Nondirectional and Directional Wave Data Analysis Procedures
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Glossary Physics (I-Introduction)
1 Glossary Physics (I-introduction) - Efficiency: The percent of the work put into a machine that is converted into useful work output; = work done / energy used [-]. = eta In machines: The work output of any machine cannot exceed the work input (<=100%); in an ideal machine, where no energy is transformed into heat: work(input) = work(output), =100%. Energy: The property of a system that enables it to do work. Conservation o. E.: Energy cannot be created or destroyed; it may be transformed from one form into another, but the total amount of energy never changes. Equilibrium: The state of an object when not acted upon by a net force or net torque; an object in equilibrium may be at rest or moving at uniform velocity - not accelerating. Mechanical E.: The state of an object or system of objects for which any impressed forces cancels to zero and no acceleration occurs. Dynamic E.: Object is moving without experiencing acceleration. Static E.: Object is at rest.F Force: The influence that can cause an object to be accelerated or retarded; is always in the direction of the net force, hence a vector quantity; the four elementary forces are: Electromagnetic F.: Is an attraction or repulsion G, gravit. const.6.672E-11[Nm2/kg2] between electric charges: d, distance [m] 2 2 2 2 F = 1/(40) (q1q2/d ) [(CC/m )(Nm /C )] = [N] m,M, mass [kg] Gravitational F.: Is a mutual attraction between all masses: q, charge [As] [C] 2 2 2 2 F = GmM/d [Nm /kg kg 1/m ] = [N] 0, dielectric constant Strong F.: (nuclear force) Acts within the nuclei of atoms: 8.854E-12 [C2/Nm2] [F/m] 2 2 2 2 2 F = 1/(40) (e /d ) [(CC/m )(Nm /C )] = [N] , 3.14 [-] Weak F.: Manifests itself in special reactions among elementary e, 1.60210 E-19 [As] [C] particles, such as the reaction that occur in radioactive decay. -
Test of Self-Organization in Beach Cusp Formation Giovanni Coco,1 T
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 108, NO. C3, 3101, doi:10.1029/2002JC001496, 2003 Test of self-organization in beach cusp formation Giovanni Coco,1 T. K. Burnet, and B. T. Werner Complex Systems Laboratory, Cecil and Ida Green Institute of Geophysics and Planetary Physics, University of California, San Diego, La Jolla, California, USA Steve Elgar Woods Hole Oceanographic Institution, Woods Hole, Massachusetts, USA Received 4 June 2002; revised 6 November 2002; accepted 13 November 2002; published 29 March 2003. [1] Field observations of swash flow patterns and morphology change are consistent with the hypothesis that beach cusps form by self-organization, wherein positive feedback between swash flow and developing morphology causes initial development of the pattern and negative feedback owing to circulation of flow within beach cusp bays causes pattern stabilization. The self-organization hypothesis is tested using measurements from three experiments on a barrier island beach in North Carolina. Beach cusps developed after the beach was smoothed by a storm and after existing beach cusps were smoothed by a bulldozer. Swash front motions were recorded on video during daylight hours, and morphology was measured by surveying at 3–4 hour intervals. Three signatures of self- organization were observed in all experiments. First, time lags between swash front motions in beach cusp bays and horns increase with increasing relief, representing the effect of morphology on flow. Second, differential erosion between bays and horns initially increases with increasing time lag, representing the effect of flow on morphology change because positive feedback causes growth of beach cusps. Third, after initial growth, differential erosion decreases with increasing time lag, representing the onset of negative feedback that stabilizes beach cusps. -
Part II-1 Water Wave Mechanics
