Figure 1: Left panels:
top view of
samples with four different pinning strengths:
(a) fp = 0.18 f0, (b) fp = 0.36 f0,
(c) fp = 0.57 f0, (d) fp = 0.66 f0.
The channels most often followed by vortices are darker.
The number of channels decreases as the pinning strength fp increases.
Right panels: distribution of the average rate
Γav at which vortices pass through
individual grid points in the river.
For strong pinning, the few remaining channels are frequently traveled
[see brace in (d)].
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