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Volume 12, issue 23
Biogeosciences, 12, 7251–7278, 2015
https://doi.org/10.5194/bg-12-7251-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
Biogeosciences, 12, 7251–7278, 2015
https://doi.org/10.5194/bg-12-7251-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 11 Dec 2015

Research article | 11 Dec 2015

Data-based estimates of the ocean carbon sink variability – first results of the Surface Ocean pCO2 Mapping intercomparison (SOCOM)

C. Rödenbeck et al.

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Cited articles

Claustre, H., Bishop, J., Boss, E., Bernard, S., Berthon, J.-F., Coatanoan, C., Johnson, K., Lotiker, A., Ulloa, O., Perry, M. J., D'Ortenzio, F., D'andon, O. H. F., and Uitz, J.: Bio-optical Profiling Floats as New Observational Tools for Biogeochemical and Ecosystem Studies, in Proceedings of OceanObs'09: Sustained Ocean Observations and Information for Society, Vol. 2, Venice, Italy, 21–25 September 2009, edited by: Hall, J., Harrison, D. E., and Stammer, D., ESA Publication WPP-306, 2010.
Cressman, G. P.: An operational objective analysis system, Mon. Weather Rev., 87, 367–374, 1959.
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This study investigates variations in the CO2 uptake of the ocean from year to year. These variations have been calculated from measurements of the surface-ocean carbon content by various different interpolation methods. The equatorial Pacific is estimated to be the region with the strongest year-to-year variations, tied to the El Nino phase. The global ocean CO2 uptake gradually increased from about the year 2000. The comparison of the interpolation methods identifies these findings as robust.
This study investigates variations in the CO2 uptake of the ocean from year to year. These...
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