Soliton and Rogue Wave Statistics in Supercontinuum Generation In
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Waves on Deep Water, I
Lecture 14: Waves on deep water, I Lecturer: Harvey Segur. Write-up: Adrienne Traxler June 23, 2009 1 Introduction In this lecture we address the question of whether there are stable wave patterns that propagate with permanent (or nearly permanent) form on deep water. The primary tool for this investigation is the nonlinear Schr¨odinger equation (NLS). Below we sketch the derivation of the NLS for deep water waves, and review earlier work on the existence and stability of 1D surface patterns for these waves. The next lecture continues to more recent work on 2D surface patterns and the effect of adding small damping. 2 Derivation of NLS for deep water waves The nonlinear Schr¨odinger equation (NLS) describes the slow evolution of a train or packet of waves with the following assumptions: • the system is conservative (no dissipation) • then the waves are dispersive (wave speed depends on wavenumber) Now examine the subset of these waves with • only small or moderate amplitudes • traveling in nearly the same direction • with nearly the same frequency The derivation sketch follows the by now normal procedure of beginning with the water wave equations, identifying the limit of interest, rescaling the equations to better show that limit, then solving order-by-order. We begin by considering the case of only gravity waves (neglecting surface tension), in the deep water limit (kh → ∞). Here h is the distance between the equilibrium surface height and the (flat) bottom; a is the wave amplitude; η is the displacement of the water surface from the equilibrium level; and φ is the velocity potential, u = ∇φ. -
21 Non-Linear Wave Equations and Solitons
Utah State University DigitalCommons@USU Foundations of Wave Phenomena Open Textbooks 8-2014 21 Non-Linear Wave Equations and Solitons Charles G. Torre Department of Physics, Utah State University, [email protected] Follow this and additional works at: https://digitalcommons.usu.edu/foundation_wave Part of the Physics Commons To read user comments about this document and to leave your own comment, go to https://digitalcommons.usu.edu/foundation_wave/2 Recommended Citation Torre, Charles G., "21 Non-Linear Wave Equations and Solitons" (2014). Foundations of Wave Phenomena. 2. https://digitalcommons.usu.edu/foundation_wave/2 This Book is brought to you for free and open access by the Open Textbooks at DigitalCommons@USU. It has been accepted for inclusion in Foundations of Wave Phenomena by an authorized administrator of DigitalCommons@USU. For more information, please contact [email protected]. Foundations of Wave Phenomena, Version 8.2 21. Non-linear Wave Equations and Solitons. In 1834 the Scottish engineer John Scott Russell observed at the Union Canal at Hermiston a well-localized* and unusually stable disturbance in the water that propagated for miles virtually unchanged. The disturbance was stimulated by the sudden stopping of a boat on the canal. He called it a “wave of translation”; we call it a solitary wave. As it happens, a number of relatively complicated – indeed, non-linear – wave equations can exhibit such a phenomenon. Moreover, these solitary wave disturbances will often be stable in the sense that if two or more solitary waves collide then after the collision they will separate and take their original shape. -
Shallow Water Waves and Solitary Waves Article Outline Glossary
Shallow Water Waves and Solitary Waves Willy Hereman Department of Mathematical and Computer Sciences, Colorado School of Mines, Golden, Colorado, USA Article Outline Glossary I. Definition of the Subject II. Introduction{Historical Perspective III. Completely Integrable Shallow Water Wave Equations IV. Shallow Water Wave Equations of Geophysical Fluid Dynamics V. Computation of Solitary Wave Solutions VI. Water Wave Experiments and Observations VII. Future Directions VIII. Bibliography Glossary Deep water A surface wave is said to be in deep water if its wavelength is much shorter than the local water depth. Internal wave A internal wave travels within