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Long-term river flow forecasting methoods are used for the theoretical basis for the development of river basin water balance equation : the basins with high marks nascent river basin water balance should be organized according to higher zones . Spring flood water balance equation is used for the calculation of the measure or impossibillness to get through , so they are replaced by the flow and the approximate korelyatsion connections between the key factors , including the multifactorial flow prediction recommend using multifactorial linear regression method , which is believed to be the predicted size ( prediktant ) and the variables ( factors or prediktorner ) .There is a linear connection between the above mentioned method to calculate flow of the number of rivers of Armenia which are forecasts for 25 stations. The experimental and calculated results are about 80 %.


Session R32, Hydrologic Modeling: Forecasting



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