The tendency of increasing the average annual temperature causes a significant violation of the water balance of territories and water bodies as a result of a significant increase in water losses due to evaporation. According to the estimates of [Information and Analytical Report, 2020] under Ukrainian climate conditions, the growth of the average monthly temperature by 1 °C causes an increase in total evaporation by about 9%. Thus, the total water evaporation from the territory of Ukraine in 2020 was 40−45 km 3 per year higher comparing with the corresponding value in 1990, which translates into an average growth of 1.7−1.9% annually. In many regions of the world, the evaporation layer significantly exceeds the depth of the precipitation layer. Compared to Ukraine, where the intensity of evaporation from water bodies in summer is in the range of 1−4 mm/day [Rudakov et al., 2017], in countries with hot and dry climates, this value reaches 8−10 mm/day and more [