The speed of breaking waves controls sea surface drag
Alex Ayet, Bertrand Chapron, Peter Sutherland, Gabriel G. Katul

TL;DR
This paper introduces a measurable wave breaking velocity linked to wind speed, providing a physical basis for the Beaufort scale and improving understanding of wind-wave coupling and surface drag.
Contribution
It formalizes the concept of breaking wave velocity as a physical parameter, advancing beyond roughness length models for wind-wave interaction.
Findings
Breaking wave velocity increases with wind speed.
Breaking waves impede turbulent eddy formation.
The wave velocity can be measured remotely.
Abstract
The coupling between wind-waves and atmospheric surface layer turbulence sets surface drag. This coupling is however usually represented through a roughness length. Originally suggested on purely dimensional grounds, this roughness length does not directly correspond to a measurable physical quantity of the wind-and-wave system. Here, to go beyond this representation, we formalize ideas underlying the Beaufort scale by quantifying the velocity of breaking short waves that are the most coupled to near-surface wind. This velocity increases with wind speed, reflecting the fact that stronger winds can be visually identified by longer (and faster) breakers becoming predominant on the sea surface. A phenomenological turbulence model further shows that this velocity is associated with breaking waves that impede the most the formation of turbulent eddies. Scales of such eddies are then…
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Taxonomy
TopicsOcean Waves and Remote Sensing · Aeolian processes and effects · Tropical and Extratropical Cyclones Research
