Seasonal uptake of anthropogenic CO₂ in an ocean general circulation model

References

• Bacastow, R. B. 1981. Numerical evaluation of the eva-sion factor. In: Carbon cycle modelling (ed. B. Bolin). New York. John Wiley, pp. 95–101.
   Google Scholar
• Bacastow, R. B. and Maier-Reimer, E. 1990. Ocean-circulation model of the carbon cycle. aim. Dyn. 4, 95–125.
   Google Scholar
• Bottomley, M., Folland, C. K., Hsiung, J., Newell, R. E. and Parker, D. E. 1990. Global ocean surface temperature atlas (GOSTA). A joint project of the Meteorological Office and Dept. of Earth, Atmospheric and Planetary Sciences, Massachusetts Institute of Technology. HMSO, London, 333 pp.
   Google Scholar
• Broecker, W. S. and Peng, T. H. 1982. Tracers in the sea. Lamont-Doherty Geological Observatory, Palisades, NY, 690 pp.
   Google Scholar
• Bryan, F. 1987. Parameter sensitivity of primitive equation ocean general circulation models. J. Phys. Oceanogr. 17, 970–985.
   Web of Science ®Google Scholar
• Bryan, K. 1969. A numerical method for the study of the circulation of the world ocean. J. Comput. Phys. 4, 347–379.
   Google Scholar
• Bryan, K. 1984. Accelerating the convergence to equi-librium of ocean climate models. J. Phys. Oceanogr. 14, 666–673.
   Web of Science ®Google Scholar
• Bryan, K. and Lewis, L. J. 1979. A water mass model of the world ocean. J. Geophys. Res. 84, 2503–2517.
   Web of Science ®Google Scholar
• Carrissimo, B. C., Oort, A. H. and Yonder Haar, T. H. 1985. Estimates of the meridional energy transports in the atmosphere and ocean. J. Phys. Oceanogr. 15, 82–91.
   Web of Science ®Google Scholar
• Chen, C.-T. A. 1982a. On the distribution of anthropogenic CO, in the Atlantic and Southern oceans. Deep-Sea Res. 5, 563–580.
   Google Scholar
• Chen, C.-T. A. 1982b. Oceanic penetration of excess CO2 in a cross section between Alaska and Hawaii. Geophys. Res. Lett. 9, 117–119.
   Web of Science ®Google Scholar
• Cox, M. D. 1984. A primitive equation, 3-dimensional model of the ocean. GFDL Ocean Group Tech. Rep. No. 1,143 pp.
   Google Scholar
• Cox, M. D. 1987. Isopycnal diffusion in a z-coordinate ocean model. Ocean Modelling 74, 1–5.
   Google Scholar
• England, M. H. 1992. On the formation of antarctic intermediate and bottom water in ocean general circulation models. J. Phys. Oceanogr. 22, 918–926.
   Web of Science ®Google Scholar
• England, M. H. 1993. Representing the global-scale water masses in ocean general circulation models. J. Phys. Oceanogr. 23, 1523–1552.
   Web of Science ®Google Scholar
• Esbensen, S. K. and Kushnir, Y. 1981. The heat budget of the global ocean: an atlas based on estimates from sur-face marine observations. Climate Research Institute, Rep. No. 29, Oregon State University, Corvallis, USA.
   Google Scholar
• Etcheto, J. and Merlivat, L. 1988. Satellite determination of the carbon dioxide exchange coefficient at the ocean-atmosphere interface: A first step. J. Geophys. Res. 93, 15669–15678.
   Web of Science ®Google Scholar
• Gargett, A. E. and Holloway, G. 1992. Sensitivity of the GFDL ocean model to different diffusivities for heat and salt./. Phys. Oceanogr. 22, 1158–1177.
   Web of Science ®Google Scholar
• Godfrey, J. S. 1989. A Sverdrup model of the depth-integrated flow for the world ocean allowing for island circulations. Geophys. Astrophys. Fluid Dyn. 45, 89–112.
