Lecture 10. Lidar Effective Cross-Section vs. Convolution
|
|
- Leo Caldwell
- 5 years ago
- Views:
Transcription
1 Lecture 10. Lidar Effective Cross-Section vs. Convolution q Introduction q Convolution in Lineshape Determination -- Voigt Lineshape (Lorentzian Gaussian) q Effective Cross Section for Single Isotope -- Na Resonance Fluorescence Lidar q Effective Cross Section for multiple Isotopes -- K Resonance Fluorescence Lidar q Convoluted Rayleigh Doppler Lineshape -- Influence of Laser Lineshape 1
2 3 Introduction 1 0 Absorption & Fluorescence Elastic Scattering (Rayleigh) Inelastic Scattering (Raman) Here, 0, 1, and are real energy states, while 3 is a virtual state. q Resonance fluorescence contains two single-photon processes: Absorption of a photon by an atom, and spontaneous emission of another photon by the atom. Fluorescence can be quenched by collisions. q Rayleigh scattering or Raman scattering is a two-photon process, in which two photons are involved simultaneously. Therefore, Rayleigh/ Raman scattering has much smaller scattering cross-section than absorption, about & orders of magnitude smaller, respectively.
3 Atomic Absorption Lineshape Determined by Convolution + I(ω) = I 0 n( ω!,ω 0 )g Lorentzian ( ω!,ω)d ω! 3
4 Natural Linewidth Determined by Finite Radiative Lifetime Usually only the ground state can have infinite radiative lifetime, therefore infinite thin energy level. Excited states all have finite radiative lifetime, therefore finite energy level widths. 4
5 Natural Linewidth Determined by Finite Radiative Lifetime Infinite lifetime à harmonic oscillator à narrow linewidth Finite radiative lifetime à damped oscillator à natural linewidth 5
6 Atomic Absorption Cross-Section q σ abs is proportional to the probability of a single-frequency photon being absorbed by an atom: λ g σ abs (ν,ν 0 ) = A k ki 8πn g g A (ν,ν 0 ) (10.1) i where A ki is the spontaneous transition probability per unit time, i.e., the Einstein A coefficient; g k and g i are the degeneracy factors for the upper and lower energy levels k and i, respectively; λ is the wavelength; n is the refraction index, and g A is the absorption lineshape. ν and ν o are the laser frequency and the central frequency of the atomic absorption line, respectively. q For single atom, the absorption lineshape g A is determined by natural linewidth and collisional broadening, which has Lorentzian shape Δν g A (ν,ν 0 ) = g H (ν,ν 0 ) = H & π ( ν ν 0 ) + Δν H / '( where Δν H is the homogeneous broadened linewidth. ( ) ) * + (10.) Refer to our textbook Chapter 5 and references therein 6
7 Absorption Cross Section Under Doppler Effects q For many atoms in thermal equilibrium, the lineshape is the integration of the Doppler broadening (Gaussian shape) with the Lorentzian natural lineshape. The absorption lineshape g A is given by Voigt integration + g A (ω) = g Gaussian (ω 0, ω!)g Lorentzian (ω, ω!)d ω! 7
8 Absorption Cross Section Under Doppler Effects q When ignoring the Lorentzian natural linewidth (~10 MHz), the Doppler broadening (~1 GHz) dominates the lineshape. The statically averaged absorption cross section for each atomic transition line is then given by a Gaussian % [ σ abs (ν,ν o ) = σ o exp ν(1 V R /c) ν o] ( ' * (10.3) ' & σ D * ) where σ o = 1 e πσ D 4ε o m e c f ik (10.4) and σ D = σ o peak absorption cross section (m or cm ) e charge of electron; m e mass of electron ε o electric constant; c speed of light f ik absorption oscillator strength; V R radial velocity k B T Mλ 0 (10.5) σ D Doppler broadened line width k B Boltzmann constant; T temperature M mass of atom; λ o wavelength 8
