Abstract:
The paper presents the analysis of the influence of the lower stratiform clouds (Sc, St, Ns) on long-term changes in surface temperature, performed for Siberia using the results of zoning of the territory according to cloudiness conditions. It has been shown that there is a weakly marked increase in the amount of low stratiform clouds during all seasons in the last 45-year period (from 1969 to 2013), which is accompanied by a quite noticeable increase in the surface temperature, especially in the polar regions.
Keywords:
lower stratiform clouds, cloud amount, air temperature, trends, Siberian region
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