Climate dynamics of southern chernozems in Western Siberia due to climatic warming

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The current warming is accompanied an increase in thermo-provision of southern chernozeoms in the warm season, a decrease in the depth of seasonal freesing and duration of soil in the frozen state.

Climate, soil, climatic norm

Короткий адрес: https://sciup.org/148201008

IDR: 148201008

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