Wind forcing of salinity anomalies in the Denmark Strait overflow
The overflow of dense water from the Nordic Seas to the North Atlantic through Denmark Strait is an important part of the global thermohaline circulation. The salinity of the overflow plume has been measured by an array of current meters across the continental slope off the coast of Angmagssalik, so...
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Copernicus Publications
2011
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fttriple:oai:gotriple.eu:oai:doaj.org/article:ae17a86c44874951975fe4e7ceecefb9 2023-05-15T13:25:48+02:00 Wind forcing of salinity anomalies in the Denmark Strait overflow S. Hall S. R. Dye K. J. Heywood M. R. Wadley 2011-11-01 https://doi.org/10.5194/os-7-821-2011 http://www.ocean-sci.net/7/821/2011/os-7-821-2011.pdf https://doaj.org/article/ae17a86c44874951975fe4e7ceecefb9 en eng Copernicus Publications doi:10.5194/os-7-821-2011 1812-0784 1812-0792 http://www.ocean-sci.net/7/821/2011/os-7-821-2011.pdf https://doaj.org/article/ae17a86c44874951975fe4e7ceecefb9 undefined Ocean Science, Vol 7, Iss 6, Pp 821-834 (2011) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2011 fttriple https://doi.org/10.5194/os-7-821-2011 2023-01-22T19:10:02Z The overflow of dense water from the Nordic Seas to the North Atlantic through Denmark Strait is an important part of the global thermohaline circulation. The salinity of the overflow plume has been measured by an array of current meters across the continental slope off the coast of Angmagssalik, southeast Greenland since September 1998. During 2004 the salinity of the overflow plume changed dramatically; the entire width of the array (70 km) freshened between January 2004 and July 2004, with a significant negative salinity anomaly of about 0.06 in May. The event in May represents a fresh anomaly of over 3 standard deviations from the mean since recording began in 1998. The OCCAM 1/12° Ocean General Circulation Model not only reproduces the 2004 freshening event (r=0.96, pr=0.54, p−3, flowing towards the Denmark Strait sill in the East Greenland Current. This is caused by an increase in southward wind stress upstream of the sill at around 75° N 20° W four and a half months earlier, and an associated strengthening of the East Greenland Current. Article in Journal/Newspaper Angmagssalik Denmark Strait East Greenland east greenland current Greenland Nordic Seas North Atlantic Unknown Greenland Ocean Science 7 6 821 834 |
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language |
English |
topic |
geo envir |
spellingShingle |
geo envir S. Hall S. R. Dye K. J. Heywood M. R. Wadley Wind forcing of salinity anomalies in the Denmark Strait overflow |
topic_facet |
geo envir |
description |
The overflow of dense water from the Nordic Seas to the North Atlantic through Denmark Strait is an important part of the global thermohaline circulation. The salinity of the overflow plume has been measured by an array of current meters across the continental slope off the coast of Angmagssalik, southeast Greenland since September 1998. During 2004 the salinity of the overflow plume changed dramatically; the entire width of the array (70 km) freshened between January 2004 and July 2004, with a significant negative salinity anomaly of about 0.06 in May. The event in May represents a fresh anomaly of over 3 standard deviations from the mean since recording began in 1998. The OCCAM 1/12° Ocean General Circulation Model not only reproduces the 2004 freshening event (r=0.96, pr=0.54, p−3, flowing towards the Denmark Strait sill in the East Greenland Current. This is caused by an increase in southward wind stress upstream of the sill at around 75° N 20° W four and a half months earlier, and an associated strengthening of the East Greenland Current. |
format |
Article in Journal/Newspaper |
author |
S. Hall S. R. Dye K. J. Heywood M. R. Wadley |
author_facet |
S. Hall S. R. Dye K. J. Heywood M. R. Wadley |
author_sort |
S. Hall |
title |
Wind forcing of salinity anomalies in the Denmark Strait overflow |
title_short |
Wind forcing of salinity anomalies in the Denmark Strait overflow |
title_full |
Wind forcing of salinity anomalies in the Denmark Strait overflow |
title_fullStr |
Wind forcing of salinity anomalies in the Denmark Strait overflow |
title_full_unstemmed |
Wind forcing of salinity anomalies in the Denmark Strait overflow |
title_sort |
wind forcing of salinity anomalies in the denmark strait overflow |
publisher |
Copernicus Publications |
publishDate |
2011 |
url |
https://doi.org/10.5194/os-7-821-2011 http://www.ocean-sci.net/7/821/2011/os-7-821-2011.pdf https://doaj.org/article/ae17a86c44874951975fe4e7ceecefb9 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Angmagssalik Denmark Strait East Greenland east greenland current Greenland Nordic Seas North Atlantic |
genre_facet |
Angmagssalik Denmark Strait East Greenland east greenland current Greenland Nordic Seas North Atlantic |
op_source |
Ocean Science, Vol 7, Iss 6, Pp 821-834 (2011) |
op_relation |
doi:10.5194/os-7-821-2011 1812-0784 1812-0792 http://www.ocean-sci.net/7/821/2011/os-7-821-2011.pdf https://doaj.org/article/ae17a86c44874951975fe4e7ceecefb9 |
op_rights |
undefined |
op_doi |
https://doi.org/10.5194/os-7-821-2011 |
container_title |
Ocean Science |
container_volume |
7 |
container_issue |
6 |
container_start_page |
821 |
op_container_end_page |
834 |
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1766388361181790208 |