Phase-suppressed hydrodynamics of solitons on constant-background plane wave

A. Chabchoub, T. Waseda, M. Klein, S. Trillo, and M. Onorato
Phys. Rev. Fluids 5, 114801 – Published 9 November 2020

Abstract

Soliton and breather solutions of the nonlinear Schrödinger equation (NLSE) are known to model localized structures in nonlinear dispersive media such as on the water surface. One of the conditions for an accurate propagation of such exact solutions is the proper generation of the exact initial phase-shift profile in the carrier wave, as defined by the NLSE envelope at a specific time or location. Here, we show experimentally the significance of such initial exact phase excitation during the hydrodynamic propagation of localized envelope solitons and breathers, which modulate a plane wave of constant amplitude (finite background). Using the example of stationary black solitons in intermediate water depth and pulsating Peregrine breathers in deep water, we show how these localized envelopes disintegrate while they evolve over a significant long distance when the initial phase shift is zero. By setting the envelope phases to zero, the dark solitons will disintegrate into two gray-type solitons and dispersive elements. In the case of the doubly localized Peregrine breather the maximal amplification is considerably retarded; however, locally, the shape of the maximal focused wave measured together with the respective signature phase-shift are almost identical to the exact analytical Peregrine characterization at its maximal compression location. The experiments, conducted in large-scaled shallow-water as well as deep-water wave facilities, are in very good agreement with NLSE simulations for all cases.

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  • Received 3 July 2020
  • Accepted 30 September 2020

DOI:https://doi.org/10.1103/PhysRevFluids.5.114801

©2020 American Physical Society

Physics Subject Headings (PhySH)

Nonlinear DynamicsInterdisciplinary PhysicsFluid Dynamics

Authors & Affiliations

A. Chabchoub1,2,3,*, T. Waseda3, M. Klein4, S. Trillo5, and M. Onorato6,7

  • 1Centre for Wind, Waves and Water, School of Civil Engineering, The University of Sydney, Sydney, New South Wales 2006, Australia
  • 2Marine Studies Institute, The University of Sydney, Sydney, New South Wales 2006, Australia
  • 3Department of Ocean Technology, Policy, and Environment, Graduate School of Frontier Sciences, The University of Tokyo, Kashiwa, Chiba 277-8563, Japan
  • 4Institute for Structural Dynamics, Hamburg University of Technology, 21073 Hamburg, Germany
  • 5Department of Engineering, University of Ferrara, 44122 Ferrara, Italy
  • 6Dipartimento di Fisica, Università degli Studi di Torino, 10125 Torino, Italy
  • 7Istituto Nazionale di Fisica Nucleare, INFN, Sezione di Torino, 10125 Torino, Italy

  • *amin.chabchoub@sydney.edu.au

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Issue

Vol. 5, Iss. 11 — November 2020

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