Chapter 1 EM 1110-2-1100 WATER WAVE MECHANICS (Part II) 1 August 2008 (Change 2) Table of Contents Page II-1-1. Introduction ............................................................II-1-1 II-1-2. Regular Waves .........................................................II-1-3 a. Introduction ...........................................................II-1-3 b. Definition of wave parameters .............................................II-1-4 c. Linear wave theory ......................................................II-1-5 (1) Introduction .......................................................II-1-5 (2) Wave celerity, length, and period.......................................II-1-6 (3) The sinusoidal wave profile...........................................II-1-9 (4) Some useful functions ...............................................II-1-9 (5) Local fluid velocities and accelerations .................................II-1-12 (6) Water particle displacements .........................................II-1-13 (7) Subsurface pressure ................................................II-1-21 (8) Group velocity ....................................................II-1-22 (9) Wave energy and power.............................................II-1-26 (10)Summary of linear wave theory.......................................II-1-29 d. Nonlinear wave theories .................................................II-1-30 (1) Introduction ......................................................II-1-30 (2) Stokes finite-amplitude wave theory ...................................II-1-32 -
Surface Waves NOAA Tech Refresh 20 Jan 2012 Kipp Shearman, OSU Outline
Surface Waves NOAA Tech Refresh 20 Jan 2012 Kipp Shearman, OSU Outline – Surface winds • Wind stress • Beaufort scale • Buoy measurements – Surface Gravity Waves • Wave characteristics • Deep/Shallow water waves • Generation • Modeling January mean atmospheric circulation and surface winds Fig 2.3 Ocean Circulation July mean atmospheric circulation and surface winds Fig 2.3 Ocean Circulation Wind Forcing at the Ocean Surface • Wind-forcing can generate currents and waves, as wind transfers some of its momentum into the ocean" •! Wind acts via friction at the surface: wind stress τ# " # # Stresses have units of N/m2, (force/area), like pressure.# Stresses are forces parallel to a surface, pressure is force perpendicular to the surface." •! Force/Area depends on the square of the wind speed u, and it points in the same direction as the wind: " 2 τ ∝ u C drag coefficient 1.4 10−3 " D = ≈ × C u u 3 τ = ρa D density of air 1.3 kg / m " ρa = ≈ Example: 20kt wind $ 10 m/s → 0.18 N/m2 = 1.8 dyne/cm2" 0, <1 knot 1, 1-3 knots 2, 4-6 knots 3, 7-10 knots 4, 11-17 knots 5, 17-21 knots 6, 22-27 knots 7, 28-33 knots 8, 33-40 knots 9, 41-47 knots 10, 48-55 knots 11, 56-63 knots Beaufort scale, after http://www.geology.wmich.edu/Kominz/windwater.html Beaufort scale still provides climatological data Look at buoy winds off oregon coast. http://www.wrh.noaa.gov/pqr/ Outline –! Surface winds •! Wind stress •! Beaufort scale •! Buoy measurements –! Surface Gravity Waves •! Wave characteristics •! Deep/Shallow water waves •! Generation •! Modeling Wave Propagation • Wave Period T: time between arrival of successive wave crests at a given place • Wave Length L: distance between successive wave crests • Wave (phase) speed c: cp = L / T By definition, the definition of cp is valid for all Segar waves. -
Chapter 16: Fourier Series
Chapter 16: Fourier Series 16.1 Fourier Series Analysis: An Overview A periodic function can be represented by an infinite sum of sine and cosine functions that are harmonically related: Ϧ ͚ʚͨʛ Ɣ ͕1 ƍ ȕ ͕) cos ͢!*ͨ ƍ ͖) sin ͢!*ͨ Fourier Coefficients: are)Ͱͥ calculated from ͕1; ͕); ͖) ͚ʚͨʛ Fundamental Frequency: ͦ_ where multiples of this frequency are called !* Ɣ ; ͢! * harmonic frequencies Conditions that ensure that f(t) can be expressed as a convergent Fourier series: (Dirichlet’s conditions) 1. f(t) be single-values 2. f(t) have a finite number of discontinuities in the periodic interval 3. f(t) have a finite number of maxima and minima in the periodic interval 4. the integral /tͮ exists Ȅ/ |͚ʚͨʛ|ͨ͘; t These are sufficient conditions not necessary conditions; therefore if these conditions exist the functions can be expressed as a Fourier series. However if the conditions are not met the function may still be expressible as a Fourier series. 16.2 The Fourier Coefficients Defining the Fourier coefficients: /tͮ 1 ͕1 Ɣ ǹ ͚ʚͨʛͨ͘ ͎ /t /tͮ 2 ͕& Ɣ ǹ ͚ʚͨʛ cos ͟!*ͨ ͨ͘ ͎ /t /tͮ 2 ͖& Ɣ ǹ ͚ʚͨʛ sin ͟!*ͨ ͨ͘ ͎ / t Example 16.1 Find the Fourier series for the periodic waveform shown. Assessment problems 16.1 & 16.2 ECEN 2633 Spring 2011 Page 1 of 5 16.3 The Effects of Symmetry on the Fourier Coefficients Four types of symmetry used to simplify Fourier analysis 1. Even-function symmetry 2. Odd-function symmetry 3. -