the interior of a fluid. The maximum velocity and maximum amplitude occur within the fluid or at an internal boundary (interface). Internal waves depend on the density-stratification of the fluid. Shallow water A surface wave is said to be in shallow water if its wavelength is much larger than the local water depth. Shallow water waves Shallow water waves correspond to the flow at the free surface of a body of shallow water under the force of gravity, or to the flow below a horizontal pressure surface in a fluid. Shallow water wave equations Shallow water wave equations are a set of partial differential equations that describe shallow water waves. 1 Solitary wave A solitary wave is a localized gravity wave that maintains its coherence and, hence, its visi- bility through properties of nonlinear hydrodynamics. Solitary waves have finite amplitude and propagate with constant speed and constant shape. Soliton Solitons are solitary waves that have an elastic scattering property: they retain their shape and speed after colliding with each other. -
Soliton and Some of Its Geophysical/Oceanographic Applications
Introduction Historical KdV equation Other equations Theory Applications Higher dimensions Problems Soliton and Some of its Geophysical/Oceanographic Applications M. Lakshmanan Centre for Nonlinear Dynamics Bharathidasan University Tiruchirappalli – 620024 India Discussion Meeting, ICTS-TIFR 21 July 2016 M. Lakshmanan Soliton and Some of its Geophysical Introduction Historical KdV equation Other equations Theory Applications Higher dimensions Problems Theme Soliton is a counter-intuitive wave entity arising because of a delicate balance between dispersion and nonlinearity. Its major attraction is its localized nature, finite energy and preservation of shape under collision = a remark- ably stable structure. Consequently, it has⇒ ramifications in as wider areas as hydrodynamics, tsunami dynamics, condensed matter, magnetism, particle physics, nonlin- ear optics, cosmology and so on. A brief overview will be presented with emphasis on oceanographic applications and potential problems will be indicated. M. Lakshmanan Soliton and Some of its Geophysical Introduction Historical KdV equation Other equations Theory Applications Higher dimensions Problems Plan 1 Introduction 2 Historical: (i) Scott-Russel (ii) Zabusky/Kruskal 3 Korteweg-de Vries equation and solitary wave/soliton 4 Other ubiquitous equations 5 Mathematical theory of solitons 6 Geophysical/Oceanographic applications 7 Solitons in higher dimensions 8 Problems and potentialities M. Lakshmanan Soliton and Some of its Geophysical Introduction Historical KdV equation Other equations Theory -
Santa Rosa County Tsunami/Rogue Wave
SANTA ROSA COUNTY TSUNAMI/ROGUE WAVE EVACUATION PLAN Banda Aceh, Indonesia, December 2004, before/after tsunami photos 1 Table of Contents Introduction …………………………………………………………………………………….. 3 Purpose…………………………………………………………………………………………. 3 Definitions………………………………………………………………………………………… 3 Assumptions……………………………………………………………. ……………………….. 4 Participants……………………………………………………………………………………….. 4 Tsunami Characteristics………………………………………………………………………….. 4 Tsunami Warning Procedure…………………………………………………………………….. 6 National Weather Service Tsunami Warning Procedures…………………………………….. 7 Basic Plan………………………………………………………………………………………….. 10 Concept of Operations……………………………………………………………………………. 12 Public Awareness Campaign……………………………………………………………………. 10 Resuming Normal Operations…………………………………………………………………….13 Tsunami Evacuation Warning Notice…………………………………………………………….14 2 INTRODUCTION: Santa Rosa County Emergency Management developed a Santa Rosa County-specific Tsunami/Rogue wave Evacuation Plan. In the event a Tsunami1 threatens Santa Rosa County, the activation of this plan will guide the actions of the responsible agencies in the coordination and evacuation of Navarre Beach residents and visitors from the beach and other threatened areas. The goal of this plan is to provide for the timely evacuation of the Navarre Beach area in the event of a Tsunami Warning. An alternative to evacuating Navarre Beach residents off of the barrier island involves vertical evacuation. Vertical evacuation consists of the evacuation of persons from an entire area, floor, or wing of a building -
