Stress-gradient coupling in glacier flow: I. Longitudinal averaging of the influence of ice thickness and surface slope
For a glacier flowing over a bed of longitudinally varying slope, the influence of longitudinal stress gradients on the flow is analyzed by means of a longitudinal flow-coupling equation derived from the "vertically" (cross-sectionally) integrated longitudinal stress equilibrium equation,...
Main Authors: | , |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
International Glaciological Society
1986
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Subjects: | |
Online Access: | https://authors.library.caltech.edu/49684/ https://authors.library.caltech.edu/49684/1/Kamb_1986p267.pdf https://resolver.caltech.edu/CaltechAUTHORS:20140915-081135893 |