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      A perturbation simulation of CO2uptake in an ocean general circulation model

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          Most cited references62

          • Record: found
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          Carbon dioxide in water and seawater: the solubility of a non-ideal gas

          R.F. Weiss (1974)
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            Observational contrains on the global atmospheric co2 budget.

            Observed atmospheric concentrations of CO(2) and data on the partial pressures of CO(2) in surface ocean waters are combined to identify globally significant sources and sinks of CO(2). The atmospheric data are compared with boundary layer concentrations calculated with the transport fields generated by a general circulation model (GCM) for specified source-sink distributions. In the model the observed north-south atmospheric concentration gradient can be maintained only if sinks for CO(2) are greater in the Northern than in the Southern Hemisphere. The observed differences between the partial pressure of CO(2) in the surface waters of the Northern Hemisphere and the atmosphere are too small for the oceans to be the major sink of fossil fuel CO(2). Therefore, a large amount of the CO(2) is apparently absorbed on the continents by terrestrial ecosystems.
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              A numerical method for the study of the circulation of the world ocean

              Kirk Bryan (1969)
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                Author and article information

                Journal
                JGREA2
                Journal of Geophysical Research
                J. Geophys. Res.
                American Geophysical Union (AGU)
                0148-0227
                1992
                1992
                : 97
                : C3
                : 3621
                Article
                10.1029/91JC02849
                d0c84584-6624-4b39-b00f-2cb69756a91f
                © 1992

                http://doi.wiley.com/10.1002/tdm_license_1.1

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