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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Bibliographic Details
Published inPolar research Vol. 30; no. 1; p. 15787
Main Authors Overland, James E., Wood, Kevin R., Wang, Muyin
Format Journal Article
LanguageEnglish
Published Routledge 01.01.2011
Norwegian Polar Institute
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