Abstract
Lake Basaka is expanding at a very fast rate. An appropriate method of estimating the surface runoff from
such dynamic catchment is extremely important to delineate sensitive areas to be protected and to
develop suitable management measures. In this study, the surface (direct) runoff was estimated using
SCS-CN model, assisted by remote sensing and GIS. The result indicated that Lake Basaka catchment
showed significant variability (temporal and spatial) in runoff responses depending on the rainfall amount
and distribution pattern and land use/cover change. The significant increase of surface runoff (runoff
coefficient) was observed to occur after 1973, which is in line with the significant increment of lake level
after that period. The reduction in vegetation cover also resulted in increase of runoff coefficient of the
Lake catchment from 0.07 in 1960s to about 0.23 in 2000s.