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Consistent coupled-mode theory for the propagation of small-amplitude water waves over variable bathymetry regions

机译:小幅度水波在可变测深区域上传播的一致耦合模式理论

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摘要

Extended mild-slope equations for the propagation of small-amplitude water waves over variable bathymetry regions, recently proposed by Massel (1993) and Porter & Staziker (1995), are shown to exhibit an inconsistency concerning the sloping-bottom boundary condition, which renders them non-conservative with respect to wave energy. In the present work, a consistent coupled-mode theory is derived from a variational formulation of the complete linear problem, by representing the vertical distribution of the wave potential as a uniformly convergent series of local vertical modes at each horizontal position. This series consists of the vertical eigenfunctions associated with the propagating and all evanescent modes and, when the slope of the bottom is different from zero, an additional mode, carrying information about the bottom slope. The coupled-mode system obtained in this way contains an additional equation, as well as additional interaction terms in all other equations, and reduces to the previous extended mild-slope equations when the additional mode is neglected. Extensive numerical results demonstrate that the present model leads to the exact satisfaction of the bottom boundary condition and, thus, it is energy conservative. Moreover, it is numerically shown that the rate of decay of the modal-amplitude functions is improved from O(n-2), where n is the mode number, to O(n-4), when the additional sloping-bottom mode is included in the representation. This fact substantially accelerates the convergence of the modal series and ensures the uniform convergence of the velocity field up to and including the boundaries.
机译:Massel(1993)和Porter&Staziker(1995)最近提出的扩展小幅度水波在可变测深区域上传播的扩展的缓坡方程,显示出与坡底边界条件不一致的现象,这使得它们相对于波能是非保守的。在当前的工作中,通过将波势的垂直分布表示为每个水平位置的局部垂直模式的一致收敛系列,从完整线性问题的变分公式中得出一致的耦合模式理论。该系列由与传播模式和所有渐逝模式相关的垂直本​​征函数组成,并且当底部的斜率不同于零时,将附加模式携带有关底部斜率的信息。以这种方式获得的耦合模式系统包含一个附加方程,以及所有其他方程中的附加相互作用项,并且当忽略附加模式时,可以简化为先前的扩展的缓坡方程。大量的数值结果表明,该模型可以精确满足底部边界条件,因此它是能量保守的。此外,从数值上显示,当附加倾斜底模式为时,模态振幅函数的衰减率从O(n-2)(其中n为模式编号)提高到O(n-4)。包含在表示中。这一事实大大加速了模态级数的收敛,并确保了速度场直至边界(包括边界)的均匀收敛。

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