Atmospheric surface-layer measurements of terms in the equation for the streamwise heat flux confirm previous results in both laboratory and atmosphere that the temperature-pressure gradient correlation acts as a sink, approximately equal in magnitude to the production term. The measured viscous dis
โฆ LIBER โฆ
Radiative heat flux divergence and heat regime in the lowest layer of the atmosphere
โ Scribed by G. N. Gaevskaya; K. Y. Kondrati'ev; K. E. Yakushevskaya
- Publisher
- Springer
- Year
- 1962
- Tongue
- English
- Weight
- 851 KB
- Volume
- 12
- Category
- Article
- ISSN
- 1434-4483
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