Abstract
A knowledge of the conditions under which unsteady flows become turbulent is important in many applications, e.g. the transport of sediment along the ocean bed (Li 1954), physiological investigations of the larger blood vessels (e.g. Pedley 1980), and various pipe-line and aerodynamic problems.
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Cowley, S.J. (1987). High Frequency Rayleigh Instability of Stokes Layers. In: Dwoyer, D.L., Hussaini, M.Y. (eds) Stability of Time Dependent and Spatially Varying Flows. ICASE NASA LaRC Series. Springer, New York, NY. https://doi.org/10.1007/978-1-4612-4724-1_14
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DOI: https://doi.org/10.1007/978-1-4612-4724-1_14
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