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

A single isotope ratio (δD or δ 18 O) 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 oceanic mois...

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Bibliographic Details
Published in:Climate of the Past
Main Authors: R. Uemura, V. Masson-Delmotte, J. Jouzel, A. Landais, H. Motoyama, B. Stenni
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2012
Subjects:
Online Access:https://doi.org/10.5194/cp-8-1109-2012
https://doaj.org/article/be30f0cb6bfe46eeb9db2b98348a5735