Dissipative Cnoidal Waves (Turing Rolls) and the Soliton Limit in Microring Resonators
Research Article Vol. X, No. X / Febrary 1046 B.C. / OSA Journal 1 Dissipative cnoidal waves (Turing rolls) and the soliton limit in microring resonators ZHEN QI1,*,S HAOKANG WANG1,J OSÉ JARAMILLO-VILLEGAS2,M INGHAO QI3, ANDREW M. WEINER3,G IUSEPPE D’AGUANNO1,T HOMAS F. CARRUTHERS1, AND CURTIS R. MENYUK1 1University of Maryland at Baltimore County, 1000 Hilltop Circle, Baltimore, MD 21250, USA 2Technological University of Pereira, Cra. 27 10-02, Pereira, Risaralda 660003, Colombia 3Purdue University, 610 Purdue Mall, West Lafayette, IN 47907, USA *Corresponding author: [email protected] Compiled May 27, 2019 Single solitons are a special limit of more general waveforms commonly referred to as cnoidal waves or Turing rolls. We theoretically and computationally investigate the stability and acces- sibility of cnoidal waves in microresonators. We show that they are robust and, in contrast to single solitons, can be easily and deterministically accessed in most cases. Their bandwidth can be comparable to single solitons, in which limit they are effectively a periodic train of solitons and correspond to a frequency comb with increased power. We comprehensively explore the three-dimensional parameter space that consists of detuning, pump amplitude, and mode cir- cumference in order to determine where stable solutions exist. To carry out this task, we use a unique set of computational tools based on dynamical system theory that allow us to rapidly and accurately determine the stable region for each cnoidal wave periodicity and to find the instabil- ity mechanisms and their time scales. Finally, we focus on the soliton limit, and we show that the stable region for single solitons almost completely overlaps the stable region for both con- tinuous waves and several higher-periodicity cnoidal waves that are effectively multiple soliton trains. -
Three-Dimensional Dynamics of Baroclinic Tides Over a Seamount
University of Plymouth PEARL https://pearl.plymouth.ac.uk Faculty of Science and Engineering School of Biological and Marine Sciences 2018-02 Three-dimensional dynamics of baroclinic tides over a seamount Vlasenko, V http://hdl.handle.net/10026.1/10845 10.1002/2017JC013287 Journal of Geophysical Research: Oceans American Geophysical Union All content in PEARL is protected by copyright law. Author manuscripts are made available in accordance with publisher policies. Please cite only the published version using the details provided on the item record or document. In the absence of an open licence (e.g. Creative Commons), permissions for further reuse of content should be sought from the publisher or author. JOURNAL OF GEOPHYSICAL RESEARCH, VOL. ???, XXXX, DOI:10.1002/, Three-dimensional dynamics of baroclinic tides over a seamount 1 1 1 Vasiliy Vlasenko , Nataliya Stashchuk , and W. Alex M. Nimmo-Smith Vasiliy Vlasenko, School of Biological and Marine Sciences, Plymouth University, Plymouth, PL4 8AA, UK ([email protected]) 1School of Biological and Marine Sciences, Plymouth University, Plymouth, PL4 8AA, UK. D R A F T January 17, 2018, 10:45am D R A F T X-2 VLASENKO ET AL.: BAROCLINIC TIDES OVER A SEAMOUNT 1 Abstract. 2 The Massachusetts Institute of Technology general circulation model is used 3 for the analysis of baroclinic tides over Anton Dohrn Seamount (ADS), in 4 the North Atlantic. The model output is validated against in-situ data col- 5 lected during the 136-th cruise of the RRS “James Cook” in May-June 2016. 6 The observational data set includes velocity time series recorded at two moor- 7 ings as well as temperature, salinity and velocity profiles collected at 22 hy- 8 drological stations. -
Deep Ocean Wind Waves Ch