9 Resonance Fluorescence Lidar: Effective Cross Section q Refer to the textbook Section for effective cross section σ eff q Resonance fluorescence contains two single-photon processes: Absorption of a photon by an atom, and spontaneous emission of another photon by the atom. q Because resonance fluorescence is isotropic, the differential backscatter cross-section dσ/dω can be replaced by the total effective scattering cross-section σ eff divided by 4π. q The total effective scattering cross-section σ eff is defined as the ratio of the average photon number scattered by an individual atoms (in all directions) to the total incident photon number per unit area. q The σ eff is determined by the convolution of the atomic absorption cross-section σ abs and the laser spectral lineshape g L (ν). q The absorption cross-section σ abs is defined as the ratio of the average absorbed single-frequency photons per atom to the total incident photons per unit area. 9
10 Na Atomic Energy Levels q Na (sodium) is probably one of the most well studied alkali species. 3 Na is the only stable isotope for Na, and it has hyperfine structures. Refer to our textbook Chapter 5 and references therein 10
11 Na Atomic Parameters 11
12 Doppler-Limited Na Spectroscopy q Doppler-broadened Na absorption cross-section is approximated as a Gaussian with rms width σ D 1 e f 6 ' σ abs (ν) = A n exp [ν n ν(1 V R ) /c)] πσ D 4ε 0 m e c n=1 ( σ D *, + (10.6) q Assume the laser lineshape is a Gaussian with rms width σ L q The effective cross-section is the convolution of the atomic absorption cross-section and the laser lineshape σ eff (ν) = where 1 πσ e e f 4ε 0 m e c 6 n=1 ' A n exp [ν n ν(1 V R /c)] * ), ( σ e + σ e = σ D + σ σ D = L (10.8) and k B T Mλ 0 (10.5) (10.7) 1
13 Effective Cross-Section q The effective cross section is a convolution of the atomic absorption cross section and the laser line shape. When the laser has finite spectral linewidth with lineshape (its intensity distribution along frequency) of g L (ν,ν L )dν =1 (10.9) 0 q The effective cross-section σ eff is given by the convolution of σ abs with the laser lineshape g L : σ eff (ν L,ν o ) = + q If the laser spectral lineshape is a Gaussian shape: 1 & g L (ν,ν L ) = exp (ν ν L ) ) ( + πσ L ' σ L * σ abs (ν,ν o )g L (ν,ν L )dν (10.11) (10.10) q then σ eff can be written as σ eff (ν L,ν 0 ) = % σ D σ 0 exp ' ν L (1 V R /c) ν 0 σ D +σ ' L & (σ D +σ L ) [ ] ( * * ) (10.1) 13
14 Effective Cross-Section for K Atoms total effective cross section x m K lidar effective cross laser FWHM=70MHz frequency offset from the line center (MHz) 15 K 00 K 75 K Atomic K energy levels Reference our textbook Chapter 5 q K (potassium) is another alkali species, and it has several stable isotopes ( 39 K, 40 K, and 41 K) with hyperfine structures. 14
15 Effective Cross-Section for K Atoms q Absorption cross section of K atom s D1 line is given by σ abs (ν) = 41 A=39. 0 / IsotopeAbdn(A) 10 1 πσ D e f 4ε 0 m e c 4 n=1 ' A n exp [ν n ν(1 V R /c)] * 0 ), 3 ( σ D + 40 Isotope abundance: % ( 39 K), % ( 40 K), 6.730% ( 41 K) Line strength: An = 5/16, 1/16, 5/16, 5/16 Oscillator strength: f, Doppler broadening: σ D q The effective total scattering cross section of K atom s D1 line is the convolution of the absorption cross section and the laser lineshape. Under the assumption of Gaussian lineshape of the laser, it is given by σ eff (ν) = where 41 A=39. 0 / IsotopeAbdn(A) 10 1 πσ e e f 4ε 0 m e c 4 n=1 ' A n exp [ν n ν(1 V R /c)] * 0 ), 3 ( σ e + 40 k B T σ e = σ D + σ σ L (11.11) and D = (11.1) Mλ 0 Refer to our textbook Chapter 5 and references therein (11.9) (11.10) 15
16 Convoluted Rayleigh Doppler Lineshape q If scattering is produced with a single-frequency laser beam and without pressure broadening, Rayleigh scattering from atmosphere molecules experiences pure Doppler effects (Doppler shift and Doppler broadening) and exhibits a Gaussian shape. q When the laser has finite spectral linewidth with lineshape, the return Rayleigh Doppler lineshape is a convolution of the pure Doppler Gaussian with the laser line shape. q If the laser spectral lineshape is a Gaussian, g L (ν,ν L ) = σ eff (ν L,ν o ) = + 1 & exp (ν ν L ) ) ( + πσ L ' σ L * σ abs (ν,ν o )g L (ν,ν L )dν where the laser spectral lineshape is normalized: g L (ν,ν L )dν =1 0 then the convolution leads to another Gaussian with RMS linewidth σ convoluted = σ D +σ L 16
