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    A Study of the Wavenumber Spectra of Short Water Waves in the Ocean. Part II: Spectral Model and Mean Square Slope

    Source: Journal of Atmospheric and Oceanic Technology:;1997:;volume( 014 ):;issue: 005::page 1174
    Author:
    Hwang, Paul A.
    DOI: 10.1175/1520-0426(1997)014<1174:ASOTWS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: This paper presents a wavenumber spectral model of the surface water waves in the capillary?gravity regime. The database for the analysis consists of spatial and temporal measurements of surface slopes obtained from a scanning slope sensor buoy operating in free-drift mode in the Atlantic Ocean. These data indicate that the contribution of mean square slopes from capillary?gravity waves (wavelengths from 4 mm to 6 cm) is a significant portion of the total mean square slopes. The resulting mean square slopes derived from the proposed spectral model are in excellent agreement with existing field datasets. The properties of short waves, including the mean square slopes and wind speed dependence of the spectral intensity of individual wave components, derived from optical and microwave sensors are also compared. Significant differences in terms of the magnitudes of the mean square slopes and the exponents of wind speed dependence are found. Some of the possible explanations of the discrepancies are explored.
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      A Study of the Wavenumber Spectra of Short Water Waves in the Ocean. Part II: Spectral Model and Mean Square Slope

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4148646
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    contributor authorHwang, Paul A.
    date accessioned2017-06-09T14:08:40Z
    date available2017-06-09T14:08:40Z
    date copyright1997/10/01
    date issued1997
    identifier issn0739-0572
    identifier otherams-1322.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4148646
    description abstractThis paper presents a wavenumber spectral model of the surface water waves in the capillary?gravity regime. The database for the analysis consists of spatial and temporal measurements of surface slopes obtained from a scanning slope sensor buoy operating in free-drift mode in the Atlantic Ocean. These data indicate that the contribution of mean square slopes from capillary?gravity waves (wavelengths from 4 mm to 6 cm) is a significant portion of the total mean square slopes. The resulting mean square slopes derived from the proposed spectral model are in excellent agreement with existing field datasets. The properties of short waves, including the mean square slopes and wind speed dependence of the spectral intensity of individual wave components, derived from optical and microwave sensors are also compared. Significant differences in terms of the magnitudes of the mean square slopes and the exponents of wind speed dependence are found. Some of the possible explanations of the discrepancies are explored.
    publisherAmerican Meteorological Society
    titleA Study of the Wavenumber Spectra of Short Water Waves in the Ocean. Part II: Spectral Model and Mean Square Slope
    typeJournal Paper
    journal volume14
    journal issue5
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1997)014<1174:ASOTWS>2.0.CO;2
    journal fristpage1174
    journal lastpage1186
    treeJournal of Atmospheric and Oceanic Technology:;1997:;volume( 014 ):;issue: 005
    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
    yabeshDSpacePersian