Coating Provides Infrared Camouflage
COURTESY OF PATRICK RONEY, ALIREZA SHAHSAFI AND MIKHAIL KATS February 1, 2020 Coating Provides Infrared Camouflage February 1, 2020 Coating Provides Infrared Camouflage About this Guide This Guide, based on the Science News article “Coating provides infrared camouflage,” asks students to explore the physics and potential technological applications of a material, discuss the various types of electromagnetic radiation, analyze infrared images and research how infrared imaging is used across a range of fields. This Guide includes: Article-based Comprehension Q&A — These questions, based on the Science News article “Coating provides infrared camouflage,” Readability: 12.7, ask students to explore the physics and potential technological applications of a material. Related standards include NGSS-DCI: HS-PS4; HS-PS3; HS-PS2; HS-ETS1. Student Comprehension Worksheet — These questions are formatted so it’s easy to print them out as a worksheet. Cross-curricular Discussion Q&A — Students will watch a NASA video about the electromagnetic spectrum to learn about properties of the various types of radiation. Then, students will explore and discuss technologies that use specific types of electromagnetic radiation. Related standards include NGSS- DCI: HS-PS4; HS-PS3; HS-PS2. Student Discussion Worksheet — These questions are formatted so it’s easy to print them out as a worksheet. Activity: Seeing in Infrared Summary: In this activity, students will analyze infrared images and then explore how infrared imaging is used across a range of fields of work. Skills include researching, evaluating, synthesizing and presenting information. Related standards include NGSS-DCI: HS-PS4; HS-PS3; HS-ETS1. Approximate class time: 1 class period to complete the discussion, research, presentations and debriefing as a class. -
Sound and Vision: Visualization of Music with a Soap Film, and the Physics Behind It C Gaulon, C Derec, T Combriat, P Marmottant, F Elias
Sound and Vision: Visualization of music with a soap film, and the physics behind it C Gaulon, C Derec, T Combriat, P Marmottant, F Elias To cite this version: C Gaulon, C Derec, T Combriat, P Marmottant, F Elias. Sound and Vision: Visualization of music with a soap film, and the physics behind it. 2017. hal-01487166 HAL Id: hal-01487166 https://hal.archives-ouvertes.fr/hal-01487166 Preprint submitted on 11 Mar 2017 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Sound and Vision: Visualization of music with a soap film, and the physics behind it C. Gaulon1, C. Derec1, T. Combriat2, P. Marmottant2 and F. Elias1;3 1 Laboratoire Mati`ere et Syst`emesComplexes UMR 7057, Universit´eParis Diderot, Sorbonne Paris Cit´e,CNRS, F-75205 Paris, France 2 Laboratoire Interdisciplinaire de Physique LIPhy, Universit´eGrenoble Alpes and CNRS UMR 5588 3 Sorbonne Universit´es,UPMC Univ Paris 06, 4 place Jussieu, 75252 PARIS cedex 05, France fl[email protected] Abstract A vertical soap film, freely suspended at the end of a tube, is vi- brated by a sound wave that propagates in the tube. -
Guidance for Flood Risk Analysis and Mapping
Guidance for Flood Risk Analysis and Mapping Coastal Notations, Acronyms, and Glossary of Terms May 2016 Requirements for the Federal Emergency Management Agency (FEMA) Risk Mapping, Assessment, and Planning (Risk MAP) Program are specified separately by statute, regulation, or FEMA policy (primarily the Standards for Flood Risk Analysis and Mapping). This document provides guidance to support the requirements and recommends approaches for effective and efficient implementation. Alternate approaches that comply with all requirements are acceptable. For more information, please visit the FEMA Guidelines and Standards for Flood Risk Analysis and Mapping webpage (www.fema.gov/guidelines-and-standards-flood-risk-analysis-and- mapping). Copies of the Standards for Flood Risk Analysis and Mapping policy, related guidance, technical