Based on the time-dependent continuity equation with ice velocity specified by a combination of flow and sliding laws, this fully time-dependent flowline-oriented finite-element model is used to: comapre computed steady-state and measured velocities in the Byrd Glacier, as well as to derive driving stress patterns, and estimates of the degree of sliding and creep deformation. -from Current Antarctic Literature
CITATION STYLE
Fastook, J. L. (1987). Finite-element method applied to a time-dependent flowband model. Dynamics of the West Antarctic Ice Sheet, 203–221. https://doi.org/10.1007/978-94-009-3745-1_12
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