Standing and Transient Eddies in the Response of the Southern Ocean Meridional Overturning to the Southern Annular Mode

International audience To refine the understanding of how the Southern Ocean responds to recent intensification of the southern annular mode (SAM), a regional ocean model at two eddy-permitting resolutions was forced with two synthetic interannual forcings. The first forcing corresponds to homogeneo...

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Published in:Journal of Climate
Main Authors: Dufour, C., Le Sommer, J., Zika, J., Gehlen, M., Orr, J., Mathiot, P., Barnier, B.
Other Authors: Laboratoire des Écoulements Géophysiques et Industriels Grenoble (LEGI), Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Centre National de la Recherche Scientifique (CNRS), Modelling the Earth Response to Multiple Anthropogenic Interactions and Dynamics (MERMAID), Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA), Centre Georges Lemaître for Earth and Climate Research Louvain (TECLIM), Earth and Life Institute Louvain-La-Neuve (ELI), Université Catholique de Louvain = Catholic University of Louvain (UCL)-Université Catholique de Louvain = Catholic University of Louvain (UCL)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2012
Subjects:
Online Access:https://hal.science/hal-03113008
https://hal.science/hal-03113008/document
https://hal.science/hal-03113008/file/manuscript.pdf
https://doi.org/10.1175/JCLI-D-11-00309.1
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record_format openpolar
institution Open Polar
collection Université Grenoble Alpes: HAL
op_collection_id ftunigrenoble
language English
topic [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
spellingShingle [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
Dufour, C.
Le Sommer, J.
Zika, J.
Gehlen, M.
Orr, J.
Mathiot, P.
Barnier, B.
Standing and Transient Eddies in the Response of the Southern Ocean Meridional Overturning to the Southern Annular Mode
topic_facet [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 To refine the understanding of how the Southern Ocean responds to recent intensification of the southern annular mode (SAM), a regional ocean model at two eddy-permitting resolutions was forced with two synthetic interannual forcings. The first forcing corresponds to homogeneously intensified winds, while the second concerns their poleward intensification, consistent with positive phases of the SAM. Resulting wind-driven responses differ greatly between the nearly insensitive Antarctic Circumpolar Current (ACC) and the more sensitive meridional overturning circulation (MOC). As expected, eddies mitigate the response of the ACC and MOC to poleward-intensified winds. However, transient eddies do not necessarily play an increasing role in meridional transport with increasing resolution. As winds and resolution increase, meridional transport from standing eddies becomes more efficient at balancing wind-enhanced overturning. These results question the current paradigms on the role of eddies and present new challenges for eddy flux parameterization. Results also indicate that spatial patterns of wind anomalies are at least as important as the overall change in intensity in influencing the Southern Ocean’s dynamic response to wind events. Poleward-intensified wind anomalies from the positive trend in the SAM are far more efficient in accelerating the ACC than homogeneous wind anomalies.
author2 Laboratoire des Écoulements Géophysiques et Industriels Grenoble (LEGI)
Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Centre National de la Recherche Scientifique (CNRS)
Modelling the Earth Response to Multiple Anthropogenic Interactions and Dynamics (MERMAID)
Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA))
Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA))
Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)
Centre Georges Lemaître for Earth and Climate Research Louvain (TECLIM)
Earth and Life Institute Louvain-La-Neuve (ELI)
Université Catholique de Louvain = Catholic University of Louvain (UCL)-Université Catholique de Louvain = Catholic University of Louvain (UCL)
format Article in Journal/Newspaper
author Dufour, C.
Le Sommer, J.
Zika, J.
Gehlen, M.
Orr, J.
Mathiot, P.
Barnier, B.
author_facet Dufour, C.
Le Sommer, J.
Zika, J.
Gehlen, M.
Orr, J.
Mathiot, P.
