Anomalous accumulation rates in the Vostok ice-core resulting from ice flow over Lake Vostok
The accumulation rate of snow is crucial to the development of accurate age-depth models for ice-cores. The dating of the Vostok ice-core assumes that accumulation rates generally vary linearly between the core site and the ice divide 250 km to the west [Jouzel et al., 1996; Lorius et al., 1985; Pet...
Main Authors: | , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2004
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Subjects: | |
Online Access: | https://doi.org/10.7916/D8W95KR0 |