Mechanisms for millennial-scale global synchronization during the last glacial period

Paleoceanography

Volumn 20, Issue 4, 2005, Pages

  Timmermann, Axel ^a   Krebs, U ^b   Justino, F ^c   Goosse, H ^d   Ivanochko, T ^e  

^a JAPAN AGENCY FOR MARINE EARTH SCIENCE AND TECHNOLOGY   (Japan)

^b GEOMAR HELMHOLTZ CENTRE FOR OCEAN RESEARCH KIEL   (Germany)

^c UNIVERSITY OF TORONTO   (Canada)

^d UNIVERSITÉ CATHOLIQUE DE LOUVAIN   (Belgium)

^e UNIVERSITY OF BRITISH COLUMBIA   (Canada)

Author keywords

[No Author keywords available]

Indexed keywords

LAST GLACIAL; PALEOCLIMATE;

EID: 26844480048     PISSN: 08838305     EISSN: None     Source Type: Journal    
DOI: 10.1029/2004PA001090     Document Type: Article

References (56)

1. Annamalei, H., P. Liu, and S.-P. Xie (2005), Southwest Indian Ocean SST variability: Its local effect and remote influence on Asian monsoons, J. Clim., in press.
2. Bard, E. (2001), Comparison of alkenones estimates with other paleotemperature proxies, Geochem. Geophys, Geosyst., 2, 1-12.
3. Blunier, T., and E. Brook (2001), Timing of millennial-scale climate change in Antarctica and Greenland during the last glacial period, Science, 291, 109-112.
4. Campin, J. M., and H. Goosse (1999), A parameterization of dense overflow in large-scale ocean models in z coordinate, Tellus, Ser. A, 51, 412-430.
5. Cane, M., and A. C. Clement (1999), A role for the tropical Pacific coupled ocean-atmosphere system on Milankovitch and millentrial timescales. part II, Global impacts, in Mechanisms of Global Climate Change at Millennial Time Scales, Geophys. Monogr. Ser., vol. 112, edited by P. U. Clark, R. S. Webb, and L. D. Keigwin, pp. 59-61, AGU, Washington, D. C.
6. Cessi, P., K. Bryan, and R. Zhang (2004), Global seiching of thermocline waters between the Atlantic and the Indian-Pacific Ocean basins, Geophys. Res. Lett., 31, L04302, doi:10.1029/2003GL019091.
7. Climate: Long-Range Investigation, Mapping, and Prediction (CLIMAP) (1981), Seasonal reconstruction of the Earth's surface of the Last Glacial Maximum, Geol. Soc. Am. Map. Chart Ser., MC-36.
8. Crowley, T. J., and S. K. Baum (1997), Effect of vegetation on an ice-age climate model simulation, J. Geophys. Res., 102, 16,463-16,480.
9. Dansgaard, W., et al. (1993), Evidence for general instability of past climate from a 250-kyr ice-core record, Nature, 364, 218-220.
10. Dong, B. W., and R. T. Sutton (2002), Adjustment of the coupled ocean-atmosphere system to a sudden change in the thermohaline circulation, Geophys. Res. Lett., 29(15), 1728, doi:10.1029/2002GL015229.
11. Gent, P. R., and J. C. McWilliams (1990), Isopycnal mixing in ocean general circulation model, J. Phys. Oceanogr., 20, 150-155.
12. Gill, A. E. (1980), Some simple solutions for heat-induced tropical circulation, Q. J. R. Meteorol. Soc., 106, 447-462.
13. Goosse, H., and T. Fichefet (1999), Importance of ice-ocean interactions for the global ocean circulation: A model study, J. Geophys. Res., 104, 23,337-23,355.
14. Goosse, H., E. Deleersnijder, T. Fichefet, and M. H. England (1999), Sensitivity of a global coupled ocean-sea ice model to the parameterization of vertical mixing, J. Geophys. Res., 104, 13,681-13,695.
15. Grootes, P. M., M. Stuiver, J. W. C. White, S. J. Johnsen, and J. Jouzel (1993), Comparison of oxygen isotope records from the GISP2 and GRIP Greenland ice cores, Nature, 366, 552-554.
