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The Cryosphere An interactive open-access journal of the European Geosciences Union
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Volume 11, issue 5
The Cryosphere, 11, 2345–2361, 2017
https://doi.org/10.5194/tc-11-2345-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
The Cryosphere, 11, 2345–2361, 2017
https://doi.org/10.5194/tc-11-2345-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

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 et al.
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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Elisabeth Schlosser on behalf of the Authors (10 May 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (23 May 2017) by Joel Savarino
RR by Anonymous Referee #1 (23 May 2017)
ED: Reconsider after major revisions (23 May 2017) by Joel Savarino
AR by Elisabeth Schlosser on behalf of the Authors (30 Aug 2017)  Author's response    Manuscript
ED: Publish as is (08 Sep 2017) by Joel Savarino
AR by Elisabeth Schlosser on behalf of the Authors (12 Sep 2017)  Author's response    Manuscript
Publications Copernicus
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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.
To derive paleotemperatures from ice cores we must know all processes involved in ice formation....
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