Sea ice switch mechanism and glacial-interglacial CO2 variations

Global Biogeochemical Cycles

Volumn 16, Issue 3, 2002, Pages

  Gildor, Hezi ^a   Tziperman, Eli ^a   Toggweiler, J R ^b  

^a WEIZMANN INSTITUTE OF SCIENCE   (Israel)

^b NOAA EARTH SYSTEM RESEARCH LABORATORY   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

AIR-SEA INTERACTION; CARBON CYCLE; GLACIAL-INTERGLACIAL CYCLE; PALEOCEANOGRAPHY; SEA ICE; VERTICAL MIXING;

SOUTHERN OCEAN;

EID: 0036770724     PISSN: 08866236     EISSN: None     Source Type: Journal    
DOI: 10.1029/2001gb001446     Document Type: Article

References (54)

1. 2 sensitivity to the biological pump in the ocean. Global Biogeochem. Cycles, 14, 1219-1230, 2000a.
2. 2 cycles?, Rev. Geophys., 38, 159-189, 2000b.
3. 2 in the Southern Ocean, Science, 283, 365-367, 1999.
4. 2, Global Biogeochem. Cycles, 10, 319-333, 1996.
5. Bacastow, R., and E. Maier-Reimer, Ocean circulation model of the carbon cycle, Clim. Dyn., 4, 95-125, 1990.
6. 2 exchange, Geophys. Res. Lett., 28, 3281-3284, 2001.
7. Boyle, E. A., and L. Keigwin, North Atlantic thermohaline circulation during the past 20,000 years linked to high-latitude surface temperature, Nature, 330, 35-40, 1987.
8. Broecker, W., J. Lynch-Stieglitz, D. Archer, M. Hofmann, E. Maier-Reimer, O. Marchal, T. Stocker, and N. Gruber, How strong is the Harvadton-Bear constraint?. Global Biogeochem. Cycles, 13, 817-820, 1999.
9. Crosta, X., J. Pichon, and L. Burckle, Application of modern analog technique to marine Antarctic diatoms: Reconstruction of maximum sea ice extent at the Last Glacial Maximum, Paleoceanography, 13, 284-297, 1998.
10. Dansgaard, W., J. White, and S. Johnsen, The abrupt termination of the Younger Dryas climate event, Nature, 339, 532-534, 1989.
11. Daskal Hausman, E., and M. B. McElroy, Role of sea surface temperature and ocean circulation changes in the reorganization of the global carbon cycle at the last glacial termination. Global Biogeochem. Cycles, 13, 371-381, 1999.
12. de Vernal, A., Sea-surface conditions in the northwest North Atlantic during the Last Glacial Maximum. GEOTOP contrib. 97-001, Cent. for Res. in Isotopic Geochem. and Geochronol., Univ. of Quebec, Montreal, Que., Canada, 1997. (Available at http://www.unites.uqam.ca/geotop/ 18ka.html)
13. de Vernal, A., and C. Hillaire-Marcel, Sea-ice cover, sea-surface salinity and halo/thermo-cline structure of the northwest North Atlantic: Modern versus full glacial condition, Quater. Res., 19, 65-85, 2000.
14. de Vernal, A., and T. F. Pedersen, Micropaleontology and palynology of core par87a-10: A 23,000 year record of paleoenvironmental changes in the Gulf of Alaska, northeast North Pacific, Paleoceanography, 12, 821-830, 1997.
15. 2 concentrations during the last glacial period, Nature, 389, 929-935, 1997.
16. Ganopolski, S., A. Rahmstorf, V. Petoukhov, and M. Claussen, Simulation of modern and glacial climates with a coupled global model of intermediate complexity, Nature, 391, 351-356, 1998.
17. Gargent, A., Vertical eddy diffusivity in the ocean interior, J. Mar. Res., 42, 359-393, 1984.
18. Gersonde, R., and U. Zielinski, The reconstruction of late quaternary Antarctic sea-ice distribution: The use of diatoms as a proxy for sea-ice, Paleogeogr. Paleoclimatol. Paleoecol., 162, 263-286, 2000.
19. Ghil, M., Cryothermodynamics: The chaotic dynamics of paleoclimate, Physica D, 77, 130-159, 1994.
20. Ghil, M., A. Mulhaupt, and P. Pestiaux, Deep water formations and Quaternary glaciations. Clim. Dyn., 2, 1-10, 1987.
21. Gildor, H., and E. Tziperman, Sea ice as the glacial cycles climate switch: Role of seasonal and Milankovitch solar forcing, Paleoceanography, 15, 605-615, 2000.
22. Gildor, H., and E. Tziperman, A sea ice climate switch mechanism for the 100-kyr glacial cycles, J. Geophys. Res., 106, 9117-9133, 2001a.
23. 2 variations, Geophys. Res. Lett., 28, 2421-2424, 2001b.
24. Gnanadesikan, A., A simple predictive model for the structure of the oceanic pycnocline, Science, 283, 2077-2079, 1999.
