YaBeSH Engineering and Technology Library

    • Journals
    • PaperQuest
    • YSE Standards
    • YaBeSH
    • Login
    View Item 
    •   YE&T Library
    • AMS
    • Bulletin of the American Meteorological Society
    • View Item
    •   YE&T Library
    • AMS
    • Bulletin of the American Meteorological Society
    • View Item
    • All Fields
    • Source Title
    • Year
    • Publisher
    • Title
    • Subject
    • Author
    • DOI
    • ISBN
    Advanced Search
    JavaScript is disabled for your browser. Some features of this site may not work without it.

    Archive

    Oceanic Regulation of the Atmospheric Walker Circulation

    Source: Bulletin of the American Meteorological Society:;1997:;volume( 078 ):;issue: 003::page 407
    Author:
    Liu, Zhengyu
    DOI: 10.1175/1520-0477(1997)078<0407:OROTAW>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A coupled theory is proposed to account for the magnitude of the Walker circulation in the tropical Pacific. It is suggested that the Pacific Walker circulation is at a saturation state, at which the zonal sea surface temperature difference is bounded by about a quarter of the latitudinal difference of the radiative?convective equilibrium sea surface temperature.
    • Download: (124.2Kb)
    • Show Full MetaData Hide Full MetaData
    • Item Order
    • Go To Publisher
    • Price: 5000 Rial
    • Statistics

      Oceanic Regulation of the Atmospheric Walker Circulation

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4161421
    Collections
    • Bulletin of the American Meteorological Society

    Show full item record

    contributor authorLiu, Zhengyu
    date accessioned2017-06-09T14:41:54Z
    date available2017-06-09T14:41:54Z
    date copyright1997/03/01
    date issued1997
    identifier issn0003-0007
    identifier otherams-24718.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4161421
    description abstractA coupled theory is proposed to account for the magnitude of the Walker circulation in the tropical Pacific. It is suggested that the Pacific Walker circulation is at a saturation state, at which the zonal sea surface temperature difference is bounded by about a quarter of the latitudinal difference of the radiative?convective equilibrium sea surface temperature.
    publisherAmerican Meteorological Society
    titleOceanic Regulation of the Atmospheric Walker Circulation
    typeJournal Paper
    journal volume78
    journal issue3
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/1520-0477(1997)078<0407:OROTAW>2.0.CO;2
    journal fristpage407
    journal lastpage412
    treeBulletin of the American Meteorological Society:;1997:;volume( 078 ):;issue: 003
    contenttypeFulltext
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian
     
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian