2015
DOI: 10.1016/j.crma.2015.10.017
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A simple criterion for transverse linear instability of nonlinear waves

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Cited by 6 publications
(6 citation statements)
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“…has a solution of the form e σt u σ (z), where Re σ > 0 and u σ is bounded (see Section 2.1 for a precise definition). The following theorem, which is due to Godey [10], shows that the existence of a pair of simple purely imaginary eigenvalues of L = df [u ] implies the transverse linear instability of u . Theorem 1.3 Consider the differential equation…”
Section: Introductionmentioning
confidence: 99%
“…has a solution of the form e σt u σ (z), where Re σ > 0 and u σ is bounded (see Section 2.1 for a precise definition). The following theorem, which is due to Godey [10], shows that the existence of a pair of simple purely imaginary eigenvalues of L = df [u ] implies the transverse linear instability of u . Theorem 1.3 Consider the differential equation…”
Section: Introductionmentioning
confidence: 99%
“…Finally, we demonstrate the transverse linear instability of the line soliton using the following general result due to Godey [5]. Theorem 5.1 (Godey) Consider the differential equation…”
Section: Transverse Linear Instabilitymentioning
confidence: 99%
“…Finally, we demonstrate the transverse linear instability of the line soliton using the following general result due to Godey [5]. Theorem 5.1 (Godey) Consider the differential equation Under these hypotheses equation (25) has a solution of the form e λt v λ (τ ), where v λ ∈ C 1 (R, X ) ∩ C(R, Z) is periodic, for each sufficiently small positive value of λ; its period tends to 2π/ω 0 as λ → 0.…”
Section: Transverse Linear Instabilitymentioning
confidence: 99%
“…This is the key, and most challenging, part of our analysis. The transverse stability of periodic waves was mostly studied for simpler model equations obtained from the Euler equations (1.1)-(1.2) in different parameter regimes: the Kadomtsev-Petviashvili-I equation for the regime of large surface tension (α ∼ 1, β > 1/3) was considered in [21,22,34], the Davey-Stewartson system for the regime of weak surface tension ((α, β) close to the curve Γ) in [13], and a fifth order KP equation for the regime of critical surface tension (α ∼ 1, β ∼ 1/3) in [25]; see also the recent review paper [24]. All these results predict that gravity-capillary periodic waves are linearly transversely unstable.…”
Section: Introductionmentioning
confidence: 99%
“…For the transverse linear instability problem, we consider the linearization of this dynamical system at a two-dimensional periodic wave and apply a simple general instability criterion [13] adapted to the Euler equations in [20]. In Region I, we show that the periodic waves…”
Section: Introductionmentioning
confidence: 99%