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References

  • Beck, J. W., J. Récy, F. Taylor, R. L. Edwards, and G. Cabioch, Abrupt changes in early Holocene tropical sea surface temperature derived from coral records, Nature, 385, 705707, 1997.
  • Billups, K., and D. P. Schrag, Surface ocean density gradients during the Last Glacial Maximum, Paleoceangr., 15, 110123, 2000.
  • Boyle, E. A., Quaternary deep-water paleoceanography, Science, 249, 863870, 1990.
  • Boyle, E. A., and L. D. Keigwin, North Atlantic thermohaline circulation during the past 20,000 years linked to high latitude surface temperature, Nature, 330, 3540, 1987.
  • Broecker, W. S., Glacial climate in the tropics, Science, 272, 19021904, 1996.
  • Broecker, W. S., Thermohaline circulation, the Achilles heel of our climate system: Will man-made CO2 upset the current balance? Science, 278, 15821588, 1997.
  • Broecker, W. S., D. M. Peteet, and D. Rind, Does the ocean-atmosphere system have more than one stable mode of operation? Nature, 315, 2126, 1985.
  • Broecker, W. S., T.-H. Peng, J. Jouzel, and G. Russel, The magnitude of global fresh-water transports of importance to ocean circulation, Clim. Dyn., 4, 7379, 1990.
  • Bryan, K., Climate and the ocean circulation: III. The ocean model, Mon. Weather Rev., 97, 806827, 1969.
  • Bryan, K., Poleward heat transport by the ocean: Observations and models, Annu. Rev. Earth Planet. Sci., 10, 1538, 1982.
  • Bryden, H., D. H. Roemmich, and J. A. Church, Ocean heat transport across 24°N in the Pacific, Deep Sea Res., Part A, 38, 297324, 1991.
  • Burckle, L. H., and R. Mortlock, Sea-ice extent in the Southern Ocean during the Last Glacial Maximum: Another approach to the problem, Ann. Glaciol., 27, 302304, 1998.
  • Bush, A. B. G., and S. G. H. Philander, The climate of Last Glacial Maximum: Results from a coupled atmosphere-ocean general circulation model, J. Geophys. Res., 104, 24,50924,525, 1999.
  • Cortijo, E., S. Lehman, L. Keigwin, M. Chapman, D. Paillard, and L. Labeyrie, Changes in meridional temperature and salinity gradients in the North Atlantic Ocean (30 degrees–72 degrees N) during the last interglacial period, Paleoceanography, 14, 2333, 1999.
  • Crosta, X., J. J. Pichon, and L. H. Burckle, Application of modern analog technique to marine Antarctic diatoms: Reconstruction of maximum sea-ice extent at the Last Glacial Maximum, Paleoceanography, 13, 284297, 1998a.
  • Crosta, X., J. J. Pichon, and L. H. Burckle, Reappraisal of Antarctic seasonal sea-ice at the Last Glacial Maximum, Geophys. Res. Lett., 25, 27032706, 1998b.
  • Crowley, T. J., and G. R. North, Paleoclimatology, 339 pp., Oxford Univ. Press, New York, 1991.
  • De Vernal, A., C. Hillaire-Marcel, J. L. Turon, and J. Mattgiessen, Reconstruction of sea-surface temperature, salinity, and sea-ice cover in the northern North Atlantic during the Last Glacial Maximum based on dinocyst assemblages, Can. J. Earth. Sci., 37, 725750, 2000.
  • Duplessy, J. C., and L. Labeyrie, Global ocean circulation during the last ice age: Enhanced Intermediate Water formation and reduced deep water circulation, Oceanography 988, edited by A. Ayala-Castañares, W. Wooster, and A. Yáñez-Arancibia, pp. 8186, UNAM Press, Mexico City, 1989.
  • Duplessy, J. C., N. J. Shackleton, R. G. Fairbanks, L. Labeyrie, D. Oppo, and N. Kallel, Deepwater source variations during the last climate cycle and their impact on the global deepwater circulation, Paleoceanography, 3, 343360, 1988.
  • Fairbanks, R. G., A 17,000-year glacio-eustatic sea-level record: Influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation, Nature, 342, 637642, 1989.
  • Farrera, I., et al., Tropical climates at the Last Glacial Maximum: A new synthesis of terrestrial paleoclimate data. part I. Vegetation, lake levels and geochemistry, Clim. Dyn., 15, 823856, 1999.
  • Fichefet, T., S. Hovine, and J. C. Duplessy, A model study of the Atlantic thermohaline circulation during the Last Glacial Maximum, Nature, 372, 252255, 1994.
