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

机译:浅水流中孤立波和波浪孔的演化   在具有底部摩擦的渐变斜坡上

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摘要

This paper considers the propagation of shallow-water solitary and nonlinearperiodic waves over a gradual slope with bottom friction in the framework of avariable-coefficient Korteweg-de Vries equation. We use the Whitham averagingmethod, using a recent development of this theory for perturbed integrableequations. This general approach enables us not only to improve known resultson the adiabatic evolution of isolated solitary waves and periodic wave trainsin the presence of variable topography and bottom friction, modeled by theChezy law, but also importantly, to study the effects of these factors on thepropagation of undular bores, which are essentially unsteady in the systemunder consideration. In particular, it is shown that the combined action ofvariable topography and bottom friction generally imposes certain globalrestrictions on the undular bore propagation so that the evolution of theleading solitary wave can be substantially different from that of an isolatedsolitary wave with the same initial amplitude. This non-local effect is due tononlinear wave interactions within the undular bore and can lead to anadditional solitary wave amplitude growth, which cannot be predicted in theframework of the traditional adiabatic approach to the propagation of solitarywaves 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,研究这些因素对传播的影响。孔洞,在所考虑的系统中基本上是不稳定的。特别地,表明了可变形貌和底部摩擦的共同作用通常对波状孔的传播施加一定的整体限制,使得主导孤波的演化可能与具有相同初始振幅的孤立孤波的演化实质上不同。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,并可能导致孤波振幅的增加,这在传统绝热方法在缓慢变化的介质中传播孤波的传统方法中无法预测。

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