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Stage 2: Valley-Piedmont Transition Flow


data
Location of Data Points Used in
Stage 2 Analyses
Velocity
Velocity is centered just above the valley-to-plain transition, with deceleration at the toe on the flat continental plain and towards the walls.  Velocity gradiaents at the toe are not well constrained by data points (see figure to left).
Lateral
Compression/Tension
Longitudinal
Compression/Tension

Shear Strain Rate
Large center of extension (blue) associated with the lateral spreading of the glacier across the unconfined continental plain once beyond the mouth of the valley.  Contour "knots" are an artifact of few data points.
Area of compression (red) at the mouth of the valley due to deceleration in the y-direction as the glacier moves to the lower surface slope of the continental plain. 
Shear strain plot shows same pattern as in valley flow, with a region of 0 shear strain along the center y-axis of the glacier and opposing shear on either side due to drag along the valley walls. 
Dilatation
Vorticity
Dilatiation is minimal and without obvious patterns as observed in valley flow.
Vorticity is focused at the corners of the valley mouth with opposing rotation on either side of the valley.  Rotation in these regions is moderately constrained by data points.

On to Stage 3:
 Piedmont Flow

Back to Stage 1:
Valley Flow

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Analysis