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    Geostrophic Departure, Local Turning, Speed Change, and Eddy Flux: A New Perspective

    Source: Journal of Physical Oceanography:;1991:;Volume( 021 ):;issue: 011::page 1684
    Author:
    Chew, Frank
    ,
    Bushnell, Mark H.
    DOI: 10.1175/1520-0485(1991)021<1684:GDLTSC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Conjunctions of meander passages and cross-stream eddy momentum fluxes are common in western boundary currents. To explore the mechanism linking them, we offer a diagnostic equation of their time-dependent motions. The equation is embodied in the more explicit form of a hodograph with two characteristics: a tilt and a veering/backing. The veering/backing is in response to the changing geostrophic departure, and the tilt to the change in the speed of the flow, which can be zero, positive, or negative. This direct approach to the kinematic field?its pattern and its change?led to a hypothesis on the linkage that the cross-stream eddy momentum flux is driven by the downstream pressure gradient force in the supergeostrophic segment of the meandering flow.
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      Geostrophic Departure, Local Turning, Speed Change, and Eddy Flux: A New Perspective

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4164883
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    contributor authorChew, Frank
    contributor authorBushnell, Mark H.
    date accessioned2017-06-09T14:50:10Z
    date available2017-06-09T14:50:10Z
    date copyright1991/11/01
    date issued1991
    identifier issn0022-3670
    identifier otherams-27834.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4164883
    description abstractConjunctions of meander passages and cross-stream eddy momentum fluxes are common in western boundary currents. To explore the mechanism linking them, we offer a diagnostic equation of their time-dependent motions. The equation is embodied in the more explicit form of a hodograph with two characteristics: a tilt and a veering/backing. The veering/backing is in response to the changing geostrophic departure, and the tilt to the change in the speed of the flow, which can be zero, positive, or negative. This direct approach to the kinematic field?its pattern and its change?led to a hypothesis on the linkage that the cross-stream eddy momentum flux is driven by the downstream pressure gradient force in the supergeostrophic segment of the meandering flow.
    publisherAmerican Meteorological Society
    titleGeostrophic Departure, Local Turning, Speed Change, and Eddy Flux: A New Perspective
    typeJournal Paper
    journal volume21
    journal issue11
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1991)021<1684:GDLTSC>2.0.CO;2
    journal fristpage1684
    journal lastpage1689
    treeJournal of Physical Oceanography:;1991:;Volume( 021 ):;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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