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    GLACE: The Global Land–Atmosphere Coupling Experiment. Part I: Overview

    Source: Journal of Hydrometeorology:;2006:;Volume( 007 ):;issue: 004::page 590
    Author:
    Koster, Randal D.
    ,
    Sud, Y. C.
    ,
    Guo, Zhichang
    ,
    Dirmeyer, Paul A.
    ,
    Bonan, Gordon
    ,
    Oleson, Keith W.
    ,
    Chan, Edmond
    ,
    Verseghy, Diana
    ,
    Cox, Peter
    ,
    Davies, Harvey
    ,
    Kowalczyk, Eva
    ,
    Gordon, C. T.
    ,
    Kanae, Shinjiro
    ,
    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/JHM510.1
    Publisher: American Meteorological Society
    Abstract: The Global Land?Atmosphere Coupling Experiment (GLACE) is a model intercomparison study focusing on a typically neglected yet critical element of numerical weather and climate modeling: land?atmosphere coupling strength, or the degree to which anomalies in land surface state (e.g., soil moisture) can affect rainfall generation and other atmospheric processes. The 12 AGCM groups participating in GLACE performed a series of simple numerical experiments that allow the objective quantification of this element for boreal summer. The derived coupling strengths vary widely. Some similarity, however, is found in the spatial patterns generated by the models, with enough similarity to pinpoint multimodel ?hot spots? of land?atmosphere coupling. For boreal summer, such hot spots for precipitation and temperature are found over large regions of Africa, central North America, and India; a hot spot for temperature is also found over eastern China. The design of the GLACE simulations are described in full detail so that any interested modeling group can repeat them easily and thereby place their model?s coupling strength within the broad range of those documented here.
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      GLACE: The Global Land–Atmosphere Coupling Experiment. Part I: Overview

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4224528
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    • Journal of Hydrometeorology

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    contributor authorKoster, Randal D.
    contributor authorSud, Y. C.
    contributor authorGuo, Zhichang
    contributor authorDirmeyer, Paul A.
    contributor authorBonan, Gordon
    contributor authorOleson, Keith W.
    contributor authorChan, Edmond
    contributor authorVerseghy, Diana
    contributor authorCox, Peter
    contributor authorDavies, Harvey
    contributor authorKowalczyk, Eva
    contributor authorGordon, C. T.
    contributor authorKanae, Shinjiro
    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-81516.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4224528
    description abstractThe Global Land?Atmosphere Coupling Experiment (GLACE) is a model intercomparison study focusing on a typically neglected yet critical element of numerical weather and climate modeling: land?atmosphere coupling strength, or the degree to which anomalies in land surface state (e.g., soil moisture) can affect rainfall generation and other atmospheric processes. The 12 AGCM groups participating in GLACE performed a series of simple numerical experiments that allow the objective quantification of this element for boreal summer. The derived coupling strengths vary widely. Some similarity, however, is found in the spatial patterns generated by the models, with enough similarity to pinpoint multimodel ?hot spots? of land?atmosphere coupling. For boreal summer, such hot spots for precipitation and temperature are found over large regions of Africa, central North America, and India; a hot spot for temperature is also found over eastern China. The design of the GLACE simulations are described in full detail so that any interested modeling group can repeat them easily and thereby place their model?s coupling strength within the broad range of those documented here.
    publisherAmerican Meteorological Society
    titleGLACE: The Global Land–Atmosphere Coupling Experiment. Part I: Overview
    typeJournal Paper
    journal volume7
    journal issue4
    journal titleJournal of Hydrometeorology
    identifier doi10.1175/JHM510.1
    journal fristpage590
    journal lastpage610
    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