Qualitative difference between large waves in deep and shallow fluid formulations

IF 2.1 3区 物理与天体物理 Q2 ACOUSTICS
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引用次数: 0

Abstract

The note addresses a qualitative difference between shallow (vertically confined) and deep (vertically non-confined) fluid geometries for stationary internal solitary waves. It is shown that in a deep fluid, the propagation velocity of large amplitude wave (with a vortex inside) is greater than the velocity predicted by small but finite amplitude theory, known as the Benjamin-Ono model. This effect has been found both asymptotically and experimentally. For the case of a shallow fluid, the situation is qualitatively different. The speed of a wave with vortex inside is smaller than that predicted by the Korteweg-de Vries theory. The reported observation could distinguish wave motions in shallow (confined) and deep (non-confined) geometries and seems to be important in a variety of applications.

深层和浅层流体公式中大波浪的定性差异。
本说明讨论了静止内孤波在浅层(垂直约束)和深层(垂直非约束)流体几何之间的定性差异。研究表明,在深层流体中,大振幅波(内部有涡旋)的传播速度大于小振幅但有限振幅理论(即本杰明-奥诺模型)预测的速度。这种效应在渐近和实验中都有发现。对于浅层流体,情况则有本质区别。内含漩涡的波的速度小于 Korteweg-de Vries 理论预测的速度。报告中的观察结果可以区分浅层(封闭)和深层(非封闭)几何中的波运动,似乎在各种应用中都很重要。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Wave Motion
Wave Motion 物理-力学
CiteScore
4.10
自引率
8.30%
发文量
118
审稿时长
3 months
期刊介绍: Wave Motion is devoted to the cross fertilization of ideas, and to stimulating interaction between workers in various research areas in which wave propagation phenomena play a dominant role. The description and analysis of wave propagation phenomena provides a unifying thread connecting diverse areas of engineering and the physical sciences such as acoustics, optics, geophysics, seismology, electromagnetic theory, solid and fluid mechanics. The journal publishes papers on analytical, numerical and experimental methods. Papers that address fundamentally new topics in wave phenomena or develop wave propagation methods for solving direct and inverse problems are of interest to the journal.
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