Spatiotemporal dynamics of water balance elements in water catchments of Southern Siberia mountains under the influence of natural and anthropogenic factors
It was found that trends of annual river flows, basins of which were completed cutting, differ both in sign and in value. On the one hand this is due, apparently, to characteristics of forest cover recovery dynamics, which determines the amount of total evaporation and annual runoff respectively, on the other hand due to the direct influence of local climatic changes.