Oceanic Radiocarbon Between Antarctica and South Africa Along Woce Section 16 at 30°E

International audience Accelerator mass spectrometry (AMS) radiocarbon measurements were made on 120 samples collected between Antarctica and South Africa along 30°E during the WOCE-France CIVA 1 campaign in February 1993. Our principal objective was to complement the Southern Ocean's sparse ex...

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Published in:Radiocarbon
Main Authors: Leboucher, Viviane, Orr, James C., Jean-Baptiste, Philippe, Arnold, Maurice, Monfray, Patrick, Tisnérat-Laborde, Nadine, Poisson, Alain, Duplessy, Jean-Claude
Other Authors: 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), Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE), Institut de Recherche pour le Développement (IRD)-Institut National de la Recherche Agronomique (INRA)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Géochrononologie Traceurs Archéométrie (GEOTRAC), 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)), Laboratoire de Physique et Chimie Marines (LPCM), Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS), Paléocéanographie (PALEOCEAN)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 1999
Subjects:
Online Access:https://hal.science/hal-02500995
https://hal.science/hal-02500995/document
https://hal.science/hal-02500995/file/oceanic-radiocarbon-between-antarctica-and-south-africa-along-woce-section-16-at-30-e-div.pdf
https://doi.org/10.1017/S0033822200019330
id ftunivaixmarseil:oai:HAL:hal-02500995v1
record_format openpolar
institution Open Polar
collection Aix-Marseille Université: HAL
op_collection_id ftunivaixmarseil
language English
topic [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
spellingShingle [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
Leboucher, Viviane
Orr, James C.
Jean-Baptiste, Philippe
Arnold, Maurice
Monfray, Patrick
Tisnérat-Laborde, Nadine
Poisson, Alain
Duplessy, Jean-Claude
Oceanic Radiocarbon Between Antarctica and South Africa Along Woce Section 16 at 30°E
topic_facet [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
description International audience Accelerator mass spectrometry (AMS) radiocarbon measurements were made on 120 samples collected between Antarctica and South Africa along 30°E during the WOCE-France CIVA 1 campaign in February 1993. Our principal objective was to complement the Southern Ocean's sparse existing data set in order to improve the 14C benchmark used for validating ocean carbon-cycle models, which disagree considerably in this region. Measured 14C is consistent with the 0-S characteristics of CIVA1. Antarctic Intermediate Water (AAIW) forming north of the Polar Front (PF) is rich in'4C, whereas surface waters south of the PF are depleted in 14C. A distinct old 14C signal was found for the contribution of the Pacific Deep Water (PDW) to the return flow of Circumpolar Deep Waters (CDW). Comparison to previous measurements shows a 4C decrease in surface waters, consistent with northward displacement of surface waters, replacement by old deep waters upwelled at the Antarctic Divergence, and atmospheric decline in 14C. Conversely, an increase was found in deeper layers, in the AAIW. Large uncertainties, associated with previous methods for separating natural and bomb 14C when in the Southern Ocean south of 45°S, motivated us to develop a new approach that relies on a simple mixing model and on chlorofluorocarbon (CFC) measurements also taken during CIVA1. This approach leads to inventories for CIVA1 that are equal to or higher than those calculated with previous methods. Differences between old and new methods are especially high south of approximately 55°S, where bomb 14C inventories are relatively modest.
author2 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)
Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE)
Institut de Recherche pour le Développement (IRD)-Institut National de la Recherche Agronomique (INRA)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
Géochrononologie Traceurs Archéométrie (GEOTRAC)
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))
Laboratoire de Physique et Chimie Marines (LPCM)
Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS)
Paléocéanographie (PALEOCEAN)
format Article in Journal/Newspaper
author Leboucher, Viviane
Orr, James C.
Jean-Baptiste, Philippe
Arnold, Maurice
Monfray, Patrick
Tisnérat-Laborde, Nadine
Poisson, Alain
Duplessy, Jean-Claude
author_facet Leboucher, Viviane
Orr, James C.