Lecture 11. Classification of Lidar by Topics
Lecture 11. Classification of Lidar by Topics Effective cross section for resonance fluorescence Various lidar classifications What are topical lidars and why? Temperature techniques Wind techniques Aerosol
More informationLecture 10. Lidar Classification and Envelope Estimation
Lecture 10. Lidar Classification and Envelope Estimation Various Lidar Classifications Lidar Classification by Topics Temperature lidar technologies Wind lidar technologies Constituent lidar technologies
More informationLecture 15. Temperature Lidar (4) Doppler Techniques
Lecture 15. Temperature Lidar (4) Doppler Techniques q Doppler effects in absorption and backscatter coefficient vs. cross-section q Doppler Technique to Measure Temperature and Wind Ø Doppler Shift and
More informationLecture 06. Fundamentals of Lidar Remote Sensing (4) Physical Processes in Lidar
Lecture 06. Fundamentals of Lidar Remote Sensing (4) Physical Processes in Lidar Physical processes in lidar (continued) Doppler effect (Doppler shift and broadening) Boltzmann distribution Reflection
More informationFundamentals of Spectroscopy for Optical Remote Sensing. Course Outline 2009
Fundamentals of Spectroscopy for Optical Remote Sensing Course Outline 2009 Part I. Fundamentals of Quantum Mechanics Chapter 1. Concepts of Quantum and Experimental Facts 1.1. Blackbody Radiation and
More informationLecture 12. Temperature Lidar (1) Overview and Physical Principles
Lecture 2. Temperature Lidar () Overview and Physical Principles q Concept of Temperature Ø Maxwellian velocity distribution & kinetic energy q Temperature Measurement Techniques Ø Direct measurements:
More informationOPTI 511, Spring 2016 Problem Set 9 Prof. R. J. Jones
OPTI 5, Spring 206 Problem Set 9 Prof. R. J. Jones Due Friday, April 29. Absorption and thermal distributions in a 2-level system Consider a collection of identical two-level atoms in thermal equilibrium.
More informationLecture 13. Temperature Lidar (2) Resonance Fluorescence Doppler Tech
LIDAR REMOTE SENSING PROF. XINZHAO CHU CU-BOULDER, FALL 01 Lecture 13. Temperature Lidar () Resonance Fluorescence Doppler Tech Resonance Fluorescence Na Doppler Lidar Na Structure and Spectroscopy Scanning
More informationOPTI 511R, Spring 2018 Problem Set 10 Prof. R.J. Jones Due Thursday, April 19
OPTI 511R, Spring 2018 Problem Set 10 Prof. R.J. Jones Due Thursday, April 19 1. (a) Suppose you want to use a lens focus a Gaussian laser beam of wavelength λ in order to obtain a beam waist radius w
More informationLecture 06. Fundamentals of Lidar Remote Sensing (4) Physical Processes in Lidar
Lecture 06. Fundamentals of Lidar Remote Sensing (4) Physical Processes in Lidar Light interactions with objects (continued) Resonance fluorescence Laser induced fluorescence Doppler effect (Doppler shift
More informationLecture 05. Fundamentals of Lidar Remote Sensing (3)
Lecture 05. Fundamentals of Lidar Remote Sensing (3) Physical Processes in Lidar Overview of physical processes in lidar Light transmission through the atmosphere Light interaction with objects Elastic
More informationLecture 17. Temperature Lidar (6) Integration Technique
Lecture 17. Temperature Lidar (6) Integration Technique Doppler effects in absorption/backscatter coefficient Integration technique for temperature Searchlight integration lidar Rayleigh integration temperature
More informationLecture 18. Temperature Lidar (7) Rayleigh Doppler Technique
Lecture 18. Temperature Lidar (7) Rayleigh Doppler Technique Review of integration technique Resonance fluorescence Doppler technique vs. Rayleigh Doppler technique Rayleigh Doppler lidar High-spectral-resolution
