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    A Mechanism for Land–Atmosphere Feedback Involving Planetary Wave Structures

    Source: Journal of Climate:;2014:;volume( 027 ):;issue: 024::page 9290
    Author:
    Koster, Randal D.
    ,
    Chang, Yehui
    ,
    Schubert, Siegfried D.
    DOI: 10.1175/JCLI-D-14-00315.1
    Publisher: American Meteorological Society
    Abstract: hile the ability of land surface conditions to influence the atmosphere has been demonstrated in various modeling and observational studies, the precise mechanisms by which land?atmosphere feedback occurs are still largely unknown: particularly the mechanisms that allow land moisture state in one region to affect atmospheric conditions in another. Such remote impacts are examined here in the context of atmospheric general circulation model (AGCM) simulations, leading to the identification of one potential mechanism: the phase locking and amplification of a planetary wave through the imposition of a spatial pattern of soil moisture at the land surface. This mechanism, shown here to be relevant in the AGCM, apparently also operates in nature, as suggested by supporting evidence found in reanalysis data.
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      A Mechanism for Land–Atmosphere Feedback Involving Planetary Wave Structures

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    contributor authorKoster, Randal D.
    contributor authorChang, Yehui
    contributor authorSchubert, Siegfried D.
    date accessioned2017-06-09T17:10:35Z
    date available2017-06-09T17:10:35Z
    date copyright2014/12/01
    date issued2014
    identifier issn0894-8755
    identifier otherams-80596.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4223505
    description abstracthile the ability of land surface conditions to influence the atmosphere has been demonstrated in various modeling and observational studies, the precise mechanisms by which land?atmosphere feedback occurs are still largely unknown: particularly the mechanisms that allow land moisture state in one region to affect atmospheric conditions in another. Such remote impacts are examined here in the context of atmospheric general circulation model (AGCM) simulations, leading to the identification of one potential mechanism: the phase locking and amplification of a planetary wave through the imposition of a spatial pattern of soil moisture at the land surface. This mechanism, shown here to be relevant in the AGCM, apparently also operates in nature, as suggested by supporting evidence found in reanalysis data.
    publisherAmerican Meteorological Society
    titleA Mechanism for Land–Atmosphere Feedback Involving Planetary Wave Structures
    typeJournal Paper
    journal volume27
    journal issue24
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-14-00315.1
    journal fristpage9290
    journal lastpage9301
    treeJournal of Climate:;2014:;volume( 027 ):;issue: 024
    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