Abstract

Relationships have been formulated and the software developed in support of the construction the model for the temporal dynamics of the monthly mean water flow rate in the lower measuring section of catchment. In terms of the model, the runoff observed is formed depending on the monthly mean air temperature and monthly precipitation amount characteristic for catchment. It is suggested that the resulting flow rate comprises three types of river alimentation: the now, rain and subterranean types. The parameters of the postulated runoff formation mechanism are estimated for three catchments on the territory of the Kuda river basin.

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