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    The Detection by ERTS-1 of Wind-Induced Ocean Surface Features in the Lee of the Antilles Islands

    Source: Journal of Physical Oceanography:;1974:;Volume( 004 ):;issue: 004::page 594
    Author:
    Cram, Richard
    ,
    Hanson, Kirby
    DOI: 10.1175/1520-0485(1974)004<0594:TDBEOW>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Photographic data received from the ERTS-1 satellite over the Lesser Antilles Islands show distinct ocean features on the leeward side of each island. Attempts to relate these features to ocean eddy formations with the aid of ground truth data proved unsuccessful. However, surface and upper air wind data indicate a good correlation with the size, shape, and downwind extent of the ocean features. Studies to date indicate strongly that these features result from horizontal differences in sea surface roughness due to the wind-shadow effect of the islands. The results suggest that horizontal variations in the reflectance of the sea surface will make remote sensing of the ocean mixed layer more difficult than previously anticipated. The surface reflection seems to be large enough to mask the smaller variations in backscattered energy from the mixed layer. Efforts to limit the effect of surface reflectance by photographic differencing of two multi-spectral scanner bands were unsuccessful.
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      The Detection by ERTS-1 of Wind-Induced Ocean Surface Features in the Lee of the Antilles Islands

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4162250
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    contributor authorCram, Richard
    contributor authorHanson, Kirby
    date accessioned2017-06-09T14:43:58Z
    date available2017-06-09T14:43:58Z
    date copyright1974/10/01
    date issued1974
    identifier issn0022-3670
    identifier otherams-25464.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162250
    description abstractPhotographic data received from the ERTS-1 satellite over the Lesser Antilles Islands show distinct ocean features on the leeward side of each island. Attempts to relate these features to ocean eddy formations with the aid of ground truth data proved unsuccessful. However, surface and upper air wind data indicate a good correlation with the size, shape, and downwind extent of the ocean features. Studies to date indicate strongly that these features result from horizontal differences in sea surface roughness due to the wind-shadow effect of the islands. The results suggest that horizontal variations in the reflectance of the sea surface will make remote sensing of the ocean mixed layer more difficult than previously anticipated. The surface reflection seems to be large enough to mask the smaller variations in backscattered energy from the mixed layer. Efforts to limit the effect of surface reflectance by photographic differencing of two multi-spectral scanner bands were unsuccessful.
    publisherAmerican Meteorological Society
    titleThe Detection by ERTS-1 of Wind-Induced Ocean Surface Features in the Lee of the Antilles Islands
    typeJournal Paper
    journal volume4
    journal issue4
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1974)004<0594:TDBEOW>2.0.CO;2
    journal fristpage594
    journal lastpage600
    treeJournal of Physical Oceanography:;1974:;Volume( 004 ):;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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