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    Transient Response of an Atmospheric GCM to North Atlantic SST Anomalies

    Source: Journal of Climate:;2003:;volume( 016 ):;issue: 023::page 3993
    Author:
    Li, Z. X.
    ,
    Conil, S.
    DOI: 10.1175/1520-0442(2003)016<3993:TROAAG>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A high-resolution atmospheric general circulation model (GCM) is used to evaluate the atmospheric response to North Atlantic sea surface temperature (SST) anomalies. The transient evolution of the response is studied in detail. The linear and nonlinear effects can thus be contrasted and separated by their different time scales. Baroclinic patterns related directly to the surface anomalies quickly reach their maximum manifestation. However, barotropic patterns related to the mid- and upper troposphere eddy vorticity fluxes have longer time scales with much more important amplitude, able to gradually replace the initial baroclinic response. This study thus provides an evolutional picture of the two types of response in a GCM.
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      Transient Response of an Atmospheric GCM to North Atlantic SST Anomalies

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4205401
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    contributor authorLi, Z. X.
    contributor authorConil, S.
    date accessioned2017-06-09T16:15:28Z
    date available2017-06-09T16:15:28Z
    date copyright2003/12/01
    date issued2003
    identifier issn0894-8755
    identifier otherams-6430.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4205401
    description abstractA high-resolution atmospheric general circulation model (GCM) is used to evaluate the atmospheric response to North Atlantic sea surface temperature (SST) anomalies. The transient evolution of the response is studied in detail. The linear and nonlinear effects can thus be contrasted and separated by their different time scales. Baroclinic patterns related directly to the surface anomalies quickly reach their maximum manifestation. However, barotropic patterns related to the mid- and upper troposphere eddy vorticity fluxes have longer time scales with much more important amplitude, able to gradually replace the initial baroclinic response. This study thus provides an evolutional picture of the two types of response in a GCM.
    publisherAmerican Meteorological Society
    titleTransient Response of an Atmospheric GCM to North Atlantic SST Anomalies
    typeJournal Paper
    journal volume16
    journal issue23
    journal titleJournal of Climate
    identifier doi10.1175/1520-0442(2003)016<3993:TROAAG>2.0.CO;2
    journal fristpage3993
    journal lastpage3998
    treeJournal of Climate:;2003:;volume( 016 ):;issue: 023
    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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