Observing Antarctic Bottom Water in the Southern Ocean

International audience Dense, cold waters formed on Antarctic continental shelves descend along the Antarctic continental margin, where they mix with other Southern Ocean waters to form Antarctic Bottom Water (AABW). AABW then spreads into the deepest parts of all major ocean basins, isolating heat...

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Published in:Frontiers in Marine Science
Main Authors: Silvano, Alessandro, Purkey, Sarah, Gordon, Arnold, Castagno, Pasquale, Stewart, Andrew, Rintoul, Stephen, Foppert, Annie, Gunn, Kathryn, Herraiz-Borreguero, Laura, Aoki, Shigeru, Nakayama, Yoshihiro, Naveira Garabato, Alberto, Spingys, Carl, Akhoudas, Camille Hayatte, Sallée, Jean-Baptiste, de Lavergne, Casimir, Abrahamsen, E. Povl, Meijers, Andrew, Meredith, Michael, Zhou, Shenjie, Tamura, Takeshi, Yamazaki, Kaihe, Ohshima, Kay, Falco, Pierpaolo, Budillon, Giorgio, Hattermann, Tore, Janout, Markus, Llanillo, Pedro, Bowen, Melissa, Darelius, Elin, Østerhus, Svein, Nicholls, Keith, Stevens, Craig, Fernandez, Denise, Cimoli, Laura, Jacobs, Stanley, Morrison, Adele, Hogg, Andrew Mcc., Haumann, F. Alexander, Mashayek, Ali, Wang, Zhaomin, Kerr, Rodrigo, Williams, Guy, Lee, Won Sang
Other Authors: National Oceanography Centre (NOC), Scripps Institution of Oceanography (SIO - UC San Diego), University of California San Diego (UC San Diego), University of California (UC)-University of California (UC), Lamont-Doherty Earth Observatory (LDEO), Columbia University New York, Università degli Studi di Messina = University of Messina (UniMe), Department of Atmospheric and Oceanic Sciences Montréal, McGill University = Université McGill Montréal, Canada, CSIRO Agriculture Flagship, Commonwealth Scientific and Industrial Research Organisation Canberra (CSIRO), Institute for Marine and Antarctic Studies Hobart (IMAS), University of Tasmania Hobart, Australia (UTAS), Institute of Low Temperature Science Sapporo, Hokkaido University Sapporo, Japan, Department of Geological Sciences Stockholm, Stockholm University, Processus et interactions de fine échelle océanique (PROTEO), 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), Nucleus for European Modeling of the Ocean (NEMO R&D )
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2023
Subjects:
Online Access:https://hal.science/hal-04454886
https://hal.science/hal-04454886/document
https://hal.science/hal-04454886/file/fmars-10-1221701.pdf
https://doi.org/10.3389/fmars.2023.1221701
id ftuniparissaclay:oai:HAL:hal-04454886v1
record_format openpolar
institution Open Polar
collection Archives ouvertes de Paris-Saclay
op_collection_id ftuniparissaclay
language English
topic [SDU]Sciences of the Universe [physics]
spellingShingle [SDU]Sciences of the Universe [physics]
Silvano, Alessandro
Purkey, Sarah
Gordon, Arnold
Castagno, Pasquale
Stewart, Andrew
Rintoul, Stephen
Foppert, Annie
Gunn, Kathryn
Herraiz-Borreguero, Laura
Aoki, Shigeru
Nakayama, Yoshihiro
Naveira Garabato, Alberto
Spingys, Carl
Akhoudas, Camille Hayatte
Sallée, Jean-Baptiste
de Lavergne, Casimir
Abrahamsen, E. Povl
Meijers, Andrew
Meredith, Michael
Zhou, Shenjie
Tamura, Takeshi
Yamazaki, Kaihe
Ohshima, Kay
Falco, Pierpaolo
Budillon, Giorgio
Hattermann, Tore
Janout, Markus
Llanillo, Pedro
Bowen, Melissa
Darelius, Elin
Østerhus, Svein
Nicholls, Keith
Stevens, Craig
Fernandez, Denise
Cimoli, Laura
Jacobs, Stanley
Morrison, Adele
Hogg, Andrew Mcc.
