Links between the Southern Annular Mode and the Atlantic Meridional Overturning Circulation in a Climate Model

International audience The links between the atmospheric southern annular mode (SAM), the Southern Ocean, and the Atlantic meridional overturning circulation (AMOC) at interannual to multidecadal time scales are investigated in a 500-yr control integration of the L'Institut Pierre-Simon Laplace...

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Published in:Journal of Climate
Main Authors: Marini, Camille, Frankignoul, Claude, Mignot, Juliette
Other Authors: Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN), Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-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)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-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)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2011
Subjects:
Online Access:https://hal.science/hal-00994602
https://hal.science/hal-00994602/document
https://hal.science/hal-00994602/file/Marini_JCLI_2011.pdf
https://doi.org/10.1175/2010JCLI3576.1
id ftunivnantes:oai:HAL:hal-00994602v1
record_format openpolar
institution Open Polar
collection Université de Nantes: HAL-UNIV-NANTES
op_collection_id ftunivnantes
language English
topic Annular mode
Meridional overturning circulation
Atlantic Ocean
Climate models
ENSO
[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]
spellingShingle Annular mode
Meridional overturning circulation
Atlantic Ocean
Climate models
ENSO
[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]
Marini, Camille
Frankignoul, Claude
Mignot, Juliette
Links between the Southern Annular Mode and the Atlantic Meridional Overturning Circulation in a Climate Model
topic_facet Annular mode
Meridional overturning circulation
Atlantic Ocean
Climate models
ENSO
[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph]
description International audience The links between the atmospheric southern annular mode (SAM), the Southern Ocean, and the Atlantic meridional overturning circulation (AMOC) at interannual to multidecadal time scales are investigated in a 500-yr control integration of the L'Institut Pierre-Simon Laplace Coupled Model, version 4 (IPSL CM4) climate model. The Antarctic Circumpolar Current, as described by its transport through the Drake Passage, is well correlated with the SAM at the yearly time scale, reflecting that an intensification of the westerlies south of 45°S leads to its acceleration. Also in phase with a positive SAM, the global meridional overturning circulation is modified in the Southern Hemisphere, primarily reflecting a forced barotropic response. In the model, the AMOC and the SAM are linked at several time scales. An intensification of the AMOC lags a positive SAM by about 8 yr. This is due to a correlation between the SAM and the atmospheric circulation in the northern North Atlantic that reflects a symmetric ENSO influence on the two hemispheres, as well as an independent, delayed interhemispheric link driven by the SAM. Both effects lead to an intensification of the subpolar gyre and, by salinity advection, increased deep convection and a stronger AMOC. A slower oceanic link between the SAM and the AMOC is found at a multidecadal time scale. Salinity anomalies generated by the SAM enter the South Atlantic from the Drake Passage and, more importantly, the Indian Ocean; they propagate northward, eventually reaching the northern North Atlantic where, for a positive SAM, they decrease the vertical stratification and thus increase the AMOC.
author2 Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN)
Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-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)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-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)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)
format Article in Journal/Newspaper
author Marini, Camille
Frankignoul, Claude
Mignot, Juliette
author_facet Marini, Camille
Frankignoul, Claude
Mignot, Juliette
author_sort Marini, Camille
title Links between the Southern Annular Mode and the Atlantic Meridional Overturning Circulation in a Climate Model
title_short Links between the Southern Annular Mode and the Atlantic Meridional Overturning Circulation in a Climate Model
title_full Links between the Southern Annular Mode and the Atlantic Meridional Overturning Circulation in a Climate Model
title_fullStr Links between the Southern Annular Mode and the Atlantic Meridional Overturning Circulation in a Climate Model
title_full_unstemmed Links between the Southern Annular Mode and the Atlantic Meridional Overturning Circulation in a Climate Model
title_sort links between the southern annular mode and the atlantic meridional overturning circulation in a climate model
