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    A Composite Spectrum of Vertical Shear in the Upper Ocean

    Source: Journal of Physical Oceanography:;1981:;Volume( 011 ):;issue: 009::page 1258
    Author:
    Gargett, A. E.
    ,
    Hendricks, P. J.
    ,
    Sanford, T. B.
    ,
    Osborn, T. R.
    ,
    Williams, A. J.
    DOI: 10.1175/1520-0485(1981)011<1258:ACSOVS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Results from three separate velocity profilers operated nearly simultaneously in the northwest Atlantic in 1975 are used to form a composite shear spectrum over vertical wavelengths from 100 m down to a few centimeters. This exercise constitutes an intercomparison of the three different measurement techniques and reveals a shear spectrum which is approximately fiat at a WKB-scaled level from k = 0.01 cpm through k0 ≈ 0.1 cpm, then falls as k?1 to a buoyancy wavenumber k0 = (N3/?)1/2 determined by the local average Väisälä frequency N and the volume-averaged dissipation rate ?. Various consequences of the observed shear spectral shape are explored.
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      A Composite Spectrum of Vertical Shear in the Upper Ocean

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    contributor authorGargett, A. E.
    contributor authorHendricks, P. J.
    contributor authorSanford, T. B.
    contributor authorOsborn, T. R.
    contributor authorWilliams, A. J.
    date accessioned2017-06-09T14:45:58Z
    date available2017-06-09T14:45:58Z
    date copyright1981/09/01
    date issued1981
    identifier issn0022-3670
    identifier otherams-26275.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4163151
    description abstractResults from three separate velocity profilers operated nearly simultaneously in the northwest Atlantic in 1975 are used to form a composite shear spectrum over vertical wavelengths from 100 m down to a few centimeters. This exercise constitutes an intercomparison of the three different measurement techniques and reveals a shear spectrum which is approximately fiat at a WKB-scaled level from k = 0.01 cpm through k0 ≈ 0.1 cpm, then falls as k?1 to a buoyancy wavenumber k0 = (N3/?)1/2 determined by the local average Väisälä frequency N and the volume-averaged dissipation rate ?. Various consequences of the observed shear spectral shape are explored.
    publisherAmerican Meteorological Society
    titleA Composite Spectrum of Vertical Shear in the Upper Ocean
    typeJournal Paper
    journal volume11
    journal issue9
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1981)011<1258:ACSOVS>2.0.CO;2
    journal fristpage1258
    journal lastpage1271
    treeJournal of Physical Oceanography:;1981:;Volume( 011 ):;issue: 009
    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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