Titlebook: Climate Change in Eurasian Arctic Shelf Seas; Centennial Ice Cover Ivan E. Frolov,Zalman M. Gudkovich,Vasily M. Smoly Book 2009 Springer-Ve

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R. L. Moss,G. M. Diffee,M. L. Greaseradian region of the Arctic Ocean (e.g., Zakharov, 1996; Smirnov, 1974). Based on the major characteristics of the area’s ice regime, the Greenland, Iceland, Norwegian, Barents, and Kara Seas are collectively known as the Nordic Seas, as proposed by Vinje (1998).

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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. .978-3-642-24228-1978-3-540-85875-1

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M. P. Blaustein,R. Greger,M. Schweiger, and other astronomical factors. Internal factors encompass natural hydrometeorological, geological, and biological processes and self-oscillation phenomena related to interactions in the lithosphere-ocean-sea ice-atmosphere-land system, with the latter including glaciers, rivers, etc. Anthropogeni

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Possible causes of changes in climate and in Arctic Seas ice extent,, and other astronomical factors. Internal factors encompass natural hydrometeorological, geological, and biological processes and self-oscillation phenomena related to interactions in the lithosphere-ocean-sea ice-atmosphere-land system, with the latter including glaciers, rivers, etc. Anthropogeni

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