Water balance models have been used to examine trends in the level of
Lake Victoria over this century. A monthly model developed in a previo
us study for the period 1925 to 1978 has been improved and the simulat
ion period extended to 1990. Also, an annual model has been used to ex
tend the water balance back to the start of the century. The simulatio
ns confirm the results from previous studies which showed that the obs
erved variations in lake level can be explained primarily in terms of
natural variations in rainfall over the lake and surrounding basin. An
idealized interpretation of these variations is presented which illus
trates the long response time of this large lake and which is used to
speculate on the likely future behaviour of the lake.