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THERMODYNAMIC PROPERTIES AND ROLE OF THERMALS IN THE STRATUS-TOPPED BOUNDARY LAYER
作者姓名:申绍华  周明煜
作者单位:National Research Center for Marine Environmental Forecasts Beijing 100081,National Research Center for Marine Environmental Forecasts,Beijing 100081
基金项目:This work is partly supported by the National Natural Science Foundation of China(approval number of item:49236110).
摘    要:From results of two large-eddy simulation of stratus-topped boundary layer,the structure,thermodynamic prop-erties and role of thermals are investigated by using conditional sampling methods,which divided the thermals into thewarm/moist,cool/dry,warm/dry and cool/moist events.The results show that the main turbulent circulation in thestratus-topped boundary layer is composed of the warm/moist updraft and cool/dry downdraft.Below entrainmentregion,the warm/moist updrafts and cool/dry downdrafts are,respectively,positively and negatively buoyant andcontribute most to total fluxes and variances.Evaporative cooling has important effect on the structure and thermodynamic properties of thermals instratus-topped boundary layer.


THERMODYNAMIC PROPERTIES AND ROLE OF THERMALS IN THE STRATUS-TOPPED BOUNDARY LAYER
Shen Shaohua Zhou Mingyu National Research Center for Marine Environmental Forecasts,Beijing.THERMODYNAMIC PROPERTIES AND ROLE OF THERMALS IN THE STRATUS-TOPPED BOUNDARY LAYER[J].Acta Meteorologica Sinica,1994(3).
Authors:Shen Shaohua Zhou Mingyu National Research Center for Marine Environmental Forecasts  Beijing
Affiliation:Shen Shaohua Zhou Mingyu National Research Center for Marine Environmental Forecasts,Beijing 100081
Abstract:From results of two large-eddy simulation of stratus-topped boundary layer,the structure,thermodynamic prop- erties and role of thermals are investigated by using conditional sampling methods,which divided the thermals into the warm/moist,cool/dry,warm/dry and cool/moist events.The results show that the main turbulent circulation in the stratus-topped boundary layer is composed of the warm/moist updraft and cool/dry downdraft.Below entrainment region,the warm/moist updrafts and cool/dry downdrafts are,respectively,positively and negatively buoyant and contribute most to total fluxes and variances. Evaporative cooling has important effect on the structure and thermodynamic properties of thermals in stratus-topped boundary layer.
Keywords:thermals  stratus-topped boundary layer  thermodynamic properties  large-eddy simulation  entrainment
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