Journal of Fluid Mechanics · 1977 · 329 citations · 12 references
Natural SciencesGeophysicsPhysicsDifferential EquationsDynamical SystemsTheoretical PhysicsGravity WavesNonlinear DynamicsNonlinear Wave DynamicsSurface Gravity WavesSurface Wave DynamicsWave InteractionKorteweg - De Vries EquationNonlinear Wave InteractionsNonlinear WavesSolitary Wave InteractionsSolitary WavesWave - Wave Interactions
Nonlinear oblique interactions between two slightly dispersive gravity waves (in particular, solitary waves) of dimensionless amplitudes α 1 and α 2 (relative to depth) and relative inclination 2ϕ (between wave normals) are classified as weak if sin 2 ϕ α 1,2 or strong if ϕ 2 = O (α 1,2 ). Weak interactions permit superposition of the individual solutions of the Korteweg-de Vries equation in first approximation; the interaction term, which is O (α 1 α 2 ), then is determined from these basic solutions. Strong interactions are intrinsically nonlinear. It is shown that these interactions are phase-conserving (the sum of the phases of the incoming waves is equal to the sum of the phases of the outgoing waves) if |α 2 -α 1 > (2ϕ) 2 but not if |α 2 -α 1 | (2ϕ) 2 (e.g. the reflexion problem, for which the interacting waves are images and α 2 = α 1 ). It also is shown that the interactions are singular, in the sense that regular incoming waves with sech 2 profiles yield singular outgoing waves with - csch 2 profiles, if \[ \psi_{-}< |\psi| < \psi_{+},\quad{\rm where}\quad\psi_{\pm}={\textstyle\frac{1}{2}}\left|(3\alpha_2)^{\frac{1}{2}}\pm(3\alpha_1)^{\frac{1}{2}}\right|. \] Regular interactions appear to be impossible within this singular regime, and its end points, |ϕ| = ϕ±, are associated with resonant interactions.
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<i>Linear and Nonlinear Waves</i>
G. B. Whitham, Richard Fowler · Physics Today · 1975 · 8.3K citations
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