## Abstract The variation of heat flux with height in inversionβcapped convective boundary layers is discussed. Cospectral shapes at levels above approximately oneβtenth the height of the lowest inversion base (__z__~1~) are shown to depart significantly from surface layer forms. the characteristic
Heat and moisture flux in the stratified boundary layer
β Scribed by Z. Warhaft
- Publisher
- John Wiley and Sons
- Year
- 1976
- Tongue
- English
- Weight
- 346 KB
- Volume
- 102
- Category
- Article
- ISSN
- 0035-9009
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β¦ Synopsis
Abstract
Using simple models for the form of the pressure strain terms in the heat and moisture flux transport equations, it is shown that the magnitude of the heat and moisture flux depends on the crossβcorrelation coefficient of the temperature and humidity fluctuations. When the temperature and humidity fluctuations are weakly correlated it is shown that the coefficient of eddy conductivity may be significantly different from the coefficient of moisture eddy diffusivity.
π SIMILAR VOLUMES
R&urn& On ttablit ici une formulation du flux de chaleur ascendant dam le cas courant ou l'on dispose des fluctuations de tempkrature, tandis que les fluctuations du mouvement vertical ne sont pas disponibles ou sont de qua& inadtquate. On obtient 6galement une relation qui permet de dkduire la stru