Abstract
Potential mechanisms producing high or low seasonal rainfall in tropical West Africa are investigated for the period 1963–74 using monthly data of precipitation, surface pressure in the South Atlantic and rawinsondes, mainly in Africa. Contrary to widespread opinion, the South Atlantic pressures yielded no correlation; the best connection was between rainfall and upper-level African observations. DOI: 10.1111/j.2153-3490.1976.tb00700.x
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