Jean-Baptiste, Philippe
Arnold, Maurice
Monfray, Patrick
Tisnérat-Laborde, Nadine
Poisson, Alain
Duplessy, Jean-Claude
author_sort Leboucher, Viviane
title Oceanic Radiocarbon Between Antarctica and South Africa Along Woce Section 16 at 30°E
title_short Oceanic Radiocarbon Between Antarctica and South Africa Along Woce Section 16 at 30°E
title_full Oceanic Radiocarbon Between Antarctica and South Africa Along Woce Section 16 at 30°E
title_fullStr Oceanic Radiocarbon Between Antarctica and South Africa Along Woce Section 16 at 30°E
title_full_unstemmed Oceanic Radiocarbon Between Antarctica and South Africa Along Woce Section 16 at 30°E
title_sort oceanic radiocarbon between antarctica and south africa along woce section 16 at 30°e
publisher HAL CCSD
publishDate 1999
url https://hal.science/hal-02500995
https://hal.science/hal-02500995/document
https://hal.science/hal-02500995/file/oceanic-radiocarbon-between-antarctica-and-south-africa-along-woce-section-16-at-30-e-div.pdf
https://doi.org/10.1017/S0033822200019330
genre Antarc*
Antarctic
Antarctica
Southern Ocean
genre_facet Antarc*
Antarctic
Antarctica
Southern Ocean
op_source ISSN: 0033-8222
EISSN: 1945-5755
Radiocarbon
https://hal.science/hal-02500995
Radiocarbon, 1999, 41 (1), pp.51-73. ⟨10.1017/S0033822200019330⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1017/S0033822200019330
hal-02500995
https://hal.science/hal-02500995
https://hal.science/hal-02500995/document
https://hal.science/hal-02500995/file/oceanic-radiocarbon-between-antarctica-and-south-africa-along-woce-section-16-at-30-e-div.pdf
doi:10.1017/S0033822200019330
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1017/S0033822200019330
container_title Radiocarbon
container_volume 41
container_issue 1
container_start_page 51
op_container_end_page 73
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spelling ftunivaixmarseil:oai:HAL:hal-02500995v1 2024-04-28T07:56:11+00:00 Oceanic Radiocarbon Between Antarctica and South Africa Along Woce Section 16 at 30°E Leboucher, Viviane Orr, James C. Jean-Baptiste, Philippe Arnold, Maurice Monfray, Patrick Tisnérat-Laborde, Nadine Poisson, Alain Duplessy, Jean-Claude 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) Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE) Institut de Recherche pour le Développement (IRD)-Institut National de la Recherche Agronomique (INRA)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) Géochrononologie Traceurs Archéométrie (GEOTRAC) 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)) Laboratoire de Physique et Chimie Marines (LPCM) Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS) Paléocéanographie (PALEOCEAN) 1999 https://hal.science/hal-02500995 https://hal.science/hal-02500995/document https://hal.science/hal-02500995/file/oceanic-radiocarbon-between-antarctica-and-south-africa-along-woce-section-16-at-30-e-div.pdf https://doi.org/10.1017/S0033822200019330 en eng HAL CCSD University of Arizona info:eu-repo/semantics/altIdentifier/doi/10.1017/S0033822200019330 hal-02500995 https://hal.science/hal-02500995 https://hal.science/hal-02500995/document https://hal.science/hal-02500995/file/oceanic-radiocarbon-between-antarctica-and-south-africa-along-woce-section-16-at-30-e-div.pdf doi:10.1017/S0033822200019330 info:eu-repo/semantics/OpenAccess ISSN: 0033-8222 EISSN: 1945-5755 Radiocarbon https://hal.science/hal-02500995 Radiocarbon, 1999, 41 (1), pp.51-73. ⟨10.1017/S0033822200019330⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment info:eu-repo/semantics/article Journal articles 1999 ftunivaixmarseil https://doi.org/10.1017/S0033822200019330 2024-04-11T00:28:20Z International audience Accelerator mass spectrometry (AMS) radiocarbon measurements were made on 120 samples collected between Antarctica and South Africa along 30°E during the WOCE-France CIVA 1 campaign in February 1993. Our principal objective was to complement the Southern Ocean's sparse existing data set in order to improve the 14C benchmark used for validating ocean carbon-cycle models, which disagree considerably in this region. Measured 14C is consistent with the 0-S characteristics of CIVA1. Antarctic Intermediate Water (AAIW) forming north of the Polar Front (PF) is rich in'4C, whereas surface waters south of the PF are depleted in 14C. A distinct old 14C signal was found for the contribution of the Pacific Deep Water (PDW) to the return flow of Circumpolar Deep Waters (CDW). Comparison to previous measurements shows a 4C decrease in surface waters, consistent with northward displacement of surface waters, replacement by old deep waters upwelled at the Antarctic Divergence, and atmospheric decline in 14C. Conversely, an increase was found in deeper layers, in the AAIW. Large uncertainties, associated with previous methods for separating natural and bomb 14C when in the Southern Ocean south of 45°S, motivated us to develop a new approach that relies on a simple mixing model and on chlorofluorocarbon (CFC) measurements also taken during CIVA1. This approach leads to inventories for CIVA1 that are equal to or higher than those calculated with previous methods. Differences between old and new methods are especially high south of approximately 55°S, where bomb 14C inventories are relatively modest. Article in Journal/Newspaper Antarc* Antarctic Antarctica Southern Ocean Aix-Marseille Université: HAL Radiocarbon 41 1 51 73