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    An Upper Bound on the Size of Sub-mesoscale Coherent Vortices

    Source: Journal of Physical Oceanography:;1989:;Volume( 019 ):;issue: 002::page 233
    Author:
    Thompson, Luanne
    ,
    Young, W. R.
    DOI: 10.1175/1520-0485(1989)019<0233:AUBOTS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Laboratory experiments show that ageostrophic instability can ?break up? a parallel flow into a sequence of axisymmetric eddies. This is a plausible scenario for the generation of sub-mesoscale coherent Vortices (SCVs). Here we show that conservation of mass, energy and potential vorticity enables one to very simply calculate the radius of the axisymmetric eddy and the wavelength of the nonlinear instability. The latter agrees more closely with laboratory experiments than does the wavelength predicted by linearized stability theory. It energy is not conserved, say because of wave radiation into the lower layer, then the preceding calculation establishes an upper bound on the radius of the eddy. We offer this as an explanation of the observed small size of SCVs.
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      An Upper Bound on the Size of Sub-mesoscale Coherent Vortices

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    contributor authorThompson, Luanne
    contributor authorYoung, W. R.
    date accessioned2017-06-09T14:49:07Z
    date available2017-06-09T14:49:07Z
    date copyright1989/02/01
    date issued1989
    identifier issn0022-3670
    identifier otherams-27466.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4164474
    description abstractLaboratory experiments show that ageostrophic instability can ?break up? a parallel flow into a sequence of axisymmetric eddies. This is a plausible scenario for the generation of sub-mesoscale coherent Vortices (SCVs). Here we show that conservation of mass, energy and potential vorticity enables one to very simply calculate the radius of the axisymmetric eddy and the wavelength of the nonlinear instability. The latter agrees more closely with laboratory experiments than does the wavelength predicted by linearized stability theory. It energy is not conserved, say because of wave radiation into the lower layer, then the preceding calculation establishes an upper bound on the radius of the eddy. We offer this as an explanation of the observed small size of SCVs.
    publisherAmerican Meteorological Society
    titleAn Upper Bound on the Size of Sub-mesoscale Coherent Vortices
    typeJournal Paper
    journal volume19
    journal issue2
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1989)019<0233:AUBOTS>2.0.CO;2
    journal fristpage233
    journal lastpage237
    treeJournal of Physical Oceanography:;1989:;Volume( 019 ):;issue: 002
    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