2009
DOI: 10.1007/s00348-009-0747-x
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Evolution of isolated streamwise vortices in the late stages of boundary layer transition

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Cited by 7 publications
(17 citation statements)
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“…The mechanism of the formation of an isolated streamwise vortex downstream of the hill has been described before [23]. The half-span configuration generates streamwise vorticity by tilting of the spanwise vorticity of the boundary layer and by viscous generation at the wall due to the cross-stream pressure gradient.…”
Section: Description Of Experimentsmentioning
confidence: 99%
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“…The mechanism of the formation of an isolated streamwise vortex downstream of the hill has been described before [23]. The half-span configuration generates streamwise vorticity by tilting of the spanwise vorticity of the boundary layer and by viscous generation at the wall due to the cross-stream pressure gradient.…”
Section: Description Of Experimentsmentioning
confidence: 99%
“…The half-span configuration generates streamwise vorticity by tilting of the spanwise vorticity of the boundary layer and by viscous generation at the wall due to the cross-stream pressure gradient. The dominant flow structure downstream of the hill is a single, streamwise vortex whose size is of the order of the hill height h; this flow development was examined with a laminar flow simulation of the vicinity of the hill [23], and is shown in Fig. 2.…”
Section: Description Of Experimentsmentioning
confidence: 99%
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