Wavelength and Amplitude
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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. -
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. -
Oscillating Currents
Oscillating Currents • Ch.30: Induced E Fields: Faraday’s Law • Ch.30: RL Circuits • Ch.31: Oscillations and AC Circuits Review: Inductance • If the current through a coil of wire changes, there is an induced emf proportional to the rate of change of the current. •Define the proportionality constant to be the inductance L : di εεε === −−−L dt • SI unit of inductance is the henry (H). LC Circuit Oscillations Suppose we try to discharge a capacitor, using an inductor instead of a resistor: At time t=0 the capacitor has maximum charge and the current is zero. Later, current is increasing and capacitor’s charge is decreasing Oscillations (cont’d) What happens when q=0? Does I=0 also? No, because inductor does not allow sudden changes. In fact, q = 0 means i = maximum! So now, charge starts to build up on C again, but in the opposite direction! Textbook Figure 31-1 Energy is moving back and forth between C,L 1 2 1 2 UL === UB === 2 Li UC === UE === 2 q / C Textbook Figure 31-1 Mechanical Analogy • Looks like SHM (Ch. 15) Mass on spring. • Variable q is like x, distortion of spring. • Then i=dq/dt , like v=dx/dt , velocity of mass. By analogy with SHM, we can guess that q === Q cos(ωωω t) dq i === === −−−ωωωQ sin(ωωω t) dt Look at Guessed Solution dq q === Q cos(ωωω t) i === === −−−ωωωQ sin(ωωω t) dt q i Mathematical description of oscillations Note essential terminology: amplitude, phase, frequency, period, angular frequency. You MUST know what these words mean! If necessary review Chapters 10, 15. -
Estimating Fire Properties by Remote Sensing
Estimating Fire Properties by Remote Sensing1. Philip J. Riggan USDA Forest Service Pacific Southwest Research Station 4955 Canyon Crest Drive Riverside, CA 92507 909 680 1534 [email protected] James W. Hoffman Space Instruments, Inc. 4403 Manchester Avenue, Suite 203 Encinitas, CA 92024 760 944 7001 [email protected] James A. Brass NASA Ames Research Center Moffett Federal Airfield, CA 94035 650 604 5232 [email protected] Abstract---Contemporary knowledge of the role of fire in the TABLE OF CONTENTS global environment is limited by inadequate measurements of the extent and impact of individual fires. Observations by 1. INTRODUCTION operational polar-orbiting and geostationary satellites provide an 2. ESTIMATING FIRE PROPERTIES indication of fire occurrence but are ill-suited for estimating the 3. ESTIMATES FROM TWO CHANNELS temperature, area, or radiant emissions of active wildland and 4. MULTI-SPECTRAL FIRE IMAGING agricultural fires. Simulations here of synthetic remote sensing 5. APPLICATIONS FOR FIRE MONITORING pixels comprised of observed high resolution fire data together with ash or vegetation background demonstrate that fire properties including flame temperature, fractional area, and INTRODUCTION radiant-energy flux can best be estimated from concurrent radiance measurements at wavelengths near 1.6, 3.9, and 12 µm, More than 30,000 fire observations were recorded over central Successful observations at night may be made at scales to at Brazil during August 1999 by Advanced Very High Resolution least I km for the cluster of fire data simulated here. During the Radiometers operating aboard polarorbiting satellites of the U.S. daytime, uncertainty in the composition of the background and National Oceanic and Atmospheric Administration. -
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. -
The Electromagnetic Spectrum
The Electromagnetic Spectrum Wavelength/frequency/energy MAP TAP 2003-2004 The Electromagnetic Spectrum 1 Teacher Page • Content: Physical Science—The Electromagnetic Spectrum • Grade Level: High School • Creator: Dorothy Walk • Curriculum Objectives: SC 1; Intro Phys/Chem IV.A (waves) MAP TAP 2003-2004 The Electromagnetic Spectrum 2 MAP TAP 2003-2004 The Electromagnetic Spectrum 3 What is it? • The electromagnetic spectrum is the complete spectrum or continuum of light including radio waves, infrared, visible light, ultraviolet light, X- rays and gamma rays • An electromagnetic wave consists of electric and magnetic fields which vibrates thus making waves. MAP TAP 2003-2004 The Electromagnetic Spectrum 4 Waves • Properties of waves include speed, frequency and wavelength • Speed (s), frequency (f) and wavelength (l) are related in the formula l x f = s • All light travels at a speed of 3 s 108 m/s in a vacuum MAP TAP 2003-2004 The Electromagnetic Spectrum 5 Wavelength, Frequency and Energy • Since all light travels at the same speed, wavelength and frequency have an indirect relationship. • Light with a short wavelength will have a high frequency and light with a long wavelength will have a low frequency. • Light with short wavelengths has high energy and long wavelength has low energy MAP TAP 2003-2004 The Electromagnetic Spectrum 6 MAP TAP 2003-2004 The Electromagnetic Spectrum 7 Radio waves • Low energy waves with long wavelengths • Includes FM, AM, radar and TV waves • Wavelengths of 10-1m and longer • Low frequency • Used in many -
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 -
Hydraulics Manual Glossary G - 3
Glossary G - 1 GLOSSARY OF HIGHWAY-RELATED DRAINAGE TERMS (Reprinted from the 1999 edition of the American Association of State Highway and Transportation Officials Model Drainage Manual) G.1 Introduction This Glossary is divided into three parts: · Introduction, · Glossary, and · References. It is not intended that all the terms in this Glossary be rigorously accurate or complete. Realistically, this is impossible. Depending on the circumstance, a particular term may have several meanings; this can never change. The primary purpose of this Glossary is to define the terms found in the Highway Drainage Guidelines and Model Drainage Manual in a manner that makes them easier to interpret and understand. A lesser purpose is to provide a compendium of terms that will be useful for both the novice as well as the more experienced hydraulics engineer. This Glossary may also help those who are unfamiliar with highway drainage design to become more understanding and appreciative of this complex science as well as facilitate communication between the highway hydraulics engineer and others. Where readily available, the source of a definition has been referenced. For clarity or format purposes, cited definitions may have some additional verbiage contained in double brackets [ ]. Conversely, three “dots” (...) are used to indicate where some parts of a cited definition were eliminated. Also, as might be expected, different sources were found to use different hyphenation and terminology practices for the same words. Insignificant changes in this regard were made to some cited references and elsewhere to gain uniformity for the terms contained in this Glossary: as an example, “groundwater” vice “ground-water” or “ground water,” and “cross section area” vice “cross-sectional area.” Cited definitions were taken primarily from two sources: W.B. -
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. -
X-Ray Production Compton Scattering Pair Production
Welcome back to PHY 3305 Today’s Lecture: X-ray Production Compton Scattering Pair Production Arthur Compton 1892 - 1962 Physics 3305 - Modern Physics Professor Jodi Cooley Meeting of the Texas Section of the American Physical Society When: Fri-Sat Oct 20-21 Where: UT Dallas ñ Physics majors are expected to attend, and present any research project if applicable. ñ See the email from Dr. Dalley about registration (deadline Sept 27). ñ See Michele Hill (Physics office) well before the meeting to get set up for registration and banquet fee reimbursement. Physics 3305 - Modern Physics Professor Jodi Cooley Anouncements • Reading Assignment: Chapter 3.6; 4.1 - 4.2 • Problem set 5 is due Tuesday, Sept. 26th at 12:30 pm. • Regrade for problem set 4 is due Tuesday, Sept 26th at 12:30 pm. • Midterm exam 1 covering chapters 1-2 and related material will be in class on Thursday, Sept 21st. There will be a seating chart. Physics 3305 - Modern Physics Professor Jodi Cooley Review Question 1 In a photoelectric effect experiment, if the intensity of the incident light is doubled the stopping potential will: a) Double b) Double, but only of if the light’s frequency is above the cut-off Current between the electrodes c) Half stops when the opposing potential energy difference equals the d) Remain unchanged maximum KE of the photoelectrons. KE = hf φ max − Physics 3305 - Modern Physics Professor Jodi Cooley Electrons are accelerated in television tubes through a potential difference of 10.0 kV. Find the lowest wavelength of the electromagnetic waves emitted when these electrons strike the screen.