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    GLACE: The Global Land–Atmosphere Coupling Experiment. Part II: Analysis

    Source: Journal of Hydrometeorology:;2006:;Volume( 007 ):;issue: 004::page 611
    Author:
    Guo, Zhichang
    ,
    Dirmeyer, Paul A.
    ,
    Koster, Randal D.
    ,
    Sud, Y. C.
    ,
    Bonan, Gordon
    ,
    Oleson, Keith W.
    ,
    Chan, Edmond
    ,
    Verseghy, Diana
    ,
    Cox, Peter
    ,
    Gordon, C. T.
    ,
    McGregor, J. L.
    ,
    Kanae, Shinjiro
    ,
    Kowalczyk, Eva
    ,
    Lawrence, David
    ,
    Liu, Ping
    ,
    Mocko, David
    ,
    Lu, Cheng-Hsuan
    ,
    Mitchell, Ken
    ,
    Malyshev, Sergey
    ,
    McAvaney, Bryant
    ,
    Oki, Taikan
    ,
    Yamada, Tomohito
    ,
    Pitman, Andrew
    ,
    Taylor, Christopher M.
    ,
    Vasic, Ratko
    ,
    Xue, Yongkang
    DOI: 10.1175/JHM511.1
    Publisher: American Meteorological Society
    Abstract: The 12 weather and climate models participating in the Global Land?Atmosphere Coupling Experiment (GLACE) show both a wide variation in the strength of land?atmosphere coupling and some intriguing commonalities. In this paper, the causes of variations in coupling strength?both the geographic variations within a given model and the model-to-model differences?are addressed. The ability of soil moisture to affect precipitation is examined in two stages, namely, the ability of the soil moisture to affect evaporation, and the ability of evaporation to affect precipitation. Most of the differences between the models and within a given model are found to be associated with the first stage?an evaporation rate that varies strongly and consistently with soil moisture tends to lead to a higher coupling strength. The first-stage differences reflect identifiable differences in model parameterization and model climate. Intermodel differences in the evaporation?precipitation connection, however, also play a key role.
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      GLACE: The Global Land–Atmosphere Coupling Experiment. Part II: Analysis

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4224529
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    • Journal of Hydrometeorology

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    contributor authorGuo, Zhichang
    contributor authorDirmeyer, Paul A.
    contributor authorKoster, Randal D.
    contributor authorSud, Y. C.
    contributor authorBonan, Gordon
    contributor authorOleson, Keith W.
    contributor authorChan, Edmond
    contributor authorVerseghy, Diana
    contributor authorCox, Peter
    contributor authorGordon, C. T.
    contributor authorMcGregor, J. L.
    contributor authorKanae, Shinjiro
    contributor authorKowalczyk, Eva
    contributor authorLawrence, David
    contributor authorLiu, Ping
    contributor authorMocko, David
    contributor authorLu, Cheng-Hsuan
    contributor authorMitchell, Ken
    contributor authorMalyshev, Sergey
    contributor authorMcAvaney, Bryant
    contributor authorOki, Taikan
    contributor authorYamada, Tomohito
    contributor authorPitman, Andrew
    contributor authorTaylor, Christopher M.
    contributor authorVasic, Ratko
    contributor authorXue, Yongkang
    date accessioned2017-06-09T17:13:58Z
    date available2017-06-09T17:13:58Z
    date copyright2006/08/01
    date issued2006
    identifier issn1525-755X
    identifier otherams-81517.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4224529
    description abstractThe 12 weather and climate models participating in the Global Land?Atmosphere Coupling Experiment (GLACE) show both a wide variation in the strength of land?atmosphere coupling and some intriguing commonalities. In this paper, the causes of variations in coupling strength?both the geographic variations within a given model and the model-to-model differences?are addressed. The ability of soil moisture to affect precipitation is examined in two stages, namely, the ability of the soil moisture to affect evaporation, and the ability of evaporation to affect precipitation. Most of the differences between the models and within a given model are found to be associated with the first stage?an evaporation rate that varies strongly and consistently with soil moisture tends to lead to a higher coupling strength. The first-stage differences reflect identifiable differences in model parameterization and model climate. Intermodel differences in the evaporation?precipitation connection, however, also play a key role.
    publisherAmerican Meteorological Society
    titleGLACE: The Global Land–Atmosphere Coupling Experiment. Part II: Analysis
    typeJournal Paper
    journal volume7
    journal issue4
    journal titleJournal of Hydrometeorology
    identifier doi10.1175/JHM511.1
    journal fristpage611
    journal lastpage625
    treeJournal of Hydrometeorology:;2006:;Volume( 007 ):;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