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    The Interannual Variability of the Ocean-Atmosphere System

    Source: Journal of the Atmospheric Sciences:;1978:;Volume( 035 ):;issue: 003::page 349
    Author:
    Reiter, Elmar R.
    DOI: 10.1175/1520-0469(1978)035<0349:TIVOTO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Evidence is derived from observational data that the trade wind circulations in both hemispheres over the Pacific are related to the sea surface temperature (SST) anomalies in the North Pacific. The equatorward component of the surface trade winds leads the North Pacific SST anomalies by approximately 20 months, equivalent to the half-rotation time of the Pacific gyre. Long-term trends in the Pacific trade wind regime appear to have an influence on hemispheric and global mean temperatures. The trade wind anomalies also seem to be tied to meridional atmospheric pressure- and temperature-gradient anomalies which, in turn, appear to respond to anomalies in the meridional SST gradients. Thus a closed feedback loop is demonstrated, in which SST anomalies in the North Pacific generate trade wind anomalies which promote the development of North Pacific SST anomalies of opposite sign. The trade wind surges also are related to El Niño through a feedback involving the hydrological cycle and upwelling of cold water forced by Ekman pumping.
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      The Interannual Variability of the Ocean-Atmosphere System

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4153331
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    contributor authorReiter, Elmar R.
    date accessioned2017-06-09T14:19:59Z
    date available2017-06-09T14:19:59Z
    date copyright1978/03/01
    date issued1978
    identifier issn0022-4928
    identifier otherams-17437.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4153331
    description abstractEvidence is derived from observational data that the trade wind circulations in both hemispheres over the Pacific are related to the sea surface temperature (SST) anomalies in the North Pacific. The equatorward component of the surface trade winds leads the North Pacific SST anomalies by approximately 20 months, equivalent to the half-rotation time of the Pacific gyre. Long-term trends in the Pacific trade wind regime appear to have an influence on hemispheric and global mean temperatures. The trade wind anomalies also seem to be tied to meridional atmospheric pressure- and temperature-gradient anomalies which, in turn, appear to respond to anomalies in the meridional SST gradients. Thus a closed feedback loop is demonstrated, in which SST anomalies in the North Pacific generate trade wind anomalies which promote the development of North Pacific SST anomalies of opposite sign. The trade wind surges also are related to El Niño through a feedback involving the hydrological cycle and upwelling of cold water forced by Ekman pumping.
    publisherAmerican Meteorological Society
    titleThe Interannual Variability of the Ocean-Atmosphere System
    typeJournal Paper
    journal volume35
    journal issue3
    journal titleJournal of the Atmospheric Sciences
    identifier doi10.1175/1520-0469(1978)035<0349:TIVOTO>2.0.CO;2
    journal fristpage349
    journal lastpage370
    treeJournal of the Atmospheric Sciences:;1978:;Volume( 035 ):;issue: 003
    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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