“…For nonlinear stages of boundary-layer transition, the first theories of resonant interactions of TS waves were developed by Maseev (1968) and Craik (1971) and later by Herbert (1975), Volodin & Zelman (1978), Smith & Stewart (1987), Goldstein & Lee (1992), Mankbadi, Wu & Lee (1993) and Wu (1995) and in a great number of other subsequent studies; for a review see Borodulin, Kachanov & Koptsev (2002b), for example. The classical Craik's triad consists of a two-dimensional (2D) primary (fundamental) instability wave, with frequency f 1 , having relatively large amplitude and two weak oblique subharmonic waves, with frequency f s = f 1 /2, propagating at angles to the mean flow direction with the same values but opposite signs.…”