Atlantic multidecadal oceanic variability and its influence on the atmosphere in a climate model
International audience The mechanisms controlling the decadal to multidecadal variability of the Atlantic Meridional Overturning Circulation (MOC) and its influence on the atmosphere are investigated using a control simulation with the IPSL-CM4 climate model. The multidecadal fluctuations of the MOC...
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ftsorbonneuniv:oai:HAL:hal-00760271v1 2024-05-19T07:42:57+00:00 Atlantic multidecadal oceanic variability and its influence on the atmosphere in a climate model M'Sadek, Rym Frankignoul, Claude 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) 2009-07 https://hal.science/hal-00760271 https://doi.org/10.1007/S00382-008-0452-0 en eng HAL CCSD Springer Verlag info:eu-repo/semantics/altIdentifier/doi/10.1007/S00382-008-0452-0 hal-00760271 https://hal.science/hal-00760271 BIBCODE: 2009ClDy.33.45M doi:10.1007/S00382-008-0452-0 ISSN: 0930-7575 EISSN: 1432-0894 Climate Dynamics https://hal.science/hal-00760271 Climate Dynamics, 2009, 33, pp.45-62. ⟨10.1007/S00382-008-0452-0⟩ Atlantic Meridional Overturning Circulation (MOC) Atlantic Multidecadal Oscillation (AMO) Ocean-to-atmosphere feedback Air-sea interactions [PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] info:eu-repo/semantics/article Journal articles 2009 ftsorbonneuniv https://doi.org/10.1007/S00382-008-0452-0 2024-04-25T03:36:26Z International audience The mechanisms controlling the decadal to multidecadal variability of the Atlantic Meridional Overturning Circulation (MOC) and its influence on the atmosphere are investigated using a control simulation with the IPSL-CM4 climate model. The multidecadal fluctuations of the MOC are mostly driven by deep convection in the subpolar gyre, which occurs south of Iceland in the model. The latter is primarily influenced by the anomalous advection of salinity due to changes in the East Atlantic Pattern (EAP), which is the second mode of atmospheric variability in the North Atlantic region. The North Atlantic Oscillation is the dominant mode, but it plays a secondary role in the MOC fluctuations. During summer, the MOC variability is shown to have a significant impact on the atmosphere in the North Atlantic-European sector. The MOC influence is due to an interhemispheric sea surface temperature (SST) anomaly with opposite signs in the two hemispheres but largest amplitude in the northern one. The SST pattern driven by the MOC mostly resembles the model Atlantic Multidecadal Oscillation (AMO) and bears some similarity with the observed one. It is shown that the AMO reflects both the MOC influence and the local atmospheric forcing. Hence, the MOC influence on climate is best detected using lagged relations between climatic fields. The atmospheric response resembles the EAP, in a phase that might induce a weak positive feedback on the MOC. Article in Journal/Newspaper Iceland North Atlantic North Atlantic oscillation HAL Sorbonne Université Climate Dynamics 33 1 45 62 |
institution |
Open Polar |
collection |
HAL Sorbonne Université |
op_collection_id |
ftsorbonneuniv |
language |
English |
topic |
Atlantic Meridional Overturning Circulation (MOC) Atlantic Multidecadal Oscillation (AMO) Ocean-to-atmosphere feedback Air-sea interactions [PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] |
spellingShingle |
Atlantic Meridional Overturning Circulation (MOC) Atlantic Multidecadal Oscillation (AMO) Ocean-to-atmosphere feedback Air-sea interactions [PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] M'Sadek, Rym Frankignoul, Claude Atlantic multidecadal oceanic variability and its influence on the atmosphere in a climate model |
topic_facet |
Atlantic Meridional Overturning Circulation (MOC) Atlantic Multidecadal Oscillation (AMO) Ocean-to-atmosphere feedback Air-sea interactions [PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] |
description |
International audience The mechanisms controlling the decadal to multidecadal variability of the Atlantic Meridional Overturning Circulation (MOC) and its influence on the atmosphere are investigated using a control simulation with the IPSL-CM4 climate model. The multidecadal fluctuations of the MOC are mostly driven by deep convection in the subpolar gyre, which occurs south of Iceland in the model. The latter is primarily influenced by the anomalous advection of salinity due to changes in the East Atlantic Pattern (EAP), which is the second mode of atmospheric variability in the North Atlantic region. The North Atlantic Oscillation is the dominant mode, but it plays a secondary role in the MOC fluctuations. During summer, the MOC variability is shown to have a significant impact on the atmosphere in the North Atlantic-European sector. The MOC influence is due to an interhemispheric sea surface temperature (SST) anomaly with opposite signs in the two hemispheres but largest amplitude in the northern one. The SST pattern driven by the MOC mostly resembles the model Atlantic Multidecadal Oscillation (AMO) and bears some similarity with the observed one. It is shown that the AMO reflects both the MOC influence and the local atmospheric forcing. Hence, the MOC influence on climate is best detected using lagged relations between climatic fields. The atmospheric response resembles the EAP, in a phase that might induce a weak positive feedback on the MOC. |
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 |
M'Sadek, Rym Frankignoul, Claude |
author_facet |
M'Sadek, Rym Frankignoul, Claude |
author_sort |
M'Sadek, Rym |
title |
Atlantic multidecadal oceanic variability and its influence on the atmosphere in a climate model |
title_short |
Atlantic multidecadal oceanic variability and its influence on the atmosphere in a climate model |
title_full |
Atlantic multidecadal oceanic variability and its influence on the atmosphere in a climate model |
title_fullStr |
Atlantic multidecadal oceanic variability and its influence on the atmosphere in a climate model |
title_full_unstemmed |
Atlantic multidecadal oceanic variability and its influence on the atmosphere in a climate model |
title_sort |
atlantic multidecadal oceanic variability and its influence on the atmosphere in a climate model |
publisher |
HAL CCSD |
publishDate |
2009 |
url |
https://hal.science/hal-00760271 https://doi.org/10.1007/S00382-008-0452-0 |
genre |
Iceland North Atlantic North Atlantic oscillation |
genre_facet |
Iceland North Atlantic North Atlantic oscillation |
op_source |
ISSN: 0930-7575 EISSN: 1432-0894 Climate Dynamics https://hal.science/hal-00760271 Climate Dynamics, 2009, 33, pp.45-62. ⟨10.1007/S00382-008-0452-0⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1007/S00382-008-0452-0 hal-00760271 https://hal.science/hal-00760271 BIBCODE: 2009ClDy.33.45M doi:10.1007/S00382-008-0452-0 |
op_doi |
https://doi.org/10.1007/S00382-008-0452-0 |
container_title |
Climate Dynamics |
container_volume |
33 |
container_issue |
1 |
container_start_page |
45 |
op_container_end_page |
62 |
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1799482646498115584 |