SST-induced climate change in tropical North Africa: The intermediary role of lower tropospheric oscillations |
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Authors: | J A Adedoyin |
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Institution: | (1) Department of Physics, University of Botswana, Gaborone, Botswana, BW |
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Abstract: | Summary The growth rates of amplifying mid-tropospheric perturbations in tropical North Africa is known to reduce with increased
vertical shear in the troposphere. This phenomenon leads to a reduction in the frequency of generation of squall lines – the
main rain-producing mechanism in tropical North Africa – because squalls are initiated by amplifying modes of African Easterly
Waves (AEW). Ultimately, therefore, tropical North Africa experiences a shortfall, with respect to long-term averages, in
annual rainfall. Weakening of AEW intensity is shown to be linked with the warming up to the sea-surface temperatures (SST)
of the South Atlantic, Pacific and Indian Oceans. These findings are consistent with the observed reduction in the incidence
of intense hurricanes along the entire westem Atlantic in Sahelian dry years. It is shown that the frequency of occurrence
of Atlantic tropical storms and hurricanes is unaffected by the dryness or otherwise in the Sahel, but the paths of the storms
are determined by the zonal exit point, from the African continental land mass to the Atlantic, of West African disturbance
lines. These results have applications, and implications, in the level of preparedness for the economic impacts of Atlantic
storms and hurricanes.
Received June 8, 1996 Revised June 8, 2000 |
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