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首页> 外文期刊>Proceedings of the International Conference on Coastal Engineering >FULLY NONLINEAR MODELING OF NEARSHORE WAVE PROPAGATION INCLUDING THE EFFECTS OF WAVE BREAKING
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FULLY NONLINEAR MODELING OF NEARSHORE WAVE PROPAGATION INCLUDING THE EFFECTS OF WAVE BREAKING

机译:近岸波传播的完全非线性建模,包括波折断的影响

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Nearshore wave modeling over spatial scales of several kilometers requires balancing the fine-scale modeling of physical processes with the model’s accuracy and efficiency. In this work, a fully nonlinear potential flow model is proposed as a compromise between simplified linear, weakly nonlinear or weakly dispersive models and direct CFD approaches. The core of present approach is the use of a series representation for the velocity potential. This series contains prescribed vertical functions and allows the determination of the velocity potential in terms of unknown horizontal functions. The resulting dimensionally reduced model retains the structure of the Hamiltonian water wave system Zakharov (1968), Craig & Sulem (1993), avoiding the solution of the Laplace problem for the potential. Instead, a numerically convenient linear system of horizontal equations needs to be solved at each step in the temporal evolution. No simplifications concerning the deformation of the physical boundaries are introduced, apart from the typical requirement of a smooth, non-overturning free surface and seabed. The main limitation of this formulation is its inability to account for wave breaking. The treatment of this process is the subject of the present work. Two different techniques are implemented in the present model. Simulation results are compared to laboratory measurements for two test cases: (1) shoaling and breaking of regular waves over a barred bathymetry Beji & Battjes (1993) and (2) shoaling and breaking of regular waves on a plane beach Ting & Kirby (1994).
机译:在几千米的空间尺度上进行近岸波浪建模需要平衡物理过程的精细建模与模型的准确性和效率。在这项工作中,提出了一个完全非线性的势流模型,作为简化的线性,弱非线性或弱色散模型与直接CFD方法之间的折衷。本方法的核心是对速度势的级数表示。该系列包含规定的垂直函数,并允许根据未知的水平函数确定速度势。所得的降维模型保留了哈密顿水波系统Zakharov(1968),Craig&Sulem(1993)的结构,从而避免了潜在的拉普拉斯问题的求解。取而代之的是,需要在时间演化的每个步骤中求解水平方程式的数值便捷线性系统。除了对光滑,不倾覆的自由表面和海床的典型要求外,没有引入有关物理边界变形的简化方法。该公式的主要局限性在于它无法解决波浪破裂问题。该过程的处理是当前工作的主题。在本模型中实现了两种不同的技术。在两个测试案例中,将模拟结果与实验室测量结果进行了比较:(1)在禁止的测深仪上浅滩和常规波的破碎和破裂Beji&Battjes(1993)和(2)在平面海滩上浅滩和常规波的破碎和破裂Ting&Kirby(1994) )。

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