16. Heinrich, H. (1988), Origin and consequences of cyclic ice rafting in the northeast Atlantic Ocean during the past 130,000 years, Quat. Res., 29, 143-152.
17. Held, I. M., and M. J. Suarez (1978), A two-level primitive equation atmospheric model designed for climate sensitivity experiments, J. Atmos. Sci., 35, 206-229.
18. Honjo, S., J. Dymond, W. Prell, and V. Ittekot (1999), Monsoon-controlled export fluxes to the interior of the Arabian Sea, Deep Sea Res., Part II, 46, 1859-1902.
19. Hostetler, S. W., and A. C. Mix (1999), Reassessment of ice-age cooling of the tropical ocean and atmosphere, Nature, 399, 673-676.
20. Hsieh, W. W., and K. Bryan (1996), Redistribution of sea level rise associated with enhanced greenhouse warming: A simple model study, Clim. Dyn., 12, 535-544.
21. Hsieh, W. M., M. K. Davey, and R. C. Wajsowicz (1983), The free Kelvin wave in finite-difference numerical models, J. Phys. Oceanogr., 3, 1381-1397.
22. Huang, R. X., M. A. Cane, N. Naik, and P. Goodman (2000), Global adjustment of the thermocline in response to deepwater formation, Geophys. Res. Lett., 27, 759-762.
23. Ivanochko, T. S., R. S. Ganeshram, G. J. A. Brummer, G. Ganssen, S. J. A. Jung, S. G. Moreton, and D. Kroon (2005), Variations in tropical convection as an amplifier of global climate change at the millennial scale, Earth. Planet. Sci. Lett., 253, 302-314.
24. Johnson, H., and D. P. Marshall (2002), A theory for the surface Atlantic response to thermohaline variability, J. Phys. Oceanogr., 32, 1121-1132.
25. Kawase, M. (1987), Establishment of deep ocean circulation driven by deep-water production, J. Phys. Oceanogr., 17, 2294-2317.
26. Keigwin, L. D., and S. J. Lehman (1994), Deep circulation change linked to Heinrich event 1 and Younger Dryas in a middepth North Atlantic core, Paleoceanography, 9, 185-194.
27. Kiefer, T., M. Samthein, H. Erlenkeuser, P. M. Grootes, and A. P. Roberts (2001), North Pacific response to millennial-scale changes in ocean circulation over the last 60 kyr, Paleoceanography, 16, 179-189.
28. Kitoh, A., S, Muakami, and H. Koide (2001), A simulation of the Last Glacial Maximum with a coupled atmosphere-ocean GCM, Geophys. Res. Lett, 28, 2221-2224.
29. Knutti, R., J. Flückiger, T. Stocker, and A. Timmermann (2004), Strong hemispheric coupling of glacial climate through freshwater discharge and ocean circulation, Nature, 430, 851-856.
30. Koutavas, A., J. Lynch-Stieglitz Jr., T. M. Marchitto, and J. P. Sachs (2002), El Niño-like pattern in ice age tropical Pacific sea surface temperature, Science, 297, 226-230.
31. Lang, C., M. Leuenberger, J. Schwander, and S. Johnsen (1999), 16°C rapid temperature variation in central Greenland 70,000 years ago, Science, 286, 934-937.
32. Lea, D. W., D. K. Pak, and H. J. Spero (2000), Climate impact of late Quaternary equatorial Pacific sea surface temperature variations, Science, 289, 1719-1724.
33. Livezey, R. E., M. Masutani, A. Leetmaa, H. Rui, M. Ji, and A. Kumar (1997), Teleconnective response of the Pacific-North American region atmosphere to large central equatorial Pacific SST anomalies, J. Clim., 10, 1787-1820.
34. Lyle, M., F. Prahl, and M. Sparrow (1992), Upwelling and productivity changes inferred from a temperature record in the equatorial Pacific, Nature, 355, 812-815.
35. Marshall, J., and F. Molteni (1993), Toward a dynamic understanding of planetary-scale flow regimes, J. Atmos. Sci., 50, 1792-1818.
36. Mellor, G. L., and T. Yamada (1982), Development of a turbulence closure model for geophysical fluid problems, Rev. Geophys., 20, 851-875.
