Simulation of the August 1979 sudden discharge of glacier-dammed Flood Lake, British Columbia
In August 1979 a glacier outburst from Flood Lake, British Columbia, released 150 × 10 6 m 3 of water. The resulting flood was routed through the Stikine River and yielded a maximum discharge rate of 1200 m 3 s −1 at a gauging station 90 km downstream from the glacier dam. We have used a computer mo...
Published in: | Canadian Journal of Earth Sciences |
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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Canadian Science Publishing
1984
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Subjects: | |
Online Access: | http://dx.doi.org/10.1139/e84-054 http://www.nrcresearchpress.com/doi/pdf/10.1139/e84-054 |
Summary: | In August 1979 a glacier outburst from Flood Lake, British Columbia, released 150 × 10 6 m 3 of water. The resulting flood was routed through the Stikine River and yielded a maximum discharge rate of 1200 m 3 s −1 at a gauging station 90 km downstream from the glacier dam. We have used a computer model to simulate this outburst in order to test the usefulness of the model as a predictor of flood magnitude. The predicted peak discharge is 2160 m 3 s −1 at the outlet tunnel of the ice dam and 1700 m 3 s −1 at the gauging station. |
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