The Role of Southern Ocean Surface Forcings and Mixing in the Global Conveyor

International audience Despite the renewed interest in the Southern Ocean, there are yet many unknowns because of the scarcity of measurements and the complexity of the thermohaline circulation. Hence the authors present here the analysis of the thermohaline circulation of the Southern Ocean of a st...

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Published in:Journal of Physical Oceanography
Main Authors: Iudicone, Daniele, Madec, Gurvan, Blanke, Bruno, Speich, Sabrina
Other Authors: Stazione Zoologica Anton Dohrn (SZN), 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), Laboratoire de physique des océans (LPO), Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2008
Subjects:
Online Access:https://hal.science/hal-00308922
https://hal.science/hal-00308922/document
https://hal.science/hal-00308922/file/%5B15200485%20-%20Journal%20of%20Physical%20Oceanography%5D%20The%20Role%20of%20Southern%20Ocean%20Surface%20Forcings%20and%20Mixing%20in%20the%20Global%20Conveyor-1.pdf
https://doi.org/10.1175/2008JPO3519.1
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record_format openpolar
institution Open Polar
collection Institut national des sciences de l'Univers: HAL-INSU
op_collection_id ftinsu
language English
topic [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
spellingShingle [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
Iudicone, Daniele
Madec, Gurvan
Blanke, Bruno
Speich, Sabrina
The Role of Southern Ocean Surface Forcings and Mixing in the Global Conveyor
topic_facet [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
[PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph]
description International audience Despite the renewed interest in the Southern Ocean, there are yet many unknowns because of the scarcity of measurements and the complexity of the thermohaline circulation. Hence the authors present here the analysis of the thermohaline circulation of the Southern Ocean of a steady-state simulation of a coupled ice–ocean model. The study aims to clarify the roles of surface fluxes and internal mixing, with focus on the mechanisms of the upper branch of the overturning. A quantitative dynamical analysis of the water-mass transformation has been performed using a new method. Surface fluxes, including the effect of the penetrative solar radiation, produce almost 40 Sv (1 Sv ≡ 10 6 m 3 s -1 ) of Subantarctic Mode Water while about 5 Sv of the densest water masses (γ > 28.2) are formed by brine rejection on the shelves of Antarctica and in the Weddell Sea. Mixing transforms one-half of the Subantarctic Mode Water into intermediate water and Upper Circumpolar Deep Water while bottom water is produced by Lower Circumpolar Deep Water and North Atlantic Deep Water mixing with shelf water. The upwelling of part of the North Atlantic Deep Water inflow is due to internal processes, mainly downward propagation of the surface freshwater excess via vertical mixing at the base of the mixed layer. A complementary Lagrangian analysis of the thermohaline circulation will be presented in a companion paper.
author2 Stazione Zoologica Anton Dohrn (SZN)
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)
Laboratoire de physique des océans (LPO)
Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)
format Article in Journal/Newspaper
author Iudicone, Daniele
Madec, Gurvan
Blanke, Bruno
Speich, Sabrina
author_facet Iudicone, Daniele
Madec, Gurvan
Blanke, Bruno
Speich, Sabrina
author_sort Iudicone, Daniele
title The Role of Southern Ocean Surface Forcings and Mixing in the Global Conveyor
title_short The Role of Southern Ocean Surface Forcings and Mixing in the Global Conveyor
title_full The Role of Southern Ocean Surface Forcings and Mixing in the Global Conveyor
title_fullStr The Role of Southern Ocean Surface Forcings and Mixing in the Global Conveyor
title_full_unstemmed The Role of Southern Ocean Surface Forcings and Mixing in the Global Conveyor
title_sort role of southern ocean surface forcings and mixing in the global conveyor
publisher HAL CCSD
publishDate 2008
url https://hal.science/hal-00308922
https://hal.science/hal-00308922/document
https://hal.science/hal-00308922/file/%5B15200485%20-%20Journal%20of%20Physical%20Oceanography%5D%20The%20Role%20of%20Southern%20Ocean%20Surface%20Forcings%20and%20Mixing%20in%20the%20Global%20Conveyor-1.pdf
