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The uniqueness of steady state flows of glaciers and ice sheets
A. C. Fowler
, D. A. Larson
Trinity College Dublin
Indiana University Bloomington
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Engineering
Steady State Flow
100%
Melting Point
100%
Free Surface
50%
Peclet Number
50%
Arrhenius
50%
Graetz Number
50%
Essential Feature
50%
Advective Heat Transport
50%
Exponential Approximation
50%
Infinitesimal Perturbation
50%
Boundary Condition
50%
Flow Distribution
50%
Advection
50%
Physics
Steady State
100%
Melting Point
100%
Boundary Condition
50%
Flow Distribution
50%
Heat Transfer
50%
Advection
50%
nonNewtonian Flow
50%
Basal Ice
50%
Peclet Number
50%
Free Boundary
50%
Earth and Planetary Sciences
Ice Sheet
100%
Flow Distribution
50%
Basal Ice
50%
Boundary Condition
50%
Free Boundary
50%
nonNewtonian Flow
50%
Peclet Number
50%
Advection
50%
Material Science
Surface (Surface Science)
100%
Chemical Engineering
Peclet Number
100%