Numerical Study of Penetrative and “Solid Lid” Nonpenetrative Convective Boundary LayersSource: Journal of the Atmospheric Sciences:;1996:;Volume( 053 ):;issue: 001::page 101Author:Sorbjan, Zbigniew
DOI: 10.1175/1520-0469(1996)053<0101:NSOPAL>2.0.CO;2Publisher: American Meteorological Society
Abstract: A 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.
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| contributor author | Sorbjan, Zbigniew | |
| date accessioned | 2017-06-09T14:33:38Z | |
| date available | 2017-06-09T14:33:38Z | |
| date copyright | 1996/01/01 | |
| date issued | 1996 | |
| identifier issn | 0022-4928 | |
| identifier other | ams-21669.pdf | |
| identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4158033 | |
| description abstract | A 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. | |
| publisher | American Meteorological Society | |
| title | Numerical Study of Penetrative and “Solid Lid” Nonpenetrative Convective Boundary Layers | |
| type | Journal Paper | |
| journal volume | 53 | |
| journal issue | 1 | |
| journal title | Journal of the Atmospheric Sciences | |
| identifier doi | 10.1175/1520-0469(1996)053<0101:NSOPAL>2.0.CO;2 | |
| journal fristpage | 101 | |
| journal lastpage | 112 | |
| tree | Journal of the Atmospheric Sciences:;1996:;Volume( 053 ):;issue: 001 | |
| contenttype | Fulltext |