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    Flux Parameterization over Land Surfaces for Atmospheric Models

    Source: Journal of Applied Meteorology:;1991:;volume( 030 ):;issue: 003::page 327
    Author:
    Beljaars, A. C. M.
    ,
    Holtslag, A. A. M.
    DOI: 10.1175/1520-0450(1991)030<0327:FPOLSF>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: In this paper a summary is given of observations and modeling efforts on surface fluxes, carried out at Cabauw in The Netherlands and during MESOGERS-84 in the south of France. Emphasis is put on those aspects that are important from a modeling point of view, e.g., surface roughness lengths for momentum and heat, stomatal resistance for evaporation, and related quantities. Special attention is paid to the problem of subgrid surface inhomogeneities up to horizontal scales of a few kilometers. A qualitative explanation is given for the apparent low values of the roughness length for heat. Simple flux parameterizations are compared with observations, and empirical closure functions are proposed to model the transfer coefficients between the surface and the first model layer.
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      Flux Parameterization over Land Surfaces for Atmospheric Models

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4146913
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    contributor authorBeljaars, A. C. M.
    contributor authorHoltslag, A. A. M.
    date accessioned2017-06-09T14:03:26Z
    date available2017-06-09T14:03:26Z
    date copyright1991/03/01
    date issued1991
    identifier issn0894-8763
    identifier otherams-11660.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146913
    description abstractIn this paper a summary is given of observations and modeling efforts on surface fluxes, carried out at Cabauw in The Netherlands and during MESOGERS-84 in the south of France. Emphasis is put on those aspects that are important from a modeling point of view, e.g., surface roughness lengths for momentum and heat, stomatal resistance for evaporation, and related quantities. Special attention is paid to the problem of subgrid surface inhomogeneities up to horizontal scales of a few kilometers. A qualitative explanation is given for the apparent low values of the roughness length for heat. Simple flux parameterizations are compared with observations, and empirical closure functions are proposed to model the transfer coefficients between the surface and the first model layer.
    publisherAmerican Meteorological Society
    titleFlux Parameterization over Land Surfaces for Atmospheric Models
    typeJournal Paper
    journal volume30
    journal issue3
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(1991)030<0327:FPOLSF>2.0.CO;2
    journal fristpage327
    journal lastpage341
    treeJournal of Applied Meteorology:;1991:;volume( 030 ):;issue: 003
    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