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The assessment of the water regime transformation is one of the most urgent tasks in modern hydrology. Over the past 30 years significant changes in the interconnection between the phases of the water regime, the mechanisms of their influence on each other, associated mainly with the change in the processes of runoff formation have been detected. Most likely, this is due to the changes in the temperature-humidity regime of large geographic regions, caused by the global climate dynamics. At the moment, it is quite difficult to analyze simultaneously the shifts in rates and indicators of all phases of the hydrological year.