## Abstract The mean meridional circulation in winter and summer is derived as a function of latitude and height from an analysis of observed winds in the area 160Β°Wβ0β40Β°E, 75Β°Nβ15Β°N. The results confirm the classical idea of a direct circulation in low latitudes, but the indirect circulation in m
β¦ LIBER β¦
On the role of mean meridional circulations in the energy balance of the atmosphere
β Scribed by Holopainen, E. O.
- Book ID
- 114986791
- Publisher
- John Wiley and Sons
- Year
- 1965
- Tongue
- English
- Weight
- 762 KB
- Volume
- 17
- Category
- Article
- ISSN
- 0280-6495
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