Soliton-like coherent structures in transitional sphere wakes form as wave packets, peak at velocity discontinuities after T-S wave breakdown, conserve amplitude downstream, and cause vortex structures rather than being caused by them.
Physical Mechanisms of Laminar -Boundary-Layer Transi tion
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Solitary wave structure of transitional flow in the wake of a sphere
Soliton-like coherent structures in transitional sphere wakes form as wave packets, peak at velocity discontinuities after T-S wave breakdown, conserve amplitude downstream, and cause vortex structures rather than being caused by them.