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In this book the eminent authors analyse the ice cover variability in the Arctic Seas during the 20th and early 21st centuries. In the first two chapters, they show that multiyear changes of the seaice extent in the Arctic Seas were formed by linear trends and longterm (climatic) cycles lasting about 10, 20 and 60 years. The structure of temporal variability of the western region (Greenland Kara) differs significantly from the eastern region seas (Laptev and Chukchi). In the latter region, unlike the former area, relatively shortperiod cycles (up to 10 years) predominate. The linear trends can be related to a supersecular cycle of climatic changes over about 200 years. The most significant of these cycles, lasting 60 years, is most pronounced in the western region seas.
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