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Cited by 262

The DOI matches its Crossref record; 24 of the 24 references it cites were found in a registry or an index.

An Oceanic Cold Reversal During the Last Deglaciation

Stenni, Barbara, Masson-Delmotte, Valerie, Johnsen, Sigfus, Jouzel, Jean, Longinelli, Antonio, Monnin, Eric, Röthlisberger, Regine, Selmo, Enrico·2001·Science

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.

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Crossref · 10.1126/science.1059702

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Metadata

Authors
Stenni, B., Masson-Delmotte, V., Johnsen, S., Jouzel, J., Longinelli, A., Monnin, E., Röthlisberger, R., & Selmo, E.
Venue
Science
Published
2001-09-14
Volume
293
Issue
5537
Pages
2074-2077
ISSN
  • 0036-8075 (ISSN-L)
  • 1095-9203
OpenAlex
W2056050376
Cited by
262
References
24
FWCI
10.35
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: An Oceanic Cold Reversal During the Last Deglaciation. https://app.cochat.ai/papers/10.1126/science.1059702
The paper
Stenni, B., Masson-Delmotte, V., Johnsen, S., Jouzel, J., Longinelli, A., Monnin, E., Röthlisberger, R., & Selmo, E. (2001). An Oceanic Cold Reversal During the Last Deglaciation. Science. https://doi.org/10.1126/science.1059702

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