1979
DOI: 10.1007/bf01050233
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Three-wave resonance interaction of disturbances in a boundary layer

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Cited by 21 publications
(7 citation statements)
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“…Such behavior of the fundamental wave and the subharmonic agrees with the results of calculations of the nonlinear resonant interaction of waves in a three-dimensional triplet [14].…”
Section: Development Of Finite-amplitude Perturbations In the Case Ofsupporting
confidence: 85%
See 1 more Smart Citation
“…Such behavior of the fundamental wave and the subharmonic agrees with the results of calculations of the nonlinear resonant interaction of waves in a three-dimensional triplet [14].…”
Section: Development Of Finite-amplitude Perturbations In the Case Ofsupporting
confidence: 85%
“…In [12], it is asserted that there is complete agreement between the experimental results and the theoretical model of Craik [13,14]. In [12], it is asserted that there is complete agreement between the experimental results and the theoretical model of Craik [13,14].…”
mentioning
confidence: 91%
“…A systematic theory of the resonant interaction of inviscid Rayleigh waves developing in a boundary layer with a weak adverse pressure gradient was developed by Goldstein & Lee (1992). The double-exponential resonant growth of three-dimensional subharmonics, found in previous, less strict weakly nonlinear theory by Volodin & Zelman (1978), has been corroborated. At a fully nonlinear stage of development the disturbances exhibited rapid explosive growth, which was, again, qualitatively similar to that found by other theoretical approaches (see Spalart & Yang 1987;Zelman & Maslennikova 1993).…”
mentioning
confidence: 86%
“…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.…”
Section: Introductionmentioning
confidence: 98%
“…A similar anomalous behavior is also characteristic of the boundary layer transition to turbulent state in the sub-harmonic regime [3].…”
mentioning
confidence: 60%