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The Record of Aerosol Deposited Species in Ice Cores, and Problems of Interpretation

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Chemical Exchange Between the Atmosphere and Polar Snow

Part of the book series: NATO ASI Series ((ASII,volume 43))

Abstract

Ice cores have now become established as one of the primary archives of paleoclimatic information, covering timescales from seasonal up to 100,000 years or more. In the polar ice sheets, where there is little or no melting, snow layers build up year by year. Included in them are samples of the atmosphere: trace gases in air bubbles, particles and adsorbed gases, and the water molecules themselves. By drilling into the ice at suitable places, we can collect cores that give profiles of chemical content and physical properties of the ice. These are then used to infer the state of the atmosphere in the past.

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Author information

Authors and Affiliations

  1. British Antarctic Survey, Natural Environment Research Council, High Cross, Madingley Road, Cambridge, CB3 0ET, UK

    Eric W. Wolff

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  1. Eric W. Wolff
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Editors and Affiliations

  1. British Antarctic Survey, High Cross, Madingley Road, CB3 OET, Cambridge, UK

    Eric W. Wolff

  2. Department of Hydrology and Water Resources, University of Arizona, 85721, Tucson, Arizona, USA

    Roger C. Bales

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© 1996 Springer-Verlag Berlin Heidelberg

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Wolff, E.W. (1996). The Record of Aerosol Deposited Species in Ice Cores, and Problems of Interpretation. In: Wolff, E.W., Bales, R.C. (eds) Chemical Exchange Between the Atmosphere and Polar Snow. NATO ASI Series, vol 43. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-61171-1_1

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  • DOI: https://doi.org/10.1007/978-3-642-61171-1_1

  • Publisher Name: Springer, Berlin, Heidelberg

  • Print ISBN: 978-3-642-64730-7

  • Online ISBN: 978-3-642-61171-1

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