Experiments demonstrate that wave scale and wind affect breaking dissipation via onset threshold changes, yielding a scaling ΔE_br/E0 proportional to crest asymmetry, steepness, and breaking duration.
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Breaking-induced energy dissipation of surface gravity waves at varying scales and co-flowing wind stresses
Experiments demonstrate that wave scale and wind affect breaking dissipation via onset threshold changes, yielding a scaling ΔE_br/E0 proportional to crest asymmetry, steepness, and breaking duration.