AMOC Recent and Future Trends: A Crucial Role for Oceanic Resolution and Greenland Melting?
International audience The Atlantic Meridional Overturning Circulation (AMOC) is a crucial element of the Earth climate. It is a complex circulation system difficult to monitor and to model. There is considerable debate regarding its evolution over the last century as well as large uncertainty about...
Published in: | Frontiers in Climate |
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Main Authors: | , , , , , |
Other Authors: | , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2022
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Subjects: | |
Online Access: | https://hal.science/hal-03841884 https://hal.science/hal-03841884/document https://hal.science/hal-03841884/file/Swingedouw_FC_2022.pdf https://doi.org/10.3389/fclim.2022.838310 |
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ftunivnantes:oai:HAL:hal-03841884v1 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
Université de Nantes: HAL-UNIV-NANTES |
op_collection_id |
ftunivnantes |
language |
English |
topic |
North Atlantic AMOC Greenland melting numerical modeling high resolution [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology |
spellingShingle |
North Atlantic AMOC Greenland melting numerical modeling high resolution [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology Swingedouw, Didier Houssais, Marie-Noëlle Herbaut, Christophe Blaizot, Anne-Cécile Devilliers, Marion Deshayes, Julie AMOC Recent and Future Trends: A Crucial Role for Oceanic Resolution and Greenland Melting? |
topic_facet |
North Atlantic AMOC Greenland melting numerical modeling high resolution [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology |
description |
International audience The Atlantic Meridional Overturning Circulation (AMOC) is a crucial element of the Earth climate. It is a complex circulation system difficult to monitor and to model. There is considerable debate regarding its evolution over the last century as well as large uncertainty about its fate at the end of this century. We depict here the progress since the IPCC SROCC report, offering an update of its chapter 6.7. We also show new results from a high-resolution ocean model and a CMIP6 model to investigate the impact of Greenland Ice Sheet (GrIS) melting, a key uncertainty for past and future AMOC changes. The ocean-only simulation at 1/24° resolution in the Arctic-North Atlantic Ocean performed over the period 2004–2016 indicates that the spread of the Greenland freshwater runoff toward the center of the Labrador Sea, where oceanic convection occurs, seems larger in this model than in a CMIP6 model. Potential explanations are related to the model spatial resolution and the representation of mesoscale processes, which more realistically transport the freshwater released around the shelves and, through eddies, provides strong lateral exchanges between the fine-scale boundary current and the convective basin in the Labrador Sea. The larger freshening of the Labrador Sea in the high-resolution model then strongly affects deep convection activity. In the simulation including GrIS melting, the AMOC weakens by about 2 Sv after only 13 years, far more strongly than what is found in the CMIP6 model. This difference raises serious concerns on the ability of CMIP6 models to correctly assess the potential impact of GrIS melting on the AMOC changes over the last few decades as well as on its future fate. To gain confidence in the GrIS freshwater impacts on climate simulations and therefore in AMOC projections, urgent progress should be made on the parameterization of mesoscale processes in ocean models. |
author2 |
Environnements et Paléoenvironnements OCéaniques (EPOC) Observatoire aquitain des sciences de l'univers (OASU) Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-École pratique des hautes études (EPHE) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS) Variabilité de l'Océan et de la Glace de mer (VOG) Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) École normale supérieure - Paris (ENS-PSL) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-École normale supérieure - Paris (ENS-PSL) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité) Danish Meteorological Institute (DMI) Nucleus for European Modeling of the Ocean (NEMO R&D ) |
format |
Article in Journal/Newspaper |
author |
Swingedouw, Didier Houssais, Marie-Noëlle Herbaut, Christophe Blaizot, Anne-Cécile Devilliers, Marion Deshayes, Julie |
author_facet |
Swingedouw, Didier Houssais, Marie-Noëlle Herbaut, Christophe Blaizot, Anne-Cécile Devilliers, Marion Deshayes, Julie |
author_sort |
Swingedouw, Didier |
title |
AMOC Recent and Future Trends: A Crucial Role for Oceanic Resolution and Greenland Melting? |
title_short |
AMOC Recent and Future Trends: A Crucial Role for Oceanic Resolution and Greenland Melting? |
title_full |
AMOC Recent and Future Trends: A Crucial Role for Oceanic Resolution and Greenland Melting? |
title_fullStr |
AMOC Recent and Future Trends: A Crucial Role for Oceanic Resolution and Greenland Melting? |
title_full_unstemmed |
