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contributor authorHuang, Norden E.
contributor authorLong, Steven R.
contributor authorBliven, L. F.
date accessioned2017-06-09T14:45:50Z
date available2017-06-09T14:45:50Z
date copyright1981/04/01
date issued1981
identifier issn0022-3670
identifier otherams-26219.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4163089
description abstractThe significant slope of a random wave field is found to be an important parameter in empirical wind-wave studies. This significant slope Ss is defined as Ss = (?2)½/?0, with ?2 as the mean-square surface elevation and ?0 as the wavelength corresponding to the waves at the peak of the spectrum. With this parameter, the relationship between ? and ñ is reduced to an identity expressing a pure geometric measure of the sea state, because ?ñ4 = (2πSs)2. By applying the significant slope as a parameter explicitly, we proposed that the traditional empirical formulas relating the nondimensional energy ?, fetch x? and frequency ñ be combined into a single unified relationship as ?ñ/x? = (9/40)Ss9/4. This unified empirical formula governs the wind-wave data equally as well in the field as in the laboratory.
publisherAmerican Meteorological Society
titleOn the Importance of the Significant Slope in Empirical Wind-Wave Studies
typeJournal Paper
journal volume11
journal issue4
journal titleJournal of Physical Oceanography
identifier doi10.1175/1520-0485(1981)011<0569:OTIOTS>2.0.CO;2
journal fristpage569
journal lastpage573
treeJournal of Physical Oceanography:;1981:;Volume( 011 ):;issue: 004
contenttypeFulltext


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