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    Self-Propagating Eddies on the Stratified f Plane

    Source: Journal of Physical Oceanography:;2000:;Volume( 030 ):;issue: 012::page 3134
    Author:
    Radko, Timour
    ,
    Stern, Melvin E.
    DOI: 10.1175/1520-0485(2000)030<3134:SPEOTS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Analytical solutions of the shallow-water system of equations in a 1½-layer f-plane model are obtained for stable quasi-monopolar vortices propagating due to a dipolar (azimuthal mode m = 1) component whose amplitude is small compared to the circularly symmetric (m = 0) part. The ability of the f-plane eddies with O(1) Rossby number to propagate distances greater than their size is demonstrated by finite amplitude numerical calculations. Numerical and analytical considerations also indicate that significant departures may occur between the ?centroid of mass anomaly? (commonly used in theoretical estimates of the speed of oceanic vortices) and other measures of the eddy center.
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      Self-Propagating Eddies on the Stratified f Plane

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4166565
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    contributor authorRadko, Timour
    contributor authorStern, Melvin E.
    date accessioned2017-06-09T14:54:17Z
    date available2017-06-09T14:54:17Z
    date copyright2000/12/01
    date issued2000
    identifier issn0022-3670
    identifier otherams-29348.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4166565
    description abstractAnalytical solutions of the shallow-water system of equations in a 1½-layer f-plane model are obtained for stable quasi-monopolar vortices propagating due to a dipolar (azimuthal mode m = 1) component whose amplitude is small compared to the circularly symmetric (m = 0) part. The ability of the f-plane eddies with O(1) Rossby number to propagate distances greater than their size is demonstrated by finite amplitude numerical calculations. Numerical and analytical considerations also indicate that significant departures may occur between the ?centroid of mass anomaly? (commonly used in theoretical estimates of the speed of oceanic vortices) and other measures of the eddy center.
    publisherAmerican Meteorological Society
    titleSelf-Propagating Eddies on the Stratified f Plane
    typeJournal Paper
    journal volume30
    journal issue12
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(2000)030<3134:SPEOTS>2.0.CO;2
    journal fristpage3134
    journal lastpage3144
    treeJournal of Physical Oceanography:;2000:;Volume( 030 ):;issue: 012
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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