Summer and winter distribution of δ 13 C DIC in surface waters of the South Indian Ocean [20°S-60°S]

International audience This paper describes for the first time the summer and winter distributions of sea surface δ 13 C DIC in the Southern Indian Ocean (20°S-60°S). For this we used δ 13 C DIC measurements from 10 cruises conducted between 1998 and 2005. For summer and winter, the highest δ 13 C D...

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Published in:Tellus B: Chemical and Physical Meteorology
Main Authors: Racapé, Virginie, Lo Monaco, Claire, Metzl, Nicolas, Pierre, Catherine
Other Authors: Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN), Institut Pierre-Simon-Laplace (IPSL), 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)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X), Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS-PSL), Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: CCSD 2010
Subjects:
Online Access:https://hal.science/hal-00759242
https://doi.org/10.1111/J.1600-0889.2010.00504.X
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author Racapé, Virginie
Lo Monaco, Claire
Metzl, Nicolas
Pierre, Catherine
author2 Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN)
Institut Pierre-Simon-Laplace (IPSL)
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)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)
Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS-PSL)
Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS)
author_facet Racapé, Virginie
Lo Monaco, Claire
Metzl, Nicolas
Pierre, Catherine
author_sort Racapé, Virginie
collection Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQ
container_issue 5
container_start_page 660
container_title Tellus B: Chemical and Physical Meteorology
container_volume 62
description International audience This paper describes for the first time the summer and winter distributions of sea surface δ 13 C DIC in the Southern Indian Ocean (20°S-60°S). For this we used δ 13 C DIC measurements from 10 cruises conducted between 1998 and 2005. For summer and winter, the highest δ 13 C DIC values (>2‰) are observed in sub-Antarctic waters (40°S-50°S) and attributed mainly to biological activity, enhanced in the vicinity of Crozet and Kerguelen Archipelagoes. The lowest δ 13 C DIC values are found in subtropical waters (25°S-35°S), with a minimum (<1‰) in the Agulhas Current region and in the Mozambique channel. On the seasonal scale, δ 13 C DIC is higher during summer than during winter in all regions. The largest seasonal amplitude of variation (~0.3‰), observed in the region 35°S-40°S, is attributed to biological activity during summer and to deep vertical mixing during winter. In subtropical oligotrophic waters, the mean seasonal amplitude of variation (~0.15‰) is mainly explained by air-sea CO 2 fluxes. On the interannual scale, we also identified a large negative anomaly of δ 13 C DIC in the subtropical waters during austral summer 2002, associated to an anomalous ocean CO 2 sink due to cold conditions during this period.
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spelling ftuniversailles:oai:HAL:hal-00759242v1 2025-04-20T14:24:41+00:00 Summer and winter distribution of δ 13 C DIC in surface waters of the South Indian Ocean [20°S-60°S] Racapé, Virginie Lo Monaco, Claire Metzl, Nicolas Pierre, Catherine Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) Institut Pierre-Simon-Laplace (IPSL) 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)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X) Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS-PSL) Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS) 2010-11 https://hal.science/hal-00759242 https://doi.org/10.1111/J.1600-0889.2010.00504.X en eng CCSD Taylor & Francis info:eu-repo/semantics/altIdentifier/doi/10.1111/J.1600-0889.2010.00504.X BIBCODE: 2010TellB.62.660R ISSN: 0280-6509 EISSN: 1600-0889 Tellus B - Chemical and Physical Meteorology https://hal.science/hal-00759242 Tellus B - Chemical and Physical Meteorology, 2010, 62, pp.660-673. &#x27E8;10.1111/J.1600-0889.2010.00504.X&#x27E9; [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] [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/article Journal articles 2010 ftuniversailles https://doi.org/10.1111/J.1600-0889.2010.00504.X 2025-03-26T05:13:34Z International audience This paper describes for the first time the summer and winter distributions of sea surface δ 13 C DIC in the Southern Indian Ocean (20°S-60°S). For this we used δ 13 C DIC measurements from 10 cruises conducted between 1998 and 2005. For summer and winter, the highest δ 13 C DIC values (>2‰) are observed in sub-Antarctic waters (40°S-50°S) and attributed mainly to biological activity, enhanced in the vicinity of Crozet and Kerguelen Archipelagoes. The lowest δ 13 C DIC values are found in subtropical waters (25°S-35°S), with a minimum (<1‰) in the Agulhas Current region and in the Mozambique channel. On the seasonal scale, δ 13 C DIC is higher during summer than during winter in all regions. The largest seasonal amplitude of variation (~0.3‰), observed in the region 35°S-40°S, is attributed to biological activity during summer and to deep vertical mixing during winter. In subtropical oligotrophic waters, the mean seasonal amplitude of variation (~0.15‰) is mainly explained by air-sea CO 2 fluxes. On the interannual scale, we also identified a large negative anomaly of δ 13 C DIC in the subtropical waters during austral summer 2002, associated to an anomalous ocean CO 2 sink due to cold conditions during this period. Article in Journal/Newspaper Antarc* Antarctic Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQ Antarctic Austral Indian Kerguelen Tellus B: Chemical and Physical Meteorology 62 5 660 673
spellingShingle [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]
[SDE.MCG]Environmental Sciences/Global Changes
Racapé, Virginie
Lo Monaco, Claire
Metzl, Nicolas
Pierre, Catherine
Summer and winter distribution of δ 13 C DIC in surface waters of the South Indian Ocean [20°S-60°S]
title Summer and winter distribution of δ 13 C DIC in surface waters of the South Indian Ocean [20°S-60°S]
title_full Summer and winter distribution of δ 13 C DIC in surface waters of the South Indian Ocean [20°S-60°S]
title_fullStr Summer and winter distribution of δ 13 C DIC in surface waters of the South Indian Ocean [20°S-60°S]
title_full_unstemmed Summer and winter distribution of δ 13 C DIC in surface waters of the South Indian Ocean [20°S-60°S]
title_short Summer and winter distribution of δ 13 C DIC in surface waters of the South Indian Ocean [20°S-60°S]
title_sort summer and winter distribution of δ 13 c dic in surface waters of the south indian ocean [20°s-60°s]
topic [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]
[SDE.MCG]Environmental Sciences/Global Changes
topic_facet [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]
[SDE.MCG]Environmental Sciences/Global Changes
url https://hal.science/hal-00759242
https://doi.org/10.1111/J.1600-0889.2010.00504.X