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    Interannual to Decadal Variability in the Tropical Atlantic

    Source: Journal of Climate:;2000:;volume( 013 ):;issue: 004::page 777
    Author:
    Dommenget, Dietmar
    ,
    Latif, Mojib
    DOI: 10.1175/1520-0442(2000)013<0777:ITDVIT>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Analyses of annual mean sea surface temperatures (SST) from observations for the period 1903?94 and four different general circulation models (GCMs) were conducted. The two dominant EOFs of all datasets are characterized by two patterns, which are centered in the trade wind zones, at roughly 15°N and 15°S, respectively. The two patterns are uncorrelated at any lag and the time spectra of the corresponding principle components are consistent with red noise. The SST variability is strongly correlated with wind stress anomalies in the trade wind zones. The correlations between the wind stress and the SST, as well as the correlation between the net heat flux and the SST anomalies are consistent with the assumption that the variability of the upper tropical Atlantic Ocean is forced by the atmosphere. Dynamic feedbacks of the tropical Atlantic Ocean are less important. The variability in the trade wind zones shows a weak correlation with the ENSO mode in the tropical Pacific.
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      Interannual to Decadal Variability in the Tropical Atlantic

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4193990
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    contributor authorDommenget, Dietmar
    contributor authorLatif, Mojib
    date accessioned2017-06-09T15:48:33Z
    date available2017-06-09T15:48:33Z
    date copyright2000/02/01
    date issued2000
    identifier issn0894-8755
    identifier otherams-5403.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4193990
    description abstractAnalyses of annual mean sea surface temperatures (SST) from observations for the period 1903?94 and four different general circulation models (GCMs) were conducted. The two dominant EOFs of all datasets are characterized by two patterns, which are centered in the trade wind zones, at roughly 15°N and 15°S, respectively. The two patterns are uncorrelated at any lag and the time spectra of the corresponding principle components are consistent with red noise. The SST variability is strongly correlated with wind stress anomalies in the trade wind zones. The correlations between the wind stress and the SST, as well as the correlation between the net heat flux and the SST anomalies are consistent with the assumption that the variability of the upper tropical Atlantic Ocean is forced by the atmosphere. Dynamic feedbacks of the tropical Atlantic Ocean are less important. The variability in the trade wind zones shows a weak correlation with the ENSO mode in the tropical Pacific.
    publisherAmerican Meteorological Society
    titleInterannual to Decadal Variability in the Tropical Atlantic
    typeJournal Paper
    journal volume13
    journal issue4
    journal titleJournal of Climate
    identifier doi10.1175/1520-0442(2000)013<0777:ITDVIT>2.0.CO;2
    journal fristpage777
    journal lastpage792
    treeJournal of Climate:;2000:;volume( 013 ):;issue: 004
    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
    yabeshDSpacePersian