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The article discusses the change in river flow with glacial nutrition during global warming. It was established that on the Sokh river with a large share of glacial nutrition, a low-water period had been observed until the mid-seventies, after during a period of global warming a high-water period. Accordingly, in the cool period there was an increase in the area of glaciers, during the period of warming a decrease. The latter can lead to a significant negative trend in runoff and an increase in its variation, which has been observed in recent decades in the river basin Isfayram.

ABOUT THE REACTION OF THE DRAIN OF RIVERS WITH GLACIER FOOD TO CLIMATE HEATING.