Fate of the Atlantic Meridional Overturning Circulation: Strong decline under continued warming and Greenland melting
The most recent Intergovernmental Panel on Climate Change assessment report concludes that the Atlantic Meridional Overturning Circulation (AMOC) could weaken substantially but is very unlikely to collapse in the 21st century. However, the assessment largely neglected Greenland Ice Sheet (GrIS) mass...
Published in: | Geophysical Research Letters |
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AMER GEOPHYSICAL UNION
2016
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Online Access: | http://hdl.handle.net/10150/622754 https://doi.org/10.1002/2016GL070457 |
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ftunivarizona:oai:repository.arizona.edu:10150/622754 2023-05-15T16:28:29+02:00 Fate of the Atlantic Meridional Overturning Circulation: Strong decline under continued warming and Greenland melting Bakker, P. Schmittner, A. Lenaerts, J. T. M. Abe-Ouchi, A. Bi, D. van den Broeke, M. R. Chan, W.-L. Hu, A. Beadling, R. L. Marsland, S. J. Mernild, S. H. Saenko, O. A. Swingedouw, D. Sullivan, A. Yin, J. Univ Arizona, Dept Geosci College or Earth, Ocean, and Atmospheric Sciences; Oregon State University; Corvallis Oregon USA Institute for Marine and Atmospheric research; Utrecht University; Utrecht Netherlands Atmosphere and Ocean Research Institute; University of Tokyo; Tokyo Japan CSIRO Oceans and Atmosphere; Aspendale Victoria Australia National Center for Atmospheric Research; Boulder Colorado USA Department of Geosciences; University of Arizona; Tucson Arizona USA Faculty of Engineering and Science; Sogn og Fjordane University College; Sogndal Norway Canadian Centre for Climate Modelling and Analysis; Victoria British Columbia Canada Institut Pierre-Simon Laplace; Paris France 2016-12-16 http://hdl.handle.net/10150/622754 https://doi.org/10.1002/2016GL070457 en eng AMER GEOPHYSICAL UNION http://doi.wiley.com/10.1002/2016GL070457 Fate of the Atlantic Meridional Overturning Circulation: Strong decline under continued warming and Greenland melting 2016, 43 (23):12,252 Geophysical Research Letters 00948276 doi:10.1002/2016GL070457 http://hdl.handle.net/10150/622754 Geophysical Research Letters ©2016. American Geophysical Union and Her Majesty The Queen in Right of Canada. Atlantic Meridional Overturning Circulation climate change general circulation model Article 2016 ftunivarizona https://doi.org/10.1002/2016GL070457 2020-06-14T08:15:14Z The most recent Intergovernmental Panel on Climate Change assessment report concludes that the Atlantic Meridional Overturning Circulation (AMOC) could weaken substantially but is very unlikely to collapse in the 21st century. However, the assessment largely neglected Greenland Ice Sheet (GrIS) mass loss, lacked a comprehensive uncertainty analysis, and was limited to the 21st century. Here in a community effort, improved estimates of GrIS mass loss are included in multicentennial projections using eight state-of-the-science climate models, and an AMOC emulator is used to provide a probabilistic uncertainty assessment. We find that GrIS melting affects AMOC projections, even though it is of secondary importance. By years 2090-2100, the AMOC weakens by 18% [-3%, -34%; 90% probability] in an intermediate greenhouse-gas mitigation scenario and by 37% [-15%, -65%] under continued high emissions. Afterward, it stabilizes in the former but continues to decline in the latter to -74% [+4%, -100%] by 2290-2300, with a 44% likelihood of an AMOC collapse. This result suggests that an AMOC collapse can be avoided by CO2 mitigation. National Oceanographic and Atmospheric Administration [NA15OAR4310239]; Netherlands Earth System Science Center (NESSC); Polar Program of the Netherlands Organization for Scientific Research (NWO); Regional and Global Climate Modelling Program (RGCM) of the U.S. Department of Energy's Office of Science (BER) [DE-FC02-97ER62402]; Office of Science of the U.S. Department of Energy; ArCS; ICA-RUS; Natural Environment Research Council 6 month embargo; First Published: 13 December 2016. This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu. Article in Journal/Newspaper Greenland Ice Sheet The University of Arizona: UA Campus Repository Greenland Rus’ ENVELOPE(155.950,155.950,54.200,54.200) Geophysical Research Letters 43 23 12,252 12,260 |
institution |
Open Polar |
collection |
The University of Arizona: UA Campus Repository |
op_collection_id |
ftunivarizona |
language |
English |
topic |
Atlantic Meridional Overturning Circulation climate change general circulation model |
spellingShingle |
Atlantic Meridional Overturning Circulation climate change general circulation model Bakker, P. Schmittner, A. Lenaerts, J. T. M. Abe-Ouchi, A. Bi, D. van den Broeke, M. R. Chan, W.-L. Hu, A. Beadling, R. L. Marsland, S. J. Mernild, S. H. Saenko, O. A. Swingedouw, D. Sullivan, A. Yin, J. Fate of the Atlantic Meridional Overturning Circulation: Strong decline under continued warming and Greenland melting |
