Diurnal variations of the vertical profiles of wind and temperature have been surveyed, and the diffusivity and the dimensionless gradient function in the atmospheric boundary layer have been estimated. Even in the middle of the atmospheric boundary layer (e.g., below a height of 442 m), the vertica
โฆ LIBER โฆ
An analysis of the topographical effect on turbulence and diffusion in the atmosphere's boundary layer
โ Scribed by S. K. Kao; H. N. Lee; K. I. Smidy
- Publisher
- Springer
- Year
- 1975
- Tongue
- English
- Weight
- 472 KB
- Volume
- 8
- Category
- Article
- ISSN
- 0006-8314
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