## Abstract The variation of heat flux with height in inversion‐capped convective boundary layers is discussed. Cospectral shapes at levels above approximately one‐tenth the height of the lowest inversion base (__z__~1~) are shown to depart significantly from surface layer forms. the characteristic
✦ LIBER ✦
The vertical convective heat flux in the atmosphere—a critical essay
✍ Scribed by G. D. Robinson
- Publisher
- John Wiley and Sons
- Year
- 1951
- Tongue
- English
- Weight
- 797 KB
- Volume
- 77
- Category
- Article
- ISSN
- 0035-9009
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