Articles | Volume 10, issue 4
https://doi.org/10.5194/tc-10-1647-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tc-10-1647-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Isotopic exchange on the diurnal scale between near-surface snow and lower atmospheric water vapor at Kohnen station, East Antarctica
François Ritter
CORRESPONDING AUTHOR
Alfred-Wegener-Institut (AWI) Helmholtz Zentrum für Polar und Meeresforschung, Bremerhaven, Germany
Laboratoire des Sciences du Climat et de l'Environnement (LSCE), IPSL/CEA-CNRS-UVSQ, Saclay, Gif-sur-Yvette, France
Hans Christian Steen-Larsen
Laboratoire des Sciences du Climat et de l'Environnement (LSCE), IPSL/CEA-CNRS-UVSQ, Saclay, Gif-sur-Yvette, France
Centre for Ice and Climate, Niels Bohr Institute, University of Copenhagen, Copenhagen, Denmark
Martin Werner
Alfred-Wegener-Institut (AWI) Helmholtz Zentrum für Polar und Meeresforschung, Bremerhaven, Germany
Valérie Masson-Delmotte
Laboratoire des Sciences du Climat et de l'Environnement (LSCE), IPSL/CEA-CNRS-UVSQ, Saclay, Gif-sur-Yvette, France
Anais Orsi
Laboratoire des Sciences du Climat et de l'Environnement (LSCE), IPSL/CEA-CNRS-UVSQ, Saclay, Gif-sur-Yvette, France
Melanie Behrens
Alfred-Wegener-Institut (AWI) Helmholtz Zentrum für Polar und Meeresforschung, Bremerhaven, Germany
Gerit Birnbaum
Alfred-Wegener-Institut (AWI) Helmholtz Zentrum für Polar und Meeresforschung, Bremerhaven, Germany
Johannes Freitag
Alfred-Wegener-Institut (AWI) Helmholtz Zentrum für Polar und Meeresforschung, Bremerhaven, Germany
Camille Risi
Laboratoire de Météorologie Dynamique (LMD), IPSL/CNRS-UPMC, Paris, France
Sepp Kipfstuhl
Alfred-Wegener-Institut (AWI) Helmholtz Zentrum für Polar und Meeresforschung, Bremerhaven, Germany
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- Baffin Bay sea ice extent and synoptic moisture transport drive water vapor isotope (<i>δ</i><sup>18</sup>O, <i>δ</i><sup>2</sup>H, and deuterium excess) variability in coastal northwest Greenland P. Akers et al. 10.5194/acp-20-13929-2020
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- Climatic information archived in ice cores: impact of intermittency and diffusion on the recorded isotopic signal in Antarctica M. Casado et al. 10.5194/cp-16-1581-2020
- Importance of the advection scheme for the simulation of water isotopes over Antarctica by atmospheric general circulation models: A case study for present-day and Last Glacial Maximum with LMDZ-iso A. Cauquoin et al. 10.1016/j.epsl.2019.115731
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- A versatile water vapor generation module for vapor isotope calibration and liquid isotope measurements H. Steen-Larsen & D. Zannoni 10.5194/amt-17-4391-2024
- Temporal variations of stable isotopic compositions in atmospheric water vapor on the Southeastern Tibetan Plateau and their controlling factors M. Chen et al. 10.1016/j.atmosres.2024.107328
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- The role of sublimation as a driver of climate signals in the water isotope content of surface snow: laboratory and field experimental results A. Hughes et al. 10.5194/tc-15-4949-2021
- Spatial and temporal stable water isotope data from the upper snowpack at the EastGRIP camp site, NE Greenland, sampled in summer 2018 A. Zuhr et al. 10.5194/essd-16-1861-2024
4 citations as recorded by crossref.
- Water Isotopic Signature of Surface Snow Metamorphism in Antarctica M. Casado et al. 10.1029/2021GL093382
- High stability in near-infrared spectroscopy: part 2, optomechanical analysis of an optical contacted V-shaped cavity N. Jobert et al. 10.1007/s00340-022-07779-x
- Acquisition of isotopic composition for surface snow in East Antarctica and the links to climatic parameters A. Touzeau et al. 10.5194/tc-10-837-2016
- Climate dependent contrast in surface mass balance in East Antarctica over the past 216 ka F. PARRENIN et al. 10.1017/jog.2016.85
Saved (preprint)
Latest update: 14 Dec 2024
Short summary
We present successful continuous measurements of water vapor isotopes performed in Antarctica in January 2013. The interest is to understand the impact of the water vapor isotopic composition on the near-surface snow isotopes. Our study reveals a diurnal cycle in the snow isotopic composition in phase with the vapor. This finding suggests fractionation during the sublimation of the ice, which has an important consequence on the interpretation of water isotope variations in ice cores.
We present successful continuous measurements of water vapor isotopes performed in Antarctica in...