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Aspects of Integrable Models
Aspects of Integrable Models Undergraduate Thesis Submitted in partial fulfillment of the requirements of BITS F421T Thesis By Pranav Diwakar ID No. 2014B5TS0711P Under the supervision of: Dr. Sujay Ashok & Dr. Rishikesh Vaidya BIRLA INSTITUTE OF TECHNOLOGY AND SCIENCE PILANI, PILANI CAMPUS January 2018 Declaration of Authorship I, Pranav Diwakar, declare that this Undergraduate Thesis titled, `Aspects of Integrable Models' and the work presented in it are my own. I confirm that: This work was done wholly or mainly while in candidature for a research degree at this University. Where any part of this thesis has previously been submitted for a degree or any other qualification at this University or any other institution, this has been clearly stated. Where I have consulted the published work of others, this is always clearly attributed. Where I have quoted from the work of others, the source is always given. With the exception of such quotations, this thesis is entirely my own work. I have acknowledged all main sources of help. Signed: Date: i Certificate This is to certify that the thesis entitled \Aspects of Integrable Models" and submitted by Pranav Diwakar, ID No. 2014B5TS0711P, in partial fulfillment of the requirements of BITS F421T Thesis embodies the work done by him under my supervision. Supervisor Co-Supervisor Dr. Sujay Ashok Dr. Rishikesh Vaidya Associate Professor, Assistant Professor, The Institute of Mathematical Sciences BITS Pilani, Pilani Campus Date: Date: ii BIRLA INSTITUTE OF TECHNOLOGY AND SCIENCE PILANI, PILANI CAMPUS Abstract Master of Science (Hons.) Aspects of Integrable Models by Pranav Diwakar The objective of this thesis is to study the isotropic XXX-1/2 spin chain model using the Algebraic Bethe Ansatz. -
Slow Persistent Mixing in the Abyss
Reference: van Haren, H., 2020. Slow persistent mixing in the abyss. Ocean Dyn., 70, 339- 352. Slow persistent mixing in the abyss by Hans van Haren* Royal Netherlands Institute for Sea Research (NIOZ) and Utrecht University, P.O. Box 59, 1790 AB Den Burg, the Netherlands. *e-mail: [email protected] Abstract Knowledge about deep-ocean turbulent mixing and flow circulation above abyssal hilly plains is important to quantify processes for the modelling of resuspension and dispersal of sediments in areas where turbulence sources are expected to be relatively weak. Turbulence may disperse sediments from artificial deep-sea mining activities over large distances. To quantify turbulent mixing above the deep-ocean floor around 4000 m depth, high-resolution moored temperature sensor observations have been obtained from the near-equatorial southeast Pacific (7°S, 88°W). Models demonstrate low activity of equatorial flow dynamics, internal tides and surface near-inertial motions in the area. The present observations demonstrate a Conservative Temperature difference of about 0.012°C between 7 and 406 meter above the bottom (hereafter, mab, for short), which is a quarter of the adiabatic lapse rate. The very weakly stratified waters with buoyancy periods between about six hours and one day allow for slowly varying mixing. The calculated turbulence dissipation rate values are half to one order of magnitude larger than those from open-ocean turbulent exchange well away from bottom topography and surface boundaries. In the deep, turbulent overturns extend up to 100 m tall, in the ocean-interior, and also reach the lowest sensor. The overturns are governed by internal-wave-shear and -convection. -
Ocean Acoustic Tomography Has Heat Content, Velocity, and Vorticity in the North Pacific Thermohaline Circulation and Climate
B. Dushaw, G. Bold, C.-S. Chiu, J. Colosi, B. Cornuelle, Y. Desaubies, M. Dzieciuch, A. Forbes, F. Gaillard, Brian Dushaw, Bruce Howe A. Gavrilov, J. Gould, B. Howe, M. Lawrence, J. Lynch, D. Menemenlis, J. Mercer, P. Mikhalevsky, W. Munk, Applied Physics Laboratory and School of Oceanography I. Nakano, F. Schott, U. Send, R. Spindel, T. Terre, P. Worcester, C. Wunsch, Observing the Ocean in the 2000’s: College of Ocean and Fisheries Sciences A Strategy for the Role of Acoustic Tomography in Ocean Climate Observation. In: Observing the Ocean Ocean Acoustic Tomography: 1970–21st Century University of Washington Ocean Acoustic Tomography: 1970–21st Century http://staff.washington.edu/dushaw in the 21st Century, C.J. Koblinsky and N.R. Smith (eds), Bureau of Meteorology, Melbourne, Australia, 2001. ABSTRACT PROCESS EXPERIMENTS Deep Convection—Greenland and Labrador Seas ATOC—Acoustic Thermometry of Ocean Climate Oceanic convection connects the surface ocean to the deep ocean with important consequences for the global Since it was first proposed in the late 1970’s (Munk and Wunsch 1979, 1982), ocean acoustic tomography has Heat Content, Velocity, and Vorticity in the North Pacific thermohaline circulation and climate. Deep convection occurs in only a few locations in the world, and is difficult The goal of the ATOC project is to measure the ocean temperature on basin scales and to understand the evolved into a remote sensing technique employed in a wide variety of physical settings. In the context of to observe. Acoustic arrays provide both the spatial coverage and temporal resolution necessary to observe variability. The acoustic measurements inherently average out mesoscale and internal wave noise that long-term oceanic climate change, acoustic tomography provides integrals through the mesoscale and other The 1987 reciprocal acoustic tomography experiment (RTE87) obtained unique measurements of gyre-scale deep-water formation. -
A New Two-Component Integrable System with Peakon Solutions
A new two-component integrable system with peakon solutions 1 2 Baoqiang Xia ∗, Zhijun Qiao † 1School of Mathematics and Statistics, Jiangsu Normal University, Xuzhou, Jiangsu 221116, P. R. China 2Department of Mathematics, University of Texas-Pan American, Edinburg, Texas 78541, USA Abstract A new two-component system with cubic nonlinearity and linear dispersion: 1 1 mt = bux + 2 [m(uv uxvx)]x 2 m(uvx uxv), 1 − −1 − nt = bvx + [n(uv uxvx)]x + n(uvx uxv), 2 − 2 − m = u uxx, n = v vxx, − − where b is an arbitrary real constant, is proposed in this paper. This system is shown integrable with its Lax pair, bi-Hamiltonian structure, and infinitely many conservation laws. Geometrically, this system describes a nontrivial one-parameter family of pseudo-spherical surfaces. In the case b = 0, the peaked soliton (peakon) and multi-peakon solutions to this two-component system are derived. In particular, the two-peakon dynamical system is explicitly solved and their interactions are investigated in details. Moreover, a new integrable cubic nonlinear equation with linear dispersion 1 2 2 1 ∗ ∗ arXiv:1211.5727v4 [nlin.SI] 10 May 2015 mt = bux + [m( u ux )]x m(uux uxu ), m = u uxx, 2 | | − | | − 2 − − is obtained by imposing the complex conjugate reduction v = u∗ to the two-component system. The complex valued N-peakon solution and kink wave solution to this complex equation are also derived. Keywords: Integrable system, Lax pair, Peakon. Mathematics Subject Classifications (2010): 37K10, 35Q51. ∗E-mail address: [email protected] †Corresponding author, E-mail address: [email protected] 1 2 1 Introduction In recent years, the Camassa-Holm (CH) equation [1] mt bux + 2mux + mxu = 0, m = u uxx, (1.1) − − where b is an arbitrary constant, derived by Camassa and Holm [1] as a shallow water wave model, has attracted much attention in the theory of soliton and integrable system. -
Internal Tides in the Solomon Sea in Contrasted ENSO Conditions
Ocean Sci., 16, 615–635, 2020 https://doi.org/10.5194/os-16-615-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Internal tides in the Solomon Sea in contrasted ENSO conditions Michel Tchilibou1, Lionel Gourdeau1, Florent Lyard1, Rosemary Morrow1, Ariane Koch Larrouy1, Damien Allain1, and Bughsin Djath2 1Laboratoire d’Etude en Géophysique et Océanographie Spatiales (LEGOS), Université de Toulouse, CNES, CNRS, IRD, UPS, Toulouse, France 2Helmholtz-Zentrum Geesthacht, Max-Planck-Straße 1, Geesthacht, Germany Correspondence: Michel Tchilibou ([email protected]), Lionel Gourdeau ([email protected]), Florent Lyard (fl[email protected]), Rosemary Morrow ([email protected]), Ariane Koch Larrouy ([email protected]), Damien Allain ([email protected]), and Bughsin Djath ([email protected]) Received: 1 August 2019 – Discussion started: 26 September 2019 Revised: 31 March 2020 – Accepted: 2 April 2020 – Published: 15 May 2020 Abstract. Intense equatorward western boundary currents the tidal effects over a longer time. However, when averaged transit the Solomon Sea, where active mesoscale structures over the Solomon Sea, the tidal effect on water mass transfor- exist with energetic internal tides. In this marginal sea, the mation is an order of magnitude less than that observed at the mixing induced by these features can play a role in the ob- entrance and exits of the Solomon Sea. These localized sites served water mass transformation. The objective of this paper appear crucial for diapycnal mixing, since most of the baro- is to document the M2 internal tides in the Solomon Sea and clinic tidal energy is generated and dissipated locally here, their impacts on the circulation and water masses, based on and the different currents entering/exiting the Solomon Sea two regional simulations with and without tides. -