25. Gordon, A., Seasonality of Southern Ocean sea ice, J. Geophys. Res., 86, 4193-4197, 1981.
26. Gordon, A., and B. Huber, Southern Ocean winter mixed layer, J. Geophys. Res., 95, 11,655-11,672, 1990.
27. 2 reduction by the world ocean: Experiments with the Hamburg carbon model, Paleoceanography, 4, 395-430, 1991.
28. Källén, E., C. Crafoord, and M. Ghil, Free oscillations in a climate model with ice-sheet dynamics, J. Atmos. Sci., 36, 2292-2303, 1979.
29. 2, Geophys. Res. Lett., 27, 783-786, 2000.
30. Maier-Reimer, E., Geochemical cycles in an ocean general circulation model: Preindustrial tracer distribution, Global Biogeochem. Cycles, 7, 645-677, 1993.
31. Martinson, D., Evolution of the Southern Ocean winter mixed layer and sea ice: Open ocean deepwater formation and ventilation, J. Geophys. Res., 95, 11,641-11,654, 1990.
32. Matsumoto, K., and J. Lynch-Stieglitz, Similar glacial and holocene deep water circulation inferred from southeast Pacific benthic foraminiferal carbon isotope composition, Paleoceanography, 14, 149-163, 1999.
33. Maykut, G., and D. Perovich, The role of shortwave radiation in summer decay of a sea ice cover, J. Geophys. Res., 92, 7032-7044, 1987.
34. Orr, J., et al., Estimates of anthropogenic carbon uptake from four three- dimensional global ocean models. Global Biogeochem. Cycles, 15, 43-60, 2001.
35. 2 content during the late Quaternary, Quat. Sci. Rev., 19, 273-283, 2000.
36. Petit, J. R., et al., Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica. Nature, 399, 429-436, 1999.
37. Ramanathan, V., et al., Climate-chemical interaction and effects of changing atmospheric trace gases, Rev. Geophys., 25, 1441-1482, 1987.
38. 2, Nature, 308, 621-624, 1984.
39. Schrag, D., G. Hampt, and D. Murray, Pore fluid constraints on the temperature and oxygen isotopic composition of the glacial ocean, Science, 272, 1930-1932, 1996.
40. Siegenthaler, U., and J. Sarmiento, Atmospheric carbon dioxide and the ocean, Nature, 365, 119-125, 1993.
41. Sigman, D. M., and E. A. Boyle, Glacial/interglacial variations in atmospheric carbon dioxide, Nature, 407, 859-869, 2000.
42. Sikes, E. L., C. R. Samson, T. P. Guilderson, and W. R. Howard, Old radiocarbon ages in the southwest Pacific Ocean during the last glacial period and deglaciation, Nature, 405, 555-559, 2000.
43. 2 variations. Nature, 404, 171-174, 2000.
44. Stommel, H., Thermohaline convection with two stable regimes of flow, Tellus, 13, 224-230, 1961.
45. Suess, E., Particulate organic carbon flux in the oceans: Surface and oxygen utilization, Nature, 288, 260-262, 1980.
46. 2 by ventilation of the ocean's deepest water, Paleoceanography, 14, 572-588, 1999.
47. Toggweiler, J. R., and B. Samuels, Is the magnitude of the deep outflow from the Atlantic Ocean actually governed by the Southern Hemisphere winds?, in The Global Carbon Cycle, NATO ASI Ser. 1, vol. 15, edited by M. Heimann, pp. 303-331, Springer-Verlag, New York, 1993.
48. U.N. Educational, Scientific, and Cultural Organization, Tenth report of the Joint Panel on Oceanographic Tables and Standards, Tech. Rep., 36, Paris, 1981.
49. 2: Natural Variations Archean to Present, Geophys. Monogr. Ser., vol. 32, edited by E. T. Sundquist and W. S. Broecker, pp. 99-110, AGU, Washington, D. C., 1985.
50. Weaver, A. J., M. Eby, A. Fanning, and E. C. Wiebe, Simulated influence of carbon dioxide, orbital forcing and ice sheets on the climate of the Last Glacial Maximum, Nature, 394, 847-853, 1998.
51. Weertman, J., Milankovitch solar radiation variations and ice age ice sheet sizes, Nature, 261, 17-20, 1976.
52. 2: Natural Variations Archean to Present, Geophys. Monogr. Ser., vol. 32, edited by E. T. Sundquist and W. S. Broecker, pp. 185-194, AGU, Washington, D. C., 1985.
53. Yamanaka, Y., Development of ocean biogeochemical general circulation model. Tech. Rep. 1, Cent. for Clim. Sys. Res., Univ. of Tokyo, Tokyo, 1996.
54. Yu, E.-F., R. Francois, and M. P. Bacon, Similar rates of modern and last- glacial ocean thermohaline circulation inferred from radio-chemical data, Nature, 379, 689-694, 1996.