Nonlinear stage of the Benjamin-Feir instability: Three-dimensional coherent structures and rogue waves

dc.creatorRuban, V. P.
dc.date2007-04-24
dc.date.accessioned2026-07-07T08:21:15Z
dc.date.available2026-07-07T08:21:15Z
dc.descriptionA specific, genuinely three-dimensional mechanism of rogue wave formation, in a late stage of the modulational instability of a perturbed Stokes deep-water wave, is recognized through numerical experiments. The simulations are based on fully nonlinear equations describing weakly three-dimensional potential flows of an ideal fluid with a free surface in terms of conformal variables. Spontaneous formation of zigzag patterns for wave amplitude is observed in a nonlinear stage of the instability. If initial wave steepness is sufficiently high ($ka>0.06$), these coherent structures produce rogue waves. The most tall waves appear in ``turns'' of the zigzags. For $ka<0.06$, the structures decay typically without formation of steep waves.
dc.description11 pages, 7 figures, submitted to PRL
dc.identifierhttps://arxiv.org/abs/0704.3246
dc.identifierhttp://arxiv.org/abs/0704.3246
dc.identifierPhys. Rev. Lett. 99, 044502 (2007).
dc.identifierdoi:10.1103/PhysRevLett.99.044502
dc.identifier.urihttp://salesiana.dossiersoluciones.com/handle/123456789/135300
dc.subjectFluid Dynamics
dc.subjectAtmospheric and Oceanic Physics
dc.titleNonlinear stage of the Benjamin-Feir instability: Three-dimensional coherent structures and rogue waves
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