Deep Ocean Wind Waves Ch. 1 Waves, Tides and Shallow-Water Processes: J. Wright, A. Colling, & D. Park: Butterworth-Heinemann, Oxford UK, 1999, 2nd Edition, 227 pp. AdOc 4060/5060 Spring 2013 Types of Waves Classifiers •Disturbing force •Restoring force •Type of wave •Wavelength •Period •Frequency Waves transmit energy, not mass, across ocean surfaces. Wave behavior depends on a wave’s size and water depth. Wind waves: energy is transferred from wind to water. Waves can change direction by refraction and diffraction, can interfere with one another, & reflect from solid objects. Orbital waves are a type of progressive wave: i.e. waves of moving energy traveling in one direction along a surface, where particles of water move in closed circles as the wave passes. Free waves move independently of the generating force: wind waves. In forced waves the disturbing force is applied continuously: tides Parts of an ocean wave •Crest •Trough •Wave height (H) •Wavelength (L) •Wave speed (c) •Still water level •Orbital motion •Frequency f = 1/T •Period T=L/c Water molecules in the crest of the wave •Depth of wave base = move in the same direction as the wave, ½L, from still water but molecules in the trough move in the •Wave steepness =H/L opposite direction. 1 • If wave steepness > /7, the wave breaks Group Velocity against Phase Velocity = Cg<<Cp Factors Affecting Wind Wave Development •Waves originate in a “sea”area •A fully developed sea is the maximum height of waves produced by conditions of wind speed, duration, and fetch •Swell are waves -
Plasmon-Soliton
Plasmon-Soliton Eyal Feigenbaum and Meir Orenstein Department of Electrical Engineering, Technion, Haifa 32000, Israel [email protected] Abstract : Formation of a novel hybrid-vector spatial plasmon-soliton in a Kerr slab embedded in-between metal plates is predicted and analyzed with a modified NLSE, encompassing hybrid vector field characteristics. Assisted by the transverse plasmonic effect, the self trapping dimension of the plasmon-soliton was substantially compressed (compared to the dielectrically cladded slab case) when reducing the slab width. The practical limitation of the Plasmon-soliton size reduction is determined by available nonlinear materials and metal loss. For the extreme reported values of nonlinear index change, we predict soliton with a cross section of 300nm×30nm (average dimension of 100nm). 1 The downscaling of conventional photonics is halted when approaching a transverse dimension of ~ λ/2 ( λ is the wavelength). This limitation can be alleviated by the incorporation of metals, giving rise to surface plasmon polaritons (SPP) [1,2]. Here we analyze a novel configuration where light is transversely tightly guided between two metal layers, and laterally self trapped by a nonlinear Kerr effect to yield a plasmon-soliton. The tight field confinement of this scheme is important for potential excitation of plasmon-solitons by a low power continuous wave optical source, which is further assisted by the expected small group velocity of the plasmon-soliton. In this letter we present for the first time both an analysis of TM spatial solitons, using the Non- linear Schrödinger Equation (NLSE), where the full vectorial field is considered, as well as the prediction and characteristics of SPP based solitons. -
Storm, Rogue Wave, Or Tsunami Origin for Megaclast Deposits in Western
Storm, rogue wave, or tsunami origin for megaclast PNAS PLUS deposits in western Ireland and North Island, New Zealand? John F. Deweya,1 and Paul D. Ryanb,1 aUniversity College, University of Oxford, Oxford OX1 4BH, United Kingdom; and bSchool of Natural Science, Earth and Ocean Sciences, National University of Ireland Galway, Galway H91 TK33, Ireland Contributed by John F. Dewey, October 15, 2017 (sent for review July 26, 2017; reviewed by Sarah Boulton and James Goff) The origins of boulderite deposits are investigated with reference wavelength (100–200 m), traveling from 10 kph to 90 kph, with to the present-day foreshore of Annagh Head, NW Ireland, and the multiple back and forth actions in a short space and brief timeframe. Lower Miocene Matheson Formation, New Zealand, to resolve Momentum of laterally displaced water masses may be a contributing disputes on their origin and to contrast and compare the deposits factor in increasing speed, plucking power, and run-up for tsunamis of tsunamis and storms. Field data indicate that the Matheson generated by earthquakes with a horizontal component of displace- Formation, which contains boulders in excess of 140 tonnes, was ment (5), for lateral volcanic megablasts, or by the lateral movement produced by a 12- to 13-m-high tsunami with a period in the order of submarine slide sheets. In storm waves, momentum is always im- of 1 h. The origin of the boulders at Annagh Head, which exceed portant(1cubicmeterofseawaterweighsjustover1tonne)in 50 tonnes, is disputed. We combine oceanographic, historical, throwing walls of water continually at a coastline. -
