The effects of forcing on a single stream shear layer and its parent boundary layerThe detailed response of a large single-stream shear layer to a sinusoidal forcing at x = 0 is quantitatively defined. Phase-averaged data are used to characterize the increased disturbance convection velocity and a width measure of the disturbance field. These findings are consistent with and complement those of Fiedler and Mensing (1985).
Document ID
19900048164
Acquisition Source
Legacy CDMS
Document Type
Conference Paper
Authors
Haw, R. C. (Michigan State Univ. East Lansing, MI, United States)
Foss, J. F. (Michigan State University East Lansing, United States)