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...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Norwegian Polar Institute
2011-12-01
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| Series: | Polar Research |
| Subjects: | |
| Online Access: | http://www.polarresearch.net/index.php/polar/article/view/15787/pdf_1 |