publisher HAL CCSD
publishDate 2011
url https://hal.science/hal-00994602
https://hal.science/hal-00994602/document
https://hal.science/hal-00994602/file/Marini_JCLI_2011.pdf
https://doi.org/10.1175/2010JCLI3576.1
long_lat ENVELOPE(141.467,141.467,-66.782,-66.782)
geographic Antarctic
Drake Passage
Indian
Laplace
Southern Ocean
The Antarctic
geographic_facet Antarctic
Drake Passage
Indian
Laplace
Southern Ocean
The Antarctic
genre Antarc*
Antarctic
Drake Passage
North Atlantic
Southern Ocean
genre_facet Antarc*
Antarctic
Drake Passage
North Atlantic
Southern Ocean
op_source ISSN: 0894-8755
EISSN: 1520-0442
Journal of Climate
https://hal.science/hal-00994602
Journal of Climate, 2011, 24 (3), pp.624-640. ⟨10.1175/2010JCLI3576.1⟩
http://journals.ametsoc.org/doi/abs/10.1175/2010JCLI3576.1
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1175/2010JCLI3576.1
hal-00994602
https://hal.science/hal-00994602
https://hal.science/hal-00994602/document
https://hal.science/hal-00994602/file/Marini_JCLI_2011.pdf
doi:10.1175/2010JCLI3576.1
IRD: fdi:010053437
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1175/2010JCLI3576.1
container_title Journal of Climate
container_volume 24
container_issue 3
container_start_page 624
op_container_end_page 640
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spelling ftunivnantes:oai:HAL:hal-00994602v1 2023-05-15T13:46:49+02:00 Links between the Southern Annular Mode and the Atlantic Meridional Overturning Circulation in a Climate Model Marini, Camille Frankignoul, Claude Mignot, Juliette Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-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)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-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)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) 2011-02 https://hal.science/hal-00994602 https://hal.science/hal-00994602/document https://hal.science/hal-00994602/file/Marini_JCLI_2011.pdf https://doi.org/10.1175/2010JCLI3576.1 en eng HAL CCSD American Meteorological Society info:eu-repo/semantics/altIdentifier/doi/10.1175/2010JCLI3576.1 hal-00994602 https://hal.science/hal-00994602 https://hal.science/hal-00994602/document https://hal.science/hal-00994602/file/Marini_JCLI_2011.pdf doi:10.1175/2010JCLI3576.1 IRD: fdi:010053437 info:eu-repo/semantics/OpenAccess ISSN: 0894-8755 EISSN: 1520-0442 Journal of Climate https://hal.science/hal-00994602 Journal of Climate, 2011, 24 (3), pp.624-640. ⟨10.1175/2010JCLI3576.1⟩ http://journals.ametsoc.org/doi/abs/10.1175/2010JCLI3576.1 Annular mode Meridional overturning circulation Atlantic Ocean Climate models ENSO [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] [PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] info:eu-repo/semantics/article Journal articles 2011 ftunivnantes https://doi.org/10.1175/2010JCLI3576.1 2023-02-07T23:41:52Z International audience The links between the atmospheric southern annular mode (SAM), the Southern Ocean, and the Atlantic meridional overturning circulation (AMOC) at interannual to multidecadal time scales are investigated in a 500-yr control integration of the L'Institut Pierre-Simon Laplace Coupled Model, version 4 (IPSL CM4) climate model. The Antarctic Circumpolar Current, as described by its transport through the Drake Passage, is well correlated with the SAM at the yearly time scale, reflecting that an intensification of the westerlies south of 45°S leads to its acceleration. Also in phase with a positive SAM, the global meridional overturning circulation is modified in the Southern Hemisphere, primarily reflecting a forced barotropic response. In the model, the AMOC and the SAM are linked at several time scales. An intensification of the AMOC lags a positive SAM by about 8 yr. This is due to a correlation between the SAM and the atmospheric circulation in the northern North Atlantic that reflects a symmetric ENSO influence on the two hemispheres, as well as an independent, delayed interhemispheric link driven by the SAM. Both effects lead to an intensification of the subpolar gyre and, by salinity advection, increased deep convection and a stronger AMOC. A slower oceanic link between the SAM and the AMOC is found at a multidecadal time scale. Salinity anomalies generated by the SAM enter the South Atlantic from the Drake Passage and, more importantly, the Indian Ocean; they propagate northward, eventually reaching the northern North Atlantic where, for a positive SAM, they decrease the vertical stratification and thus increase the AMOC. Article in Journal/Newspaper Antarc* Antarctic Drake Passage North Atlantic Southern Ocean Université de Nantes: HAL-UNIV-NANTES Antarctic Drake Passage Indian Laplace ENVELOPE(141.467,141.467,-66.782,-66.782) Southern Ocean The Antarctic Journal of Climate 24 3 624 640