Velocity and temperature derivatives were obtained at a height of 4 m in the atmospheric surface layer above land. With the assumption of local isotropy, these measurements are used to obtain some statistics of the turbulent energy and scalar dissipation fields. These statistics include the variance
On the analysis of wind wave-induced disturbances in the atmospheric turbulent surface layer
β Scribed by A. Yu. Benilov; O. A. Kouznetsov; G. N. Panin
- Publisher
- Springer
- Year
- 1974
- Tongue
- English
- Weight
- 984 KB
- Volume
- 6
- Category
- Article
- ISSN
- 0006-8314
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The horizontal distribution of space correlation coefficients of wind fluctuations was investigated in the atmospheric surface layer. The observational network of wind sensors was arranged to form a two-dimensional extension in the horizontal plane. The shape of the distribution of the correlation c