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Intercomparison of firn core and meteorological data

Published online by Cambridge University Press:  27 April 2004

Alison J. McMorrow
Affiliation:
Institute of Antarctic and Southern Ocean Studies, GPO Box 252-77, Hobart, TAS 7001, Australia
Mark A.J. Curran
Affiliation:
Antarctic CRC and Australian Antarctic Division, GPO Box 252-80, Hobart, TAS 7001, Australia
Tas D. Van Ommen
Affiliation:
Antarctic CRC and Australian Antarctic Division, GPO Box 252-80, Hobart, TAS 7001, Australia
Vin Morgan
Affiliation:
Antarctic CRC and Australian Antarctic Division, GPO Box 252-80, Hobart, TAS 7001, Australia
Michael J. Pook
Affiliation:
Antarctic CRC, GPO Box 252-80, Hobart, TAS 7001, Australia
Ian Allison
Affiliation:
Antarctic CRC and Australian Antarctic Division, GPO Box 252-80, Hobart, TAS 7001, Australia

Abstract

High resolution firn core records of the oxygen isotope ratio (δ18O) and trace chemical species were extracted from a high accumulation site on Law Dome, East Antarctica. Inter-core comparisons were conducted and regional events identified in cores 5 km apart. High resolution dating of one of the firn cores was established using a co-located Automatic Weather Station (AWS) equipped with a snow accumulation sensor, allowing dating of individual precipitation events in the firn core record. Variations in the δ18O and trace chemical records were compared with meteorological conditions at the mesoscale and the synoptic-scale. Particular focus was given to an abrupt change in sea salt concentrations and δ18O within a depth range that appears from AWS accumulation data to have been deposited over a 24 hour period. The abrupt change in the firn core record was found to be consistent with an abrupt change in meteorological conditions. Direct comparisons between high resolution firn core records and meteorological conditions will greatly facilitate the interpretation of signals preserved in deep ice cores.

Type
Papers—Earth Sciences and Glaciology
Copyright
© Antarctic Science Ltd 2001

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