Articles | Volume 18, issue 9
https://doi.org/10.5194/tc-18-3911-2024
https://doi.org/10.5194/tc-18-3911-2024
Research article
 | 
03 Sep 2024
Research article |  | 03 Sep 2024

A decade (2008–2017) of water stable isotope composition of precipitation at Concordia Station, East Antarctica

Giuliano Dreossi, Mauro Masiol, Barbara Stenni, Daniele Zannoni, Claudio Scarchilli, Virginia Ciardini, Mathieu Casado, Amaëlle Landais, Martin Werner, Alexandre Cauquoin, Giampietro Casasanta, Massimo Del Guasta, Vittoria Posocco, and Carlo Barbante

Data sets

A decade (2008-2017) of water stable-isotope composition of precipitation at Concordia Station, East Antarctica Giuliano Dreossi et al. https://doi.org/10.5281/zenodo.10197160

Daily, monthly and annual data from A decade (2008-2017) of water stable-isotope composition of precipitation at Concordia Station, East Antarctica Giuliano Dreossi et al. https://doi.org/10.5281/zenodo.11613330

ati meteorologici della Stazione meteorologica CONCORDIA presso la 45 Base CONCORDIA STATION (DomeC) P. Grigioni et al. https://doi.org/10.12910/DATASET2022-002

Dati meteorologici della Stazione di Radiosondaggio presso la 50 Base CONCORDIA STATION (DomeC) P. Grigioni et al. https://doi.org/10.12910/DATASET2022-004

ECHAM6-wiso and ECHAM5-wiso isotope daily data at Dome Concordia station, East Antarctica A. Cauquoin and M. Werner https://doi.org/10.5281/zenodo.11468043

Daily, monthly and annual data from A decade (2008-2017) of water stable-isotope composition of precipitation at Concordia Station, East Antarctica G. Dreossi et al. https://doi.org/10.5281/zenodo.11613330

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Short summary
Oxygen and hydrogen stable isotopes have been extensively used to reconstruct past temperatures, with precipitation representing the input signal of the isotopic records in ice cores. We present a 10-year record of stable isotopes in daily precipitation at Concordia Station: this is the longest record for inland Antarctica and represents a benchmark for quantifying post-depositional processes and improving the paleoclimate interpretation of ice cores.