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References and Notes

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Clark P. U., Pisias N. G., Stocker T. F., Weaver A. J., Nature415, 863 (2002).
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This behavior is sometimes called “antiphasing” between north and south. The term “antiphasing” ignores, however, the fact that adjustment to thermal anomalies in the Southern Hemisphere evolves qualitatively differently from that in the north. Because of the large thermal heat capacity of the Southern Ocean, an abrupt cooling in the Northern Hemisphere due to a collapse ot the THC within less than a decade leads to a millennial warming trend in the south Atlantic.
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Rind D., et al., J. Geophys. Res.106, 27335 (2001).
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Vellinga M., Wood R. A., Clim. Change54, 251 (2002).
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Vimeux F., Masson V., Jouzel J., Stievenard M., Petit J.-R., Nature398, 410 (1999).
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Stenni B., et al., Science293, 2074 (2001).
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The deglacial OCR can also be detected in the deuterium excess records of other Antarctic ice cores (F. Vimeux, personal communication).
12
The identification of annual layers would be an independent constraint on the accumulation rate, but annual layer thickness is estimated to be less than 2 mm at 14,000 years B.P. Generally, at high concentrations, cosmogenic isotopes (10Be, 36Cl) carry a global signal. Used as a complementary method for synchronization, they circumvent the problem of age. 10Be and 36Cl concentrations were highest from 36,000 to 42,000 years B.P. It will be crucial to determine the north-south connections during this earlier time of abrupt climate changes.
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Raisbeck G. M., Yiou F., Jouzel J., Geochim. Cosmochim. Acta66, A623 (2002).
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Deep ice-core drillings at Siple Dome (81.6°S, 148.8°W) by the United States, at Dome F (77.3°S, 39.7°E) by Japan, and at Kohnen Station (75°S, 0.07°E) as part of the European EPICA project.
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Koutavas A., Lynch-Stieglitz J., Marchitto T. M., Sachs J. P., Science297, 226 (2002).
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This work is supported by the European Commission project POP. I thank G. Schmidt and M. Vellinga for providing data from their model runs; R. Pawlowicz for producing and sharing Matlab code for geophysical mapping; and T. Blunier, G. Delaygue, J. Jouzel, V. Masson, G. Raisbeck, J. Schwander, B. Stauffer, T. van Ommen, and F. Vimeux for valuable discussions.

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Science
Volume 297 | Issue 5588
13 September 2002

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Published in print: 13 September 2002

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Thomas F. Stocker [email protected]
The author is in the Climate and Environmental Physics Division, University of Bern, 3012 Bern, Switzerland. He is currently at Institut Pierre Simon Laplace/Laboratoire du Climat et de l'Environnement, 91198 Gif-sur-Yvette, France. E-mail: [email protected]

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