Articles | Volume 11, issue 5
https://doi.org/10.5194/tc-11-2345-2017
https://doi.org/10.5194/tc-11-2345-2017
Research article
 | 
20 Oct 2017
Research article |  | 20 Oct 2017

The influence of the synoptic regime on stable water isotopes in precipitation at Dome C, East Antarctica

Elisabeth Schlosser, Anna Dittmann, Barbara Stenni, Jordan G. Powers, Kevin W. Manning, Valérie Masson-Delmotte, Mauro Valt, Anselmo Cagnati, Paolo Grigioni, and Claudio Scarchilli

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Latest update: 22 Jul 2024
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Short summary
To derive paleotemperatures from ice cores we must know all processes involved in ice formation. At the Antarctic base Dome C, a unique precipitation data set plus stable water isotope data enabled us to study atmospheric processes influencing isotope ratios of precipitation in detail. Meteorological data from both automatic weather station and an atmospheric model were used to investigate how different atmospheric flow patterns determine the precipitation parameters used in paleoclimatology.