Northern Hemisphere forcing of Southern Hemisphere climate during the last deglaciation

Nature

Volumn 494, Issue 7435, 2013, Pages 81-85

  He, Feng ^a   Shakun, Jeremy D ^b   Clark, Peter U ^c   Carlson, Anders E ^a,c   Liu, Zhengyu ^a   Otto Bliesner, Bette L ^d   Kutzbach, John E ^a  

^a UNIVERSITY OF WISCONSIN MADISON   (United States)

^b HARVARD UNIVERSITY   (United States)

^c OREGON STATE UNIVERSITY   (United States)

^d NATIONAL CENTER FOR ATMOSPHERIC RESEARCH   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

ALBEDO; ATMOSPHERIC FORCING; CARBON DIOXIDE; CONCENTRATION (COMPOSITION); GLACIAL ENVIRONMENT; ICE SHEET; LAST DEGLACIATION; MASS BALANCE; NORTHERN HEMISPHERE; PALEOCLIMATE; PROXY CLIMATE RECORD; SEA ICE; SOUTHERN HEMISPHERE; TEMPERATURE EFFECT;

ARTICLE; ATMOSPHERE; CLIMATE; DEGLACIATION; LATITUDE; NORTHERN HEMISPHERE; PRIORITY JOURNAL; SEA ICE; SEA SURFACE TEMPERATURE; SIGNAL PROCESSING; SOUTHERN HEMISPHERE; SPRING; SUMMER;

EID: 84877723722     PISSN: 00280836     EISSN: 14764687     Source Type: Journal    
DOI: 10.1038/nature11822     Document Type: Article

References (30)

1. Milankovic, M. Canon of Insolation and the Ice-age Problem [Kanon der Erdbestrahlung und seine Anwendung auf das Eiszeitenproblem] Belgrade. 1941. (Israel Program for Scientific Translations, 1969).
2. Hays, J. D., Imbrie, J. & Shackleton, N. J. Variations in Earth's orbit-pacemaker of ice ages. Science 194, 1121-1132 (1976).
3. Imbrie, J. et al. On the structure and origin of major glaciation cycles. 1 Linear responses to Milankovitch forcing. Paleoceanography 7, 701-738 (1992).
4. Stott, L., Timmermann, A. & Thunell, R. Southern hemisphere and deep-sea warming led deglacial atmospheric CO2 rise and tropical warming. Science 318, 435-438 (2007).
5. Huybers, P. & Denton, G. Antarctic temperature at orbital timescales controlled by local summer duration. Nature Geosci. 1, 787-792 (2008).
6. Timmermann, A., Timm, O., Stott, L. & Menviel, L. The roles of CO2 and orbital forcing in driving Southern Hemispheric temperature variations during the last 21000yr. J. Clim. 22, 1626-1640 (2009).
7. Huybers, P. Antarctica's orbital beat. Science 325, 1085-1086 (2009).
8. Shakun, J. D. & Carlson, A. E. A global perspective on Last Glacial Maximum to Holocene climate change. Quat. Sci. Rev. 29, 1801-1816 (2010).
9. Shakun, J. D. et al. Global warming preceded by increasing carbon dioxide concentrations during the last deglaciation. Nature 484, 49-54 (2012).
10. Clark, P. U. et al. The Last Glacial Maximum. Science 325, 710-714 (2009).
11. Ruddiman, W. F. Ice-driven CO2 feedback on ice volume. Clim. Past Discuss. 2, 43-55 (2006).
12. Liu, Z. et al. Transient simulation of last deglaciation with a new mechanism for Bolling-Allerod warming. Science 325, 310-314 (2009).
13. Berger, A. L. Long-term variations of daily insolation and Quaternary climatic changes. J. Atmos. Sci. 35, 2362-2367 (1978).
14. Joos, F. & Spahni, R.Rates ofchange in naturaland anthropogenic radiative forcing over the past 20, 000 years. Proc. Natl Acad. Sci. USA 105, 1425-1430 (2008).
15. Peltier, W. R. Global glacial isostasy and the surface of the ice-age earth: the ICE-5G (VM2) model and GRACE. Annu. Rev. Earth Planet. Sci. 32, 111-149 (2004).
16. Timm, O., Timmermann, A., Abe-Ouchi, A., Saito, F. & Segawa, T.Onthe definition of seasons in paleoclimate simulations with orbital forcing. Paleoceanography 23, PA2221 (2008).
17. Chen, G. S., Kutzbach, J. E., Gallimore, R. & Liu, Z. Y. Calendar effect on phase study in paleoclimate transient simulation with orbital forcing. Clim. Dyn. 37, 1949-1960 (2011).
18. Huybers, P. & Wunsch, C. Obliquity pacing of the late Pleistocene glacial terminations. Nature 434, 491-494 (2005).
19. Fischer, H. et al. The role ofSouthern Ocean processes in orbital and millennialCO2 variations-a synthesis. Quat. Sci. Rev. 29, 193-205 (2010).
20. Pedro, J. B., Rasmussen, S. O. & van Ommen, T. D. Tightened constraints on the time-lag between Antarctic temperature and CO2 during the last deglaciation. Clim. Past 8, 1213-1221 (2012).
21. Cheng, H. et al. Ice age terminations. Science 326, 248-252 (2009).
22. Denton, G. H. et al. The last glacial termination. Science 328, 1652-1656 (2010).
23. Crowley, T. J. North Atlantic deep water cools the Southern Hemisphere. Paleoceanography 7, 489-497 (1992).
24. Caillon, N. et al. Timing of atmospheric CO2 and Antarctic temperature changes across termination. III. Science 299, 1728-1731 (2003).
25. Hansen, J. et al. Climate change and trace gases. Phil. Trans. R. Soc. A 365, 1925-1954 (2007).
26. McManus, J. F., Oppo, D. W. & Cullen, J. L. A 0.5-million-year record of millennial-scale climate variability in the North Atlantic. Science 283, 971-975 (1999).
27. Martrat, B. et al. Four climate cycles of recurring deep and surface water destabilizations on the Iberian margin. Science 317, 502-507 (2007).
28. Carlson, A. E. & Clark, P. U. Ice-sheet sources of sea level rise and freshwater discharge during the last deglaciation. Rev. Geophys. 50, RG4007 http://dx.doi.org/10.1029/2011RG000371 (2012).
29. McManus, J. F., Francois, R., Gherardi, J. M., Keigwin, L. D. & Brown-Leger, S. Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes. Nature 428, 834-837 (2004).
30. Cuffey, K. M. & Clow, G. D. Temperature, accumulation, and ice sheet elevation in central Greenland through the last deglacial transition. J. Geophys. Res. 102 (C12) 26383-26396 (1997).