Role of wind stress and heat fluxes in interannual-to-decadal variability of air-sea CO 2 and O 2 fluxes in the North Atlantic
A coupled ecosystem-circulation model of the North Atlantic is used to examine the individual contributions by wind stress and surface heat fluxes to naturally driven interannual-to-decadal variability of air-sea fluxes of CO 2 and O 2 during 1948–2002. The model results indicate that variations in...
| Published in: | Geophysical Research Letters |
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| Main Authors: | , , |
| Format: | Article in Journal/Newspaper |
| Language: | unknown |
| Published: |
2006
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| Subjects: | |
| Online Access: | https://eprints.soton.ac.uk/44682/ http://www.agu.org/journals/gl/gl0618/2006GL026538/ |
| Summary: | A coupled ecosystem-circulation model of the North Atlantic is used to examine the individual contributions by wind stress and surface heat fluxes to naturally driven interannual-to-decadal variability of air-sea fluxes of CO 2 and O 2 during 1948–2002. The model results indicate that variations in O 2 fluxes are mainly driven by variations in surface heat fluxes in the extratropics (15°N to 70°N), and by wind stress in the tropics (10°S to 15°N). Conversely, variations in simulated CO 2 fluxes are predominantly wind-stress driven over the entire model domain (18°S to 70°N); while variability in piston velocity and surface heat fluxes is less important. The simulated uptake of O 2 by the North Atlantic amounts to 70 ± 11 Tmol yr -1 to which the subpolar region (45°N to 70°N) contributes by 62 ± 10 Tmol yr -1 . Whereas the subpolar North Atlantic takes up more than 2/3 of the total carbon absorbed by the North Atlantic in our model (about 0.3 Pg C yr -1 ), interannual variability of air-sea CO 2 fluxes reaches similar values (about 0.01 Pg C yr -1 each) in the subpolar (45°N to 70°N), the subtropical (15°N to 45°N) and the equatorial (10°S to 15°N) Atlantic. |
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