Impacts of climate change on the Atlantic Heat Conveyor (Atlantic Meridional Overturning Circulation)

The meridional overturning circulation (MOC) is part of a global ocean circulation that redistributes heat from Equatorial to Polar regions. In the Atlantic, the MOC (AMOC) carries heat northward (the Atlantic Heat Conveyor) which is released to the atmosphere and maintains UK temperatures between 3...

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Main Authors: Smeed, David, Wood, Richard, Cunningham, Stuart, McCarthy, Gerard, Kuhlbrodt, Till, Dye, Steven
Format: Article in Journal/Newspaper
Language:English
Published: 2013
Subjects:
Online Access:https://pure.uhi.ac.uk/en/publications/9edd780a-376f-4aa2-80ea-9212006b4af8
https://doi.org/10.14465/2013.arc06.049-059
https://pureadmin.uhi.ac.uk/ws/files/1899530/2013arc_sciencereview_06_ahc_final_1_.pdf
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spelling ftuhipublicatio:oai:pure.atira.dk:publications/9edd780a-376f-4aa2-80ea-9212006b4af8 2023-05-15T17:35:43+02:00 Impacts of climate change on the Atlantic Heat Conveyor (Atlantic Meridional Overturning Circulation) Smeed, David Wood, Richard Cunningham, Stuart McCarthy, Gerard Kuhlbrodt, Till Dye, Steven 2013-12 application/pdf https://pure.uhi.ac.uk/en/publications/9edd780a-376f-4aa2-80ea-9212006b4af8 https://doi.org/10.14465/2013.arc06.049-059 https://pureadmin.uhi.ac.uk/ws/files/1899530/2013arc_sciencereview_06_ahc_final_1_.pdf eng eng info:eu-repo/semantics/openAccess Smeed , D , Wood , R , Cunningham , S , McCarthy , G , Kuhlbrodt , T & Dye , S 2013 , ' Impacts of climate change on the Atlantic Heat Conveyor (Atlantic Meridional Overturning Circulation) ' , MCCP Science Review , vol. 4 . https://doi.org/10.14465/2013.arc06.049-059 article 2013 ftuhipublicatio https://doi.org/10.14465/2013.arc06.049-059 2023-04-06T22:20:14Z The meridional overturning circulation (MOC) is part of a global ocean circulation that redistributes heat from Equatorial to Polar regions. In the Atlantic, the MOC (AMOC) carries heat northward (the Atlantic Heat Conveyor) which is released to the atmosphere and maintains UK temperatures between 3 to 5°C higher than they would otherwise be. However, the present strength and structure of the MOC may not continue. The IPCC Fourth Assessment Report (IPCC, 2007) concludes that there is greater than 90% chance that the AMOC will slow by up to half by 2100, compared to pre-industrial levels, offsetting some of the warming over the European sector of the North Atlantic, and contributing to the rate of Atlantic sea-level-rise. The IPCC also concluded that there is less than 10% chance of abrupt changes during the 21st Century. Daily observations using the RAPID MOC mooring array at 26°N are providing a continuous and growing time series of the AMOC strength and structure, the time series is not yet sufficiently long to determine if there is a long-term trend in the AMOC. There was a significant reduction in the AMOC in 2009-2010 that has since recovered. The relationships between the AMOC reduction and the anomalous winter weather over the UK at the same time are not yet understood. Other observations do not at present provide a coherent Atlantic wide picture of MOC variability, and there is little evidence of any long-term slowing. Despite substantial progress over recent years in understanding and modelling the AMOC, projections of its future fate are still subject to significant uncertainty. Article in Journal/Newspaper North Atlantic University of the Highlands and Islands: Research Database of UHI
institution Open Polar
collection University of the Highlands and Islands: Research Database of UHI
op_collection_id ftuhipublicatio
language English
description The meridional overturning circulation (MOC) is part of a global ocean circulation that redistributes heat from Equatorial to Polar regions. In the Atlantic, the MOC (AMOC) carries heat northward (the Atlantic Heat Conveyor) which is released to the atmosphere and maintains UK temperatures between 3 to 5°C higher than they would otherwise be. However, the present strength and structure of the MOC may not continue. The IPCC Fourth Assessment Report (IPCC, 2007) concludes that there is greater than 90% chance that the AMOC will slow by up to half by 2100, compared to pre-industrial levels, offsetting some of the warming over the European sector of the North Atlantic, and contributing to the rate of Atlantic sea-level-rise. The IPCC also concluded that there is less than 10% chance of abrupt changes during the 21st Century. Daily observations using the RAPID MOC mooring array at 26°N are providing a continuous and growing time series of the AMOC strength and structure, the time series is not yet sufficiently long to determine if there is a long-term trend in the AMOC. There was a significant reduction in the AMOC in 2009-2010 that has since recovered. The relationships between the AMOC reduction and the anomalous winter weather over the UK at the same time are not yet understood. Other observations do not at present provide a coherent Atlantic wide picture of MOC variability, and there is little evidence of any long-term slowing. Despite substantial progress over recent years in understanding and modelling the AMOC, projections of its future fate are still subject to significant uncertainty.
format Article in Journal/Newspaper
author Smeed, David
Wood, Richard
Cunningham, Stuart
McCarthy, Gerard
Kuhlbrodt, Till
Dye, Steven
spellingShingle Smeed, David
Wood, Richard
Cunningham, Stuart
McCarthy, Gerard
Kuhlbrodt, Till
Dye, Steven
Impacts of climate change on the Atlantic Heat Conveyor (Atlantic Meridional Overturning Circulation)
author_facet Smeed, David
Wood, Richard
Cunningham, Stuart
McCarthy, Gerard
Kuhlbrodt, Till
Dye, Steven
author_sort Smeed, David
title Impacts of climate change on the Atlantic Heat Conveyor (Atlantic Meridional Overturning Circulation)
title_short Impacts of climate change on the Atlantic Heat Conveyor (Atlantic Meridional Overturning Circulation)
title_full Impacts of climate change on the Atlantic Heat Conveyor (Atlantic Meridional Overturning Circulation)
title_fullStr Impacts of climate change on the Atlantic Heat Conveyor (Atlantic Meridional Overturning Circulation)
title_full_unstemmed Impacts of climate change on the Atlantic Heat Conveyor (Atlantic Meridional Overturning Circulation)
title_sort impacts of climate change on the atlantic heat conveyor (atlantic meridional overturning circulation)
publishDate 2013
url https://pure.uhi.ac.uk/en/publications/9edd780a-376f-4aa2-80ea-9212006b4af8
https://doi.org/10.14465/2013.arc06.049-059
https://pureadmin.uhi.ac.uk/ws/files/1899530/2013arc_sciencereview_06_ahc_final_1_.pdf
genre North Atlantic
genre_facet North Atlantic
op_source Smeed , D , Wood , R , Cunningham , S , McCarthy , G , Kuhlbrodt , T & Dye , S 2013 , ' Impacts of climate change on the Atlantic Heat Conveyor (Atlantic Meridional Overturning Circulation) ' , MCCP Science Review , vol. 4 . https://doi.org/10.14465/2013.arc06.049-059
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.14465/2013.arc06.049-059
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