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    Meridional Asymmetry and Energetics of Tropical Instability Waves

    Source: Journal of Physical Oceanography:;1995:;Volume( 025 ):;issue: 012::page 2997
    Author:
    Yu, Zuojun
    ,
    McCreary, Julian P.
    ,
    Proehl, Jeffrey A.
    DOI: 10.1175/1520-0485(1995)025<2997:MAAEOT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: One of the striking features of tropical instability waves (TIWs) is that they appear to be more prominent north of the equator. A linearized, 2½-layer ocean model is used to investigate effects of various asymmetric background states on structures of equatorial, unstable waves. Our results suggest that the meridional asymmetry of TIWs is due to asymmetries of the two branches of the South Equatorial Current (SEC) and of the equatorial, sea surface temperature front; it is not due to the presence of the North Equatorial Countercurrent. Energetics analyses indicate that frontal instability associated with the equatorial, SST front, as well as barotropic instability due to shear associated with the SEC, are energy sources for the model TIWS.
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      Meridional Asymmetry and Energetics of Tropical Instability Waves

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4165558
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    contributor authorYu, Zuojun
    contributor authorMcCreary, Julian P.
    contributor authorProehl, Jeffrey A.
    date accessioned2017-06-09T14:51:51Z
    date available2017-06-09T14:51:51Z
    date copyright1995/12/01
    date issued1995
    identifier issn0022-3670
    identifier otherams-28441.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4165558
    description abstractOne of the striking features of tropical instability waves (TIWs) is that they appear to be more prominent north of the equator. A linearized, 2½-layer ocean model is used to investigate effects of various asymmetric background states on structures of equatorial, unstable waves. Our results suggest that the meridional asymmetry of TIWs is due to asymmetries of the two branches of the South Equatorial Current (SEC) and of the equatorial, sea surface temperature front; it is not due to the presence of the North Equatorial Countercurrent. Energetics analyses indicate that frontal instability associated with the equatorial, SST front, as well as barotropic instability due to shear associated with the SEC, are energy sources for the model TIWS.
    publisherAmerican Meteorological Society
    titleMeridional Asymmetry and Energetics of Tropical Instability Waves
    typeJournal Paper
    journal volume25
    journal issue12
    journal titleJournal of Physical Oceanography
    identifier doi10.1175/1520-0485(1995)025<2997:MAAEOT>2.0.CO;2
    journal fristpage2997
    journal lastpage3007
    treeJournal of Physical Oceanography:;1995:;Volume( 025 ):;issue: 012
    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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