A large number of environmental management decisions such as the remediatio
n of a mine site require the best possible knowledge of the water balance o
f the site or the catchment area. For precipitation a large number of obser
vations exists and usually some data are available which are more or less r
epresentative for the precipitation conditions in the catchment. However, t
o close the water balance knowledge about evaporation is also required. Thi
s is usually not available from observations. Also bulk formulas cannot be
used to reconstruct evaporation for a sufficiently long time, since observa
tions of the input variables are limited as well. In this article an approa
ch is presented showing how local potential evaporation may be reconstructe
d from other local and non-local atmospheric variables for which long-term
observations are available. The method is demonstrated for the planned arti
ficial lakes in the closed down mine sites in the Geiseltal (Germany) and a
ims at the estimation of the probability distribution of the difference bet
ween precipitation and evaporation for the surface water balance.