Haumann, F. Alexander
Mashayek, Ali
Wang, Zhaomin
Kerr, Rodrigo
Williams, Guy
Lee, Won Sang
Observing Antarctic Bottom Water in the Southern Ocean
topic_facet [SDU]Sciences of the Universe [physics]
description International audience Dense, cold waters formed on Antarctic continental shelves descend along the Antarctic continental margin, where they mix with other Southern Ocean waters to form Antarctic Bottom Water (AABW). AABW then spreads into the deepest parts of all major ocean basins, isolating heat and carbon from the atmosphere for centuries. Despite AABW’s key role in regulating Earth’s climate on long time scales and in recording Southern Ocean conditions, AABW remains poorly observed. This lack of observational data is mostly due to two factors. First, AABW originates on the Antarctic continental shelf and slope where in situ measurements are limited and ocean observations by satellites are hampered by persistent sea ice cover and long periods of darkness in winter. Second, north of the Antarctic continental slope, AABW is found below approximately 2 km depth, where in situ observations are also scarce and satellites cannot provide direct measurements. Here, we review progress made during the past decades in observing AABW. We describe 1) long-term monitoring obtained by moorings, by ship-based surveys, and beneath ice shelves through bore holes; 2) the recent development of autonomous observing tools in coastal Antarctic and deep ocean systems; and 3) alternative approaches including data assimilation models and satellite-derived proxies. The variety of approaches is beginning to transform our understanding of AABW, including its formation processes, temporal variability, and contribution to the lower limb of the global ocean meridional overturning circulation. In particular, these observations highlight the key role played by winds, sea ice, and the Antarctic Ice Sheet in AABW-related processes. We conclude by discussing future avenues for observing and understanding AABW, impressing the need for a sustained and coordinated observing system.
author2 National Oceanography Centre (NOC)
Scripps Institution of Oceanography (SIO - UC San Diego)
University of California San Diego (UC San Diego)
University of California (UC)-University of California (UC)
Lamont-Doherty Earth Observatory (LDEO)
Columbia University New York
Università degli Studi di Messina = University of Messina (UniMe)
Department of Atmospheric and Oceanic Sciences Montréal
McGill University = Université McGill Montréal, Canada
CSIRO Agriculture Flagship
Commonwealth Scientific and Industrial Research Organisation Canberra (CSIRO)
Institute for Marine and Antarctic Studies Hobart (IMAS)
University of Tasmania Hobart, Australia (UTAS)
Institute of Low Temperature Science Sapporo
Hokkaido University Sapporo, Japan
Department of Geological Sciences Stockholm
Stockholm University
Processus et interactions de fine échelle océanique (PROTEO)
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)
Nucleus for European Modeling of the Ocean (NEMO R&D )
format Article in Journal/Newspaper
author Silvano, Alessandro
Purkey, Sarah
Gordon, Arnold
Castagno, Pasquale
Stewart, Andrew
Rintoul, Stephen
Foppert, Annie
Gunn, Kathryn
Herraiz-Borreguero, Laura
Aoki, Shigeru
Nakayama, Yoshihiro
Naveira Garabato, Alberto
Spingys, Carl
Akhoudas, Camille Hayatte
Sallée, Jean-Baptiste
de Lavergne, Casimir
Abrahamsen, E. Povl
Meijers, Andrew
Meredith, Michael
Zhou, Shenjie
Tamura, Takeshi
Yamazaki, Kaihe
Ohshima, Kay
Falco, Pierpaolo
Budillon, Giorgio
Hattermann, Tore
Janout, Markus
Llanillo, Pedro
Bowen, Melissa
Darelius, Elin
Østerhus, Svein
Nicholls, Keith
Stevens, Craig
Fernandez, Denise
Cimoli, Laura
Jacobs, Stanley
Morrison, Adele
Hogg, Andrew Mcc.
