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An Oceanic Cold Reversal During the Last Deglaciation

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Science  14 Sep 2001:
Vol. 293, Issue 5537, pp. 2074-2077
DOI: 10.1126/science.1059702

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Abstract

A detailed deuterium excess profile measured along the Dome C EPICA (European Project for Ice Coring in Antarctica) core reveals the timing and strength of the sea surface temperature changes at the source regions for Dome C precipitation. We infer that an Oceanic Cold Reversal took place in the southern Indian Ocean, 800 years after the Antarctic Cold Reversal. The temperature gradient between the oceanic moisture source and Antarctica is similar to the Dome C sodium profile during the deglaciation, illustrating the strong link between this gradient and the strength of the atmospheric circulation.

  • * To whom correspondence should be addressed. E-mail: stenni{at}univ.trieste.it

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