Other
Scientific paper
Dec 2006
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006georl..3323502v&link_type=abstract
Geophysical Research Letters, Volume 33, Issue 23, CiteID L23502
Other
4
Cryosphere: Ice Sheets, Cryosphere: Thermal Regime, Global Change: Sea Level Change (1222, 1225, 4556), Volcanology: General Or Miscellaneous, Geographic Location: Antarctica (4207)
Scientific paper
Subglacial volcanism in West Antarctica may play a crucial role in the dynamics and stability of the West Antarctic Ice Sheet (WAIS). Evidence supporting the existence of an individual subglacial volcanic center (Mt. Casertz) in the upper catchments of Whillans and Kamb Ice Stream (WIS and KIS), comes from a comparison of ice sheet modeling results with measured ice velocities. Lubrication of an area, which otherwise should be frozen to its bed, is best explained by basal melt water generated in the vicinity of Mt. Casertz. The estimated melt water production of Mt. Casertz corresponds to ~8 % of the total melt water production in the two catchments. This would be sufficient to offset basal freezing in the dormant KIS, relubricating its bed and potentially causing a restart. Near future volcanic activity changes are speculative, but would have far reaching implications on the dynamics and stability of the WAIS requiring further investigation.
Tulaczyk Slawek
Vogel Stefan W.
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