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    On the Importance of the Significant Slope in Empirical Wind-Wave Studies

    Source: Journal of Physical Oceanography:;1981:;Volume( 011 ):;issue: 004::page 569
    Author:
    Huang, Norden E.
    ,
    Long, Steven R.
    ,
    Bliven, L. F.
    DOI: 10.1175/1520-0485(1981)011<0569:OTIOTS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: The 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.
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      On the Importance of the Significant Slope in Empirical Wind-Wave Studies

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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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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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