“…In some areas of the world, and in particular in Sub-Saharan Africa, vegetation change has been suggested as a potential feedback mechanism for prolonging and intensifying drought. Although other processes (e.g., the role of evapotranspiration changes) are undoubtedly involved (Hare, 1977(Hare, , 1985Kidson, 1977;Barry, 1978;Lamb, 1978;Henderson-Sellers, 1980;Nicholson, 1983;Henderson-Sellers and Gornitz, 1984;Lockwood, 1986), increasing albedo with decreasing vegetation cover has been suggested as a contributor to the desertiflcation process. Whether cooling would occur in a desert environment of decreasing vegetation coverage has been argued since the publication of Charney's (1975) research.…”