  • Ganopolski, A., S. Rahmstorf, V. Petoukhov, and M. Claussen, Simulation of modern and glacial climates with a coupled global model of intermediate complexity, Nature, 391, 351356, 1998.
  • Gent, P. R., F. O. Bryan, G. Danabasoglu, S. C. Doney, W. R. Holland, W. G. Large, and J. C. McWilliams, The NCAR climate system model ocean component, J. Clim., 11, 12871306, 1998.
  • Ghil, M., Cryothermodynamics: The chaotic dynamics of paleoclimate, Physica D, 77, 130159, 1994.
  • Gildor, H., and E. Tziperman, Sea ice as the glacial cycles' climate switch: Role of seasonal and orbital forcing, Paleoceanography, 15, 605615, 2000.
  • Gildor, H., and E. Tziperman, A sea ice climate switch mechanism for the 100-kyr glacial cycles, J. Geophys. Res, 106, 91179133, 2001.
  • Gloersen, P., W. J. Campbell, D. J. Cavaliery, J. S. Comiso, C. L. Parkinson, and H. J. Zwally, Arctic and Antarctic Sea Ice, 1978–1987: Satellite Passive-Microwave Observations and Analysis, 290 pp., Sci. and Tech. Inf. Program, NASA, Washington, D.C., 1992.
  • Gordon, A. L., Interocean exchange of thermocline water, J. Geophys. Res., 91, 50315046, 1986.
  • Guilderson, T. P., R. G. Fairbanks, and J. L. Rubenstone, Tropical temperature variations since 20,000 years ago: Modulating interhemispheric climate change, Science, 263, 663665, 1994.
  • Hall, M. M., and H. Bryden, Direct estimates and mechanisms of ocean heat transport, Deep Sea Res., Part A, 29, 339359, 1982.
  • Haney, R. L., Surface thermal boundary conditions for ocean circulation models, J. Phys. Oceanogr., 1, 241248, 1971.
  • Hays, J. D., J. Imbrie, and N. J. Shackleton, Variations in the Earth's orbit: Pacemaker in the ice ages, Science, 194, 11211132, 1976.
  • Hibler, W. D.III, and K. Bryan, A diagnostic ice-ocean model, J. Phys. Oceanogr., 17, 9871015, 1987.
  • Hughes, T. M. C., and A. J. Weaver, Multiple equilibria of an asymmetric two-basin ocean model, J. Phys. Oceanogr., 24, 619637, 1994.
  • Jayne, S. R., and J. Marotzke, A destabilizing thermohaline circulation-atmosphere-sea-ice feedback, J. Clim., 12, 642651, 1999.
  • Keigwin, L. D., North Pacific deep water formation during the latest glaciation, Nature, 330, 362364, 1987.
  • Khodri, M., Y. Leclainche, G. Ramstein, P. Braconnot, O. Marti, and E. Cortijo, Simulating the amplification of orbital forcing by ocean feedbacks in the last glaciation, Nature, 410, 570574, 2001.
  • Kim, S.-J., G. M. Flato, G. J. Boer, and N. A. McFarlane, A coupled climate model simulation of the Last Glacial Maximum. part 1: Transient multi-decadal response, Clim. Dyn., 19, 515537, 2002.
  • Kim, S.-J., G. M. Flato, and G. J. Boer, A coupled climate model simulation of the Last Glacial Maximum, part 2: Approach to equilibrium, Clim. Dyn., 20, 635661, 2003.
  • Kitoh, A., S. Murakami, and H. Koide, A simulation of the Last Glacial Maximum with a coupled ocean-atmosphere GCM, Geophys. Res. Lett., 28, 22212224, 2001.
  • Kohfeld, K. E., and S. P. Harrison, How well can we simulate past climates? Evaluating the models using global palaeoenvironmental datasets, Q. Sci. Rev., 19, 321346, 2000.
  • Kravtsov, S. V., Sea ice and climate sensitivity, Ph.D. thesis, 259 pp., Fla. State Univ., Tallahassee, 1998.
  • Kravtsov, S. V., Sea ice and climate. part II: Model climate stability to perturbations of the hydrologic cycle, J. Clim., 13, 463487, 2000.
  • Krinner, G., and C. Genthon, GCM simulations of the Last Glacial Maximum surface climate of Greenland and Antarctica, Clim. Dyn., 14, 741758, 1998.
  • Lenderink, G., and R. J. Haarsma, Modeling convective transitions in the presence of sea ice, J. Phys. Oceanogr., 26, 14481467, 1996.
