Gravity Water Waves over Constant Vorticity Flows: From Laminar Flows to Touching Waves.

IF 0.7
Water waves (Cham, Switzerland) Pub Date : 2026-01-01 Epub Date: 2025-10-27 DOI:10.1007/s42286-025-00127-4
Francisco Gonçalves
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Abstract

In a recent paper, Hur and Wheeler (J Fluid Mech 896:1, 2020) proved the existence of periodic steady water waves over an infinitely deep, two-dimensional and constant vorticity flow under the influence of gravity. These solutions include overhanging wave profiles, some of which exhibit surfaces that touch at a point and thereby enclose a bubble of air. We extend these results by formulating a problem that encompasses both infinitely deep and finitely deep flows, and by proving the existence of a continuous curve of water waves that connects a laminar flow to a touching wave for fixed, nonzero gravity. This implies the existence of a wave profile featuring a vertical tangent at a point, which is not overhanging, and is referred to as a breaking wave. We also study the behavior of critical layers, which are points where the horizontal velocity vanishes, near the surface. In particular, this result holds for arbitrary vorticity.

恒定涡度流上的重力水波:从层流到接触波。
在最近的一篇论文中,Hur和Wheeler (J Fluid Mech 896:1, 2020)证明了在重力影响下的无限深、二维、恒涡度流中存在周期性稳定水波。这些解决方案包括悬垂的波浪剖面,其中一些波浪剖面的表面在一点上接触,从而包围了一个气泡。我们通过制定一个包含无限深和有限深流动的问题来扩展这些结果,并通过证明在固定的非零重力下连接层流和接触波的水波连续曲线的存在。这意味着存在一个波浪剖面,其特征是在某一点上具有垂直切线,而不是悬垂,并且被称为破碎波。我们还研究了临界层的行为,临界层是水平速度消失的点,靠近地表。特别地,这个结果适用于任意涡度。
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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