Abstract
In this paper a model for estimation of snowmelt distribution using insolation, air temperature and precipitation is presented. This model includes net radiation, degreehour approach and condensation and convection in a rainy day. At first the model is determined at the observational base. And it is applied to the slopes and the forested area. The results of the application of the model to the base, the slopes and the forested area are in good agreement with observed data.
