Abstract
Principles of estimation of infiltration groundwater recharge based on modeling the formation of water balance on the land surface and in the vadose zone are considered. The application of such models for regional discharge evaluation involves zoning of the territory by a set of meteorological, landscape, geological, soil, and hydrogeological factors. The reliability of the obtained estimates of water balance components, including infiltration recharge, should be assessed by correlating the calculated and measured river runoff characteristics for drainage basins within which the water-bearing section in the zone of active water exchange is completely drained. The application of such approach is illustrated by calculations for southwestern Moscow Artesian Basin.
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