More informationLecture 12. Temperature Lidar (2) Resonance Fluorescence Doppler Lidar
LIDAR REMOTE SENSING PROF. XINZHAO CHU CU-BOULDER, FALL 04 Lecture. Temperature Lidar () Resonance Fluorescence Doppler Lidar Resonance Fluorescence Na Doppler Lidar Na Structure and Spectroscopy Scanning
More informationMolecular spectroscopy
Molecular spectroscopy Origin of spectral lines = absorption, emission and scattering of a photon when the energy of a molecule changes: rad( ) M M * rad( ' ) ' v' 0 0 absorption( ) emission ( ) scattering
More informationAll-Optical Delay with Large Dynamic Range Using Atomic Dispersion
All-Optical Delay with Large Dynamic Range Using Atomic Dispersion M. R. Vanner, R. J. McLean, P. Hannaford and A. M. Akulshin Centre for Atom Optics and Ultrafast Spectroscopy February 2008 Motivation
More informationLecture 32. Lidar Error and Sensitivity Analysis
Lecture 3. Lidar Error and Sensitivity Analysis Introduction Accuracy in lidar measurements Precision in lidar measurements Error analysis for Na Doppler lidar Sensitivity analysis Summary 1 Errors vs.
More informationQuantum Electronics/Laser Physics Chapter 4 Line Shapes and Line Widths
Quantum Electronics/Laser Physics Chapter 4 Line Shapes and Line Widths 4.1 The Natural Line Shape 4.2 Collisional Broadening 4.3 Doppler Broadening 4.4 Einstein Treatment of Stimulated Processes Width
More informationOptical and Photonic Glasses. Lecture 31. Rare Earth Doped Glasses I. Professor Rui Almeida
Optical and Photonic Glasses : Rare Earth Doped Glasses I Professor Rui Almeida International Materials Institute For New Functionality in Glass Lehigh University Rare-earth doped glasses The lanthanide
More informationTHREE MAIN LIGHT MATTER INTERRACTION
Chapters: 3and 4 THREE MAIN LIGHT MATTER INTERRACTION Absorption: converts radiative energy into internal energy Emission: converts internal energy into radiative energy Scattering; Radiative energy is
More informationChem 442 Review of Spectroscopy
Chem 44 Review of Spectroscopy General spectroscopy Wavelength (nm), frequency (s -1 ), wavenumber (cm -1 ) Frequency (s -1 ): n= c l Wavenumbers (cm -1 ): n =1 l Chart of photon energies and spectroscopies
More informationPhoton Physics. Week 4 26/02/2013
Photon Physics Week 4 6//13 1 Classical atom-field interaction Lorentz oscillator: Classical electron oscillator with frequency ω and damping constant γ Eqn of motion: Final result: Classical atom-field
More informationATOMIC AND LASER SPECTROSCOPY
ALAN CORNEY ATOMIC AND LASER SPECTROSCOPY CLARENDON PRESS OXFORD 1977 Contents 1. INTRODUCTION 1.1. Planck's radiation law. 1 1.2. The photoelectric effect 4 1.3. Early atomic spectroscopy 5 1.4. The postulates
More informationLecture 07. Fundamentals of Lidar Remote Sensing (5) Physical Processes in Lidar
Lecture 07. Fundamentals of Lidar Remote Sensing (5) Physical Processes in Lidar Light interaction with objects (continued) Polarization of light Polarization in scattering Comparison of lidar equations
More information3: Interstellar Absorption Lines: Radiative Transfer in the Interstellar Medium. James R. Graham University of California, Berkeley
3: Interstellar Absorption Lines: Radiative Transfer in the Interstellar Medium James R. Graham University of California, Berkeley Interstellar Absorption Lines Example of atomic absorption lines Structure
More informationLecture 16. Temperature Lidar (5) Resonance Doppler Techniques
LIDAR REMOTE SENSING PROF. XINZHAO CHU CU-BOULDER, SPRING 06 Lecture 6. Temperature Lidar (5) Resonance Doppler Techniques q Resonance Fluorescence Na Doppler Lidar Ø Na Structure and Spectroscopy Ø Scanning
More informationLecture 6 - spectroscopy
Lecture 6 - spectroscopy 1 Light Electromagnetic radiation can be thought of as either a wave or as a particle (particle/wave duality). For scattering of light by particles, air, and surfaces, wave theory
