Abstract
Formation of a flow and loss on slopes, as is known, is provided with a number of factors, leaders among which are characteristics of atmospheric precipitation and a spreading surface (Wischmeier and Smith in Agricultural Handbook, 1978; Gorchichko in J Soil Sci 2:130–134, 1979). Their variability in time and space defines the size of a flow and loss from slopes. Importance and diversity of influence and interaction of the factors defining a flow and loss have found reflection in numerous researches. Were studied both questions on the character of atmospheric precipitation, and questions of an opportunity of forecasting of their characteristics and others.
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Budnik, S.V. (2019). Change of Erosive Activity in the Context of Change of the Climate. In: Chalov, S., Golosov, V., Li, R., Tsyplenkov, A. (eds) Climate Change Impacts on Hydrological Processes and Sediment Dynamics: Measurement, Modelling and Management. Springer Proceedings in Earth and Environmental Sciences. Springer, Cham. https://doi.org/10.1007/978-3-030-03646-1_4
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