data.Computations have been carried out for a range of wave propagation/transformation problems. Agreement of computed results with analytical results, existing laboratory data and the present laboratory data is very good.The so-called mild-slope equation, which includes the combined effects of shoaling, refraction, diffraction and reflection is adopted as the basis of the numerical model. Solutions are obtained on unstructured triangular meshes using a Godunov-type, second-order, upwind, cell-centred finite volume formulation, whereby the numerical fluxes are computed using Roe's flux function. Appropriate conditions for driving, transparent and fully reflecting boundaries are derived. The unknown variables are updated in time through an accurate implicit scheme. It is the first time that such a solution methodology is used for the solution of the mild-slope equation.
机译:目前的研究工作集中在开发和验证能够模拟不平坦二维测深的沿海水域波浪转换的数值模型,除单色波外,还考虑了自然界中实际遇到的不规则波。此外,该模型还包含了由于振幅分散而引起的非线性波相速度畸变以及由于底部摩擦而引起的能量耗散的过程,其作用在浅水中得到增强。使用新的规则和不规则波浪破碎标准对波浪破碎开始进行建模,这些标准将空间表面高程斜率作为参数。这些是根据实验室实验制定的,这些实验是在椭圆形浅滩上的盆地中传播的波上进行的(二维测深法),然后是在平面斜面上的水槽中传播的波,然后是水平平台(一维测深法)。现有的常规和不规则波浪破碎标准将根据收集到的数据进行审查和评估。已针对一系列波浪传播/变形问题进行了计算。计算结果与分析结果,现有实验室数据和现有实验室数据的一致性非常好。采用所谓的缓坡方程,其中包括浅滩,折射,衍射和反射的综合影响,是数值计算的基础。模型。使用Godunov型,二阶,迎风,以单元为中心的有限体积公式在非结构三角网格上获得解,从而使用Roe的通量函数计算数值通量。得出了合适的驾驶条件,透明且完全反映边界的条件。未知变量通过精确的隐式方案及时更新。这是第一次将这种求解方法用于平缓坡度方程的求解。

著录项

  • 作者

    Bokaris, Jack.;

  • 作者单位

    University of London (United Kingdom).;

  • 授予单位 University of London (United Kingdom).;
  • 学科 Engineering Marine and Ocean.
  • 学位 Ph.D.
  • 年度 2000
  • 页码 208 p.
  • 总页数 208
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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