Barnier, B.
author_sort Dufour, C.
title Standing and Transient Eddies in the Response of the Southern Ocean Meridional Overturning to the Southern Annular Mode
title_short Standing and Transient Eddies in the Response of the Southern Ocean Meridional Overturning to the Southern Annular Mode
title_full Standing and Transient Eddies in the Response of the Southern Ocean Meridional Overturning to the Southern Annular Mode
title_fullStr Standing and Transient Eddies in the Response of the Southern Ocean Meridional Overturning to the Southern Annular Mode
title_full_unstemmed Standing and Transient Eddies in the Response of the Southern Ocean Meridional Overturning to the Southern Annular Mode
title_sort standing and transient eddies in the response of the southern ocean meridional overturning to the southern annular mode
publisher HAL CCSD
publishDate 2012
url https://hal.science/hal-03113008
https://hal.science/hal-03113008/document
https://hal.science/hal-03113008/file/manuscript.pdf
https://doi.org/10.1175/JCLI-D-11-00309.1
geographic Antarctic
Southern Ocean
geographic_facet Antarctic
Southern Ocean
genre Antarc*
Antarctic
Southern Ocean
genre_facet Antarc*
Antarctic
Southern Ocean
op_source ISSN: 0894-8755
EISSN: 1520-0442
Journal of Climate
https://hal.science/hal-03113008
Journal of Climate, 2012, 25 (20), pp.6958-6974. ⟨10.1175/JCLI-D-11-00309.1⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1175/JCLI-D-11-00309.1
hal-03113008
https://hal.science/hal-03113008
https://hal.science/hal-03113008/document
https://hal.science/hal-03113008/file/manuscript.pdf
doi:10.1175/JCLI-D-11-00309.1
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1175/JCLI-D-11-00309.1
container_title Journal of Climate
container_volume 25
container_issue 20
container_start_page 6958
op_container_end_page 6974
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spelling ftunigrenoble:oai:HAL:hal-03113008v1 2024-05-12T07:54:10+00:00 Standing and Transient Eddies in the Response of the Southern Ocean Meridional Overturning to the Southern Annular Mode Dufour, C. Le Sommer, J. Zika, J. Gehlen, M. Orr, J. Mathiot, P. Barnier, B. Laboratoire des Écoulements Géophysiques et Industriels Grenoble (LEGI) Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Centre National de la Recherche Scientifique (CNRS) Modelling the Earth Response to Multiple Anthropogenic Interactions and Dynamics (MERMAID) Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) Centre Georges Lemaître for Earth and Climate Research Louvain (TECLIM) Earth and Life Institute Louvain-La-Neuve (ELI) Université Catholique de Louvain = Catholic University of Louvain (UCL)-Université Catholique de Louvain = Catholic University of Louvain (UCL) 2012 https://hal.science/hal-03113008 https://hal.science/hal-03113008/document https://hal.science/hal-03113008/file/manuscript.pdf https://doi.org/10.1175/JCLI-D-11-00309.1 en eng HAL CCSD American Meteorological Society info:eu-repo/semantics/altIdentifier/doi/10.1175/JCLI-D-11-00309.1 hal-03113008 https://hal.science/hal-03113008 https://hal.science/hal-03113008/document https://hal.science/hal-03113008/file/manuscript.pdf doi:10.1175/JCLI-D-11-00309.1 info:eu-repo/semantics/OpenAccess ISSN: 0894-8755 EISSN: 1520-0442 Journal of Climate https://hal.science/hal-03113008 Journal of Climate, 2012, 25 (20), pp.6958-6974. ⟨10.1175/JCLI-D-11-00309.1⟩ [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 2012 ftunigrenoble https://doi.org/10.1175/JCLI-D-11-00309.1 2024-04-18T03:17:46Z International audience To refine the understanding of how the Southern Ocean responds to recent intensification of the southern annular mode (SAM), a regional ocean model at two eddy-permitting resolutions was forced with two synthetic interannual forcings. The first forcing corresponds to homogeneously intensified winds, while the second concerns their poleward intensification, consistent with positive phases of the SAM. Resulting wind-driven responses differ greatly between the nearly insensitive Antarctic Circumpolar Current (ACC) and the more sensitive meridional overturning circulation (MOC). As expected, eddies mitigate the response of the ACC and MOC to poleward-intensified winds. However, transient eddies do not necessarily play an increasing role in meridional transport with increasing resolution. As winds and resolution increase, meridional transport from standing eddies becomes more efficient at balancing wind-enhanced overturning. These results question the current paradigms on the role of eddies and present new challenges for eddy flux parameterization. Results also indicate that spatial patterns of wind anomalies are at least as important as the overall change in intensity in influencing the Southern Ocean’s dynamic response to wind events. Poleward-intensified wind anomalies from the positive trend in the SAM are far more efficient in accelerating the ACC than homogeneous wind anomalies. Article in Journal/Newspaper Antarc* Antarctic Southern Ocean Université Grenoble Alpes: HAL Antarctic Southern Ocean Journal of Climate 25 20 6958 6974