The turbulent characteristics in the lowest part of the sea breeze front in the atmospheric surface layer
β Scribed by Osamu Chiba
- Publisher
- Springer
- Year
- 1993
- Tongue
- English
- Weight
- 749 KB
- Volume
- 65
- Category
- Article
- ISSN
- 0006-8314
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π SIMILAR VOLUMES
By non-dimensionalizing a trajectory-simulation (TS) model of turbulent dispersion, it is shown that the dimensionless concentrationz,cu./kQ (cu./kQ)due to a continuous line (area) source ofstrength Q in the atmospheric surface layer depends only on z/z,, x/zc, z,,/L and z,/z,, where z, is the sourc
## Abstract A semiβempirical treatment of the vertical diffusion of matter in the lowest layers of the atmosphere is given in the following and shown to be in good agreement with the results of carefully conducted field experiments made over two different types of natural land surface. The present
Wind characteristics in the lowest 340m (agl) of the atmospheric boundary layer at Pune (Ho32 N, 73% E, 559 m ASL) have been investigated using the pilot balloon wind observations obtained during the summer monsoon seasons of 1976, 1979 and 1980. Variations in the zonal and meridional components of