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contributor authorMahfouf, Jean-François
contributor authorRichard, Evelyne
contributor authorMascart, Patrick
date accessioned2017-06-09T14:02:02Z
date available2017-06-09T14:02:02Z
date copyright1987/11/01
date issued1987
identifier issn0733-3021
identifier otherams-11254.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146462
description abstractA two-dimensional mesoscale model including a detailed representation of the planetary boundary layer, the soil and the vegetation is developed. A sea breeze over flat terrain is simulated, thereby confirming the ability of the model to reproduce the known properties of this mesoscale phenomenon. The atmospheric response to soil and vegetation inhomogeneities is then examined with no synoptic flow over flat terrain. The results reveal the large influence of soil texture on surface moisture availability. The transition zone between bare soil and vegetation appears to be a preferred location for the initiation of moist convection. A vegetation canopy over very dry or very wet surfaces reduces the spread between sensible and latent heat fluxes.
publisherAmerican Meteorological Society
titleThe Influence of Soil and Vegetation on the Development of Mesoscale Circulations
typeJournal Paper
journal volume26
journal issue11
journal titleJournal of Climate and Applied Meteorology
identifier doi10.1175/1520-0450(1987)026<1483:TIOSAV>2.0.CO;2
journal fristpage1483
journal lastpage1495
treeJournal of Climate and Applied Meteorology:;1987:;Volume( 026 ):;Issue: 011
contenttypeFulltext


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