Articles | Volume 10, issue 4
https://doi.org/10.5194/bg-10-2219-2013
https://doi.org/10.5194/bg-10-2219-2013
Research article
 | 
03 Apr 2013
Research article |  | 03 Apr 2013

The non-steady state oceanic CO2 signal: its importance, magnitude and a novel way to detect it

B. I. McNeil and R. J. Matear

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Cited articles

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Battle, M., Bender, M. L., Tans, P. P., White, J. W. C., Ellis, J. T., Conway, T., and Francey, R. J.: Global carbon sinks and their variability inferred from atmospheric O-2 and delta C-13, Science, 287, 2467–2470, 2000.
Bender, M. L., Ho, D. T., Hendricks, M. B., Mika, R., Battle, M. O., Tans, P. P., Conway, T. J., Sturtevant, B., and Cassar, N.: Atmospheric O(2)/N(2) changes, 1993–2002: Implications for the partitioning of fossil fuel CO(2) sequestration, Global Biogeochem. Cy., 19, GB4017, https://doi.org/10.1029/2004GB002410, 2005.
Bousquet, P., Peylin, P., Ciais, P., Le Quere, C., Friedlingstein, P., and Tans, P.: Regional changes in carbon dioxide fluxes of land and oceans since 1980, Science, 290, 1342–1346, 2000.
Chen, C.: Oceanic penetration of excess CO2 in a cross section between Alaska and Hawaii, Geophys. Res. Lett., 9, 117–119, 1982.
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