Abstract
Hydrological factors determine the features of relief formation in all territories where surface runoff is formed. They determine the degree of ruggedness and the nature of the relief. Changing from year to year, they interact with the underlying surface, activating the processes of erosion and planar flush of the fertile topsoil on it. The need to model and determine their intensity in different periods is due to the annual use of these territories for agricultural needs, during their plowing and sowing. The article analyses the main characteristics of surface runoff on the territory of the Krasnoyarsk forest-steppe. The result of hydrological and geomorphological analysis of the catchment area in the key study area is presented. The main indicators of autumn soil moisture are characterized and their effect on the washout of the solid fraction within the key site Dolgiy Log is estimated.
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