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
✦ LIBER ✦
Heat/mass transfer in the slightly unstable atmospheric surface layer
✍ Scribed by Ann-Sofi Smedman; Ulf Högström; J.C.R. Hunt; Erik Sahlée
- Publisher
- John Wiley and Sons
- Year
- 2007
- Tongue
- English
- Weight
- 342 KB
- Volume
- 133
- Category
- Article
- ISSN
- 0035-9009
- DOI
- 10.1002/qj.7
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