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atmospheric circulation

The general movement and circulation of air, which transfers energy between different levels of the atmosphere. The mechanisms of circulation are very complicated. They involve the transfer of energy between the oceans and the atmosphere, the land and the atmosphere, as well as the different levels of the atmosphere. (Source: WRIGHT)


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Taljaard JJ 1986. Change of rainfall distribution and circulation patterns over Southern Africa in summer. Journal of Climatology 6 (6) 579-592
Website link:http://onlinelibrary.wiley.com/doi/10.1002/joc.3370060602/abstract
Kaseke KF, Mills AJ, Brown R, Esler KJ, Henschel JR, Seely MK 2012. A method for direct assessment of the "non rainfall" atmospheric water cycle: input and evaporation from the soil. Pure and applied geophysics 169 (5-6) 847-857
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A method for direct assessment of the non rainfall atmospheric water cycle.pdf 433.84 KB
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