Application of a Flow Model to the Ice-divide Region of Devon Island Ice Cap, Canada
Abstract The steady-state flow model of Reeh (1988) is applied to a flow line that starts at the highest point of the Devon Island ice cap, follows the surface crest for 7.6 km, and then runs down the slope for a further 3.7 km. The effects of bedrock undulations, divergence of the flow lines, the v...
Published in: | Journal of Glaciology |
---|---|
Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press (CUP)
1988
|
Subjects: | |
Online Access: | http://dx.doi.org/10.1017/s0022143000009060 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000009060 |