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arXiv 1909.08501physics.flu-dynphysics.ao-phphysics.geo-ph
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均匀流上深水重力波三重共振

Deep water gravity wave triad resonances on uniform flow

David Kouskoulas, Yaron Toledo

摘要:

本文介绍了重力波在均匀流中反向传播时的三重共振。它们是由多值和各向异性分散产生的,甚至在深水中也会出现。相反,现有的文献表明,非简并深水三元组需要不均匀性或毛细管效应。从这个意义上说,新的共振是第一次。共振存在的分析条件可以简化为普适常数。三波相互作用模型的解决方案,适用于波流问题,显示制度,其中占主导地位的方向,速度和强度的共振能量转移波数尺度之间的不同。这表明均匀电流是空间不均匀性的基本来源。新的共振显着修改图片的波流场的非线性相互作用。由于共振是二次的,它们也将主导众所周知的四重相互作用。

英文摘要:

Triad resonances for gravity waves propagating in opposite direction with respect to uniform current are introduced. They are produced by multivalued and anisotropic dispersion and occur even in deep water. In contrast, existing literature suggests non-degenerate deep water triads require inhomogeneity or capillary effects. In this sense, the new resonances are a first of their kind. Analytical conditions for the existence of resonance may be reduced to universal constants. Solution of a three-wave interaction model, adapted to the wave-current problem, shows regimes wherein the dominant direction, speed and strength of resonant energy transfer differs between wavenumber scales. This suggests uniform current is a fundamental source of spatial inhomogeneity. The new resonances significantly modify the picture of nonlinear interactions in wave-current fields. Since the resonances are quadratic, they will also dominate well known quartet interactions.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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