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    Recirculation Gyres Forced by a Beta-Plane Jet

    Source: Journal of Physical Oceanography:;1996:;Volume( 026 ):;issue: 004::page 492
    Author:
    Jayne, Steven R.
    ,
    Hogg, Nelson G.
    ,
    Malanotte-Rizzoli, Paola
    DOI: 10.1175/1520-0485(1996)026<0492:RGFBAB>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A numerical model, with quasigeostrophic and barotropic dynamics, is used to study the forcing of mean flows by an unstable jet. The initially zonal jet has specified shape and transport at the western inflow boundary and is sufficiently intense and narrow that the potential vorticity gradient changes sign, giving rise to barotropic instabilities. The resulting eddies act to smooth the potential vorticity anomalies transported into the domain and produce homogenized regions in which recirculations develop to the north and south of the jet. The intensity of these recirculations, as a function of nondimensional beta, is investigated and a simple, kinematic interpretation offered.
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      Recirculation Gyres Forced by a Beta-Plane Jet

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4165619
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    contributor authorJayne, Steven R.
    contributor authorHogg, Nelson G.
    contributor authorMalanotte-Rizzoli, Paola
    date accessioned2017-06-09T14:51:59Z
    date available2017-06-09T14:51:59Z
    date copyright1996/04/01
    date issued1996
    identifier issn0022-3670
    identifier otherams-28497.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4165619
    description abstractA numerical model, with quasigeostrophic and barotropic dynamics, is used to study the forcing of mean flows by an unstable jet. The initially zonal jet has specified shape and transport at the western inflow boundary and is sufficiently intense and narrow that the potential vorticity gradient changes sign, giving rise to barotropic instabilities. The resulting eddies act to smooth the potential vorticity anomalies transported into the domain and produce homogenized regions in which recirculations develop to the north and south of the jet. The intensity of these recirculations, as a function of nondimensional beta, is investigated and a simple, kinematic interpretation offered.
    publisherAmerican Meteorological Society
    titleRecirculation Gyres Forced by a Beta-Plane Jet
    typeJournal Paper
    journal volume26
    journal issue4
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1996)026<0492:RGFBAB>2.0.CO;2
    journal fristpage492
    journal lastpage504
    treeJournal of Physical Oceanography:;1996:;Volume( 026 ):;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
    yabeshDSpacePersian