Stability of the thermohaline circulation in a simple coupled model

References

• Birchfield, G. E. 1989. A coupled ocean-atmosphere climate model: temperature versus salinity effects on the thermohaline circulation. Climate Dynamics 4, 57–71.
   Web of Science ®Google Scholar
• Bolton, D. 1980. The computation of equivalent potential temperature. Month. Weath. Rev. 108, 1046–1053.
   Web of Science ®Google Scholar
• Branscome, L. E. 1983. A parameterization of transient eddy heat flux on a beta plane. J. Atm. Sci. 40, 2508–2521.
   Web of Science ®Google Scholar
• Bretherton, F. P. 1982. Ocean climate modeling. Prog. Oceanogr. 11, 93–129.
   Web of Science ®Google Scholar
• Broecker, W. S. and Peng, T.-H. 1989. The oceanic salt pump. Does it contribute to the glacial-interglacial difference in atmospheric CO2 content? Global Biochem. Cycles 3, 215–239.
   Google Scholar
• Bryan, F. 1986. High latitude salinity effects and inter-hemispheric thermohaline circulations. Nature 323, 301–304.
   Web of Science ®Google Scholar
• Chen, D., Gerdes, R. and Lohmann, G. 1995. A 1-D atmospheric energy balance model developed for ocean modelling. Theor. App!. Climatol. 51, 25–38.
   Web of Science ®Google Scholar
• Dickson, R. R. and Brown, J. 1994. The production of North Atlantic Deep Water: Sources, rates and path-ways. J. Geophys. Res. 99 (C6), 12319–12341.
   Web of Science ®Google Scholar
• Dickson, R. R., Meincke, J., Malmberg, S. A. and Lee, A. J. 1988. The “Great Salinity Anomaly” in the northern Atlantic 1968-1972. Prog. Oceanogr. 20, 103–151.
   Web of Science ®Google Scholar
• Green, J. S. A. 1970. Transport properties of large-scale eddies and the general circulation of the atmosphere. Q. J. Roy. Meteor. Soc. 96, 157–185.
   Web of Science ®Google Scholar
• Haney, R. L. 1971. Surface thermal boundary conditions for ocean circulation models. J. Phys. Oceanogr. 1, 241–248.
   Google Scholar
• Keigwin, L. D., Jones, G. A., Lehmann, S. J. and Boyle, E. A. 1991. Deglacial meltwater discharge, North Atlantic deep circulation, and abrupt climate change. J. Geophys. Res. 96, 16811–16826.
   Web of Science ®Google Scholar
• Lohmann, G., Gerdes, R. and Chen, D. 1995. Sensitivity of the thermohaline circulation in coupled oceanic GCM-atmospheric EBM experiments. Climate Dynamics, in press.
   Google Scholar
• Maas, L. R. M. 1994. A simple model for the three-dimensional thermally and wind-driven ocean circulation. Tellus 46A, 671–680.
   Google Scholar
• Manabe, S. and Stouffer, R. J. 1993. Century-scale effects of increased atmospheric CO2 on the ocean-atmosphere system. Nature 364, 215–218.
   Web of Science ®Google Scholar
• Marotzke, J. 1990.Instabilities and multiple equilibria of the thermohaline circulation. PhD Thesis, Kiel University, 126 pp.
   Google Scholar
• Marotzke, J., Welander, P. and Willebrand, J. 1988. Instability and multiple steady states in a meridional-plane model of the thermohaline circulation. Tellus 40A, 162–172.
   Google Scholar
• Mikolajewicz, U. and Maier-Reimer, E. 1994. Mixed boundary conditions in ocean general circulation models and their influence on the stability of the model’s conveyer belt. J. Geophys. Res. 99 (C11), 22633–22644.
   Web of Science ®Google Scholar
• Nakamura, M., Stone, P. H. and Marotzke, J. 1994. Destabilization of the thermohaline circulation by atmospheric eddy transports. J. Climate 7,1870–1882.
   Web of Science ®Google Scholar
• Oberhuber, J. M. 1988. An atlas based on the GOADS data set. The budgets of heat, buoyancy and turbulence kinetic energy at the surface of the global ocean. Max-Planck-Institute for Meteorology, Report No. 15.
