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...
| Published in: | Geophysical Research Letters |
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| Main Authors: | , , , , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
American Geophysical Union
2004
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| Subjects: | |
| Online Access: | http://hdl.handle.net/10261/51805 https://doi.org/10.1029/2003GL018957 |
| Summary: | 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 |
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