Soils within the steppe and dry steppe zones under anomalous weather conditions in the last tens years

Under consideration is the influence of climate changes (the air temperature rise in the cold 6 months especially in the winter and the increased atmospheric moistening in the warm 6 months) on regimes and properties of soils in dependence on zonal-provincial, geomorphological and lithological conditions as exemplified by the solonetz complex in the semi-desert Pre-Caspian plain and chernozems in central European Russia and southern regions of this country.