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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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發(fā)表于 2025-3-21 18:26:41 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書目名稱Climate Change in Eurasian Arctic Shelf Seas
副標(biāo)題Centennial Ice Cover
編輯Ivan E. Frolov,Zalman M. Gudkovich,Vasily M. Smoly
視頻videohttp://file.papertrans.cn/228/227537/227537.mp4
概述Summarizes research results of centennial changes of sea ice cover of the Arctic seas of the Eurasian shelf.Uniquely analyses ice and hydrometeorological characteristics over 80-100 years in the 20th
叢書名稱Springer Praxis Books
圖書封面Titlebook: Climate Change in Eurasian Arctic Shelf Seas; Centennial Ice Cover Ivan E. Frolov,Zalman M. Gudkovich,Vasily M. Smoly Book 2009 Springer-Ve
描述.In this book the eminent authors analyse the ice cover variability in the Arctic Seas during the 20.th .and early 21.st. 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. .
出版日期Book 2009
關(guān)鍵詞climate; climate change; temperature; climate change impacts
版次1
doihttps://doi.org/10.1007/978-3-540-85875-1
isbn_softcover978-3-642-24228-1
isbn_ebook978-3-540-85875-1
copyrightSpringer-Verlag Berlin Heidelberg 2009
The information of publication is updating

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Springer Praxis Bookshttp://image.papertrans.cn/c/image/227537.jpg
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978-3-642-24228-1Springer-Verlag Berlin Heidelberg 2009
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R. L. Moss,G. M. Diffee,M. L. Greaseric Basin as a “near-pole abyssal basin, restricted by the continental slope.” The Beaufort and Lincoln Seas are the marginal zones of the Arctic Basin. The North European Basin encompasses the Greenland, Norwegian, Barents, and White Seas as well as the Arctic Seas of Siberia (the Kara, Laptev, East
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https://doi.org/10.1007/BFb0033667ch were closed in the 1990s. To investigate the changes in landfast ice thickness for this study, we chose 11 stations with approximately equal lengths of observational time series. Five of these stations were located in the Kara Sea (Beliy Island, Dikson Island, Uyedineniya Island, Cape Sterlegov,
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M. P. Blaustein,R. Greger,M. Schweiger detailed investigation. Unfortunately, since climate change is by definition, a long-term phenomenon, it is very difficult to prove or disprove hypotheses. We have an abundance of hypotheses and a dearth of detailed long-term data. Nevertheless, where data exist, we should prefer data to computer m
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