Greenland Melt and the Atlantic Meridional Overturning Circulation
More than a decade of observations of the meridional overturning circulation in the subtropical North Atlantic show it to be highly variable on time scales of days to years and with an overall trend toward slowing down. Over the same time period, melting from Greenland (and elsewhere in the Arctic,...
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ftsouthampton:oai:eprints.soton.ac.uk:404899 2023-08-27T04:07:42+02:00 Greenland Melt and the Atlantic Meridional Overturning Circulation Frajka-Williams, Eleanor Bamber, Jonathan Våge, Kjetil 2016-12 text https://eprints.soton.ac.uk/404899/ https://eprints.soton.ac.uk/404899/1/29-4_frajka-williams.pdf en English eng https://eprints.soton.ac.uk/404899/1/29-4_frajka-williams.pdf Frajka-Williams, Eleanor, Bamber, Jonathan and Våge, Kjetil (2016) Greenland Melt and the Atlantic Meridional Overturning Circulation. Oceanography, 29 (4), 22-33. (doi:10.5670/oceanog.2016.96 <http://dx.doi.org/10.5670/oceanog.2016.96>). Article PeerReviewed 2016 ftsouthampton https://doi.org/10.5670/oceanog.2016.96 2023-08-03T22:22:06Z More than a decade of observations of the meridional overturning circulation in the subtropical North Atlantic show it to be highly variable on time scales of days to years and with an overall trend toward slowing down. Over the same time period, melting from Greenland (and elsewhere in the Arctic, including from sea ice) has been increasing, resulting in greater freshwater input to the northern North Atlantic. In this article, we examine evidence for the impact, if any, of this influx of freshwater on the large-scale ocean circulation and for potential changes. Article in Journal/Newspaper Arctic Greenland North Atlantic Sea ice University of Southampton: e-Prints Soton Arctic Greenland Oceanography 29 4 22 33 |
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Open Polar |
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University of Southampton: e-Prints Soton |
op_collection_id |
ftsouthampton |
language |
English |
description |
More than a decade of observations of the meridional overturning circulation in the subtropical North Atlantic show it to be highly variable on time scales of days to years and with an overall trend toward slowing down. Over the same time period, melting from Greenland (and elsewhere in the Arctic, including from sea ice) has been increasing, resulting in greater freshwater input to the northern North Atlantic. In this article, we examine evidence for the impact, if any, of this influx of freshwater on the large-scale ocean circulation and for potential changes. |
format |
Article in Journal/Newspaper |
author |
Frajka-Williams, Eleanor Bamber, Jonathan Våge, Kjetil |
spellingShingle |
Frajka-Williams, Eleanor Bamber, Jonathan Våge, Kjetil Greenland Melt and the Atlantic Meridional Overturning Circulation |
author_facet |
Frajka-Williams, Eleanor Bamber, Jonathan Våge, Kjetil |
author_sort |
Frajka-Williams, Eleanor |
title |
Greenland Melt and the Atlantic Meridional Overturning Circulation |
title_short |
Greenland Melt and the Atlantic Meridional Overturning Circulation |
title_full |
Greenland Melt and the Atlantic Meridional Overturning Circulation |
title_fullStr |
Greenland Melt and the Atlantic Meridional Overturning Circulation |
title_full_unstemmed |
Greenland Melt and the Atlantic Meridional Overturning Circulation |
title_sort |
greenland melt and the atlantic meridional overturning circulation |
publishDate |
2016 |
url |
https://eprints.soton.ac.uk/404899/ https://eprints.soton.ac.uk/404899/1/29-4_frajka-williams.pdf |
geographic |
Arctic Greenland |
geographic_facet |
Arctic Greenland |
genre |
Arctic Greenland North Atlantic Sea ice |
genre_facet |
Arctic Greenland North Atlantic Sea ice |
op_relation |
https://eprints.soton.ac.uk/404899/1/29-4_frajka-williams.pdf Frajka-Williams, Eleanor, Bamber, Jonathan and Våge, Kjetil (2016) Greenland Melt and the Atlantic Meridional Overturning Circulation. Oceanography, 29 (4), 22-33. (doi:10.5670/oceanog.2016.96 <http://dx.doi.org/10.5670/oceanog.2016.96>). |
op_doi |
https://doi.org/10.5670/oceanog.2016.96 |
container_title |
Oceanography |
container_volume |
29 |
container_issue |
4 |
container_start_page |
22 |
op_container_end_page |
33 |
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1775348436640464896 |