More informationPhysics 221 Lecture 31 Line Radiation from Atoms and Molecules March 31, 1999
Physics 221 Lecture 31 Line Radiation from Atoms and Molecules March 31, 1999 Reading Meyer-Arendt, Ch. 20; Möller, Ch. 15; Yariv, Ch.. Demonstrations Analyzing lineshapes from emission and absorption
More informationLecture 20. Wind Lidar (2) Vector Wind Determination
Lecture 20. Wind Lidar (2) Vector Wind Determination Vector wind determination Ideal vector wind measurement VAD and DBS technique for vector wind Coherent versus incoherent Detection Doppler wind lidar
More informationPaper B2: Radiation and Matter - Basic Laser Physics
Paper B2: Radiation and Matter - Basic Laser Physics Dr Simon Hooker Michaelmas Term 2006 ii Contents 1 The Interaction of Radiation and Matter 1 1.1 Introduction.............................. 1 1.2 Radiation...............................
More informationTeaching philosophy. learn it, know it! Learn it 5-times and you know it Read (& simple question) Lecture Problem set
Learn it 5-times and you know it Read (& simple question) Lecture Problem set Teaching philosophy Review/work-problems for Mid-term exam Review/re-work for Final exam Hand in homework every Monday (1 per
More information3. Stellar Atmospheres: Opacities
3. Stellar Atmospheres: Opacities 3.1. Continuum opacity The removal of energy from a beam of photons as it passes through matter is governed by o line absorption (bound-bound) o photoelectric absorption
More informationAbsorption Line Physics
Topics: 1. Absorption line shapes 2. Absorption line strength 3. Line-by-line models Absorption Line Physics Week 4: September 17-21 Reading: Liou 1.3, 4.2.3; Thomas 3.3,4.4,4.5 Absorption Line Shapes
More informationLecture 31. Constituent Lidar (3)
Lecture 31. Constituent Lidar (3) otational Vibrational-otational (V) aman DIAL Multiwavelength DIAL Comparison of Constituent Lidar Techniques Summary for Constituent Lidar Conventional aman DIAL for
More informationLecture 2 Line Radiative Transfer for the ISM
Lecture 2 Line Radiative Transfer for the ISM Absorption lines in the optical & UV Equation of transfer Absorption & emission coefficients Line broadening Equivalent width and curve of growth Observations
More informationLaser Types Two main types depending on time operation Continuous Wave (CW) Pulsed operation Pulsed is easier, CW more useful
What Makes a Laser Light Amplification by Stimulated Emission of Radiation Main Requirements of the Laser Laser Gain Medium (provides the light amplification) Optical Resonator Cavity (greatly increase
More informationLaser Types Two main types depending on time operation Continuous Wave (CW) Pulsed operation Pulsed is easier, CW more useful
Main Requirements of the Laser Optical Resonator Cavity Laser Gain Medium of 2, 3 or 4 level types in the Cavity Sufficient means of Excitation (called pumping) eg. light, current, chemical reaction Population
More informationOptogalvanic spectroscopy of the Zeeman effect in xenon
Optogalvanic spectroscopy of the Zeeman effect in xenon Timothy B. Smith, Bailo B. Ngom, and Alec D. Gallimore ICOPS-2006 10:45, 5 Jun 06 Executive summary What are we reporting? Xe I optogalvanic spectra
More informationApplication of IR Raman Spectroscopy
Application of IR Raman Spectroscopy 3 IR regions Structure and Functional Group Absorption IR Reflection IR Photoacoustic IR IR Emission Micro 10-1 Mid-IR Mid-IR absorption Samples Placed in cell (salt)
More informationOverview of Astronomical Concepts III. Stellar Atmospheres; Spectroscopy. PHY 688, Lecture 5 Stanimir Metchev
Overview of Astronomical Concepts III. Stellar Atmospheres; Spectroscopy PHY 688, Lecture 5 Stanimir Metchev Outline Review of previous lecture Stellar atmospheres spectral lines line profiles; broadening
More informationElectron temperature is the temperature that describes, through Maxwell's law, the kinetic energy distribution of the free electrons.