Soliton Molecules, Rational Positon Solution and Rogue Waves for the Extended Complex Modi Ed Kdv Equation
Soliton Molecules, Rational Positon Solution and Rogue Waves for the Extended Complex Modied KdV Equation Lin Huang Hangzhou Dianzi University Nannan Lv ( [email protected] ) Hangzhou Dianzi University School of Science Research Article Keywords: Darboux transformation, Soliton molecule, Positon solution, Rational positon solution, Rogue waves solution Posted Date: May 11th, 2021 DOI: https://doi.org/10.21203/rs.3.rs-434604/v1 License: This work is licensed under a Creative Commons Attribution 4.0 International License. Read Full License Version of Record: A version of this preprint was published at Nonlinear Dynamics on August 5th, 2021. See the published version at https://doi.org/10.1007/s11071-021-06764-x. Soliton molecules, rational positons and rogue waves for the extended complex modified KdV equation Lin Huang ∗and Nannan Lv† School of Science, Hangzhou Dianzi University, 310018 Zhejiang, China. May 6, 2021 Abstract We consider the integrable extended complex modified Korteweg–de Vries equation, which is generalized modified KdV equation. The first part of the article considers the construction of solutions via the Darboux transformation. We obtain some exact solutions, such as soliton molecules, positon solutions, rational positon solutions, and rogue waves solutions. The second part of the article analyzes the dynamics of rogue waves. By means of the numerical analysis, under the standard decomposition, we divide the rogue waves into three patterns: fundamental pattern, triangular pattern and ring pattern. For the fundamental pattern, we define the length and width of the rogue waves and discuss the effect of different parameters on rogue waves. Keywords: Darboux transformation, Soliton molecule, Positon solution, Rational positon so- lution, Rogue waves solution. -
Andaman Sea by Global Ocean Associates Prepared for the Office of Naval Research - Code 322PO
An Atlas of Oceanic Internal Solitary Waves (May 2002) The Andaman Sea by Global Ocean Associates Prepared for the Office of Naval Research - Code 322PO Andaman Sea Overview The Andaman Sea is located along the eastern side of the Indian Ocean between the Malay Peninsula and the Andaman and Nicobar Islands (Figure 1). It is a deep-water sea with exits to the Indian Ocean (to the west) and the Strait of Malacca (to the south). Figure 1. Bathymetry of Andaman Sea [Smith and Sandwell, 1997]. 485 An Atlas of Oceanic Internal Solitary Waves (May 2002) The Andaman Sea by Global Ocean Associates Prepared for the Office of Naval Research - Code 322PO Observations As far back as the mid-19th century surface manifestations of solitons have been observed consisting of strong bands of sea surface roughness. These bands were referred to as "ripplings", due to their mistaken association with rip tides. A description of such bands can be found in the book of Maury [1861] published in 1861 and which is quoted in Osborne and Burch [1980]: "In the entrance of the Malacca Straits, near Nicobar and Acheen Islands, and between them and Junkseylon, there are often strong ripplings, particularly in the southwest monsoon; these are alarming to persons unacquainted, for the broken water makes a great noise when the ship is passing through the ripplings at night. In most places ripplings are thought to be produced by strong currents, but here they are frequently seen when there is no perceptible current…so as to produce an error in the course and distance sailed, yet the surface if the water is impelled forward by some undiscovered cause.