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contributor authorSorbjan, Zbigniew
date accessioned2017-06-09T14:33:38Z
date available2017-06-09T14:33:38Z
date copyright1996/01/01
date issued1996
identifier issn0022-4928
identifier otherams-21669.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4158033
description abstractA large eddy simulation model was used to generate and compare statistics of turbulence during nonpenetrative and penetrative dry convection. In penetrative convection dimensionless vertical velocities in updrafts were found to have almost the same values as in the nonpenetrative case. The countergradient transport of heat and moisture was found to be present during nonpenetrative convection at z/zi > 0.6. For penetrative convection the countergradient transport of heat occurred only in a layer 0.5 < z/zi < 0.75, while the countergradient transport of humidity was not present. During nonpenetrative convection, temperature and humidity were perfectly correlated. In penetrative convection the correlation coefficient was found to be less than unity, varying from about 0.9 near the surface to about ?0.7 at the top of the mixed layer.
publisherAmerican Meteorological Society
titleNumerical Study of Penetrative and “Solid Lid” Nonpenetrative Convective Boundary Layers
typeJournal Paper
journal volume53
journal issue1
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1996)053<0101:NSOPAL>2.0.CO;2
journal fristpage101
journal lastpage112
treeJournal of the Atmospheric Sciences:;1996:;Volume( 053 ):;issue: 001
contenttypeFulltext


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