Articles | Volume 15, issue 24
https://doi.org/10.5194/acp-15-13895-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-15-13895-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
16 Dec 2015
Research article |
| 16 Dec 2015
Post-bubble close-off fractionation of gases in polar firn and ice cores: effects of accumulation rate on permeation through overloading pressure
Climate and Environmental Physics, University of Bern, Bern, Switzerland
Oeschger Center for Climate Change Research, University of Bern, Bern, Switzerland
National Institute of Polar Research, Tokyo, Japan
T. Ikeda-Fukazawa
Department of Applied Chemistry, Meiji University, Kanagawa, Japan
M. Suwa
The World Bank, Washington D.C., USA
J. Schwander
Climate and Environmental Physics, University of Bern, Bern, Switzerland
Oeschger Center for Climate Change Research, University of Bern, Bern, Switzerland
T. Kameda
Department of Civil and Environmental Engineering, Kitami Institute of Technology, Kitami, Japan
J. Lundin
Department of Earth & Space Sciences, University of Washington, Seattle, USA
A. Hori
Department of Civil and Environmental Engineering, Kitami Institute of Technology, Kitami, Japan
H. Motoyama
National Institute of Polar Research, Tokyo, Japan
M. Döring
Climate and Environmental Physics, University of Bern, Bern, Switzerland
Oeschger Center for Climate Change Research, University of Bern, Bern, Switzerland
M. Leuenberger
Climate and Environmental Physics, University of Bern, Bern, Switzerland
Oeschger Center for Climate Change Research, University of Bern, Bern, Switzerland
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Cited
12 citations as recorded by crossref.
- Phase relationships between orbital forcing and the composition of air trapped in Antarctic ice cores L. Bazin et al. 10.5194/cp-12-729-2016
- Exceptionally high biosphere productivity at the beginning of Marine Isotopic Stage 11 M. Brandon et al. 10.1038/s41467-020-15739-2
- A Pleistocene ice core record of atmospheric O 2 concentrations D. Stolper et al. 10.1126/science.aaf5445
- Early Pleistocene East Antarctic temperature in phase with local insolation Y. Yan et al. 10.1038/s41561-022-01095-x
- A 2000-year temperature reconstruction on the East Antarctic plateau from argon–nitrogen and water stable isotopes in the Aurora Basin North ice core A. Servettaz et al. 10.5194/cp-19-1125-2023
- On the relationship between δO2∕N2 variability and ice sheet surface conditions in Antarctica R. Harris Stuart et al. 10.5194/tc-18-3741-2024
- Water sources and composition of dissolved gases and bubbles in a saline high Arctic spring D. Andersen et al. 10.1371/journal.pone.0282877
- Pure rotational Raman spectroscopy applied to N2/O2 analysis of air bubbles in polar firn H. Ohno et al. 10.1017/jog.2021.40
- Fractionation of O2∕N2 and Ar∕N2 in the Antarctic ice sheet during bubble formation and bubble–clathrate hydrate transition from precise gas measurements of the Dome Fuji ice core I. Oyabu et al. 10.5194/tc-15-5529-2021
- Volcanic influence on centennial to millennial Holocene Greenland temperature change T. Kobashi et al. 10.1038/s41598-017-01451-7
- New technique for high-precision, simultaneous measurements of CH4, N2O and CO2 concentrations; isotopic and elemental ratios of N2, O2 and Ar; and total air content in ice cores by wet extraction I. Oyabu et al. 10.5194/amt-13-6703-2020
- Ice core evidence for atmospheric oxygen decline since the Mid-Pleistocene transition Y. Yan et al. 10.1126/sciadv.abj9341
12 citations as recorded by crossref.
- Phase relationships between orbital forcing and the composition of air trapped in Antarctic ice cores L. Bazin et al. 10.5194/cp-12-729-2016
- Exceptionally high biosphere productivity at the beginning of Marine Isotopic Stage 11 M. Brandon et al. 10.1038/s41467-020-15739-2
- A Pleistocene ice core record of atmospheric O 2 concentrations D. Stolper et al. 10.1126/science.aaf5445
- Early Pleistocene East Antarctic temperature in phase with local insolation Y. Yan et al. 10.1038/s41561-022-01095-x
- A 2000-year temperature reconstruction on the East Antarctic plateau from argon–nitrogen and water stable isotopes in the Aurora Basin North ice core A. Servettaz et al. 10.5194/cp-19-1125-2023
- On the relationship between δO2∕N2 variability and ice sheet surface conditions in Antarctica R. Harris Stuart et al. 10.5194/tc-18-3741-2024
- Water sources and composition of dissolved gases and bubbles in a saline high Arctic spring D. Andersen et al. 10.1371/journal.pone.0282877
- Pure rotational Raman spectroscopy applied to N2/O2 analysis of air bubbles in polar firn H. Ohno et al. 10.1017/jog.2021.40
- Fractionation of O2∕N2 and Ar∕N2 in the Antarctic ice sheet during bubble formation and bubble–clathrate hydrate transition from precise gas measurements of the Dome Fuji ice core I. Oyabu et al. 10.5194/tc-15-5529-2021
- Volcanic influence on centennial to millennial Holocene Greenland temperature change T. Kobashi et al. 10.1038/s41598-017-01451-7
- New technique for high-precision, simultaneous measurements of CH4, N2O and CO2 concentrations; isotopic and elemental ratios of N2, O2 and Ar; and total air content in ice cores by wet extraction I. Oyabu et al. 10.5194/amt-13-6703-2020
- Ice core evidence for atmospheric oxygen decline since the Mid-Pleistocene transition Y. Yan et al. 10.1126/sciadv.abj9341
Saved (final revised paper)
Latest update: 30 Jun 2025
Short summary
We find that argon/nitrogen ratios of trapped air in the GISP2 ice core on “gas ages” are significantly negatively correlated with accumulation rate changes over the past 6000 years. Lines of evidence indicate that changes in overloading pressure at bubble closeoff depths induced the gas fractionation in closed bubbles. Further understanding of the fractionation processes may lead to a new proxy for the past temperature and accumulation rate.
We find that argon/nitrogen ratios of trapped air in the GISP2 ice core on “gas ages” are...
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