Gravity water waves over constant vorticity flows: From laminar flows to touching waves

Fuente: arXiv
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Main Author: Gonçalves, Francisco
Format: Preprint
Published: 2025
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author Gonçalves, Francisco
author_facet Gonçalves, Francisco
contents In a recent paper, Hur & Wheeler [J. Differential Equations, 338:572-590, 2022] 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 behaviour of critical layers, which are points where the horizontal velocity vanishes, near the surface. In particular, this result holds for arbitrary vorticity.
format Preprint
id arxiv_https___arxiv_org_abs_2505_00417
institution arXiv
publishDate 2025
record_format arxiv
spellingShingle Gravity water waves over constant vorticity flows: From laminar flows to touching waves
Gonçalves, Francisco
Analysis of PDEs
35Q31, 35Q35, 76B03, 76B15
In a recent paper, Hur & Wheeler [J. Differential Equations, 338:572-590, 2022] 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 behaviour of critical layers, which are points where the horizontal velocity vanishes, near the surface. In particular, this result holds for arbitrary vorticity.
title Gravity water waves over constant vorticity flows: From laminar flows to touching waves
topic Analysis of PDEs
35Q31, 35Q35, 76B03, 76B15
url https://arxiv.org/abs/2505.00417