Johnson R S
School of Mathematics and Statistics, University of Newcastle upon Tyne, Newcastle upon Tyne, UK.
Philos Trans A Math Phys Eng Sci. 2007 Sep 15;365(1858):2359-76. doi: 10.1098/rsta.2007.2013.
The problem of edge waves as an example within classical water-wave theory is described by presenting an overview of some of the theories that have been offered for this phenomenon. The appropriate governing equations and boundary conditions are formulated, and then the important discoveries of Stokes and Ursell, concerning the travelling edge wave, are presented. (We do not address the corresponding problem of standing waves.) Thus, the linear problem and its spectrum are constructed; in addition, we also present the linear long-wave approximation to the problem, as well as Whitham's weakly nonlinear extension to Stokes' original theory. All these discussions are based on the same formulation of the problem, allowing an immediate comparison of the results, whether this be in terms of different approximations or whether the theory be for an irrotational flow or not. Gerstner's exact solution of the water-wave problem is then briefly described, together with a transformation that produces an exact solution of the full equations for the edge wave. The form of this solution is then used as the basis for a multiple-scale description of the edge wave over a slowly varying depth; this leads to a version of the shallow-water equations which has an exact solution that corresponds to the edge wave. Some examples of the theoretical predictions for the run-up pattern are presented. We conclude with three variants of nonlinear model equations that may prove useful in the study of edge waves and, particularly, the interaction of different modes.
通过概述针对边缘波这一现象所提出的一些理论,来描述经典水波理论中边缘波的问题。给出了合适的控制方程和边界条件,接着介绍了斯托克斯(Stokes)和厄塞尔(Ursell)关于行进边缘波的重要发现。(我们不讨论驻波的相应问题。)由此构建了线性问题及其频谱;此外,我们还给出了该问题的线性长波近似,以及惠特姆(Whitham)对斯托克斯原始理论的弱非线性扩展。所有这些讨论都基于相同的问题表述,便于直接比较结果,无论是从不同近似的角度,还是从理论是针对无旋流与否的角度。然后简要描述了格斯特纳(Gerstner)对水波问题的精确解,以及一种能得出边缘波完整方程精确解的变换。接着将此解的形式用作对缓变深度上边缘波进行多尺度描述的基础;这导出了浅水方程的一个版本,其具有与边缘波对应的精确解。给出了一些关于爬高模式理论预测的例子。最后我们给出了三个非线性模型方程的变体,它们可能在边缘波研究中,特别是在不同模式相互作用的研究中证明是有用的。