https://doi.org/10.1175/2008JPO3519.1
genre Antarc*
Antarctica
North Atlantic Deep Water
North Atlantic
Southern Ocean
Weddell Sea
genre_facet Antarc*
Antarctica
North Atlantic Deep Water
North Atlantic
Southern Ocean
Weddell Sea
op_source ISSN: 0022-3670
EISSN: 1520-0485
Journal of Physical Oceanography
https://hal.science/hal-00308922
Journal of Physical Oceanography, 2008, 38 (7), pp.1377-1400. ⟨10.1175/2008JPO3519.1⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1175/2008JPO3519.1
hal-00308922
https://hal.science/hal-00308922
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doi:10.1175/2008JPO3519.1
IRD: fdi:010083533
WOS: 000257853500002
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op_doi https://doi.org/10.1175/2008JPO3519.1
container_title Journal of Physical Oceanography
container_volume 38
container_issue 7
container_start_page 1377
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spelling ftinsu:oai:HAL:hal-00308922v1 2024-04-28T08:01:30+00:00 The Role of Southern Ocean Surface Forcings and Mixing in the Global Conveyor Iudicone, Daniele Madec, Gurvan Blanke, Bruno Speich, Sabrina Stazione Zoologica Anton Dohrn (SZN) 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) Laboratoire de physique des océans (LPO) Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS) 2008-07 https://hal.science/hal-00308922 https://hal.science/hal-00308922/document https://hal.science/hal-00308922/file/%5B15200485%20-%20Journal%20of%20Physical%20Oceanography%5D%20The%20Role%20of%20Southern%20Ocean%20Surface%20Forcings%20and%20Mixing%20in%20the%20Global%20Conveyor-1.pdf https://doi.org/10.1175/2008JPO3519.1 en eng HAL CCSD American Meteorological Society info:eu-repo/semantics/altIdentifier/doi/10.1175/2008JPO3519.1 hal-00308922 https://hal.science/hal-00308922 https://hal.science/hal-00308922/document https://hal.science/hal-00308922/file/%5B15200485%20-%20Journal%20of%20Physical%20Oceanography%5D%20The%20Role%20of%20Southern%20Ocean%20Surface%20Forcings%20and%20Mixing%20in%20the%20Global%20Conveyor-1.pdf doi:10.1175/2008JPO3519.1 IRD: fdi:010083533 WOS: 000257853500002 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 0022-3670 EISSN: 1520-0485 Journal of Physical Oceanography https://hal.science/hal-00308922 Journal of Physical Oceanography, 2008, 38 (7), pp.1377-1400. ⟨10.1175/2008JPO3519.1⟩ [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography [PHYS.PHYS.PHYS-AO-PH]Physics [physics]/Physics [physics]/Atmospheric and Oceanic Physics [physics.ao-ph] info:eu-repo/semantics/article Journal articles 2008 ftinsu https://doi.org/10.1175/2008JPO3519.1 2024-04-05T00:36:09Z International audience Despite the renewed interest in the Southern Ocean, there are yet many unknowns because of the scarcity of measurements and the complexity of the thermohaline circulation. Hence the authors present here the analysis of the thermohaline circulation of the Southern Ocean of a steady-state simulation of a coupled ice–ocean model. The study aims to clarify the roles of surface fluxes and internal mixing, with focus on the mechanisms of the upper branch of the overturning. A quantitative dynamical analysis of the water-mass transformation has been performed using a new method. Surface fluxes, including the effect of the penetrative solar radiation, produce almost 40 Sv (1 Sv ≡ 10 6 m 3 s -1 ) of Subantarctic Mode Water while about 5 Sv of the densest water masses (γ > 28.2) are formed by brine rejection on the shelves of Antarctica and in the Weddell Sea. Mixing transforms one-half of the Subantarctic Mode Water into intermediate water and Upper Circumpolar Deep Water while bottom water is produced by Lower Circumpolar Deep Water and North Atlantic Deep Water mixing with shelf water. The upwelling of part of the North Atlantic Deep Water inflow is due to internal processes, mainly downward propagation of the surface freshwater excess via vertical mixing at the base of the mixed layer. A complementary Lagrangian analysis of the thermohaline circulation will be presented in a companion paper. Article in Journal/Newspaper Antarc* Antarctica North Atlantic Deep Water North Atlantic Southern Ocean Weddell Sea Institut national des sciences de l'Univers: HAL-INSU Journal of Physical Oceanography 38 7 1377 1400