Abstract
An empirical spectral equation for fetch-limited deep-water wind waveswas derived by applying similarity analysis to wind and wave data recorded at the Lake Michigan Research Tower near Muskegon, Mich., during the autumn of 1967. The field data indicates that both the equilibrium range coefficient, β in S(ω) = βg2ω−5 and the dimensionless peak-frequency parameter, ωmU*/g, vary with Fo, where Fo = gF/U*2 is the dimensionless fetch parameter with respect to fetch F and friction velocity U*. The equation produces reasonably good results in estimating actual wave spectra, provided sufficient duration is achieved in the wind field. The equation also indicates that a fully-developed state will not be reached at a steady wind speed as the very low-frequency waves grow continuously with increasing fetch.