   Web of Science ®Google Scholar
• Goyet, C. and Poisson, A. 1989. New determination of carbonic acid dissociation constants in seawater as a function of temperature and salinity. Deep Sea Res. 36, 1635–1654.
   Google Scholar
• Haney, R. L. 1971. Surface thermal boundary condition for ocean circulation models. J. Phys. Oceanogr. 1, 241–248.
   Google Scholar
• Hellerman, S. and Rosenstein, M. 1983. Normal monthly wind stress over the world ocean with error estimates. J. Phys. Oceanogr. 13, 1093–1104.
   Web of Science ®Google Scholar
• Hibler, W. D. 1979. A dynamic-thermodynamic sea-ice model. J. Phys. Oceanogr. 9, 815–846.
   Web of Science ®Google Scholar
• Hirst, A. C. and Godfrey, J. S. 1993. The role of Indonesian throughflow in a global ocean GCM. J. Phys. Oceanogr. 23,1057–1086.
   Web of Science ®Google Scholar
• Hsuing, J. 1985. Estimates of global oceanic meridional heat transport. J. Phys. Oceanogr. 15, 1405–1413.
   Web of Science ®Google Scholar
• Meson, S. and Gordon, C. 1989. Parametrization of the upper ocean mixed layer in a tropical ocean GCM. Dynamical Climatology Technical Note No. 74. UK Meteorological Office, Bracknell.
   Google Scholar
• IPCC. 1990. Climate change: the IPCC scientific assess-ment. (eds. J. T. Houghton, G. J. Jenkins, and J. J. Cambridge, UK. Cambridge University Press, 365 pp.
   Google Scholar
• Jaeger, L. 1976. Monatskarten des Niederschlags fur die Ganze Erde. Bet Deutsch Wetterdienstes 18, no. 139.
   Google Scholar
• Kraus, E. B. and Turner, J. S. 1967. A one-dimensional model of the seasonal thermocline. II. The general theory and its consequences. Tellus 19, 98–105.
   Google Scholar
• Keeling, C. D., Piper, S. C. and Heimann, M. 1989. A three dimensional model of atmospheric CO, transport based on observed winds, 4, Mean annual gradients and interannual variations. In: Aspects of climate variability in the Pacific and the Western Americas (ed. D. H. Peterson). Washington, DC. AGU, pp. 305–363.
   Google Scholar
• Keeling, R. F. and Shertz, S. R. 1992. Seasonal and atmospheric variations in atmospheric oxygen and implications for the global carbon cycle. Nature 358, 723–727.
   Web of Science ®Google Scholar
• Knaus, J. 1969. A note on the transport of the Gulf Stream. Deep Sea Res. 16, suppl., 117–124.
   Google Scholar
• Levitus, S. 1982. Climatological atlas of the world ocean. NOAA Professional Paper 13, US Dept. of Com-merce, 173 pp.
   Google Scholar
• Liss, P. and Merlivat, L. 1986. Air-sea gas exchange rates, introduction and synthesis. In: The role of air-sea exchange in geochemical cycling (ed. P. Buat-Menard). Dordrecht. D. Reidel, pp. 113–128.
   Google Scholar
• Maier-Reimer, E. and Hasselmann, K. 1987. Transport and storage of CO, in the ocean, an inorganic ocean-circulation carbon cycle model. Clim. Dyn. 2, 63–90.
   Web of Science ®Google Scholar
• Manabe, S. and Stouffer, R. 1988. Two stable equilibria of a coupled ocean-atmosphere model. J. Climate 1, 841–866.
   Web of Science ®Google Scholar
• Marland, G. 1989. Fossil fuels CO, emissions. CDIAC Communications, Winter 1989, pp. 1–3. Carbon Dioxide Information Analysis Center, Oak Ridge National Laboratory, Oak Ridge, Tenn.