10.3.1.1 Excitation and radiation of spectra 10.3.1.1.1 Plasmas A plasma of the type occurring in spectrochemical radiation sources may be described as a gas which is at least partly ionized and contains
More informationLecture 2 Interstellar Absorption Lines: Line Radiative Transfer
Lecture 2 Interstellar Absorption Lines: Line Radiative Transfer 1. Atomic absorption lines 2. Application of radiative transfer to absorption & emission 3. Line broadening & curve of growth 4. Optical/UV
More informationSpontaneous Emission, Stimulated Emission, and Absorption
Chapter Six Spontaneous Emission, Stimulated Emission, and Absorption In this chapter, we review the general principles governing absorption and emission of radiation by absorbers with quantized energy
More informationEarly time dynamics of strongly coupled ultracold neutral Ca + and Ca 2+ plasmas
Early time dynamics of strongly coupled ultracold neutral Ca + and Ca 2+ plasmas M. Lyon and S. D. Bergeson Department of Physics and Astronomy, Brigham Young University, Provo, UT 84602, USA For interacting
More information1 Radiative transfer etc
Radiative transfer etc Last time we derived the transfer equation dτ ν = S ν I v where I ν is the intensity, S ν = j ν /α ν is the source function and τ ν = R α ν dl is the optical depth. The formal solution
More informationReflection = EM strikes a boundary between two media differing in η and bounces back
Reflection = EM strikes a boundary between two media differing in η and bounces back Incident ray θ 1 θ 2 Reflected ray Medium 1 (air) η = 1.00 Medium 2 (glass) η = 1.50 Specular reflection = situation
More information1 Interaction of radiation and matter
Physics department Modern Optics Interaction of radiation and matter To describe the interaction of radiation and matter we seek an expression for field induced transition rates W i j between energi levels
More information1. Transition dipole moment
1. Transition dipole moment You have measured absorption spectra of aqueous (n=1.33) solutions of two different chromophores (A and B). The concentrations of the solutions were the same. The absorption
More informationLaser Physics OXFORD UNIVERSITY PRESS SIMON HOOKER COLIN WEBB. and. Department of Physics, University of Oxford
Laser Physics SIMON HOOKER and COLIN WEBB Department of Physics, University of Oxford OXFORD UNIVERSITY PRESS Contents 1 Introduction 1.1 The laser 1.2 Electromagnetic radiation in a closed cavity 1.2.1
More informationSodium Guidestar Return From Broad CW Sources. CfAO Fall Workshop Comments COVER SLIDE
Sodium Guidestar Return From Broad CW Sources CfAO Fall Workshop Comments Paul Hillman Starfire Optical Range Directed Energy Directorate Air Force Research Laboratory COVER SLIDE The following slide presentation
More information5. Atomic radiation processes
5. Atomic radiation processes Einstein coefficients for absorption and emission oscillator strength line profiles: damping profile, collisional broadening, Doppler broadening continuous absorption and
More informationModel Answer (Paper code: AR-7112) M. Sc. (Physics) IV Semester Paper I: Laser Physics and Spectroscopy
Model Answer (Paper code: AR-7112) M. Sc. (Physics) IV Semester Paper I: Laser Physics and Spectroscopy Section I Q1. Answer (i) (b) (ii) (d) (iii) (c) (iv) (c) (v) (a) (vi) (b) (vii) (b) (viii) (a) (ix)
More informationRb, which had been compressed to a density of 1013
Modern Physics Study Questions for the Spring 2018 Departmental Exam December 3, 2017 1. An electron is initially at rest in a uniform electric field E in the negative y direction and a uniform magnetic
More informationAnswers to questions on exam in laser-based combustion diagnostics on March 10, 2006
Answers to questions on exam in laser-based combustion diagnostics on March 10, 2006 1. Examples of advantages and disadvantages with laser-based combustion diagnostic techniques: + Nonintrusive + High
More informationPart IV. Fundamentals of Laser Spectroscopy
