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|a 9783540858751
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|a 10.1007/978-3-540-85875-1
|2 doi
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|a (DE-He213)978-3-540-85875-1
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|a E-Book
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|a RNPG
|2 thema
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| 100 |
1 |
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|a Frolov, Ivan E.
|e author.
|4 aut
|4 http://id.loc.gov/vocabulary/relators/aut
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| 245 |
1 |
0 |
|a Climate Change in Eurasian Arctic Shelf Seas
|h [electronic resource] :
|b Centennial Ice Cover Observations /
|c by Ivan E. Frolov, Zalmann M. Gudkovich, Valery P. Karklin, Evgeny G. Kovalev, Vasily M. Smolyanitsky.
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| 250 |
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|a 1st ed. 2009.
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| 264 |
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1 |
|a Berlin, Heidelberg :
|b Springer Berlin Heidelberg :
|b Imprint: Springer,
|c 2009.
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| 300 |
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|a 166 p. 48 illus., 6 illus. in color.
|b online resource.
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| 336 |
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|a text
|b txt
|2 rdacontent
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| 337 |
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|a computer
|b c
|2 rdamedia
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|a online resource
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| 347 |
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|a text file
|b PDF
|2 rda
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| 490 |
1 |
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|a Geophysical Sciences,
|x 1615-9748
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| 490 |
1 |
|
|a Springer eBook Collection
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| 505 |
0 |
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|a Arctic sea ice as an element of the global climate system -- Long-term changes in Arctic Seas ice extent during the twentieth century -- Variability of sea ice thickness and concentration in the twentieth century -- Consistency among sea ice extent and atmospheric and hydrospheric processes -- Possible causes of changes in climate and in Arctic Seas ice extent -- Assessment of possible changes in air temperature and sea-ice extent in the Arctic Seas in the twenty-first century -- Conclusions.
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| 520 |
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|a 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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| 590 |
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|a Loaded electronically.
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| 590 |
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|a Electronic access restricted to members of the Holy Cross Community.
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| 650 |
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0 |
|a Climate change.
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| 650 |
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0 |
|a Geography.
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| 650 |
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0 |
|a Atmospheric sciences.
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| 690 |
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|a Electronic resources (E-books)
|
| 700 |
1 |
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|a Gudkovich, Zalmann M.
|e author.
|4 aut
|4 http://id.loc.gov/vocabulary/relators/aut
|
| 700 |
1 |
|
|a Karklin, Valery P.
|e author.
|4 aut
|4 http://id.loc.gov/vocabulary/relators/aut
|
| 700 |
1 |
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|a Kovalev, Evgeny G.
|e author.
|4 aut
|4 http://id.loc.gov/vocabulary/relators/aut
|
| 700 |
1 |
|
|a Smolyanitsky, Vasily M.
|e author.
|4 aut
|4 http://id.loc.gov/vocabulary/relators/aut
|
| 710 |
2 |
|
|a SpringerLink (Online service)
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| 773 |
0 |
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|t Springer eBooks
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| 830 |
|
0 |
|a Geophysical Sciences,
|x 1615-9748
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| 830 |
|
0 |
|a Springer eBook Collection.
|
| 856 |
4 |
0 |
|u https://holycross.idm.oclc.org/login?auth=cas&url=https://doi.org/10.1007/978-3-540-85875-1
|3 Click to view e-book
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