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Phase 3 Analyses |
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| Like in transition flow, velocity
in piedmont flow is centered just above the valley-to-plain transition, with
deceleration at the toe on the flat continental plain and towards the walls.
Note that velocity contours parallel the banding in the Flubber. The
density of data points is much higher in the piedmont flow analyses than in
the transition flow due to the addition of markers (see figure to left).
The large region of uniform velocity near the toe is well contrained
by data points. |
