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    The Representation of Water Vapor and Its Dependence on Vertical Resolution in the Hadley Centre Climate Model

    Source: Journal of Climate:;2001:;volume( 014 ):;issue: 014::page 3065
    Author:
    Pope, V. D.
    ,
    Pamment, J. A.
    ,
    Jackson, D. R.
    ,
    Slingo, A.
    DOI: 10.1175/1520-0442(2001)014<3065:TROWVA>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Simulations of the Hadley Centre Atmospheric Climate Model version 3, HadAM3, are used to investigate the impact of increasing vertical resolution on simulated climates. In particular, improvements in the representation of water vapor and temperature in the upper troposphere and lower stratosphere are identified with more accurate advection. Degradations in some aspects of the simulation in the Tropics are identified with undesirable resolution dependencies in the physical parameterizations. The overall improvements in the water vapor and temperature distribution lead to improvements in the clear-sky longwave radiative fluxes with higher vertical resolution.
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      The Representation of Water Vapor and Its Dependence on Vertical Resolution in the Hadley Centre Climate Model

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4198878
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    contributor authorPope, V. D.
    contributor authorPamment, J. A.
    contributor authorJackson, D. R.
    contributor authorSlingo, A.
    date accessioned2017-06-09T15:59:58Z
    date available2017-06-09T15:59:58Z
    date copyright2001/07/01
    date issued2001
    identifier issn0894-8755
    identifier otherams-5843.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4198878
    description abstractSimulations of the Hadley Centre Atmospheric Climate Model version 3, HadAM3, are used to investigate the impact of increasing vertical resolution on simulated climates. In particular, improvements in the representation of water vapor and temperature in the upper troposphere and lower stratosphere are identified with more accurate advection. Degradations in some aspects of the simulation in the Tropics are identified with undesirable resolution dependencies in the physical parameterizations. The overall improvements in the water vapor and temperature distribution lead to improvements in the clear-sky longwave radiative fluxes with higher vertical resolution.
    publisherAmerican Meteorological Society
    titleThe Representation of Water Vapor and Its Dependence on Vertical Resolution in the Hadley Centre Climate Model
    typeJournal Paper
    journal volume14
    journal issue14
    journal titleJournal of Climate
    identifier doi10.1175/1520-0442(2001)014<3065:TROWVA>2.0.CO;2
    journal fristpage3065
    journal lastpage3085
    treeJournal of Climate:;2001:;volume( 014 ):;issue: 014
    contenttypeFulltext
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian
     
    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian