PL
The summer of 2025 was a particularly contrasting period in Poland in terms of water balance. Although the water balance indicator itself is complex and takes into account both inflows (including atmospheric precipitation, surface and groundwater recharge) and losses (evaporation, plant transpiration, surface runoff), in practice its development depends primarily on precipitation and air temperature, which influences the intensity of evapotranspiration (including evaporation from soil surfaces and water bodies, as well as plant transpiration).