AMOC Recent and Future Trends: A Crucial Role for Oceanic Resolution and Greenland Melting? |
title_sort |
amoc recent and future trends: a crucial role for oceanic resolution and greenland melting? |
publisher |
HAL CCSD |
publishDate |
2022 |
url |
https://hal.science/hal-03841884 https://hal.science/hal-03841884/document https://hal.science/hal-03841884/file/Swingedouw_FC_2022.pdf https://doi.org/10.3389/fclim.2022.838310 |
geographic |
Arctic Greenland |
geographic_facet |
Arctic Greenland |
genre |
Arctic Greenland Ice Sheet Labrador Sea North Atlantic |
genre_facet |
Arctic Greenland Ice Sheet Labrador Sea North Atlantic |
op_source |
ISSN: 2624-9553 Frontiers in Climate https://hal.science/hal-03841884 Frontiers in Climate, 2022, 4, pp.838310. ⟨10.3389/fclim.2022.838310⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.3389/fclim.2022.838310 hal-03841884 https://hal.science/hal-03841884 https://hal.science/hal-03841884/document https://hal.science/hal-03841884/file/Swingedouw_FC_2022.pdf doi:10.3389/fclim.2022.838310 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.3389/fclim.2022.838310 |
container_title |
Frontiers in Climate |
container_volume |
4 |
_version_ |
1766347922967887872 |
spelling |
ftunivnantes:oai:HAL:hal-03841884v1 2023-05-15T15:17:41+02:00 AMOC Recent and Future Trends: A Crucial Role for Oceanic Resolution and Greenland Melting? Swingedouw, Didier Houssais, Marie-Noëlle Herbaut, Christophe Blaizot, Anne-Cécile Devilliers, Marion Deshayes, Julie Environnements et Paléoenvironnements OCéaniques (EPOC) Observatoire aquitain des sciences de l'univers (OASU) Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-École pratique des hautes études (EPHE) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Centre National de la Recherche Scientifique (CNRS) Variabilité de l'Océan et de la Glace de mer (VOG) Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) École normale supérieure - Paris (ENS-PSL) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-École normale supérieure - Paris (ENS-PSL) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité) Danish Meteorological Institute (DMI) Nucleus for European Modeling of the Ocean (NEMO R&D ) 2022 https://hal.science/hal-03841884 https://hal.science/hal-03841884/document https://hal.science/hal-03841884/file/Swingedouw_FC_2022.pdf https://doi.org/10.3389/fclim.2022.838310 en eng HAL CCSD Frontiers Media SA info:eu-repo/semantics/altIdentifier/doi/10.3389/fclim.2022.838310 hal-03841884 https://hal.science/hal-03841884 https://hal.science/hal-03841884/document https://hal.science/hal-03841884/file/Swingedouw_FC_2022.pdf doi:10.3389/fclim.2022.838310 info:eu-repo/semantics/OpenAccess ISSN: 2624-9553 Frontiers in Climate https://hal.science/hal-03841884 Frontiers in Climate, 2022, 4, pp.838310. ⟨10.3389/fclim.2022.838310⟩ North Atlantic AMOC Greenland melting numerical modeling high resolution [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology info:eu-repo/semantics/article Journal articles 2022 ftunivnantes https://doi.org/10.3389/fclim.2022.838310 2023-02-08T02:13:38Z International audience The Atlantic Meridional Overturning Circulation (AMOC) is a crucial element of the Earth climate. It is a complex circulation system difficult to monitor and to model. There is considerable debate regarding its evolution over the last century as well as large uncertainty about its fate at the end of this century. We depict here the progress since the IPCC SROCC report, offering an update of its chapter 6.7. We also show new results from a high-resolution ocean model and a CMIP6 model to investigate the impact of Greenland Ice Sheet (GrIS) melting, a key uncertainty for past and future AMOC changes. The ocean-only simulation at 1/24° resolution in the Arctic-North Atlantic Ocean performed over the period 2004–2016 indicates that the spread of the Greenland freshwater runoff toward the center of the Labrador Sea, where oceanic convection occurs, seems larger in this model than in a CMIP6 model. Potential explanations are related to the model spatial resolution and the representation of mesoscale processes, which more realistically transport the freshwater released around the shelves and, through eddies, provides strong lateral exchanges between the fine-scale boundary current and the convective basin in the Labrador Sea. The larger freshening of the Labrador Sea in the high-resolution model then strongly affects deep convection activity. In the simulation including GrIS melting, the AMOC weakens by about 2 Sv after only 13 years, far more strongly than what is found in the CMIP6 model. This difference raises serious concerns on the ability of CMIP6 models to correctly assess the potential impact of GrIS melting on the AMOC changes over the last few decades as well as on its future fate. To gain confidence in the GrIS freshwater impacts on climate simulations and therefore in AMOC projections, urgent progress should be made on the parameterization of mesoscale processes in ocean models. Article in Journal/Newspaper Arctic Greenland Ice Sheet Labrador Sea North Atlantic Université de Nantes: HAL-UNIV-NANTES Arctic Greenland Frontiers in Climate 4 |