37. Opsteegh, J. D., R. J. Haarsma, F. M. Selten, and A. Kattenberg (1998), ECBILT, A dynamic alternative to mixed boundary conditions in ocean models, Tellus, Ser. A, 50, 348-367.
38. Peltier, W. R. (1994), Ice age paleotopography, Science, 265, 195-201.
39. Peterson, L. C., G. H. Haug, K. A. Hughen, and U. Rohl (2000), Rapid changes in the hydrologic cycle of the tropical Atlantic during the last glacial, Science, 290, 1947-1951.
40. Rahmstorf, S. (2003), Timimg of abrupt climate change: A precise clock, Geophys. Res. Lett., 30(10), 1510, doi:10.1029/2003GL017115.
41. Roche, D., D. Paillard, and E. Cortijo (2004), Constraints on the duration and freshwater release of Heinrich event 4 through isotope modeling, Nature, 432, 379-382, doi:10.1038/nature03059.
42. Rosenthal, Y., D. W. Oppo, and B. K. Linsley (2003), The amplitude and phasing of climate change during the last deglaciation in the Sulu Sea, western equatorial Pacific, Geophys. Res. Lett., 30(8), 1428, doi:10.1029/2002GL016612.
43. Saenko, O. A., A. Schmittner, and A. J. Weaver (2004), The Atlantic-Pacific seesaw, J. Clim., 17, 2033-2038.
44. Sarnthein, M., U. Pflaumann, and M. Weinelt (2003), Past extent of sea ice in the northern North Atlantic inferred from foraminiferal paleotemperature estimates, Paleoceanography, 18(2), 1047, doi:10.1029/ 2002PA000771.
45. Schultz, H., H. Erlenkeuser, and U. von Rad (1998), Correlation between Arabian Sea and Greenland climate oscillations of the past 110,000 years, Nature, 393, 54-57.
46. Severinghaus, J. P., and E. J. Brook (1999), Abrupt climate change at the end of the last glacial period inferred from trapped air in polar ice, Science, 286, 930-934.
47. Shackleton, N. J., M. A. Hall, and E. Vincent (2000), Phase relationships between millennial-scale events 64,000 to 24,000 years ago, Paleoceanography, 15, 565-569.
48. Sidall, M., E. J. Rohling, A. Almogi-Labin, C. Hemleben, D. Meischners, I. Schmelzer, and D. A. Smeed (2003), Sea-level fluctuations during the last glacial cycle, Nature, 423, 853-858.
49. Stocker, T. F., and S. J. Johnsen (2003), A minimum thermodynamic model for the bipolar seesaw, Paleoceanography, 18(4), 1087, doi:10.1029/ 2003PA000920.
50. Stommel, H. M. (1961), Thermohaline convection with two stable regimes of flow, Tellus, 13, 224-230.
51. Stott, L., C. Poulsen, S. Lund, and R. Thuell (2002), Super ENSO and global climate oscillations at millennial time scales, Science, 297, 222-226.
52. Timmermann, A., M. Schulz, H. Gildor, and E. Tziperman (2003), Coherent resonant millennial-scale climate oscillations triggered by massive meltwater pulses, J. Clim., 16, 2569-2585.
53. Timmermann, A., F. Justino, F.-F. Jin, U. Krebs, and H. Goosse (2004), Surface temperature control in the north and tropical Pacific during the last glacial maximum, Clim. Dyn., 23, 353-370.
54. Turney, C. S., A. P. Kershaw, S. C. Clemens, N. Branch, P. T. Moss, and K. Fifield (2004), Synchronous millennial-scale climatic oscillations of the tropical Pacific and north Atlantic Oceans, Nature, 428, 306-309.
55. Watanabe, M., and F.-F. Jin (2003), A moist linear baroclinic model: Coupled dynamical-convective response to El Niño, J. Clim., 16, 1121-1139.
56. Yokoyama, Y., T. M. Esat, and K. Lambeck (2001), Coupled climate and sea-level changes deduced from Huan Peninsula coral terraces of the last ice age, Earth Planet. Sci. Lett., 193, 579-587.