Articles | Volume 20, issue 2
https://doi.org/10.5194/tc-20-1025-2026
https://doi.org/10.5194/tc-20-1025-2026
Research article
 | Highlight paper
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11 Feb 2026
Research article | Highlight paper |  | 11 Feb 2026

Water vapour isotope anomalies during an atmospheric river event at Dome C, East Antarctica

Niels Dutrievoz, Cécile Agosta, Cécile Davrinche, Amaëlle Landais, Sebastien Nguyen, Étienne Vignon, Inès Ollivier, Christophe Leroy-Dos Santos, Elise Fourré, Mathieu Casado, Jonathan Wille, Vincent Favier, Bénédicte Minster, and Frédéric Prié

Data sets

LMDZiso output - Water vapour isotope anomalies during an atmospheric river event at Dome C, East Antarctica Niels Dutrievoz et al. https://doi.org/10.5281/zenodo.15481580

YOPP-SH Radiosonde measurements from Concordia Station, Antarctica, 2018-12 Paolo Grigioni et al. https://doi.org/10.1594/PANGAEA.899638

Dati meteorologici della Stazione meteorologica CONCORDIA presso la Base CONCORDIA STATION (DomeC) Paolo Grigioni et al. https://doi.org/10.12910/DATASET2022-002

Polar specific atmospheric river detection algorithm catalogs Jonathan Wille https://doi.org/10.5281/zenodo.15830634

Model code and software

Scripts - Water vapour isotope anomalies during an atmospheric river event at Dome C, East Antarctica Niels Dutrievoz and Cécile Agosta https://doi.org/10.5281/zenodo.15481977

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Editorial statement
Ice cores comprise one of the most comprehensive records of Earth's past climate, extending back hundreds of thousands of years. However, disentangling the information contained in the ice cores's isotopic signal in order to retrieve information on specific atmospheric events remains challenging. In this study, the authors show how atmospheric rivers - an extreme event that changes temperatures and humidity - are imprinted in the water isotopes. The study represents a major step forward in closing the knowledge gap, by discerning the local versus large-scale drivers of the isotopic signal.
Short summary
In December 2018, an atmospheric river event from the Atlantic reached Dome C, East Antarctica, causing a +18 °C warming, tripled water vapour, and a strong isotopic anomaly in water vapour (+ 17 ‰ for δ18O) at the surface. During the peak of the event, we found 70 % of the water vapour came from local snow sublimation, and 30 % from the atmospheric river itself, highlighting both long-range moisture advection and interactions between the boundary layer and the snowpack.
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