   Google Scholar
• Mehrbach, C., Culberson, C. H., Hawley, J. E. and Pytkowicz, R. M. 1973. Measurement of apparent dis-sociation constants of carbonic acid in seawater at atmospheric pressure. Limnol. Oceanogr. 18, 897–907.
   Web of Science ®Google Scholar
• Murphy, J. 1994. Transient response of the Hadley Centre coupled ocean-atmosphere model to increasing carbon dioxide. Part I. Control climate and flux correction. Journal of Climate, in press.
   Google Scholar
• Nowlin, W. D. Jr. and Klinck, J. M. 1986. The physics of the Antarctic Circumpolar Current. Rev. Geophys. 24, 469–491.
   Web of Science ®Google Scholar
• Pacanowski, R. C. and Philander, S. G. H. 1981. Parameterization of vertical mixing in numerical models of tropical oceans. J. Phys. Oceanogr. 11, 1443–1451.
   Web of Science ®Google Scholar
• Pearman, G. I., Hyson, P. and Fraser, P. J. 1983. The global distribution of atmospheric carbon dioxide. J. Geophys. Res. 88, 3581–3590.
   Web of Science ®Google Scholar
• Peng, T.-H., Takahashi, T. and Broecker, W. 1987. Seasonal variability of carbon dioxide, nutrients and oxygen in the northern North Atlantic surface water: observations and a model. Tellus 39B, 439–458.
   Google Scholar
• Redi, M. H. 1982. Oceanic isopycnal mixing by coor-dinate rotation. J. Phys. Oceanogr. 12, 1154–1158.
   Web of Science ®Google Scholar
• Roberts, D. L. and Cattle, H. 1989. Simulation of sea-ice in a coupled ocean-atmosphere model. Dynamical Climatology Technical Note no. 85. UK Meteorologi-cal Office, Bracknell.
   Google Scholar
• Sarmiento, J. L., On, J. C. and Siegenthaler, U. 1992. A perturbation simulation of CO2 uptake in an ocean general circulation model. J. Geophys. Res. 97, 3621–3645.
   Web of Science ®Google Scholar
• Semtner, A. J. 1976. A model for the thermodynamic growth of sea ice in numerical investigations of climate. J. Phys. Oceanogr. 6, 379–389.
   Web of Science ®Google Scholar
• Takahashi, T., Olafsson, J., Goddard, J. G., Chipman, D. W. and Sutherland, S. C. 1993. Seasonal variation of CO2 and nutrients in the high latitude oceans: a comparative study. Global Biogeochemical Cycles 7, 843–878.
   Web of Science ®Google Scholar
• Tans, P. P., Fung, I. Y. and Takahashi, T. 1990. Observa-tional constraints on the global atmospheric CO2 budget. Science 247, 1431–1438.
   PubMed Web of Science ®Google Scholar
• Taylor, N. K. 1992. The role of the ocean in the global carbon cycle. Part 2: Climate feedbacks. Weather 47, 237–241.
   Google Scholar
• Thomas, F., Perigaud, C., Merlivat, L. and Minster, J. F. 1988. World scale monthly mapping of the CO2 ocean-atmosphere gas transfer coefficient. Philos. Trans. R. Soc. London Ser. A325, 71–83.
   Web of Science ®Google Scholar
• Toggweiler, J. R., Dixon, K. and Bryan, K. 1989. Simula-tions of radiocarbon in a coarse-resolution, world ocean model. I. Steady state, pre-bomb distributions. J. Geophys. Res. 94, 8217–8242.
   Web of Science ®Google Scholar
• Wanninkhof, R. 1992. Relationship between wind speed and gas exchange over the ocean. J. Geophys. Res. 97, 7373–7382.
   Web of Science ®Google Scholar
• Yin, F. L. and Fung, I. Y. 1991. Net diffusivity in ocean general circulation models with nonuniform grids. J. Geophys. Res. 96, 10773–10776.
   Web of Science ®Google Scholar