
A simple model for estimating the evaporation from a shallow water reservoir
Abstract
A simple model of the energy fluxes of a well-mixed water reservoir is presented based upon its energy and mass budget. The heating processes due to atmospheric-radiative and hydrological forcing are separated and parameterized in terms of two characteristic temperatures. Accordingly, two related time scales can be deduced which describe the energetical response of the reservoir on the two forcing mechanisms. Three different approximations for the latent heat fluxes are introduced. The model which includes the complete energy balance is applied to the Salton Sea (California) and shows good agreement with the observations.
© 1977 K. Fraedrich, A. Behlau, G. Kerath, G. Weber, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.