A decrease in the sink for atmospheric CO2 in the North Atlantic
4 páginas, 4 figuras, 1 tabla Global ocean carbon models and available syntheses of the oceanic CO2 flux suggest that the North Atlantic subpolar gyre (50 N–70 N, 80 W–10 W) is a region of increasing uptake of CO2 from the atmosphere, with the oceanic partial pressure of CO2 (pCO2) increasing more s...
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ftcsic:oai:digital.csic.es:10261/51805 2024-02-11T10:06:12+01:00 A decrease in the sink for atmospheric CO2 in the North Atlantic Lefèvre, Nathalie Watson, Andrew J. Olsen, Are Ríos, Aida F. Pérez, Fiz F. Johannessen, Truls 2004 http://hdl.handle.net/10261/51805 https://doi.org/10.1029/2003GL018957 en eng American Geophysical Union http://dx.doi.org/10.1029/2003GL018957 Geophysical Research Letters 31: L07306 (2004) 0094-8276 http://hdl.handle.net/10261/51805 doi:10.1029/2003GL018957 open artículo http://purl.org/coar/resource_type/c_6501 2004 ftcsic https://doi.org/10.1029/2003GL018957 2024-01-16T09:38:46Z 4 páginas, 4 figuras, 1 tabla Global ocean carbon models and available syntheses of the oceanic CO2 flux suggest that the North Atlantic subpolar gyre (50 N–70 N, 80 W–10 W) is a region of increasing uptake of CO2 from the atmosphere, with the oceanic partial pressure of CO2 (pCO2) increasing more slowly than the atmospheric CO2 over time. Our analysis of available CO2 data shows that, on the contrary, seawater pCO2 has increased faster than the atmosphere in recent decades, especially in summer, resulting in a decrease in uptake from the atmosphere. A decrease in the biological productivity of the region may be the underlying cause of this trend. From the observed trend we estimated a significant decrease in the annual carbon uptake in this region. This work has been funded by the European Commission under the program Environment and sustainable development, contract number EVK2-CT- 2000-00088, project CAVASSOO, contact number EVK2-2001-00115, project NOCES. Peer reviewed Article in Journal/Newspaper North Atlantic Digital.CSIC (Spanish National Research Council) Geophysical Research Letters 31 7 n/a n/a |
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Open Polar |
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Digital.CSIC (Spanish National Research Council) |
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ftcsic |
language |
English |
description |
4 páginas, 4 figuras, 1 tabla Global ocean carbon models and available syntheses of the oceanic CO2 flux suggest that the North Atlantic subpolar gyre (50 N–70 N, 80 W–10 W) is a region of increasing uptake of CO2 from the atmosphere, with the oceanic partial pressure of CO2 (pCO2) increasing more slowly than the atmospheric CO2 over time. Our analysis of available CO2 data shows that, on the contrary, seawater pCO2 has increased faster than the atmosphere in recent decades, especially in summer, resulting in a decrease in uptake from the atmosphere. A decrease in the biological productivity of the region may be the underlying cause of this trend. From the observed trend we estimated a significant decrease in the annual carbon uptake in this region. This work has been funded by the European Commission under the program Environment and sustainable development, contract number EVK2-CT- 2000-00088, project CAVASSOO, contact number EVK2-2001-00115, project NOCES. Peer reviewed |
format |
Article in Journal/Newspaper |
author |
Lefèvre, Nathalie Watson, Andrew J. Olsen, Are Ríos, Aida F. Pérez, Fiz F. Johannessen, Truls |
spellingShingle |
Lefèvre, Nathalie Watson, Andrew J. Olsen, Are Ríos, Aida F. Pérez, Fiz F. Johannessen, Truls A decrease in the sink for atmospheric CO2 in the North Atlantic |
author_facet |
Lefèvre, Nathalie Watson, Andrew J. Olsen, Are Ríos, Aida F. Pérez, Fiz F. Johannessen, Truls |
author_sort |
Lefèvre, Nathalie |
title |
A decrease in the sink for atmospheric CO2 in the North Atlantic |
title_short |
A decrease in the sink for atmospheric CO2 in the North Atlantic |
title_full |
A decrease in the sink for atmospheric CO2 in the North Atlantic |
title_fullStr |
A decrease in the sink for atmospheric CO2 in the North Atlantic |
title_full_unstemmed |
A decrease in the sink for atmospheric CO2 in the North Atlantic |
title_sort |
decrease in the sink for atmospheric co2 in the north atlantic |
publisher |
American Geophysical Union |
publishDate |
2004 |
url |
http://hdl.handle.net/10261/51805 https://doi.org/10.1029/2003GL018957 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
http://dx.doi.org/10.1029/2003GL018957 Geophysical Research Letters 31: L07306 (2004) 0094-8276 http://hdl.handle.net/10261/51805 doi:10.1029/2003GL018957 |
op_rights |
open |
op_doi |
https://doi.org/10.1029/2003GL018957 |
container_title |
Geophysical Research Letters |
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31 |
container_issue |
7 |
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1790603747869589504 |