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The accompanying graphic describes the meteorology of parallel streets of stratocumulus clouds in an unstable planetary boundary level. It also explains why the bands get further apart and weaken due to friction as the sun sets and the daytime heating instability dissipates. Think of the circulations as three dimensional helical coils ( a slinky) with the updraft branch supporting the formation of the cloud and the downdraft branch enforcing the clear skies in between the cloud streets. The slinky comparison is actually quite appropriate.
http://fineartamerica.com/featured/singleton-sunset-stratocumulus-phil-chadwick.html
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