Resonant Interactions of Surface and Internal Waves with Seabed Topography by Louis-Alexandre Couston a Dissertation Submitted I
Resonant Interactions of Surface and Internal Waves with Seabed Topography By Louis-Alexandre Couston A dissertation submitted in partial satisfaction of the requirements for the degree of Doctorate of Philosophy in Engineering - Mechanical Engineering in the Graduate Division of the University of California, Berkeley Committee in Charge: Professor Mohammad-Reza Alam, Chair Professor Ronald W. Yeung Professor Philip S. Marcus Professor Per-Olof Persson Spring 2016 Abstract Resonant Interactions of Surface and Internal Waves with Seabed Topography by Louis-Alexandre Couston Doctor of Philosophy in Engineering - Mechanical Engineering University of California, Berkeley Professor Mohammad-Reza Alam, Chair This dissertation provides a fundamental understanding of water-wave transformations over seabed corrugations in the homogeneous as well as in the stratified ocean. Contrary to a flat or mildly sloped seabed, over which water waves can travel long distances undisturbed, a seabed with small periodic variations can strongly affect the propagation of water waves due to resonant wave-seabed interactions{a phenomenon with many potential applications. Here, we investigate theoretically and with direct simulations several new types of wave transformations within the context of inviscid fluid theory, which are different than the classical wave Bragg reflection. Specifically, we show that surface waves traveling over seabed corrugations can become trapped and amplified, or deflected at a large angle (∼ 90◦) relative to the incident direction of propagation. Wave trapping is obtained between two sets of parallel corrugations, and we demonstrate that the amplification mechanism is akin to the Fabry-Perot resonance of light waves in optics. Wave deflection requires three-dimensional and bi-chromatic corrugations and is obtained when the surface and corrugation wavenumber vectors satisfy a newly found class I2 Bragg resonance condition. -
Remarks on the Complete Integrability of Quantum and Classical Dynamical
Remarks on the complete integrability of quantum and classical dynamical systems Igor V. Volovich Steklov Mathematical Institute of Russian Academy of Sciences, Moscow, Russia [email protected] Abstract It is noted that the Schr¨odinger equation with any self-adjoint Hamiltonian is unitary equivalent to a set of non-interacting classical harmonic oscillators and in this sense any quantum dynamics is completely integrable. Higher order integrals of motion are presented. That does not mean that we can explicitly compute the time dependence for expectation value of any quantum observable. A similar re- sult is indicated for classical dynamical systems in terms of Koopman’s approach. Explicit transformations of quantum and classical dynamics to the free evolution by using direct methods of scattering theory and wave operators are considered. Examples from classical and quantum mechanics, and also from nonlinear partial differential equations and quantum field theory are discussed. Higher order inte- grals of motion for the multi-dimensional nonlinear Klein-Gordon and Schr¨odinger equations are mentioned. arXiv:1911.01335v1 [math-ph] 4 Nov 2019 1 1 Introduction The problem of integration of Hamiltonian systems and complete integrability has already been discussed in works of Euler, Bernoulli, Lagrange, and Kovalevskaya on the motion of a rigid body in mechanics. Liouville’s theorem states that if a Hamiltonian system with n degrees of freedom has n independent integrals in involution, then it can be integrated in quadratures, see [1]. Such a system is called completely Liouville integrable; for it there is a canonical change of variables that reduces the Hamilton equations to the action-angle form. -