topic_facet |
Atlantic Meridional Overturning Circulation climate change general circulation model |
description |
The most recent Intergovernmental Panel on Climate Change assessment report concludes that the Atlantic Meridional Overturning Circulation (AMOC) could weaken substantially but is very unlikely to collapse in the 21st century. However, the assessment largely neglected Greenland Ice Sheet (GrIS) mass loss, lacked a comprehensive uncertainty analysis, and was limited to the 21st century. Here in a community effort, improved estimates of GrIS mass loss are included in multicentennial projections using eight state-of-the-science climate models, and an AMOC emulator is used to provide a probabilistic uncertainty assessment. We find that GrIS melting affects AMOC projections, even though it is of secondary importance. By years 2090-2100, the AMOC weakens by 18% [-3%, -34%; 90% probability] in an intermediate greenhouse-gas mitigation scenario and by 37% [-15%, -65%] under continued high emissions. Afterward, it stabilizes in the former but continues to decline in the latter to -74% [+4%, -100%] by 2290-2300, with a 44% likelihood of an AMOC collapse. This result suggests that an AMOC collapse can be avoided by CO2 mitigation. National Oceanographic and Atmospheric Administration [NA15OAR4310239]; Netherlands Earth System Science Center (NESSC); Polar Program of the Netherlands Organization for Scientific Research (NWO); Regional and Global Climate Modelling Program (RGCM) of the U.S. Department of Energy's Office of Science (BER) [DE-FC02-97ER62402]; Office of Science of the U.S. Department of Energy; ArCS; ICA-RUS; Natural Environment Research Council 6 month embargo; First Published: 13 December 2016. This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu. |
author2 |
Univ Arizona, Dept Geosci College or Earth, Ocean, and Atmospheric Sciences; Oregon State University; Corvallis Oregon USA Institute for Marine and Atmospheric research; Utrecht University; Utrecht Netherlands Atmosphere and Ocean Research Institute; University of Tokyo; Tokyo Japan CSIRO Oceans and Atmosphere; Aspendale Victoria Australia National Center for Atmospheric Research; Boulder Colorado USA Department of Geosciences; University of Arizona; Tucson Arizona USA Faculty of Engineering and Science; Sogn og Fjordane University College; Sogndal Norway Canadian Centre for Climate Modelling and Analysis; Victoria British Columbia Canada Institut Pierre-Simon Laplace; Paris France |
format |
Article in Journal/Newspaper |
author |
Bakker, P. Schmittner, A. Lenaerts, J. T. M. Abe-Ouchi, A. Bi, D. van den Broeke, M. R. Chan, W.-L. Hu, A. Beadling, R. L. Marsland, S. J. Mernild, S. H. Saenko, O. A. Swingedouw, D. Sullivan, A. Yin, J. |
author_facet |
Bakker, P. Schmittner, A. Lenaerts, J. T. M. Abe-Ouchi, A. Bi, D. van den Broeke, M. R. Chan, W.-L. Hu, A. Beadling, R. L. Marsland, S. J. Mernild, S. H. Saenko, O. A. Swingedouw, D. Sullivan, A. Yin, J. |
author_sort |
Bakker, P. |
title |
Fate of the Atlantic Meridional Overturning Circulation: Strong decline under continued warming and Greenland melting |
title_short |
Fate of the Atlantic Meridional Overturning Circulation: Strong decline under continued warming and Greenland melting |
title_full |
Fate of the Atlantic Meridional Overturning Circulation: Strong decline under continued warming and Greenland melting |
title_fullStr |
Fate of the Atlantic Meridional Overturning Circulation: Strong decline under continued warming and Greenland melting |
title_full_unstemmed |
Fate of the Atlantic Meridional Overturning Circulation: Strong decline under continued warming and Greenland melting |
title_sort |
fate of the atlantic meridional overturning circulation: strong decline under continued warming and greenland melting |
publisher |
AMER GEOPHYSICAL UNION |
publishDate |
2016 |
url |
http://hdl.handle.net/10150/622754 https://doi.org/10.1002/2016GL070457 |
long_lat |
ENVELOPE(155.950,155.950,54.200,54.200) |
geographic |
Greenland Rus’ |
geographic_facet |
Greenland Rus’ |
genre |
Greenland Ice Sheet |
genre_facet |
Greenland Ice Sheet |
op_relation |
http://doi.wiley.com/10.1002/2016GL070457 Fate of the Atlantic Meridional Overturning Circulation: Strong decline under continued warming and Greenland melting 2016, 43 (23):12,252 Geophysical Research Letters 00948276 doi:10.1002/2016GL070457 http://hdl.handle.net/10150/622754 Geophysical Research Letters |
op_rights |
©2016. American Geophysical Union and Her Majesty The Queen in Right of Canada. |
op_doi |
https://doi.org/10.1002/2016GL070457 |
container_title |
Geophysical Research Letters |
container_volume |
43 |
container_issue |
23 |
container_start_page |
12,252 |
op_container_end_page |
12,260 |
_version_ |
1766018145340882944 |