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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Vydané v:	Polar research Ročník 30; číslo 1; s. 15787
Hlavní autori:	Overland, James E., Wood, Kevin R., Wang, Muyin
Médium:	Journal Article
Jazyk:	English
Vydavateľské údaje:	Routledge 01.01.2011 Norwegian Polar Institute
Predmet:	atmospheric circulation Climate change Marine North Atlantic Oscillation sea ice North America PN, Arctic AN, North Atlantic, North Atlantic Oscillation
ISSN:	1751-8369, 0800-0395, 1751-8369
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