references, and other information about the guidelines and standards development process are all available here. You can also search directly by document title at www.fema.gov/library. Coastal Notation, Acronyms, and Glossary of Terms May 2016 Guidance Document 66 Page i Document History Affected Section or Date Description Subsection Initial version of new transformed guidance. The content was derived from the Guidelines and Specifications for Flood Hazard Mapping Partners, Procedure Memoranda, First Publication May 2016 and/or Operating Guidance documents. It has been reorganized and is being published separately from the standards. Coastal Notation, Acronyms, and Glossary of Terms May 2016 Guidance Document 66 -
On the Transport of Energy in Water Waves
On The Transport Of Energy in Water Waves Marshall P. Tulin Professor Emeritus, UCSB [email protected] Abstract Theory is developed and utilized for the calculation of the separate transport of kinetic, gravity potential, and surface tension energies within sinusoidal surface waves in water of arbitrary depth. In Section 1 it is shown that each of these three types of energy constituting the wave travel at different speeds, and that the group velocity, cg, is the energy weighted average of these speeds, depth and time averaged in the case of the kinetic energy. It is shown that the time averaged kinetic energy travels at every depth horizontally either with (deep water), or faster than the wave itself, and that the propagation of a sinusoidal wave is made possible by the vertical transport of kinetic energy to the free surface, where it provides the oscillating balance in surface energy just necessary to allow the propagation of the wave. The propagation speed along the surface of the gravity potential energy is null, while the surface tension energy travels forward along the wave surface everywhere at twice the wave velocity, c. The flux of kinetic energy when viewed traveling with a wave provides a pattern of steady flux lines which originate and end on the free surface after making vertical excursions into the wave, even to the bottom, and these are calculated. The pictures produced in this way provide immediate insight into the basic mechanisms of wave motion. In Section 2 the modulated gravity wave is considered in deep water and the balance of terms involved in the propagation of the energy in the wave group is determined; it is shown again that vertical transport of kinetic energy to the surface is fundamental in allowing the propagation of the modulation, and in determining the well known speed of the modulation envelope, cg. -
Modes of Wave-Chaotic Dielectric Resonators
Modes of wave-chaotic dielectric resonators H. E. Tureci, H. G. L. Schwefel, and A. Douglas Stone Department of Applied Physics, Yale University, New Haven, CT 06520, USA Ph. Jacquod D¶epartement de Physique Th¶eorique, Universit¶e de Geneve, CH-1211 Geneve 4, Switzerland (Dated: October 29, 2003) Dielectric optical micro-resonators and micro-lasers represent a realization of a wave-chaotic sys- tem, where the lack of symmetry in the resonator shape leads to non-integrable ray dynamics. Modes of such resonators display a rich spatial structure, and cannot be classi¯ed through mode indices which would require additional constants of motion in the ray dynamics. Understanding and controlling the emission properties of such resonators requires the investigation of the correspon- dence between classical phase space structures of the ray motion inside the resonator and resonant solutions of the wave equations. We ¯rst discuss the breakdown of the conventional eikonal approx- imation in the short wavelength limit, and motivate the use of phase-space ray tracing and phase space distributions. Next, we introduce an e±cient numerical method to calculate the quasi-bound modes of dielectric resonators, which requires only two diagonalizations per N states, where N is approximately equal to the number of half-wavelengths along the perimeter. The relationship be- tween classical phase space structures and modes is displayed via the Husimi projection technique. Observables related to the emission pattern of the resonator are calculated with high e±ciency. I. INTRODUCTION A promising approach to making compact and high-Q optical resonators is to base them on \totally internally reected” modes of dielectric micro-structures. -
