Releases into the Orange River from Vanderkloof Dam Row some 1400 km throug
h extremely hot and arid areas, without further control structures. Accurat
e estimates of evaporation losses are therefore: important to manage the ri
ver's resources efficiently. A study was initiated to improve estimates of
river losses downstream of Vanderkloof Darn, and to develop a methodology f
or estimating evaporation losses from South African rivers.
Theoretical losses were estimated from a measured evaporation rate multipli
ed by the water surface area and an appropriate riparian vegetation area. I
n addition, hydraulic modelling was used to perform a dynamic water balance
to verify the initial loss estimate.
Evaporation rates from a flowing river (in an arid region) were found to be
in the same order of magnitude as A pan evaporation data. The evaporation
losses from the Orange River derived from this research range from 575 mill
ion m(3)/a at an annual low Row release rate of 50 m(3)/s to 989 million m3
/a at an annual release rate of 400 m(3)/s. The variation in evaporation lo
sses is due to the change in surface area with flow. (C) 2001 Published by
Elsevier Science B.V.