Inter-annual variability of the carbon dioxide oceanic sink south of Tasmania
We compiled a large data-set from 22 cruises spanning from 1991 to 2003, of the partial pressure of CO 2 (pCO 2 ) in surface waters over the continental shelf (CS) and adjacent open ocean (43° to 46° S; 145° to 150° E), south of Tasmania. Climatological seasonal cycles of pCO 2 in the CS, the subtro...
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ftcopernicus:oai:publications.copernicus.org:bg5924 2023-05-15T18:25:46+02:00 Inter-annual variability of the carbon dioxide oceanic sink south of Tasmania Borges, A. V. Tilbrook, B. Metzl, N. Lenton, A. Delille, B. 2018-09-27 application/pdf https://doi.org/10.5194/bg-5-141-2008 https://www.biogeosciences.net/5/141/2008/ eng eng doi:10.5194/bg-5-141-2008 https://www.biogeosciences.net/5/141/2008/ eISSN: 1726-4189 Text 2018 ftcopernicus https://doi.org/10.5194/bg-5-141-2008 2019-12-24T09:58:23Z We compiled a large data-set from 22 cruises spanning from 1991 to 2003, of the partial pressure of CO 2 (pCO 2 ) in surface waters over the continental shelf (CS) and adjacent open ocean (43° to 46° S; 145° to 150° E), south of Tasmania. Climatological seasonal cycles of pCO 2 in the CS, the subtropical zone (STZ) and the subAntarctic zone (SAZ) are described and used to determine monthly pCO 2 anomalies. These are used in combination with monthly anomalies of sea surface temperature (SST) to investigate inter-annual variations of SST and pCO 2 . Monthly anomalies of SST (as intense as 2°C) are apparent in the CS, STZ and SAZ, and are indicative of strong inter-annual variability that seems to be related to large-scale coupled atmosphere-ocean oscillations. Anomalies of pCO 2 normalized to a constant temperature are negatively related to SST anomalies. A reduced winter-time vertical input of dissolved inorganic carbon (DIC) during phases of positive SST anomalies, related to a poleward shift of westerly winds, and a concomitant local decrease in wind stress is the likely cause of the negative relationship between pCO 2 and SST anomalies. The observed pattern is an increase of the sink for atmospheric CO 2 associated with positive SST anomalies, although strongly modulated by inter-annual variability of wind speed. Assuming that phases of positive SST anomalies are indicative of the future evolution of regional ocean biogeochemistry under global warming, we show using a purely observational based approach that some provinces of the Southern Ocean could provide a potential negative feedback on increasing atmospheric CO 2 . Text Southern Ocean Copernicus Publications: E-Journals Southern Ocean Biogeosciences 5 1 141 155 |
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Open Polar |
collection |
Copernicus Publications: E-Journals |
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ftcopernicus |
language |
English |
description |
We compiled a large data-set from 22 cruises spanning from 1991 to 2003, of the partial pressure of CO 2 (pCO 2 ) in surface waters over the continental shelf (CS) and adjacent open ocean (43° to 46° S; 145° to 150° E), south of Tasmania. Climatological seasonal cycles of pCO 2 in the CS, the subtropical zone (STZ) and the subAntarctic zone (SAZ) are described and used to determine monthly pCO 2 anomalies. These are used in combination with monthly anomalies of sea surface temperature (SST) to investigate inter-annual variations of SST and pCO 2 . Monthly anomalies of SST (as intense as 2°C) are apparent in the CS, STZ and SAZ, and are indicative of strong inter-annual variability that seems to be related to large-scale coupled atmosphere-ocean oscillations. Anomalies of pCO 2 normalized to a constant temperature are negatively related to SST anomalies. A reduced winter-time vertical input of dissolved inorganic carbon (DIC) during phases of positive SST anomalies, related to a poleward shift of westerly winds, and a concomitant local decrease in wind stress is the likely cause of the negative relationship between pCO 2 and SST anomalies. The observed pattern is an increase of the sink for atmospheric CO 2 associated with positive SST anomalies, although strongly modulated by inter-annual variability of wind speed. Assuming that phases of positive SST anomalies are indicative of the future evolution of regional ocean biogeochemistry under global warming, we show using a purely observational based approach that some provinces of the Southern Ocean could provide a potential negative feedback on increasing atmospheric CO 2 . |
format |
Text |
author |
Borges, A. V. Tilbrook, B. Metzl, N. Lenton, A. Delille, B. |
spellingShingle |
Borges, A. V. Tilbrook, B. Metzl, N. Lenton, A. Delille, B. Inter-annual variability of the carbon dioxide oceanic sink south of Tasmania |
author_facet |
Borges, A. V. Tilbrook, B. Metzl, N. Lenton, A. Delille, B. |
author_sort |
Borges, A. V. |
title |
Inter-annual variability of the carbon dioxide oceanic sink south of Tasmania |
title_short |
Inter-annual variability of the carbon dioxide oceanic sink south of Tasmania |
title_full |
Inter-annual variability of the carbon dioxide oceanic sink south of Tasmania |
title_fullStr |
Inter-annual variability of the carbon dioxide oceanic sink south of Tasmania |
title_full_unstemmed |
Inter-annual variability of the carbon dioxide oceanic sink south of Tasmania |
title_sort |
inter-annual variability of the carbon dioxide oceanic sink south of tasmania |
publishDate |
2018 |
url |
https://doi.org/10.5194/bg-5-141-2008 https://www.biogeosciences.net/5/141/2008/ |
geographic |
Southern Ocean |
geographic_facet |
Southern Ocean |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_source |
eISSN: 1726-4189 |
op_relation |
doi:10.5194/bg-5-141-2008 https://www.biogeosciences.net/5/141/2008/ |
op_doi |
https://doi.org/10.5194/bg-5-141-2008 |
container_title |
Biogeosciences |
container_volume |
5 |
container_issue |
1 |
container_start_page |
141 |
op_container_end_page |
155 |
_version_ |
1766207411012501504 |