   Google Scholar
• Oort, A. H. and Peixoto, J. P. 1983. Global angular momentum and energy balance requirements from observations. Adv. Geophys. 25, 355–490.
   Web of Science ®Google Scholar
• Power, S. B. and Kleeman, R. 1994. Surface heat flux parameterizations and the response of OGCMs to high latitude freshening. Tellus 46A, 86–95.
   Google Scholar
• Rahmstorf, S. 1994. Rapid climate transitions in a coupled ocean-atmosphere model. Nature 372, 82–85.
   Web of Science ®Google Scholar
• Rahmstorf, S. and Willebrand, J. 1995. The role of the temperature feedback in stabilizing the thermohaline circulation. J. Phys. Oceanogr. 25, 787–805.
   Web of Science ®Google Scholar
• Sarnthein, M., Winn, K., Jung, S. J. A., Duplessy, J.-C., Labeyrie, L., Erlenkeuser, H. and Ganssen, G. 1994. Changes in east Atlantic deep water circulation over the last 30,000 years: Eight time slice reconstructions. Palaeoceanogr. 9, 209–267.
   Google Scholar
• Schopf, P. S. 1983. On equatorial waves and El Nino. II: Effects of air-sea thermal coupling. J. Phys. Oceanogr. 21, 1725–1739.
   Google Scholar
• Stocker, T. F., Wright, D. G. and Mysak, L. A. 1992. A zonally averaged, coupled ocean-atmosphere model for paleoclimate studies. J. Climate 5, 773–797.
   Web of Science ®Google Scholar
• Stommel, H. M. 1961. Thermohaline convection with two stable regimes of flow. Tellus 13, 224–230.
   Google Scholar
• Stommel, H. M. 1993. A conjectural regulating mechanism for determining the thermohaline structure of the oceanic mixed layer. J. Phys. Oceanogr. 23, 142–148.
   Web of Science ®Google Scholar
• Stone, P. H. and Miller, D. A. 1980. Empirical relations between seasonal changes in meridional fluxes of heat. J. Atm. Sci. 37, 1708–1721.
   Web of Science ®Google Scholar
• Stone, P. H. and Yao, M. S. 1990. Development of a two-dimensional zonally averaged statistical-dynam-ical model. Part III. The parameterization of the eddy fluxes of heat and moisture. J. Climate 3, 726–740.
   Web of Science ®Google Scholar
• Tang, B. and Weaver, A. J. 1995. Climate stability as deduced from an idealized coupled atmosphere-ocean model. Climate Dynamics 11, 141–150.
   Web of Science ®Google Scholar
• Trefethen, L. N., Trefethen, A. E., Reddy, S. C. and Driscoll, T. A. 1993. Hydrodynamic stability without eigenvalues. Science 261, 578–584.
   PubMed Web of Science ®Google Scholar
• Weaver, A. J. and Sarachick, E. S. 1991. The role of mixed boundary conditions in numerical models of the ocean’s climate. J. Phys. Oceanogr. 21, 1470–1473.
   Web of Science ®Google Scholar
• Weaver, A. J., Sarachick, E. S. and Marotzke, J. 1991. Freshwater flux forcing of decadal and interdecadal oceanic variability. Nature 353, 836–838.
   Web of Science ®Google Scholar
• Vallis, G. K. 1982. A statistical-dynamical climate model with a simple hydrological cycle. Tellus 34, 211–227.
   Web of Science ®Google Scholar
• Zaucker, F. and Broecker, W. S. 1992. The influence of atmospheric moisture transport on fresh water balance of the Atlantic drainage basin: General circulation model simulations and observations. J. Geophys. Res. 97, 2765–2773.
   Web of Science ®Google Scholar
• Zhang, S., Greatbatch, R. J. and Lin, C. A. 1993. A reexamination of the polar halocline catastrophe and implications for coupled ocean-atmosphere modeling. J. Phys. Oceanogr. 23, 287–299.
   Web of Science ®Google Scholar