The equilibrium range in wind-driven wave spectra is characterized to have an f-4 form in deep water (k-5/2 shallow-water form). Absolute energy levels for six physically diverse sites are shown to be well fit by an expression involving the wind speed measured at a fraction of a wavelength above the sea surface in combination with the phase speed of the spectral peak. Observed energy levels suggest that nonlinear wave-wave interactions are capable of maintaining the observed energy-flux balance in the equilibrium range. Copyright, Published in 2004 by the American Geophysical Union.
CITATION STYLE
Resio, D. T., Long, C. E., & Vincent, C. L. (2004). Equilibrium-range constant in wind-generated wave spectra. Journal of Geophysical Research: Oceans, 109(1). https://doi.org/10.1029/2003jc001788
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