The role of constant vorticity on weakly nonlinear surface gravity waves

被引:0
|
作者
Manna, M. A. [1 ]
Noubissie, S. [2 ]
Touboul, J. [3 ]
Simon, B. [3 ]
Kraenkel, R. A. [4 ]
机构
[1] Univ Montpellier, Lab Charles Coulomb L2C, CNRS, Montpellier, France
[2] Univ Dschang, Inst Technol, POB 134, Bandjoun, Cameroon
[3] Univ Toulon & Var, Aix Marseille Univ, MIO, CNRS,IRD, Toulon, France
[4] Univ Estadual Paulista, Inst Fis Teor UNESP, Rua Dr Bento Teobaldo Ferraz 271 Bloco 2, BR-01140070 Sao Paulo, Brazil
基金
巴西圣保罗研究基金会;
关键词
Constant vorticities - Dispersive parameters - Dispersive properties - Fluid velocities - Non-linear parameters - Nonlinear dispersive - Systems of equations - Weakly non-linear;
D O I
10.1016/j.wavemoti.2020.102702
中图分类号
O42 [声学];
学科分类号
070206 ; 082403 ;
摘要
This manuscript describes the derivation of systems of equations for weakly nonlinear gravity waves in shallow water in the presence of constant vorticity. The derivation is based on a multi-layer generalization of the traditional columnar Ansatz. A perturbative development in a nonlinear parameter and a dispersive parameter allow us to obtain sets of equations, for the horizontal fluid velocity and the free surface, able to describe propagation of weakly nonlinear and dispersive surface waves moving in water with some prescribed initial constant vorticity. We have shown that vorticity plays a central role on the dispersive properties of the system. When it is weak, it acts as a correction in linear and nonlinear dispersive terms. When stronger, it can also influence the nondispersive behavior of the system. Explicit steady solutions of the system corresponding to zero, weak, normal or strong vorticity are obtained. They correspond to solitary waves. Evolution of the soliton celerity, amplitude and width for these four cases are discussed. (C) 2021 Elsevier B.V. All rights reserved.
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页数:13
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