The focus of this paper is the role of meridional distribution of vege
tation in the dynamics of monsoons and rainfall over West Africa. A mo
ist zonally symmetric atmospheric model coupled with a simple land sur
face scheme is developed to investigate these processes. Four primary
experiments have been carried out to examine the sensitivity of West A
frican monsoons to perturbations in the meridional distribution of veg
etation. In the control experiment, the authors assume a distribution
of vegetation that resembles the natural vegetation cover in West Afri
ca. Each perturbation experiment is identical to the control experimen
t except that a change in vegetation cover is imposed for a latitudina
l belt that is 10 degrees in width. The results of the numerical exper
iments demonstrate that West African monsoons and therefore rainfall d
istribution depend critically on the location of the vegetation pertur
bations. Changes in vegetation cover along the border between the Saha
ra desert and West Africa (desertification) may have a minor impact on
the simulated monsoon circulation. However, coastal deforestation may
cause the collapse of the monsoon circulation and have a dramatic imp
act on the regional rainfall. The observed deforestation in West Afric
a is then likely to be a significant contributor to the observed droug
ht.