  • Leppäranta, M., A review of analytical models of sea-ice growth, Atmos. Ocean, 31, 123138, 1993.
  • Levitus, S., Climatological atlas of the world ocean, NOAA Prof. Pap. 13, 173 pp., U.S. Govt. Print. Off., Washington, D.C., 1982.
  • Lohmann, G., and R. Gerdes, Sea ice effects on the sensitivity of the thermohaline circulation, J. Clim., 11, 27892803, 1998.
  • Lohmann, G., R. Gerdes, and D. Chen, Sensitivity of the thermohaline circulation in coupled oceanic GCM-atmospheric EBM experiments, Clim. Dyn., 12, 403416, 1996.
  • Lynch-Stieglitz, J., W. B. Curry, and N. Slowey, Weaker Gulf Stream in the Florida straits during the Last Glacial Maximum, Nature, 402, 644648, 1999.
  • Macdonald, A., and C. Wunsch, An estimate of global ocean circulation and heat fluxes, Nature, 382, 436439, 1996.
  • Manabe, S., and R. J. Stouffer, Multiple-century response of a coupled ocean-atmosphere model to an increase of atmospheric carbon dioxide, J. Clim., 7, 523, 1994.
  • Manabe, S., R. J. Stouffer, and M. Spelman, Response of a coupled ocean-atmosphere model to increasing atmospheric dioxide, Ambio, 23, 4449, 1994.
  • Marotzke, J., Instabilities and multiple equilibria of the thermohaline circulation, Ph.D. thesis, 126 pp., Inst. für Meereskunde an der Univ. Kiel, Kiel, Germany, 1990.
  • Marotzke, J., Ocean models in climate problems, in Ocean Processes in Climate Dynamics: Global and Mediterranean Examples, edited by P. Malanotte-Rizzoli, and A. R. Robinson, pp. 79109, Kluwer Acad., Norwell, Mass., 1994.
  • Marotzke, J., and P. H. Stone, Atmospheric transports, the thermohaline circulation, and flux adjustments in a simple coupled model, J. Phys. Oceanogr., 25, 13501364, 1995.
  • Marotzke, J., and J. Willebrand, Multiple equilibria of the global thermohaline circulation, J. Phys. Oceanogr., 21, 13721385, 1991.
  • Marotzke, J., P. Welander, and J. Willebrand, Instability and multiple steady states in a meridional-plane model of the thermohaline circulation, Tellus, Ser. A, 40, 162172, 1988.
  • Maykut, G. A., The surface heat and mass balance, in Geophysics of Sea Ice, edited by N. Untersteiner, pp. 395464, Plenum, New York, 1986.
  • Mikolajewicz, U., and E. Maier-Reimer, Mixed boundary conditions in ocean general circulation models and their influence on the stability of the model's conveyor belt, J. Geophys. Res., 99, 22,63322,644, 1994.
  • Milankovitch, M., Canon of insolation and the ice age problem (in Yugoslavian), K. Serb. Acad. Beogr. Spec. Publ. 132, 482 pp., Isr. Program for Sci. Transl., Jerusalem, 1969.
  • Moore, A. M., and J. C. Reason, The response of a global ocean general circulation model to climatological surface boundary conditions for temperature and salinity, J. Phys. Oceanogr., 23, 300328, 1993.
  • Moore, J. K., M. R. Abbot, J. G. Richman, and D. M. Nelson, The Southern Ocean at the Last Glacial Maximum: A strong sink for atmospheric carbon dioxide, Global Biogeochem. Cycles, 14, 455475, 2000.
  • Mysak, L. A., T. F. Stocker, and F. Huang, Century-scale variability in a randomly forced, two-dimensional thermohaline ocean circulation model, Clim. Dyn., 8, 103116, 1993.
  • Nakamura, M., P. H. Stone, and J. Marotzke, Destabilization of the thermohaline circulation by atmospheric eddy transport, J. Clim., 7, 18701882, 1994.
  • North, G. R., Theory of energy-balance climate models, J. Atmos. Sci., 32, 233243, 1975.
  • North, G. R., R. F. Cahalan, and R. F. Coakley Jr., Energy balance climate models, Rev. Geophys., 19, 91121, 1981.
  • Paillard, D., The timing of Pleistocene glaciations from a simple multiple-state climate model, Nature, 391, 378381, 1998.
  • Peixoto, J. P., and A. H. Oort, Physics of Climate, Am. Inst. of Phys., New York, 1992.
