Ice dynamics in the central Greenland sea
[ 1] Until recently a tongue-shaped sea ice feature formed over the central Greenland Sea each winter. This tongue, known to generations of Norwegian sealers as "Odden,'' sometimes protrudes several hundred kilometres in a northeast direction from the main East Greenland ice edge. Owi...
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Online Access: | https://pure.uhi.ac.uk/en/publications/63e0ad02-a564-4e7f-9e97-a69db641b83a https://doi.org/10.1029/2006JC003639 |
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ftuhipublicatio:oai:pure.atira.dk:publications/63e0ad02-a564-4e7f-9e97-a69db641b83a 2024-02-04T10:00:05+01:00 Ice dynamics in the central Greenland sea Wilkinson, Jeremy 2006 https://pure.uhi.ac.uk/en/publications/63e0ad02-a564-4e7f-9e97-a69db641b83a https://doi.org/10.1029/2006JC003639 eng eng info:eu-repo/semantics/restrictedAccess Wilkinson , J 2006 , ' Ice dynamics in the central Greenland sea ' , J GEOPHYS RES , vol. 111 , no. C12 , pp. - . https://doi.org/10.1029/2006JC003639 INTERANNUAL VARIABILITY SALT FLUX DRIFT Oceanography MODEL DEEP CONVECTION TONGUE OCEAN article 2006 ftuhipublicatio https://doi.org/10.1029/2006JC003639 2024-01-11T23:20:53Z [ 1] Until recently a tongue-shaped sea ice feature formed over the central Greenland Sea each winter. This tongue, known to generations of Norwegian sealers as "Odden,'' sometimes protrudes several hundred kilometres in a northeast direction from the main East Greenland ice edge. Owing to the high wave energy in the Greenland Sea in winter, the formation of sea ice is restricted to locally formed pancake and frazil ice. The Greenland Sea is also a key region for the formation of dense water, and the movement of ice within this tongue will play a crucial role in determining the volume of ice formed over a winter and the subsequent modification to the upper water column through brine drainage. We present results from three drifting "pancake'' buoys released in the Odden in 1997. From the analysis of data from these buoys it was found that the ice predominantly moves in a southwesterly direction, but meanders in any direction are possible, and on timescales above 6 hours the surface wind almost exclusively drives the ice dynamics. Results indicate that pancake ice within the Odden drifts at approximately 4% of the wind speed and at about 40 degrees to the right of the wind. Article in Journal/Newspaper East Greenland Greenland Greenland Sea Sea ice University of the Highlands and Islands: Research Database of UHI Greenland Odden in ENVELOPE(14.203,14.203,67.375,67.375) Odden, in ENVELOPE(14.203,14.203,67.375,67.375) Odden,in ENVELOPE(14.203,14.203,67.375,67.375) Pancake ENVELOPE(-55.815,-55.815,52.600,52.600) Journal of Geophysical Research 111 C12 |
institution |
Open Polar |
collection |
University of the Highlands and Islands: Research Database of UHI |
op_collection_id |
ftuhipublicatio |
language |
English |
topic |
INTERANNUAL VARIABILITY SALT FLUX DRIFT Oceanography MODEL DEEP CONVECTION TONGUE OCEAN |
spellingShingle |
INTERANNUAL VARIABILITY SALT FLUX DRIFT Oceanography MODEL DEEP CONVECTION TONGUE OCEAN Wilkinson, Jeremy Ice dynamics in the central Greenland sea |
topic_facet |
INTERANNUAL VARIABILITY SALT FLUX DRIFT Oceanography MODEL DEEP CONVECTION TONGUE OCEAN |
description |
[ 1] Until recently a tongue-shaped sea ice feature formed over the central Greenland Sea each winter. This tongue, known to generations of Norwegian sealers as "Odden,'' sometimes protrudes several hundred kilometres in a northeast direction from the main East Greenland ice edge. Owing to the high wave energy in the Greenland Sea in winter, the formation of sea ice is restricted to locally formed pancake and frazil ice. The Greenland Sea is also a key region for the formation of dense water, and the movement of ice within this tongue will play a crucial role in determining the volume of ice formed over a winter and the subsequent modification to the upper water column through brine drainage. We present results from three drifting "pancake'' buoys released in the Odden in 1997. From the analysis of data from these buoys it was found that the ice predominantly moves in a southwesterly direction, but meanders in any direction are possible, and on timescales above 6 hours the surface wind almost exclusively drives the ice dynamics. Results indicate that pancake ice within the Odden drifts at approximately 4% of the wind speed and at about 40 degrees to the right of the wind. |
format |
Article in Journal/Newspaper |
author |
Wilkinson, Jeremy |
author_facet |
Wilkinson, Jeremy |
author_sort |
Wilkinson, Jeremy |
title |
Ice dynamics in the central Greenland sea |
title_short |
Ice dynamics in the central Greenland sea |
title_full |
Ice dynamics in the central Greenland sea |
title_fullStr |
Ice dynamics in the central Greenland sea |
title_full_unstemmed |
Ice dynamics in the central Greenland sea |
title_sort |
ice dynamics in the central greenland sea |
publishDate |
2006 |
url |
https://pure.uhi.ac.uk/en/publications/63e0ad02-a564-4e7f-9e97-a69db641b83a https://doi.org/10.1029/2006JC003639 |
long_lat |
ENVELOPE(14.203,14.203,67.375,67.375) ENVELOPE(14.203,14.203,67.375,67.375) ENVELOPE(14.203,14.203,67.375,67.375) ENVELOPE(-55.815,-55.815,52.600,52.600) |
geographic |
Greenland Odden in Odden, in Odden,in Pancake |
geographic_facet |
Greenland Odden in Odden, in Odden,in Pancake |
genre |
East Greenland Greenland Greenland Sea Sea ice |
genre_facet |
East Greenland Greenland Greenland Sea Sea ice |
op_source |
Wilkinson , J 2006 , ' Ice dynamics in the central Greenland sea ' , J GEOPHYS RES , vol. 111 , no. C12 , pp. - . https://doi.org/10.1029/2006JC003639 |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.1029/2006JC003639 |
container_title |
Journal of Geophysical Research |
container_volume |
111 |
container_issue |
C12 |
_version_ |
1789965202823839744 |