2020
DOI: 10.1007/s11071-020-05819-9
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Stabilization of uni-directional water wave trains over an uneven bottom

Abstract: We study the evolution of nonlinear surface gravity water wave packets developing from modulational instability over an uneven bottom. A nonlinear Schrödinger equation (NLSE) with coefficients varying in space along propagation is used as a reference model. Based on a low-dimensional approximation obtained by considering only three complex harmonic modes, we discuss how to stabilize a one-dimensional pattern in the form of train of large peaks sitting on a background and propagating over a significant distance… Show more

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Cited by 10 publications
(8 citation statements)
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“…Indeed, the initial temporal phase profile, or equivalently, the input phase relationship in Fourier space (i.e. the relative phase between the MI side-bands and the central carrier) have deep impact on the type of amplitude modulation that develops upon propagation [8,9], as recently observed experimentally [10][11][12].…”
mentioning
confidence: 78%
“…Indeed, the initial temporal phase profile, or equivalently, the input phase relationship in Fourier space (i.e. the relative phase between the MI side-bands and the central carrier) have deep impact on the type of amplitude modulation that develops upon propagation [8,9], as recently observed experimentally [10][11][12].…”
mentioning
confidence: 78%
“…Furthermore, coherent seed-induced breathers in various conservative setting inevitably manifest as a synchronized periodic oscillation along longitudinal evolution [7][8][9][10]. Consequently, all possibilities to 'stabilize' a breather wave and especially to freeze breather's amplitude and phase in a controllable manner are of great interest [11][12][13][14]. Recently, Gomel et al experimentally investigated the parametric stabilization of unsteady nonlinear waves in a wave flume with an abrupt bathymetry change [11].…”
Section: Introductionmentioning
confidence: 99%
“…This jump can be described as the optimal matching of an initial AB solution to a steady dnoidal solution of the universal NLSE, illustrating the generality of this wave control process. This approach contrasts with that of a slow evolution of the system over several envelope oscillations, that also results in system stabilization [35], and from stabilization mechanisms relying on dissipation [45].…”
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confidence: 97%
“…where V (ξ, τ ) is the shoaling-corrected envelope of the free surface elevation [34,35], ξ ≡ ε 2 x, and τ ≡ ε x 0 dζ cg(ζ) − t (t being the physical time) are the coordinates in a frame moving at the envelope group velocity,…”
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confidence: 99%