Warm Arctic-cold continents: climate impacts of the newly open Arctic Sea
Recent Arctic changes are likely due to coupled Arctic amplification mechanisms with increased linkage between Arctic climate and sub-Arctic weather. Historically, sea ice grew rapidly in autumn, a strong negative radiative feedback. But increased sea-ice mobility, loss of multi-year sea ice, enhanc...
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Published in | Polar research Vol. 30; no. 1; p. 15787 |
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Main Authors | , , |
Format | Journal Article |
Language | English |
Published |
Routledge
01.01.2011
Norwegian Polar Institute |
Subjects | |
Online Access | Get full text |
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