Abstract. Lake Victoria, the second largest freshwater lake in the world, is one of the
major sources of the Nile river. The outlet to the Nile is controlled by two
hydropower dams of which the allowed discharge is dictated by the Agreed
Curve, an equation relating outflow to lake level. Some regional climate
models project a decrease in precipitation and an increase in evaporation
over Lake Victoria, with potential important implications for its water
balance and resulting level. Yet, little is known about the potential
consequences of climate change for the water balance of Lake Victoria. In
this second part of a two-paper series, we feed a new water balance model for
Lake Victoria presented in the first part with climate simulations available
through the COordinated Regional Climate Downscaling
Experiment (CORDEX) Africa
framework. Our results reveal that most regional climate models are not
capable of giving a realistic representation of the water balance of Lake
Victoria and therefore require bias correction. For two emission scenarios
(RCPs 4.5 and 8.5), the decrease in precipitation over the lake and an
increase in evaporation are compensated by an increase in basin precipitation
leading to more inflow. The future lake level projections show that the dam
management scenario and not the emission scenario is the main controlling
factor of the future water level evolution. Moreover, inter-model
uncertainties are larger than emission scenario uncertainties. The comparison
of four idealized future management scenarios pursuing certain policy
objectives (electricity generation, navigation reliability and environmental
conservation) uncovers that the only sustainable management scenario is
mimicking natural lake level fluctuations by regulating outflow according to
the Agreed Curve. The associated outflow encompasses, however, ranges from
14 m3 day−1 (−85 %) to 200 m3 day−1 (+100 %)
within this ensemble, highlighting that future hydropower generation and
downstream water availability may strongly change in the next decades even if
dam management adheres to he Agreed Curve. Our results overall underline that
managing the dam according to the Agreed Curve is a key prerequisite for
sustainable future lake levels, but that under this management scenario,
climate change might potentially induce profound changes in lake level and
outflow volume.