Haumann, F. Alexander
Mashayek, Ali
Wang, Zhaomin
Kerr, Rodrigo
Williams, Guy
Lee, Won Sang
author_facet Silvano, Alessandro
Purkey, Sarah
Gordon, Arnold
Castagno, Pasquale
Stewart, Andrew
Rintoul, Stephen
Foppert, Annie
Gunn, Kathryn
Herraiz-Borreguero, Laura
Aoki, Shigeru
Nakayama, Yoshihiro
Naveira Garabato, Alberto
Spingys, Carl
Akhoudas, Camille Hayatte
Sallée, Jean-Baptiste
de Lavergne, Casimir
Abrahamsen, E. Povl
Meijers, Andrew
Meredith, Michael
Zhou, Shenjie
Tamura, Takeshi
Yamazaki, Kaihe
Ohshima, Kay
Falco, Pierpaolo
Budillon, Giorgio
Hattermann, Tore
Janout, Markus
Llanillo, Pedro
Bowen, Melissa
Darelius, Elin
Østerhus, Svein
Nicholls, Keith
Stevens, Craig
Fernandez, Denise
Cimoli, Laura
Jacobs, Stanley
Morrison, Adele
Hogg, Andrew Mcc.
Haumann, F. Alexander
Mashayek, Ali
Wang, Zhaomin
Kerr, Rodrigo
Williams, Guy
Lee, Won Sang
author_sort Silvano, Alessandro
title Observing Antarctic Bottom Water in the Southern Ocean
title_short Observing Antarctic Bottom Water in the Southern Ocean
title_full Observing Antarctic Bottom Water in the Southern Ocean
title_fullStr Observing Antarctic Bottom Water in the Southern Ocean
title_full_unstemmed Observing Antarctic Bottom Water in the Southern Ocean
title_sort observing antarctic bottom water in the southern ocean
publisher HAL CCSD
publishDate 2023
url https://hal.science/hal-04454886
https://hal.science/hal-04454886/document
https://hal.science/hal-04454886/file/fmars-10-1221701.pdf
https://doi.org/10.3389/fmars.2023.1221701
genre Antarc*
Antarctic
Ice Sheet
Ice Shelves
Sea ice
Southern Ocean
genre_facet Antarc*
Antarctic
Ice Sheet
Ice Shelves
Sea ice
Southern Ocean
op_source ISSN: 2296-7745
Frontiers in Marine Science
https://hal.science/hal-04454886
Frontiers in Marine Science, 2023, 10, ⟨10.3389/fmars.2023.1221701⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.3389/fmars.2023.1221701
hal-04454886
https://hal.science/hal-04454886
https://hal.science/hal-04454886/document
https://hal.science/hal-04454886/file/fmars-10-1221701.pdf
doi:10.3389/fmars.2023.1221701
WOS: 001129397500001
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.3389/fmars.2023.1221701
container_title Frontiers in Marine Science
container_volume 10
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spelling ftuniparissaclay:oai:HAL:hal-04454886v1 2024-05-19T07:32:16+00:00 Observing Antarctic Bottom Water in the Southern Ocean Silvano, Alessandro Purkey, Sarah Gordon, Arnold Castagno, Pasquale Stewart, Andrew Rintoul, Stephen Foppert, Annie Gunn, Kathryn Herraiz-Borreguero, Laura Aoki, Shigeru Nakayama, Yoshihiro Naveira Garabato, Alberto Spingys, Carl Akhoudas, Camille Hayatte Sallée, Jean-Baptiste de Lavergne, Casimir Abrahamsen, E. Povl Meijers, Andrew Meredith, Michael Zhou, Shenjie Tamura, Takeshi Yamazaki, Kaihe Ohshima, Kay Falco, Pierpaolo Budillon, Giorgio Hattermann, Tore Janout, Markus Llanillo, Pedro Bowen, Melissa Darelius, Elin Østerhus, Svein Nicholls, Keith Stevens, Craig Fernandez, Denise Cimoli, Laura Jacobs, Stanley Morrison, Adele Hogg, Andrew Mcc. Haumann, F. Alexander Mashayek, Ali Wang, Zhaomin Kerr, Rodrigo Williams, Guy Lee, Won Sang National Oceanography Centre (NOC) Scripps Institution of Oceanography (SIO - UC San Diego) University of California San Diego (UC San Diego) University of California (UC)-University of California (UC) Lamont-Doherty Earth Observatory (LDEO) Columbia University New York Università degli Studi di Messina = University of Messina (UniMe) Department