Temperature regime of humus-illuvial podzols of the Kola peninsula

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The temperature regime of humus-illuvial podzols in the central part of the Kola Peninsula was studied. Tendencies of changes in air and soil temperature, precipitation and snow cover over the period 1932-2016 have been revealed. It is established that for the present period the warming of the soil and atmospheric climate is characteristic, accompanied by an increase in precipitation and a decrease in the height of the snow cover.

Climate, changes, temperature regime, soil

Короткий адрес: https://sciup.org/148205177

IDR: 148205177

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