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Simulations and experiments of short intense envelope solitons of surface water waves

机译:表面水波短强包络孤子的模拟与实验

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摘要

The problem of existence of stable nonlinear groups of gravity waves in deep water is considered by means of laboratory and numerical simulations with the focus on strongly nonlinear waves. Wave groups with steepness up to Acrωm2/g ≈ 0.30 are reproduced in laboratory experiments (Acr is the wave crest amplitude, ωm is the mean angular frequency, and g is the gravity acceleration). We show that the groups remain stable and exhibit neither noticeable radiation nor structural transformation for more than 60 wavelengths or about 15-30 group lengths. These solitary wave patterns differ from the conventional envelope solitons, as only a few individual waves are contained in the group. Very good agreement is obtained between the laboratory results and numerical simulations of the potential Euler equations. The envelope soliton solution of the nonlinear Schr?dinger equation is shown to be a reasonable first approximation for specifying the wave-maker driving signal. The short intense envelope solitons possess vertical asymmetry similar to regular Stokes waves with the same frequency and crest amplitude. Nonlinearity is found to have remarkably stronger effect on the speed of envelope solitons in comparison to the nonlinear correction to the Stokes wave velocity.
机译:通过以强非线性波为重点的实验室和数值模拟,研究了深水中稳定非线性非线性波群的存在问题。在实验室实验中,再现了高达Acrωm2/ g≈0.30的陡峭波组(Acr是波峰幅度,ωm是平均角频率,g是重力加速度)。我们表明,这些基团保持稳定,并且对于超过60个波长或大约15-30个基团长度,既没有显示出明显的辐射,也没有显示出结构转变。这些孤立的波型与常规的包络孤子不同,因为该组中仅包含几个单独的波。在实验室结果和潜在的欧拉方程数值模拟之间获得了很好的一致性。非线性薛定?方程的包络孤子解被证明是用于指定造波器驱动信号的合理一阶近似。短而强烈的包络孤子具有垂直不对称性,类似于具有相同频率和波峰振幅的常规斯托克斯波。与对斯托克斯波速的非线性校正相比,发现非线性对包络孤子的速度具有明显更强的影响。

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