of Atmospheric and Oceanic Sciences Montréal McGill University = Université McGill Montréal, Canada CSIRO Agriculture Flagship Commonwealth Scientific and Industrial Research Organisation Canberra (CSIRO) Institute for Marine and Antarctic Studies Hobart (IMAS) University of Tasmania Hobart, Australia (UTAS) Institute of Low Temperature Science Sapporo Hokkaido University Sapporo, Japan Department of Geological Sciences Stockholm Stockholm University Processus et interactions de fine échelle océanique (PROTEO) 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) Nucleus for European Modeling of the Ocean (NEMO R&D ) 2023-12-08 https://hal.science/hal-04454886 https://hal.science/hal-04454886/document https://hal.science/hal-04454886/file/fmars-10-1221701.pdf https://doi.org/10.3389/fmars.2023.1221701 en eng HAL CCSD Frontiers Media info:eu-repo/semantics/altIdentifier/doi/10.3389/fmars.2023.1221701 hal-04454886 https://hal.science/hal-04454886 https://hal.science/hal-04454886/document https://hal.science/hal-04454886/file/fmars-10-1221701.pdf doi:10.3389/fmars.2023.1221701 WOS: 001129397500001 info:eu-repo/semantics/OpenAccess ISSN: 2296-7745 Frontiers in Marine Science https://hal.science/hal-04454886 Frontiers in Marine Science, 2023, 10, ⟨10.3389/fmars.2023.1221701⟩ [SDU]Sciences of the Universe [physics] info:eu-repo/semantics/article Journal articles 2023 ftuniparissaclay https://doi.org/10.3389/fmars.2023.1221701 2024-04-22T17:25:34Z International audience Dense, cold waters formed on Antarctic continental shelves descend along the Antarctic continental margin, where they mix with other Southern Ocean waters to form Antarctic Bottom Water (AABW). AABW then spreads into the deepest parts of all major ocean basins, isolating heat and carbon from the atmosphere for centuries. Despite AABW’s key role in regulating Earth’s climate on long time scales and in recording Southern Ocean conditions, AABW remains poorly observed. This lack of observational data is mostly due to two factors. First, AABW originates on the Antarctic continental shelf and slope where in situ measurements are limited and ocean observations by satellites are hampered by persistent sea ice cover and long periods of darkness in winter. Second, north of the Antarctic continental slope, AABW is found below approximately 2 km depth, where in situ observations are also scarce and satellites cannot provide direct measurements. Here, we review progress made during the past decades in observing AABW. We describe 1) long-term monitoring obtained by moorings, by ship-based surveys, and beneath ice shelves through bore holes; 2) the recent development of autonomous observing tools in coastal Antarctic and deep ocean systems; and 3) alternative approaches including data assimilation models and satellite-derived proxies. The variety of approaches is beginning to transform our understanding of AABW, including its formation processes, temporal variability, and contribution to the lower limb of the global ocean meridional overturning circulation. In particular, these observations highlight the key role played by winds, sea ice, and the Antarctic Ice Sheet in AABW-related processes. We conclude by discussing future avenues for observing and understanding AABW, impressing the need for a sustained and coordinated observing system. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet Ice Shelves Sea ice Southern Ocean Archives ouvertes de Paris-Saclay Frontiers in Marine Science 10