IV 1 Part IV. Fundamentals of Laser Spectroscopy We have gone through the fundamentals of atomic spectroscopy and molecular spectroscopy, in which we emphasize the quantum physics and principles that govern
More informationElectromagnetic Spectra. AST443, Lecture 13 Stanimir Metchev
Electromagnetic Spectra AST443, Lecture 13 Stanimir Metchev Administrative Homework 2: problem 5.4 extension: until Mon, Nov 2 Reading: Bradt, chapter 11 Howell, chapter 6 Tenagra data: see bottom of Assignments
More informationNon-stationary States and Electric Dipole Transitions
Pre-Lab Lecture II Non-stationary States and Electric Dipole Transitions You will recall that the wavefunction for any system is calculated in general from the time-dependent Schrödinger equation ĤΨ(x,t)=i
More informationRadiation in the Earth's Atmosphere. Part 1: Absorption and Emission by Atmospheric Gases
Radiation in the Earth's Atmosphere Part 1: Absorption and Emission by Atmospheric Gases Electromagnetic Waves Electromagnetic waves are transversal. Electric and magnetic fields are perpendicular. In
More informationAbsorption and scattering
Absorption and scattering When a beam of radiation goes through the atmosphere, it encounters gas molecules, aerosols, cloud droplets, and ice crystals. These objects perturb the radiation field. Part
More informationLecture 30. Lidar Error and Sensitivity Analysis
Lecture 30. Lidar Error and Sensitivity Analysis q Introduction q Accuracy versus Precision q Accuracy in lidar measurements q Precision in lidar measurements q Propagation of errors vs. differential method
More informationSpectral Line Shapes. Line Contributions
Spectral Line Shapes Line Contributions The spectral line is termed optically thin because there is no wavelength at which the radiant flux has been completely blocked. The opacity of the stellar material
More informationWhat Makes a Laser Light Amplification by Stimulated Emission of Radiation Main Requirements of the Laser Laser Gain Medium (provides the light
What Makes a Laser Light Amplification by Stimulated Emission of Radiation Main Requirements of the Laser Laser Gain Medium (provides the light amplification) Optical Resonator Cavity (greatly increase
More informationPhysics 221B Spring 2012 Notes 42 Scattering of Radiation by Matter
Physics 221B Spring 2012 Notes 42 Scattering of Radiation by Matter 1. Introduction In the previous set of Notes we treated the emission and absorption of radiation by matter. In these Notes we turn to
More informationSpectral Resolution. Spectral resolution is a measure of the ability to separate nearby features in wavelength space.
Spectral Resolution Spectral resolution is a measure of the ability to separate nearby features in wavelength space. R, minimum wavelength separation of two resolved features. Delta lambda often set to
More informationRadiation Transport in a Gas
Radiation Transport in a Gas By analogy to a particle gas, define a photon distribution function by, f ν ν, Ω; r, t)dvdωd r = Number of photons of a frequency in ν, ν + dν), in a volume at rd r), with
More informationLaser Detection Techniques
Laser Detection Techniques K.-H. Gericke Institute for Physical Chemistry University Braunschweig E 2 E 1 = hn, λ = c /n Lambert-Beer Law Transmittance of the sample:: T = I / I 0 T = e -snl = e -α, where
More informationAy Fall 2004 Lecture 6 (given by Tony Travouillon)
Ay 122 - Fall 2004 Lecture 6 (given by Tony Travouillon) Stellar atmospheres, classification of stellar spectra (Many slides c/o Phil Armitage) Formation of spectral lines: 1.excitation Two key questions:
More informationDiffuse Interstellar Medium
Diffuse Interstellar Medium Basics, velocity widths H I 21-cm radiation (emission) Interstellar absorption lines Radiative transfer Resolved Lines, column densities Unresolved lines, curve of growth Abundances,
More informationSpectral Broadening Mechanisms