  • Pinot, S., G. Ramstein, S. P. Harrison, I.C. Prentice, J. Guiot, M. Stute, and S. Joussaume, Tropical paleoclimates at the Last Glacial Maximum: Comparison of Paleoclimate Modeling Intercomparison Project (PMIP) simulations and paleodata, Clim. Dyn., 15, 857874, 1999.
  • Rahmstorf, S., Multiple convection patterns and thermohaline flow in an idealized OGCM, J. Clim., 8, 30283039, 1995a.
  • Rahmstorf, S., Climate drift in an ocean model coupled to a simple, perfectly matched atmosphere, Clim. Dyn., 11, 447458, 1995b.
  • Rahmstorf, S., and J. Willebrand, The role of temperature feedback in stabilizing the thermohaline circulation, J. Phys. Oceanogr., 25, 787805, 1995.
  • Rosel-Mele, A., and P. Comes, Evidence for a warm Last Glacial Maximum in the Nordic seas or an example in U-37(K)′ and U-37(K) to estimate low sea surface temperature? Paleoceanography, 14, 770776, 1999.
  • Saravanan, R., and J. C. McWilliams, Multiple equilibria, natural variability, and climate transitions in an idealized ocean-atmosphere model, J. Clim., 8, 22962323, 1995.
  • Schiller, A., U. Mikolajewicz, and R. Voss, The stability of the thermohaline circulation in a coupled ocean-atmosphere general circulation model, Clim. Dyn., 13, 325347, 1997.
  • Schlesinger, M. E., Model projections of the climatic changes induced by increased atmospheric CO2, in Climate and Geo-Sciences, pp. 375415, D. Reidel, Norwell, Mass., 1989.
  • Semtner, A. J.Jr., A model for the thermodynamic growth of sea ice in numerical investigations of climate, J. Phys. Oceanogr., 6, 379389, 1976.
  • Shrag, D., G. Hampt, and D. W. Murray, The temperature and oxygen isotopic composition of the glacial ocean: Evidence from deep sea pore fluids, Science, 272, 19301932, 1996.
  • Stocker, T. F., and D. G. Wright, Rapid transitions of the ocean's deep circulation induced by changes in surface water fluxes, Nature, 351, 729732, 1991.
  • Stocker, T. F., D. G. Wright, and L. A. Mysak, A zonally averaged, coupled ocean-atmosphere model for paleoclimatic studies, J. Clim., 5, 773797, 1992.
  • Stommel, H. M., Thermohaline convection with two stable regimes of flow, Tellus, 13, 224230, 1961.
  • Tang, B., and A. J. Weaver, Climate stability as deduced from an idealized coupled atmosphere-ocean model, Clim. Dyn., 11, 141150, 1995.
  • Trenberth, K. E., Mean annual poleward energy transports by the oceans in the southern hemisphere, Dyn. Atmos. Oceans, 4, 5764, 1979.
  • Trenberth, K. E., and A. Solomon, The global heat balance: Heat transports in the atmosphere and ocean, Clim. Dyn., 10, 107134, 1994.
  • Vonder Haar, T. H., and A. H. Oort, New estimate of annual poleward energy transport by Northern Hemisphere oceans, J. Phys. Oceanogr., 3, 169172, 1973.
  • Wang, W.-C., and P. H. Stone, Effect of ice-albedo feedback on global sensitivity in a one-dimensional radiative-convective climate model, J. Atmos. Sci., 37, 545552, 1980.
  • Wang, X., P. H. Stone, and J. Marotzke, Poleward heat transport in a barotropic ocean model, J. Phys. Oceanogr., 25, 256265, 1995.
  • Weaver, A. J., and T. M. C. Hughes, Rapid interglacial climate fluctuations driven by North Atlantic ocean circulation, Nature, 367, 447450, 1994.
  • Willmott, A. J., and L. A. Mysak, A simple steady-state coupled ice-ocean model, with application to the Greenland-Norwegian Sea, J. Phys. Oceanogr., 19, 501518, 1989.
  • Winton, M., The effect of cold climate upon North Atlantic deep water formation in a simple ocean-atmosphere model, J. Clim., 10, 3751, 1997.
  • Yang, J., and J. D. Neelin, Sea-ice interaction with the thermohaline circulation, Geophys. Res. Lett., 20, 217220, 1993.
  • Yang, J., and J. D. Neelin, Decadal variability in coupled sea-ice-thermohaline circulation systems, J. Clim., 10, 30593076, 1997.
  • Yung, Y. L., T. Lee, C. H. Wang, and Y. T. Shieh, Dust: A diagnosis of the hydrologic cycle during the Last Glacial Maximum, Science, 271, 962963, 1996.