## Abstract It is demonstrated by applying a theory developed by Starr that the mean meridional circulations cannot transport atmospheric water vapour across surfaces of constant mean values of water vapour mixing ratio, and that the work of transferring the moisture from zonal regions of surplus t
The turbulent transport of heat and water vapour in an unstable atmosphere
โ Scribed by A. J. Dyer
- Publisher
- John Wiley and Sons
- Year
- 1967
- Tongue
- English
- Weight
- 470 KB
- Volume
- 93
- Category
- Article
- ISSN
- 0035-9009
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๐ SIMILAR VOLUMES
The dissipation rate of turbulent kinetic energy, E, and the temperature structure function parameter, C& have been measured over water from the near surface (Z = 3 m) to the top of the boundary layer. The near surface values of E and C; were used to calculate the velocity and temperature Monin Obuk
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