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Evolution of solitary waves and undular bores in shallow-water flows over a gradual slope with bottom friction

机译:浅水流在具有底部摩擦的缓坡上的孤立波和波浪状钻孔的演变

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摘要

This paper considers the propagation of shallow-water solitary and nonlinear periodic waves over a gradual slope with bottom friction in the framework of a variable-coefficient Korteweg-de Vries equation. We use the Whitham averaging method, using a recent development of this theory for perturbed integrable equations. This general approach enables us not only to improve known results on the adiabatic evolution of isolated solitary waves and periodic wave trains in the presence of variable topography and bottom friction, modelled by the Chezy law, but also, importantly, to study the effects of these factors on the propagation of undular bores, which are essentially unsteady in the system under consideration. In particular, it is shown that the combined action of variable topography and bottom friction generally imposes certain global restrictions on the undular bore propagation so that the evolution of the leading solitary wave can be substantially different from that of an isolated solitary wave with the same initial amplitude. This non-local effect is due to nonlinear wave interactions within the undular bore and can lead to an additional solitary wave amplitude growth, which cannot be predicted in the framework of the traditional adiabatic approach to the propagation of solitary waves in slowly varying media.
机译:本文在变系数Korteweg-de Vries方程的框架内考虑了浅水孤波和非线性周期波在具有底摩擦的缓坡上的传播。我们使用Whitham平均方法,对扰动可积方程使用该理论的最新发展。这种通用方法不仅使我们能够改进由切兹定律建模的,在具有可变地形和底部摩擦的情况下孤立孤波和周期波列的绝热演化的已知结果,而且重要的是,研究这些影响影响孔状孔扩展的因素,在所考虑的系统中这基本上是不稳定的。尤其是,已表明,形变和底部摩擦的共同作用通常会对孔状孔的传播施加一定的整体限制,因此,主导孤波的演化可能与具有相同初始初始的孤立孤波的演化大不相同。振幅。这种非局部效应是由于波状孔内的非线性波相互作用引起的,并且可能导致额外的孤立波振幅增长,这在传统的绝热方法在缓慢变化的介质中传播孤立波的框架中是无法预测的。

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