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Use of Snow and Firn Analysis to Reconstruct Past Atmospheric Composition -Discussion

  • E. W. Wolff
Conference paper
Part of the NATO ASI Series book series (volume 28)

Abstract

Polar ice cores (and cores from certain high-altitude lower latitude sites) have proved to be a rich resource of information on past atmospheres and climate. The ideal environmental archive would faithfully record the composition of the atmosphere with no post-depositional changes. Of course, the picture is not this simple even for polar ice, but it is worth recalling a few of the many successes of ice coring.

Keywords

Triple Junction Isotope Dilution Mass Spectrometry Natural Environment Research Council British Antarctic Survey Antarctic Snow 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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References

  1. Mulvaney R, Wolff EW, Oates K (1988) Sulphuric acid at grain boundaries in Antarctic ice. Nature 331:247–249CrossRefGoogle Scholar
  2. Neubauer J, Heumann KG (1988) Determination of nitrate at the ng/g level in Antarctic snow samples with ion chromatography and isotope dilution mass spectrometry. Fres Z Anal Chem 331:170–173CrossRefGoogle Scholar
  3. Oeschger H, Langway CC Jr (eds) (1989) The environmental record in glaciers and ice sheets. Wiley-Interscience, ChichesterGoogle Scholar

Copyright information

© Springer-Verlag Berlin Heidelberg 1991

Authors and Affiliations

  • E. W. Wolff
    • 1
  1. 1.British Antarctic SurveyNatural Environment Research CouncilCambridgeUK

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