Southern Ocean CO 2 sink: the contribution of the sea ice
We report first direct measurements of the partial pressure of CO 2 (pCO 2 ) within Antarctic pack sea ice brines and related CO 2 fluxes across the air-ice interface. From late winter to summer, brines encased in the ice change from a CO 2 large oversaturation, relative to the atmosphere, to a mark...
Published in: | Journal of Geophysical Research: Oceans |
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Wiley-Blackwell Publishing, Inc.
2014
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Online Access: | https://doi.org/10.1002/2014JC009941 http://ecite.utas.edu.au/100403 |
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ftunivtasecite:oai:ecite.utas.edu.au:100403 2023-05-15T14:03:25+02:00 Southern Ocean CO 2 sink: the contribution of the sea ice Delille, B Vancoppenolle, M Geilfus, N-X Tilbrook, B Lannuzel, D Schoemann, V Becquevort, S Carnat, G Delille, D Lancelot, C Chou, L Dieckmann, GS Tison, J-L 2014 application/pdf https://doi.org/10.1002/2014JC009941 http://ecite.utas.edu.au/100403 en eng Wiley-Blackwell Publishing, Inc. http://ecite.utas.edu.au/100403/2/100403 final.pdf http://dx.doi.org/10.1002/2014JC009941 Delille, B and Vancoppenolle, M and Geilfus, N-X and Tilbrook, B and Lannuzel, D and Schoemann, V and Becquevort, S and Carnat, G and Delille, D and Lancelot, C and Chou, L and Dieckmann, GS and Tison, J-L, Southern Ocean CO 2 sink: the contribution of the sea ice, Journal of Geophysical Research: Oceans, 119, (9) pp. 6340-6355. ISSN 2169-9275 (2014) [Refereed Article] http://ecite.utas.edu.au/100403 Earth Sciences Oceanography Chemical Oceanography Refereed Article PeerReviewed 2014 ftunivtasecite https://doi.org/10.1002/2014JC009941 2019-12-13T22:02:15Z We report first direct measurements of the partial pressure of CO 2 (pCO 2 ) within Antarctic pack sea ice brines and related CO 2 fluxes across the air-ice interface. From late winter to summer, brines encased in the ice change from a CO 2 large oversaturation, relative to the atmosphere, to a marked undersaturation while the underlying oceanic waters remains slightly oversaturated. The decrease from winter to summer of pCO 2 in the brines is driven by dilution with melting ice, dissolution of carbonate crystals, and net primary production. As the ice warms, its permeability increases, allowing CO 2 transfer at the air-sea ice interface. The sea ice changes from a transient source to a sink for atmospheric CO 2 . We upscale these observations to the whole Antarctic sea ice cover using the NEMO-LIM3 large-scale sea ice-ocean and provide first estimates of spring and summer CO 2 uptake from the atmosphere by Antarctic sea ice. Over the spring-summer period, the Antarctic sea ice cover is a net sink of atmospheric CO 2 of 0.029 Pg C, about 58% of the estimated annual uptake from the Southern Ocean. Sea ice then contributes significantly to the sink of CO 2 of the Southern Ocean. Article in Journal/Newspaper Antarc* Antarctic Sea ice Southern Ocean eCite UTAS (University of Tasmania) Antarctic Southern Ocean The Antarctic Journal of Geophysical Research: Oceans 119 9 6340 6355 |
institution |
Open Polar |
collection |
eCite UTAS (University of Tasmania) |
op_collection_id |
ftunivtasecite |
language |
English |
topic |
Earth Sciences Oceanography Chemical Oceanography |
spellingShingle |
Earth Sciences Oceanography Chemical Oceanography Delille, B Vancoppenolle, M Geilfus, N-X Tilbrook, B Lannuzel, D Schoemann, V Becquevort, S Carnat, G Delille, D Lancelot, C Chou, L Dieckmann, GS Tison, J-L Southern Ocean CO 2 sink: the contribution of the sea ice |
topic_facet |
Earth Sciences Oceanography Chemical Oceanography |
description |
We report first direct measurements of the partial pressure of CO 2 (pCO 2 ) within Antarctic pack sea ice brines and related CO 2 fluxes across the air-ice interface. From late winter to summer, brines encased in the ice change from a CO 2 large oversaturation, relative to the atmosphere, to a marked undersaturation while the underlying oceanic waters remains slightly oversaturated. The decrease from winter to summer of pCO 2 in the brines is driven by dilution with melting ice, dissolution of carbonate crystals, and net primary production. As the ice warms, its permeability increases, allowing CO 2 transfer at the air-sea ice interface. The sea ice changes from a transient source to a sink for atmospheric CO 2 . We upscale these observations to the whole Antarctic sea ice cover using the NEMO-LIM3 large-scale sea ice-ocean and provide first estimates of spring and summer CO 2 uptake from the atmosphere by Antarctic sea ice. Over the spring-summer period, the Antarctic sea ice cover is a net sink of atmospheric CO 2 of 0.029 Pg C, about 58% of the estimated annual uptake from the Southern Ocean. Sea ice then contributes significantly to the sink of CO 2 of the Southern Ocean. |
format |
Article in Journal/Newspaper |
author |
Delille, B Vancoppenolle, M Geilfus, N-X Tilbrook, B Lannuzel, D Schoemann, V Becquevort, S Carnat, G Delille, D Lancelot, C Chou, L Dieckmann, GS Tison, J-L |
author_facet |
Delille, B Vancoppenolle, M Geilfus, N-X Tilbrook, B Lannuzel, D Schoemann, V Becquevort, S Carnat, G Delille, D Lancelot, C Chou, L Dieckmann, GS Tison, J-L |
author_sort |
Delille, B |
title |
Southern Ocean CO 2 sink: the contribution of the sea ice |
title_short |
Southern Ocean CO 2 sink: the contribution of the sea ice |
title_full |
Southern Ocean CO 2 sink: the contribution of the sea ice |
title_fullStr |
Southern Ocean CO 2 sink: the contribution of the sea ice |
title_full_unstemmed |
Southern Ocean CO 2 sink: the contribution of the sea ice |
title_sort |
southern ocean co 2 sink: the contribution of the sea ice |
publisher |
Wiley-Blackwell Publishing, Inc. |
publishDate |
2014 |
url |
https://doi.org/10.1002/2014JC009941 http://ecite.utas.edu.au/100403 |
geographic |
Antarctic Southern Ocean The Antarctic |
geographic_facet |
Antarctic Southern Ocean The Antarctic |
genre |
Antarc* Antarctic Sea ice Southern Ocean |
genre_facet |
Antarc* Antarctic Sea ice Southern Ocean |
op_relation |
http://ecite.utas.edu.au/100403/2/100403 final.pdf http://dx.doi.org/10.1002/2014JC009941 Delille, B and Vancoppenolle, M and Geilfus, N-X and Tilbrook, B and Lannuzel, D and Schoemann, V and Becquevort, S and Carnat, G and Delille, D and Lancelot, C and Chou, L and Dieckmann, GS and Tison, J-L, Southern Ocean CO 2 sink: the contribution of the sea ice, Journal of Geophysical Research: Oceans, 119, (9) pp. 6340-6355. ISSN 2169-9275 (2014) [Refereed Article] http://ecite.utas.edu.au/100403 |
op_doi |
https://doi.org/10.1002/2014JC009941 |
container_title |
Journal of Geophysical Research: Oceans |
container_volume |
119 |
container_issue |
9 |
container_start_page |
6340 |
op_container_end_page |
6355 |
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1766274059294736384 |