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contributor authorOokouchi, Y.
contributor authorSegal, M.
contributor authorKessler, R. C.
contributor authorPielke, R. A.
date accessioned2017-06-09T16:05:06Z
date available2017-06-09T16:05:06Z
date copyright1984/11/01
date issued1984
identifier issn0027-0644
identifier otherams-60545.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4201227
description abstractThe current study provides an evaluation of thermally induced circulation over flat terrain due to nonuniform horizontal distribution of soil moisture availability. Additionally, the effect of soil moisture availability on the thermally induced upslope flow during the daylight hours is examined. The results indicate that in flat terrain, which has a nonhomogeneous moisture availability, the intensity of thermal circulations approaches that of sea-breeze circulations for the case of large contrasts. Even small amounts of water in thesoil, adjacent to dry areas, can still result in a significant mesoscale flow. The upslope flow has been indicated to be perturbed significantly when the moisture availability ii~creases or when the horizontal contrast of soil moisture availability becomes large.
publisherAmerican Meteorological Society
titleEvaluation of Soil Moisture Effects on the Generation and Modification of Mesoscale Circulations
typeJournal Paper
journal volume112
journal issue11
journal titleMonthly Weather Review
identifier doi10.1175/1520-0493(1984)112<2281:EOSMEO>2.0.CO;2
journal fristpage2281
journal lastpage2292
treeMonthly Weather Review:;1984:;volume( 112 ):;issue: 011
contenttypeFulltext


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