"Integrable Systems, Random Matrices and Random Processes"
Contents Integrable Systems, Random Matrices and Random Processes Mark Adler ..................................................... 1 1 Matrix Integrals and Solitons . 4 1.1 Random matrix ensembles . 4 1.2 Large n–limits . 7 1.3 KP hierarchy . 9 1.4 Vertex operators, soliton formulas and Fredholm determinants . 11 1.5 Virasoro relations satisfied by the Fredholm determinant . 14 1.6 Differential equations for the probability in scaling limits . 16 2 Recursion Relations for Unitary Integrals . 21 2.1 Results concerning unitary integrals . 21 2.2 Examples from combinatorics . 25 2.3 Bi-orthogonal polynomials on the circle and the Toeplitz lattice 28 2.4 Virasoro constraints and difference relations . 30 2.5 Singularity confinement of recursion relations . 33 3 Coupled Random Matrices and the 2–Toda Lattice . 37 3.1 Main results for coupled random matrices . 37 3.2 Link with the 2–Toda hierarchy . 39 3.3 L U decomposition of the moment matrix, bi-orthogonal polynomials and 2–Toda wave operators . 41 3.4 Bilinear identities and τ-function PDE’s . 44 3.5 Virasoro constraints for the τ-functions . 47 3.6 Consequences of the Virasoro relations . 49 3.7 Final equations . 51 4 Dyson Brownian Motion and the Airy Process . 53 4.1 Processes . 53 4.2 PDE’s and asymptotics for the processes . 59 4.3 Proof of the results . 62 5 The Pearcey Distribution . 70 5.1 GUE with an external source and Brownian motion . 70 5.2 MOPS and a Riemann–Hilbert problem . 73 VI Contents 5.3 Results concerning universal behavior . 75 5.4 3-KP deformation of the random matrix problem . -
On the Non-Integrability of the Popowicz Peakon System
DISCRETE AND CONTINUOUS Website: www.aimSciences.org DYNAMICAL SYSTEMS Supplement 2009 pp. 359–366 ON THE NON-INTEGRABILITY OF THE POPOWICZ PEAKON SYSTEM Andrew N.W. Hone Institute of Mathematics, Statistics & Actuarial Science University of Kent, Canterbury CT2 7NF, UK Michael V. Irle Institute of Mathematics, Statistics & Actuarial Science University of Kent, Canterbury CT2 7NF, UK Abstract. We consider a coupled system of Hamiltonian partial differential equations introduced by Popowicz, which has the appearance of a two-field coupling between the Camassa-Holm and Degasperis-Procesi equations. The latter equations are both known to be integrable, and admit peaked soliton (peakon) solutions with discontinuous derivatives at the peaks. A combination of a reciprocal transformation with Painlev´eanalysis provides strong evidence that the Popowicz system is non-integrable. Nevertheless, we are able to con- struct exact travelling wave solutions in terms of an elliptic integral, together with a degenerate travelling wave corresponding to a single peakon. We also describe the dynamics of N-peakon solutions, which is given in terms of an Hamiltonian system on a phase space of dimension 3N. 1. Introduction. The members of a one-parameter family of partial differential equations, namely mt + umx + buxm =0, m = u − uxx (1) with parameter b, have been studied recently. The case b = 2 is the Camassa-Holm equation [1], while b = 3 is the Degasperis-Procesi equation [3], and it is known that (with the possible exception of b = 0) these are the only integrable cases [14], while all of these equations (apart from b = −1) arise as a shallow water approximation to the Euler equations [6]. -
The Impact of Fortnightly Stratification Variability on the Generation Of
Journal of Marine Science and Engineering Article The Impact of Fortnightly Stratification Variability on the Generation of Baroclinic Tides in the Luzon Strait Zheen Zhang 1,*, Xueen Chen 1 and Thomas Pohlmann 2 1 College of Oceanic and Atmospheric Sciences, Ocean University of China, Qingdao 266100, China; [email protected] 2 Centre for Earth System Research and Sustainability, Institute of Oceanography, University of Hamburg, 20146 Hamburg, Germany; [email protected] * Correspondence: [email protected] Abstract: The impact of fortnightly stratification variability induced by tide–topography interaction on the generation of baroclinic tides in the Luzon Strait is numerically investigated using the MIT general circulation model. The simulation shows that advection of buoyancy by baroclinic flows results in daily oscillations and a fortnightly variability in the stratification at the main generation site of internal tides. As the stratification for the whole Luzon