Recent wind driven high sea ice area export in the Fram Strait contributes to Arctic sea ice decline

Arctic sea ice area has been decreasing for the past two decades. Apart from melting, the southward drift through Fram Strait is the main ice loss mechanism. We present high resolution sea ice drift data across 79° N from 2004 to 2010. Ice drift has been derived from radar satellite data and corresp...

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Published in:The Cryosphere
Main Authors: L. H. Smedsrud, A. Sirevaag, K. Kloster, A. Sorteberg, S. Sandven
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2011
Subjects:
Online Access:https://doi.org/10.5194/tc-5-821-2011
https://doaj.org/article/f56770fd191c44e9b450d5532ecaf72d
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spelling ftdoajarticles:oai:doaj.org/article:f56770fd191c44e9b450d5532ecaf72d 2023-05-15T14:54:51+02:00 Recent wind driven high sea ice area export in the Fram Strait contributes to Arctic sea ice decline L. H. Smedsrud A. Sirevaag K. Kloster A. Sorteberg S. Sandven 2011-10-01T00:00:00Z https://doi.org/10.5194/tc-5-821-2011 https://doaj.org/article/f56770fd191c44e9b450d5532ecaf72d EN eng Copernicus Publications http://www.the-cryosphere.net/5/821/2011/tc-5-821-2011.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 doi:10.5194/tc-5-821-2011 1994-0416 1994-0424 https://doaj.org/article/f56770fd191c44e9b450d5532ecaf72d The Cryosphere, Vol 5, Iss 4, Pp 821-829 (2011) Environmental sciences GE1-350 Geology QE1-996.5 article 2011 ftdoajarticles https://doi.org/10.5194/tc-5-821-2011 2022-12-31T00:20:00Z Arctic sea ice area has been decreasing for the past two decades. Apart from melting, the southward drift through Fram Strait is the main ice loss mechanism. We present high resolution sea ice drift data across 79° N from 2004 to 2010. Ice drift has been derived from radar satellite data and corresponds well with variability in local geostrophic wind. The underlying East Greenland current contributes with a constant southward speed close to 5 cm s −1 , and drives around a third of the ice export. We use geostrophic winds derived from reanalysis data to calculate the Fram Strait ice area export back to 1957, finding that the sea ice area export recently is about 25% larger than during the 1960's. The increase in ice export occurred mostly during winter and is directly connected to higher southward ice drift velocities, due to stronger geostrophic winds. The increase in ice drift is large enough to counteract a decrease in ice concentration of the exported sea ice. Using storm tracking we link changes in geostrophic winds to more intense Nordic Sea low pressure systems. Annual sea ice area export likely has a significant influence on the summer sea ice variability and we find low values in the 1960's, the late 1980's and 1990's, and particularly high values during 2005–2008. The study highlights the possible role of variability in ice export as an explanatory factor for understanding the dramatic loss of Arctic sea ice during the last decades. Article in Journal/Newspaper Arctic East Greenland east greenland current Fram Strait Greenland Nordic Sea Sea ice The Cryosphere Directory of Open Access Journals: DOAJ Articles Arctic Greenland The Cryosphere 5 4 821 829
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Environmental sciences
GE1-350
Geology
QE1-996.5
spellingShingle Environmental sciences
GE1-350
Geology
QE1-996.5
L. H. Smedsrud
A. Sirevaag
K. Kloster
A. Sorteberg
S. Sandven
Recent wind driven high sea ice area export in the Fram Strait contributes to Arctic sea ice decline
topic_facet Environmental sciences
GE1-350
Geology
QE1-996.5
description Arctic sea ice area has been decreasing for the past two decades. Apart from melting, the southward drift through Fram Strait is the main ice loss mechanism. We present high resolution sea ice drift data across 79° N from 2004 to 2010. Ice drift has been derived from radar satellite data and corresponds well with variability in local geostrophic wind. The underlying East Greenland current contributes with a constant southward speed close to 5 cm s −1 , and drives around a third of the ice export. We use geostrophic winds derived from reanalysis data to calculate the Fram Strait ice area export back to 1957, finding that the sea ice area export recently is about 25% larger than during the 1960's. The increase in ice export occurred mostly during winter and is directly connected to higher southward ice drift velocities, due to stronger geostrophic winds. The increase in ice drift is large enough to counteract a decrease in ice concentration of the exported sea ice. Using storm tracking we link changes in geostrophic winds to more intense Nordic Sea low pressure systems. Annual sea ice area export likely has a significant influence on the summer sea ice variability and we find low values in the 1960's, the late 1980's and 1990's, and particularly high values during 2005–2008. The study highlights the possible role of variability in ice export as an explanatory factor for understanding the dramatic loss of Arctic sea ice during the last decades.
format Article in Journal/Newspaper
author L. H. Smedsrud
A. Sirevaag
K. Kloster
A. Sorteberg
S. Sandven
author_facet L. H. Smedsrud
A. Sirevaag
K. Kloster
A. Sorteberg
S. Sandven
author_sort L. H. Smedsrud
title Recent wind driven high sea ice area export in the Fram Strait contributes to Arctic sea ice decline
title_short Recent wind driven high sea ice area export in the Fram Strait contributes to Arctic sea ice decline
title_full Recent wind driven high sea ice area export in the Fram Strait contributes to Arctic sea ice decline
title_fullStr Recent wind driven high sea ice area export in the Fram Strait contributes to Arctic sea ice decline
title_full_unstemmed Recent wind driven high sea ice area export in the Fram Strait contributes to Arctic sea ice decline
title_sort recent wind driven high sea ice area export in the fram strait contributes to arctic sea ice decline
publisher Copernicus Publications
publishDate 2011
url https://doi.org/10.5194/tc-5-821-2011
https://doaj.org/article/f56770fd191c44e9b450d5532ecaf72d
geographic Arctic
Greenland
geographic_facet Arctic
Greenland
genre Arctic
East Greenland
east greenland current
Fram Strait
Greenland
Nordic Sea
Sea ice
The Cryosphere
genre_facet Arctic
East Greenland
east greenland current
Fram Strait
Greenland
Nordic Sea
Sea ice
The Cryosphere
op_source The Cryosphere, Vol 5, Iss 4, Pp 821-829 (2011)
op_relation http://www.the-cryosphere.net/5/821/2011/tc-5-821-2011.pdf
https://doaj.org/toc/1994-0416
https://doaj.org/toc/1994-0424
doi:10.5194/tc-5-821-2011
1994-0416
1994-0424
https://doaj.org/article/f56770fd191c44e9b450d5532ecaf72d
op_doi https://doi.org/10.5194/tc-5-821-2011
container_title The Cryosphere
container_volume 5
container_issue 4
container_start_page 821
op_container_end_page 829
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