Abstract

The dependence of intensity of washing on the mountain basins and the natural-climatic factors such as precipitation, temperature of air, area of glaciations in basin is proved. New technique of quantitative estimation of washing intensity from the unexplored river basins is offered. All calculations are based on the standard hydrometeorological information.

Keywords: fluvial erosion, suspended sediments flow, washing, rapid erosion, atmospheric precipitation, glacial washing