Abstract

We demonstrate a simple cascade mechanism that drives the formation and emergence of rogue waves in the generalized non-linear Schr\"{o}dinger equation with third-order dispersion. This conceptually novel generation mechanism is based on inelastic collisions of quasi-solitons and is well described by a resonant-like scattering behaviour for the energy transfer in pair-wise quasi-soliton collisions. Our results demonstrate a threshold for rogue wave emergence and the existence of a period of reduced amplitudes - a "calm before the storm" - preceding the arrival of a rogue wave event. Comparing with ultra-long time window simulations of $3.865\times 10^{6}$ps we observe the statistics of rogue waves in optical fibres with an unprecedented level of detail and accuracy, unambiguously establishing the long-ranged character of the rogue wave power-distribution function over seven orders of magnitude.

Highlights

  • Reports of "monster" or "freak" waves [1,2,3] on the earth’s oceans have been seen largely as sea men’s tales [4, 5]

  • We see that the agreement for probability distribution function (PDF) is excellent taking into account that we have reduced the full integration of the generalized non-linear Schrödinger equations (gNLSE) to only discrete collision

  • Our results emphasize the crucial role played by quasi-soliton interactions in the energy exchange underlying the formation of rogue waves (RW) via the proposed cascade mechanism

Read more

Summary

Introduction

Reports of "monster" or "freak" waves [1,2,3] on the earth’s oceans have been seen largely as sea men’s tales [4, 5]. The recent availability of reliable experimental observations [4, 6] has proved their existence and shown that these "rogues" are rare events [7], governed by long tails in their probability distribution function (PDF) [8], and concurrent with very large wave amplitudes [9, 10] As both deep water waves in the oceans and optical waves in fibres can be described by similar generalized non-linear Schrödinger equations (gNLSE) they both show rogue waves (RW) and long-tail statistics [8, 11, 12].

Rogue waves as cascades of interacting solitons
Rare events with ultra-long tails in the PDF
Mechanisms of the cascade
A threshold for RW emergence
Calm before the storm
Methods
Conclusions
Further details of the cascade model
Determining the energy gain
Full Text
Paper version not known

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.