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

A single isotope ratio (δD or δ18O) of water is widely used as an air-temperature proxy in Antarctic ice cores. 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 moisture sour...

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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, Barbara
Other Authors: Uemura, R., Masson Delmotte, V., Jouzel, J., Landais, A., Motoyama, H., Stenni, Barbara
Format: Article in Journal/Newspaper
Language:English
Published: 2012
Subjects:
Online Access:http://hdl.handle.net/10278/42759
https://doi.org/10.5194/cp-8-1109-2012