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    Comments on “The Significance of Half-inertial Flow in the Eastern Equatorial Pacific”

    Source: Journal of Physical Oceanography:;1992:;Volume( 022 ):;issue: 007::page 811
    Author:
    Hansen, Donald V.
    DOI: 10.1175/1520-0485(1992)022<0811:COSOHI>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: It is shown that the instability waves regularly observed in the tropical Pacific and Atlantic oceans do not necessarily contain oscillations of half the local inertial frequency. Rather, it is hypothesized that the flow approaches the half-inertial conditions only at times when the instability waves develop sufficient baroclinic intensity to saturate the geostrophic vorticity limit of the gradient wind equation for anticyclonic flow.
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      Comments on “The Significance of Half-inertial Flow in the Eastern Equatorial Pacific”

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    https://yetl.yabesh.ir/yetl1/handle/yetl/4164962
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    contributor authorHansen, Donald V.
    date accessioned2017-06-09T14:50:21Z
    date available2017-06-09T14:50:21Z
    date copyright1992/07/01
    date issued1992
    identifier issn0022-3670
    identifier otherams-27905.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4164962
    description abstractIt is shown that the instability waves regularly observed in the tropical Pacific and Atlantic oceans do not necessarily contain oscillations of half the local inertial frequency. Rather, it is hypothesized that the flow approaches the half-inertial conditions only at times when the instability waves develop sufficient baroclinic intensity to saturate the geostrophic vorticity limit of the gradient wind equation for anticyclonic flow.
    publisherAmerican Meteorological Society
    titleComments on “The Significance of Half-inertial Flow in the Eastern Equatorial Pacific”
    typeJournal Paper
    journal volume22
    journal issue7
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1992)022<0811:COSOHI>2.0.CO;2
    journal fristpage811
    journal lastpage813
    treeJournal of Physical Oceanography:;1992:;Volume( 022 ):;issue: 007
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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