Аннотация:A dynamic-stochastic model of flood generation consisting of a distributed physically-based model of snowmelt runoff genesis and a stochastic weather generator has been used for the assessment of extreme flood risk. Coupling this model with the Monte Carlo simulations of meteorological series allows the calculation of long series of runoff hydrographs and the exceedence probabilities of flood characteristics, as well as avoiding the application of the hypothesis of stationarity of hydrological series. However, for very rare events, the uncertainty in estimating flood risk because of the model inadequacy and insufficient lengths of the used data series may significantly increase. To decrease this uncertainty, it has been suggested that the peak discharge series obtained by dynamic-stochastic simulations be combined with the probable maximum discharge (PMD) calculated through the physically based model of snowmelt runoff generation. This combining is achieved by fitting the estimated exceedence probabilities of simulated peak discharges by the Johnson distribution with the PMD as the parameter. Sensitivity of the fitted Johnson distribution to the errors of the PMD estimations is analysed. A case study was carried out for the Vyatka River basin of Russia (catchment area of 124 000 km2) and the Seim River basin (catchment area of 7460 km2).