Temperature dynamics of sod-podzolic soils in Preduralye due to climatic warming

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Current climatic warming caused an increase of thermal probability of sod- podzolic soils relative to climatic norm of the temperature in the soil profile up to the depth of 320 cm, resulted in increasing the time of typical manifestation of summer climatic stage and in decreasing the depth of seasonal freezing.

Climate warming, sod-podzolic soils, seasonal freezing

Короткий адрес: https://sciup.org/148199088

IDR: 148199088

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