Dynamic-stochastic modeling of spring slope Runoff in small drainage areas

摘要

The results are discussed on the development of a semiempirical dynamic-stochastic model of slope runoff during spring snow melting. The model is based on long-term water-balance monitoring on the plots of the Kursk Biospheric Station of the Institute of Geography, Russian Academy of Sciences. It is shown that this model describes rather adequately the formation of snowmelt slope runoff in small drainage areas of the central forest-steppe zone.