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,...

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Bibliographic Details
Main Authors: Kamb, Barclay, Echelmeyer, Keith A.
Format: Article in Journal/Newspaper
Language:unknown
Published: International Glaciological Society 1986
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