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    Wind-Driven Circulation in a Fjord

    Source: Journal of Physical Oceanography:;1978:;Volume( 008 ):;issue: 004::page 703
    Author:
    Svendsen, Harald
    ,
    Thompson, Rory O. R. Y.
    DOI: 10.1175/1520-0485(1978)008<0703:WDCIAF>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Currents, temperature, salinity, wind, runoff and water level were observed for a month in the J?sen-fjord of southern Norway. Tide gages and currents show little semidiurnal tide. There is a strong diurnal signal in the upper 20 m, which a linear model shows to be caused by the wind. There is a week-long event in which the entire water-mass above the sill is flushed out; this is interpreted to be caused by downwelling outside the fjord. The strong stratification near the surface of the fjord greatly modifies the diurnal response of the fjord, but any density-driven mean circulation is at least an order of magnitude smaller than the wind-driven currents.
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      Wind-Driven Circulation in a Fjord

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4162661
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    contributor authorSvendsen, Harald
    contributor authorThompson, Rory O. R. Y.
    date accessioned2017-06-09T14:44:49Z
    date available2017-06-09T14:44:49Z
    date copyright1978/07/01
    date issued1978
    identifier issn0022-3670
    identifier otherams-25834.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162661
    description abstractCurrents, temperature, salinity, wind, runoff and water level were observed for a month in the J?sen-fjord of southern Norway. Tide gages and currents show little semidiurnal tide. There is a strong diurnal signal in the upper 20 m, which a linear model shows to be caused by the wind. There is a week-long event in which the entire water-mass above the sill is flushed out; this is interpreted to be caused by downwelling outside the fjord. The strong stratification near the surface of the fjord greatly modifies the diurnal response of the fjord, but any density-driven mean circulation is at least an order of magnitude smaller than the wind-driven currents.
    publisherAmerican Meteorological Society
    titleWind-Driven Circulation in a Fjord
    typeJournal Paper
    journal volume8
    journal issue4
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1978)008<0703:WDCIAF>2.0.CO;2
    journal fristpage703
    journal lastpage712
    treeJournal of Physical Oceanography:;1978:;Volume( 008 ):;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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