Pattern Formation, Wave Propagation and Stability in Conservation Laws with Slow Diffusion and Fast Reaction
Pattern Formation, Wave Propagation and Stability in Conservation Laws with Slow Diffusion and Fast Reaction Haitao Fan ∗ and Hailiang Liu † Contents 1 Introduction 2 2 Convergence and pattern formation 4 3 Propagation speed of fronts 7 3.1Lawofmotionoffronts........................................................ 7 3.2LaxShockcondition.......................................................... 8 3.3Variationalformula.......................................................... 10 4 Existence and stability of layer solutions 11 4.1Connectingorbit............................................................ 11 4.2 Dynamic Stability and Approaching to a Wave . 15 5 Existence and Structure of the limit lim→0+ u (x, t) 19 Abstract The limiting behavior of the solution of scalar conservation laws with slow diffu- sion and fast bistable reaction is considered. In a short time the solution develops transition patterns connected by shock layers and rarefaction layers, when the initial data has finitely many monotone pieces. The existence and uniqueness of the front profiles for both shock layers and rarefaction layers are established. A variational characterization of the wave speed of these profiles is derived. These profiles are shown to be stable. Furthermore, it is proved that solutions with monotone intimal data approach to shock layer or rarefaction layer waves as time goes to infinity. Key Words: Reaction-diffusion-convection equations, Pattern formation, transition fronts, asymptotic stability. AMS subject classification: 35K65; 35K57; 41A60. Date: August 14, 2001 ∗Department of Mathematics, Georgetown University Washington, DC 20057. Email: [email protected]. Web: http://www.georgetown.edu/faculty/fanh †Department of Mathematics, University of California, Los Angeles, CA 90095-1555. Email: [email protected]. Web: http://www.math.ucla.edu/∼hliu 1 1 Introduction Front propagation and interface motion occur in many scientific areas such as chemical kinetics, combustion, biology, transport in porous media, geometry and image process- ing. -
The Emergence of Chaos in Quantum Mechanics
S S symmetry Article The Emergence of Chaos in Quantum Mechanics Emilio Fiordilino Dipartimento di Fisica e Chimica—Emilio Segrè, Università degli Studi di Palermo, Via Archirafi 36, 90123 Palermo, Italy; emilio.fi[email protected] Received: 4 April 2020; Accepted: 7 May 2020; Published: 8 May 2020 Abstract: Nonlinearity in Quantum Mechanics may have extrinsic or intrinsic origins and is a liable route to a chaotic behaviour that can be of difficult observations. In this paper, we propose two forms of nonlinear Hamiltonian, which explicitly depend upon the phase of the wave function and produce chaotic behaviour. To speed up the slow manifestation of chaotic effects, a resonant laser field assisting the time evolution of the systems causes cumulative effects that might be revealed, at least in principle. The nonlinear Schrödinger equation is solved within the two-state approximation; the solution displays features with characteristics similar to those found in chaotic Classical Mechanics: sensitivity on the initial state, dense power spectrum, irregular filling of the Poincaré map and exponential separation of the trajectories of the Bloch vector s in the Bloch sphere. Keywords: nonlinear Schrödinger equation; chaos; high order harmonic generation 1. Introduction The theory of chaos gained the role of a new paradigm of Science for explaining a large variety of phenomena by introducing the concept of unpredictability within the perimeter of Classical Physics. Chaos occurs when the trajectory of a particle is sensitive to the initial conditions and is produced by a nonlinear equation of motion [1]. As examples we quote the equation for the Duffing oscillator (1918) 3 mx¨ + gx˙ + rx = F cos(wLt) (1) or its elaborated form 3 mx¨ + gx˙ + kx + rx = F cos(wLt) (2) that are among the most studied equation of mathematical physics [1,2] and, as far as we know, cannot be analytically solved.