Ranges of moisture-source temperature estimated from Antarctic ice cores stable isotope records over glacial-interglacial cycles

A single isotope ratio (delta D or delta O-18) of water is widely used as an air-temperature proxy in Antarctic ice core records. These isotope ratios, however, do not solely depend on air-temperature but also on the extent of distillation of heavy isotopes out of atmospheric water vapor from an oce...

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Bibliographic Details
Published in:Climate of the Past
Main Authors: Uemura, R., Masson-delmotte, V., Jouzel, J., Landais, A., Motoyama, H., Stenni, B.
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Gesellschaft Mbh 2012
Subjects:
Online Access:https://archimer.ifremer.fr/doc/00139/25062/23172.pdf
https://archimer.ifremer.fr/doc/00139/25062/65520.pdf
https://doi.org/10.5194/cp-8-1109-2012
https://archimer.ifremer.fr/doc/00139/25062/