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    Evaporation Over A Heterogeneous Land Surface

    Source: Bulletin of the American Meteorological Society:;2006:;volume( 087 ):;issue: 006::page 775
    Author:
    Mengelkamp, H-T.
    ,
    Beyrich, F.
    ,
    Heinemann, G.
    ,
    Ament, F.
    ,
    Bange, J.
    ,
    Berger, F.
    ,
    Bösenberg, J.
    ,
    Foken, T.
    ,
    Hennemuth, B.
    ,
    Heret, C.
    ,
    Huneke, S.
    ,
    Johnsen, K-P.
    ,
    Kerschgens, M.
    ,
    Kohsiek, W.
    ,
    Leps, J-P.
    ,
    Liebethal, C.
    ,
    Lohse, H.
    ,
    Mauder, M.
    ,
    Meijninger, W.
    ,
    Raasch, S.
    ,
    Simmer, C.
    ,
    Spieß, T.
    ,
    Tittebrand, A.
    ,
    Uhlenbrock, J.
    ,
    Zittel, P.
    DOI: 10.1175/BAMS-87-6-775
    Publisher: American Meteorological Society
    Abstract: The representation of subgrid-scale surface heterogeneities in numerical weather and climate models has been a challenging problem for more than a decade. The Evaporation at Grid and Pixel Scale (EVA-GRIPS) project adds to the numerous studies on vegetation?atmosphere interaction processes through a comprehensive field campaign and through simulation studies with land surface schemes and mesoscale models. The mixture of surface types in the test area in eastern Germany is typical for larger parts of northern Central Europe. The spatial scale considered corresponds to the grid scale of a regional atmospheric weather prediction or climate model and to the pixel scale of satellite images. Area-averaged fluxes derived from point measurements, scin-tillometer measurements, and a helicopter-borne turbulence probe were widely consistent with respect to the sensible heat flux. The latent heat flux from the scintillometer measurements is systematically higher than the eddy covariance data. Fluxes derived from numerical simulations proved the so-called mosaic approach to be an appropriate parameterization for subgrid heterogeneity.
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      Evaporation Over A Heterogeneous Land Surface

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4214971
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    • Bulletin of the American Meteorological Society

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    contributor authorMengelkamp, H-T.
    contributor authorBeyrich, F.
    contributor authorHeinemann, G.
    contributor authorAment, F.
    contributor authorBange, J.
    contributor authorBerger, F.
    contributor authorBösenberg, J.
    contributor authorFoken, T.
    contributor authorHennemuth, B.
    contributor authorHeret, C.
    contributor authorHuneke, S.
    contributor authorJohnsen, K-P.
    contributor authorKerschgens, M.
    contributor authorKohsiek, W.
    contributor authorLeps, J-P.
    contributor authorLiebethal, C.
    contributor authorLohse, H.
    contributor authorMauder, M.
    contributor authorMeijninger, W.
    contributor authorRaasch, S.
    contributor authorSimmer, C.
    contributor authorSpieß, T.
    contributor authorTittebrand, A.
    contributor authorUhlenbrock, J.
    contributor authorZittel, P.
    date accessioned2017-06-09T16:43:08Z
    date available2017-06-09T16:43:08Z
    date copyright2006/06/01
    date issued2006
    identifier issn0003-0007
    identifier otherams-72915.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4214971
    description abstractThe representation of subgrid-scale surface heterogeneities in numerical weather and climate models has been a challenging problem for more than a decade. The Evaporation at Grid and Pixel Scale (EVA-GRIPS) project adds to the numerous studies on vegetation?atmosphere interaction processes through a comprehensive field campaign and through simulation studies with land surface schemes and mesoscale models. The mixture of surface types in the test area in eastern Germany is typical for larger parts of northern Central Europe. The spatial scale considered corresponds to the grid scale of a regional atmospheric weather prediction or climate model and to the pixel scale of satellite images. Area-averaged fluxes derived from point measurements, scin-tillometer measurements, and a helicopter-borne turbulence probe were widely consistent with respect to the sensible heat flux. The latent heat flux from the scintillometer measurements is systematically higher than the eddy covariance data. Fluxes derived from numerical simulations proved the so-called mosaic approach to be an appropriate parameterization for subgrid heterogeneity.
    publisherAmerican Meteorological Society
    titleEvaporation Over A Heterogeneous Land Surface
    typeJournal Paper
    journal volume87
    journal issue6
    journal titleBulletin of the American Meteorological Society
    identifier doi10.1175/BAMS-87-6-775
    journal fristpage775
    journal lastpage786
    treeBulletin of the American Meteorological Society:;2006:;volume( 087 ):;issue: 006
    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