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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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