Using water balance computations, the behavior of different kinds of l
akes is discussed. Simple analytical expressions relating water level
to hydrological conditions and lake bathymetry are given. The importan
ce of knowing the river basin area when analyzing lake levels is stres
sed. A conceptual rainfall-runoff model including lake routing is used
to simulate runoff and lake levels and to compute quasi-steady state
conditions and long-term transient situations. It is suggested that mo
dels can be used to construct curves relating lake levels to precipita
tion and lake evaporation. By comparing with paleo-lake levels, the an
nual precipitation related to these levels can be found, provided info
rmation is available about the seasonal distribution of the precipitat
ion.