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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Norwegian Polar Institute
2011
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Online Access: | https://doi.org/10.3402/polar.v30i0.15787 https://doaj.org/article/5fecd9f5bd624749918aab74c85a1d2d |
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fttriple:oai:gotriple.eu:oai:doaj.org/article:5fecd9f5bd624749918aab74c85a1d2d 2023-05-15T14:32:07+02:00 Warm Arctic—cold continents: climate impacts of the newly open Arctic Sea James E. Overland Kevin R. Wood Muyin Wang 2011-12-01 https://doi.org/10.3402/polar.v30i0.15787 https://doaj.org/article/5fecd9f5bd624749918aab74c85a1d2d en eng Norwegian Polar Institute doi:10.3402/polar.v30i0.15787 0800-0395 1751-8369 https://doaj.org/article/5fecd9f5bd624749918aab74c85a1d2d undefined Polar Research, Vol 30, Iss 0, Pp 1-14 (2011) Climate change sea ice atmospheric circulation North Atlantic Oscillation geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2011 fttriple https://doi.org/10.3402/polar.v30i0.15787 2023-01-22T18:03:49Z 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, enhanced heat storage in newly sea ice-free ocean areas, and modified wind fields form connected positive feedback processes. One-way shifts in the Arctic system are sensitive to the combination of episodic intrinsic atmospheric and ocean variability and persistent increasing greenhouse gases. Winter 2009/10 and December 2010 showed a unique connectivity between the Arctic and more southern weather patterns when the typical polar vortex was replaced by high geopotential heights over the central Arctic and low heights over mid-latitudes that resulted in record snow and low temperatures, a warm Arctic—cold continents pattern. The negative value of the winter (DJF 2009/10) North Atlantic Oscillation (NAO) index associated with enhanced meridional winds was the lowest observed value since the beginning of the record in 1865. Wind patterns in December 2007 and 2008 also show an impact of warmer Arctic temperatures. A tendency for higher geopotential heights over the Arctic and enhanced meridional winds are physically consistent with continued loss of sea ice over the next 40 years. A major challenge is to understand the interaction of Arctic changes with climate patterns such as the NAO, Pacific North American and El Niño–Southern Oscillation. Article in Journal/Newspaper Arctic Climate change North Atlantic North Atlantic oscillation Polar Research Sea ice Unknown Arctic Pacific Polar Research 30 1 15787 |
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Open Polar |
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op_collection_id |
fttriple |
language |
English |
topic |
Climate change sea ice atmospheric circulation North Atlantic Oscillation geo envir |
spellingShingle |
Climate change sea ice atmospheric circulation North Atlantic Oscillation geo envir James E. Overland Kevin R. Wood Muyin Wang Warm Arctic—cold continents: climate impacts of the newly open Arctic Sea |
topic_facet |
Climate change sea ice atmospheric circulation North Atlantic Oscillation geo envir |
description |
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, enhanced heat storage in newly sea ice-free ocean areas, and modified wind fields form connected positive feedback processes. One-way shifts in the Arctic system are sensitive to the combination of episodic intrinsic atmospheric and ocean variability and persistent increasing greenhouse gases. Winter 2009/10 and December 2010 showed a unique connectivity between the Arctic and more southern weather patterns when the typical polar vortex was replaced by high geopotential heights over the central Arctic and low heights over mid-latitudes that resulted in record snow and low temperatures, a warm Arctic—cold continents pattern. The negative value of the winter (DJF 2009/10) North Atlantic Oscillation (NAO) index associated with enhanced meridional winds was the lowest observed value since the beginning of the record in 1865. Wind patterns in December 2007 and 2008 also show an impact of warmer Arctic temperatures. A tendency for higher geopotential heights over the Arctic and enhanced meridional winds are physically consistent with continued loss of sea ice over the next 40 years. A major challenge is to understand the interaction of Arctic changes with climate patterns such as the NAO, Pacific North American and El Niño–Southern Oscillation. |
format |
Article in Journal/Newspaper |
author |
James E. Overland Kevin R. Wood Muyin Wang |
author_facet |
James E. Overland Kevin R. Wood Muyin Wang |
author_sort |
James E. Overland |
title |
Warm Arctic—cold continents: climate impacts of the newly open Arctic Sea |
title_short |
Warm Arctic—cold continents: climate impacts of the newly open Arctic Sea |
title_full |
Warm Arctic—cold continents: climate impacts of the newly open Arctic Sea |
title_fullStr |
Warm Arctic—cold continents: climate impacts of the newly open Arctic Sea |
title_full_unstemmed |
Warm Arctic—cold continents: climate impacts of the newly open Arctic Sea |
title_sort |
warm arctic—cold continents: climate impacts of the newly open arctic sea |
publisher |
Norwegian Polar Institute |
publishDate |
2011 |
url |
https://doi.org/10.3402/polar.v30i0.15787 https://doaj.org/article/5fecd9f5bd624749918aab74c85a1d2d |
geographic |
Arctic Pacific |
geographic_facet |
Arctic Pacific |
genre |
Arctic Climate change North Atlantic North Atlantic oscillation Polar Research Sea ice |
genre_facet |
Arctic Climate change North Atlantic North Atlantic oscillation Polar Research Sea ice |
op_source |
Polar Research, Vol 30, Iss 0, Pp 1-14 (2011) |
op_relation |
doi:10.3402/polar.v30i0.15787 0800-0395 1751-8369 https://doaj.org/article/5fecd9f5bd624749918aab74c85a1d2d |
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undefined |
op_doi |
https://doi.org/10.3402/polar.v30i0.15787 |
container_title |
Polar Research |
container_volume |
30 |
container_issue |
1 |
container_start_page |
15787 |
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1766305591110664192 |