Strait is periodically redistributed by these flows, the energy analysis indicates that the fortnightly stratification variability can significantly affect the energy transfer between barotropic and baroclinic tides. Due to this effect on stratification variability by the baroclinic flows, the phases of baroclinic potential energy variability do not match the phase of barotropic forcing in the fortnight time scale. This phenomenon leads to the fact that the maximum baroclinic tides may not be generated during the maximum barotropic forcing. Therefore, a significant impact of stratification variability on the generation of baroclinic tides is demonstrated Citation: Zhang, Z.; Chen, X.; by our modeling study, which suggests a lead–lag relation between barotropic tidal forcing and Pohlmann, T. The Impact of maximum baroclinic response in the Luzon Strait within the fortnightly tidal cycle. -
On the Fraction of Internal Tide Energy Dissipated Near Topography
On the Fraction of Internal Tide Energy Dissipated Near Topography Louis C. St. Laurent Department of Oceanography, Florida State University, Tallahassee, Florida Jonathan D. Nash College of Oceanic and Atmospheric Science, Oregon State University, Corvallis, Oregon Abstract. Internal tides have been implicated as a major source of me- chanical energy for mixing in the ocean interior. Indeed, microstructure and tracer measurements have indicated that enhanced turbulence levels occur near topography where internal tides are generated. However, the details of the energy budget and the mechanisms by which energy is transferred from the internal tide to turbulence have been uncertain. It now seems that the energy levels associated with locally enhanced mixing near topography may constitute only a small fraction of the available internal tide energy flux. In this study, the generation, radiation, and energy dissipation of deep ocean internal tides are examined. Properties of the internal tide at the Mid-Atlantic Ridge and Hawaiian Ridge are considered. It is found that most internal tide energy is generated as low modes. The Richardson number of the generated internal tide typically exceeds unity for these motions, so direct shear instability of the generated waves is not the dominant energy transfer mechanism. It also seems that wave-wave interactions are ineffective at transferring energy from the large wavelengths that dominate the energy flux. Instead, it seems that much of the generated energy radiates away from the generation site in low mode waves. These low modes must dissipate somewhere in the ocean, though this likely occurs over O(1000 km) distances as the waves propagate. -
What Are Completely Integrable Hamilton Systems
THE TEACHING OF MATHEMATICS 2011, Vol. XIII, 1, pp. 1–14 WHAT ARE COMPLETELY INTEGRABLE HAMILTON SYSTEMS BoˇzidarJovanovi´c Abstract. This paper is aimed to undergraduate students of mathematics and mechanics to draw their attention to a modern and exciting field of mathematics with applications to mechanics and astronomy. We cared to keep our exposition not to go beyond the supposed knowledge of these students. ZDM Subject Classification: M55; AMS Subject Classification: 97M50. Key words and phrases: Hamilton system; completely integrable system. 1. Introduction Solving concrete mechanical and astronomical problems was one of the main mathematical tasks until the beginning of XX century (among others, see the work of Euler, Lagrange, Hamilton, Abel, Jacobi, Kovalevskaya, Chaplygin, Poincare). The majority of problems are unsolvable. Therefore, finding of solvable systems and their analysis is of a great importance. In the second half of XX century, there was a breakthrough in the research that gave a basis of a modern theory of integrable systems. Many great mathemati- cians such as P. Laks, S. Novikov, V. Arnold, J. Mozer, B. Dubrovin, V. Kozlov contributed to the development of the theory, which connects the beauty of classi- cal mechanics and differential equations with algebraic, symplectic and differential geometry, theory of Lie groups and algebras (e.g., see [1–4] and references therein). The aim of this article is to present the basic concepts of the theory of integrable systems to readers with a minimal prior knowledge in the graduate mathematics, so we shall not use a notion of a manifold, symplectic structure, etc. The most of mechanical and physical systems are modelled by Hamiltonian equations.