Abstract
The vegetation response to the temperature changes during recent decades is observed for different areas of the West Siberian Plain. The trends in the series of the vegetation index NDVI and air temperature are analyzed for the areas of weather stations. The phases of growth (1982-1997) and stabilization (1997-2015) of NDVI values were identified against the background of the observed effects: global warming slowdown, decrease in solar activity and change in the phases of the ocean surface temperature in the El Niño region (ONI) from positive to negative. Correlation analysis of NDVI and air temperature values during the periods of growth and stabilization of NDVI was carried out. The response of vegetation to the observed increase in air temperature depends on its type and location.
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