





Kelvin-Helmholtz Instability of a Finite Shear Layer between Two Parallel Streams of Different Densities
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The .study of the hydrodynamie stability of a shear layer between parallel streams was initiated by Helmholtz (1868). He considered two streams of inviscid fluids with a discontinuous velocity profile, i.e.. the two streams are considered to be separated by a vortex sheet of zero thickness.
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