Potential evaporation (Ep) and actual evapotranspiration (EA) values for 84 East African stations were estimated and mapped using Morton [12, 13, 14] model. The data used in the study were long term averages up to and including 1974. TheEp andEA distributions for the months of January, April, and July and October; and annual are discussed. HighEp values exist in the semi-arid/arid areas of northern and northeastern Kenya and central Tanzania. LowEp values dominate on the highland areas. HighEA values are observed over the East African rainfall favoured and thickly vegetated areas whereas the lowestEA values are predominantly observed during all months in semi-arid/arid areas. BothEp andEp values show a good agreement with the north/south movement of the rain belts across East Africa.
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