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 multi-year
changes of the sea-ice extent in the Arctic Seas were formed by
linear trends and long-term (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 short-period cycles (up to 10 years)
predominate. The linear trends can be related to a super-secular
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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