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
β¦ LIBER β¦
Turbulent transfer mechanisms in the atmospheric surface layer
β Scribed by G. A. McBean; M. Miyake
- Publisher
- John Wiley and Sons
- Year
- 1972
- Tongue
- English
- Weight
- 928 KB
- Volume
- 98
- Category
- Article
- ISSN
- 0035-9009
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