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    Current Measurements along the Shelf Break in the Gulf of Alaska

    Source: Journal of Physical Oceanography:;1986:;Volume( 016 ):;issue: 011::page 1985
    Author:
    Reed, R. K.
    ,
    Schumacher, J. D.
    DOI: 10.1175/1520-0485(1986)016<1985:CMATSB>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Data from current moorings at four sites near the shelf break in the Gulf of Alaska are used to present information on the flow, to examine the effects of local winds, and especially to investigate momentum transfer between the offshore and inshore circulation. Net flow at the shelf break in the central and western appears to be similar through the year, but it intensifies appreciably in winter in the northeast Gulf. Only records in the northeast Gulf suggest significant effects on flow by local winds. The eddy fluxes of momentum at the shelf break were extremely small. Although the offshore Alaskan Stream was previously found to transfer momentum toward shore, this flux apparently does not reach the shelf break and influence shelf waters. It appears rather that the gradients of heat and salt observed near the shelf edge result from offshore effects of the coastal flow.
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      Current Measurements along the Shelf Break in the Gulf of Alaska

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4164064
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    contributor authorReed, R. K.
    contributor authorSchumacher, J. D.
    date accessioned2017-06-09T14:48:09Z
    date available2017-06-09T14:48:09Z
    date copyright1986/11/01
    date issued1986
    identifier issn0022-3670
    identifier otherams-27097.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4164064
    description abstractData from current moorings at four sites near the shelf break in the Gulf of Alaska are used to present information on the flow, to examine the effects of local winds, and especially to investigate momentum transfer between the offshore and inshore circulation. Net flow at the shelf break in the central and western appears to be similar through the year, but it intensifies appreciably in winter in the northeast Gulf. Only records in the northeast Gulf suggest significant effects on flow by local winds. The eddy fluxes of momentum at the shelf break were extremely small. Although the offshore Alaskan Stream was previously found to transfer momentum toward shore, this flux apparently does not reach the shelf break and influence shelf waters. It appears rather that the gradients of heat and salt observed near the shelf edge result from offshore effects of the coastal flow.
    publisherAmerican Meteorological Society
    titleCurrent Measurements along the Shelf Break in the Gulf of Alaska
    typeJournal Paper
    journal volume16
    journal issue11
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1986)016<1985:CMATSB>2.0.CO;2
    journal fristpage1985
    journal lastpage1990
    treeJournal of Physical Oceanography:;1986:;Volume( 016 ):;issue: 011
    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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