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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Published in:Oceanography
Main Authors: Frajka-Williams, Eleanor, Bamber, Jonathan, Våge, Kjetil
Format: Article in Journal/Newspaper
Language:English
Published: 2016
Subjects:
Online Access:https://eprints.soton.ac.uk/404899/
https://eprints.soton.ac.uk/404899/1/29-4_frajka-williams.pdf
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spelling 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
institution Open Polar
collection 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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