A windy sea surface with Stokes waves
Fluid Dynamics
2026-08-04 v1 Atmospheric and Oceanic Physics
Abstract
Predicting the transition of wind-forced, gravito-capillary surface waves from smooth to corrugated states remains a longstanding problem in nonlinear wave mechanics. Solving driven-dissipative, nonlinear potential flow equations we map these waves ( cm) onto a Reynolds number -- wave energy phase-space. We identify a transition band separating smooth from corrugated wave states - the wave steepness exhibits a non-monotonic dependence on Reynolds number within this. Subharmonic (in)stability analysis reveals that the fastest-growing mode intensifies corrugations on alternate faces of the carrier wave, offering insights with broad implications for interfacial pattern-formation and oceanic remote-sensing.
Cite
@article{arxiv.2608.03657,
title = {A windy sea surface with Stokes waves},
author = {Nikhil Yewale and Anil Kumar and Vinod Kadari and Ratul Dasgupta},
journal= {arXiv preprint arXiv:2608.03657},
year = {2026}
}