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    Mixing and Intrusions in a Rotating Cold-Core Feature off Cape Blanco, Oregon

    Source: Journal of Physical Oceanography:;1988:;Volume( 018 ):;issue: 006::page 823
    Author:
    Moum, James N.
    ,
    Caldwell, Douglas R.
    ,
    Stabeno, Phyllis J.
    DOI: 10.1175/1520-0485(1988)018<0823:MAIIAR>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: During August 1986, a large cold anomaly was observed in satellite and in situ measurements near Cape Blanco at 42°N, 126°30?W off the Pacific Coast. Detailed vertical profiles of temperature, conductivity, turbulent dissipation, and horizontal currents showed 1) surface water temperature changes as large as 2 degrees in 1 kilometer (but smaller gradients at depth); 2) a structure in the mean currents resembling that of either a cyclonic eddy or a current meander, 3) a current field in geostrophic balance on scales of 10 km and greater, 4) a region of intrusions on the northern side of the eddy; 5) a concentration of turbulence (as indicated by the kinetic-energy dissipation rate) on the edges of the eddy and in the region of intrusions, the core of the eddy being turbulence-free; and 6) a substantial change in the surface structure in 24 hours.
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      Mixing and Intrusions in a Rotating Cold-Core Feature off Cape Blanco, Oregon

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4164368
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    contributor authorMoum, James N.
    contributor authorCaldwell, Douglas R.
    contributor authorStabeno, Phyllis J.
    date accessioned2017-06-09T14:48:53Z
    date available2017-06-09T14:48:53Z
    date copyright1988/06/01
    date issued1988
    identifier issn0022-3670
    identifier otherams-27370.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4164368
    description abstractDuring August 1986, a large cold anomaly was observed in satellite and in situ measurements near Cape Blanco at 42°N, 126°30?W off the Pacific Coast. Detailed vertical profiles of temperature, conductivity, turbulent dissipation, and horizontal currents showed 1) surface water temperature changes as large as 2 degrees in 1 kilometer (but smaller gradients at depth); 2) a structure in the mean currents resembling that of either a cyclonic eddy or a current meander, 3) a current field in geostrophic balance on scales of 10 km and greater, 4) a region of intrusions on the northern side of the eddy; 5) a concentration of turbulence (as indicated by the kinetic-energy dissipation rate) on the edges of the eddy and in the region of intrusions, the core of the eddy being turbulence-free; and 6) a substantial change in the surface structure in 24 hours.
    publisherAmerican Meteorological Society
    titleMixing and Intrusions in a Rotating Cold-Core Feature off Cape Blanco, Oregon
    typeJournal Paper
    journal volume18
    journal issue6
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1988)018<0823:MAIIAR>2.0.CO;2
    journal fristpage823
    journal lastpage833
    treeJournal of Physical Oceanography:;1988:;Volume( 018 ):;issue: 006
    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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