Abstract
When a boundary layer undergoes a rapid acceleration through a strongly favourable pressure gradient, the violent eruptions away from the wall, near the edge of the viscous sublayer cease when the pressure gradient reaches a critical value given by (Schraub & Kline, 1965; Moretti & Kays, 1965):
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Piquet, J. (1999). Complex Effects in Turbulent Flows. In: Turbulent Flows. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-662-03559-7_6
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