Spectral Broadening Mechanisms Lorentzian broadening (Homogeneous) Gaussian broadening (Inhomogeneous, Inertial) Doppler broadening (special case for gas phase) The Fourier Transform NC State University
More informationLecture 4* Inherent optical properties, IOP Theory. Loss due to absorption. IOP Theory 12/2/2008
Lecture 4* Inherent optical properties, part I IOP Theory What properties of a medium affect the radiance field as it propagate through it? 1. Sinks of photons (absorbers) 2. Sources of photons (internal
More informationLasers & Holography. Ulrich Heintz Brown University. 4/5/2016 Ulrich Heintz - PHYS 1560 Lecture 10 1
Lasers & Holography Ulrich Heintz Brown University 4/5/2016 Ulrich Heintz - PHYS 1560 Lecture 10 1 Lecture schedule Date Topic Thu, Jan 28 Introductory meeting Tue, Feb 2 Safety training Thu, Feb 4 Lab
More informationThe Interaction of Light and Matter: α and n
The Interaction of Light and Matter: α and n The interaction of light and matter is what makes life interesting. Everything we see is the result of this interaction. Why is light absorbed or transmitted
More informationChemistry Instrumental Analysis Lecture 17. Chem 4631
Chemistry 4631 Instrumental Analysis Lecture 17 Introduction to Optical Atomic Spectrometry From molecular to elemental analysis there are three major techniques used for elemental analysis: Optical spectrometry
More informationThe Laboratory Measurement of Pressure Broadening Parameter for Atmospheric Remote Sensing
The Laboratory Measurement of Pressure Broadening Parameter for Atmospheric Remote Sensing YAMADA Masumi, KASAI Yasuko, and AMANO Takayoshi The upcoming JEM/SMILES (Superconducting Submillimeter-wave Limb
More informationA few Experimental methods for optical spectroscopy Classical methods Modern methods. Remember class #1 Generating fast LASER pulses
A few Experimental methods for optical spectroscopy Classical methods Modern methods Shorter class Remember class #1 Generating fast LASER pulses, 2017 Uwe Burghaus, Fargo, ND, USA W. Demtröder, Laser
More informationMEFT / Quantum Optics and Lasers. Suggested problems Set 4 Gonçalo Figueira, spring 2015
MEFT / Quantum Optics and Lasers Suggested problems Set 4 Gonçalo Figueira, spring 05 Note: some problems are taken or adapted from Fundamentals of Photonics, in which case the corresponding number is
More informationLecture 2 Solutions to the Transport Equation
Lecture 2 Solutions to the Transport Equation Equation along a ray I In general we can solve the static transfer equation along a ray in some particular direction. Since photons move in straight lines
More information24/ Rayleigh and Raman scattering. Stokes and anti-stokes lines. Rotational Raman spectroscopy. Polarizability ellipsoid. Selection rules.
Subject Chemistry Paper No and Title Module No and Title Module Tag 8/ Physical Spectroscopy 24/ Rayleigh and Raman scattering. Stokes and anti-stokes lines. Rotational Raman spectroscopy. Polarizability
More informationATMO/OPTI 656b Spring 2009
Nomenclature and Definition of Radiation Quantities The various Radiation Quantities are defined in Table 2-1. Keeping them straight is difficult and the meanings may vary from textbook to textbook. I
More informationThe last 2 million years.
Lecture 5: Earth Climate History - Continued Ice core records from both Greenland and Antarctica have produced a remarkable record of climate during the last 450,000 years. Trapped air bubbles provide
More informationhigh temp ( K) Chapter 20: Atomic Spectroscopy
high temp (2000-6000K) Chapter 20: Atomic Spectroscopy 20-1. An Overview Most compounds Atoms in gas phase high temp (2000-6000K) (AES) (AAS) (AFS) sample Mass-to-charge (ICP-MS) Atomic Absorption experiment
More informationAsymmetric Deviation of the Cross Section from the Lorentzian Around Ly Alpha
Asymmetric Deviation of the Cross Section from the Lorentzian Around Ly Alpha Hee-Won Lee in collaboration with Seok-Jun Chang Department of Physics and Astronomy, Sejong University, Seoul, Korea March
More informationX-ray Radiation, Absorption, and Scattering
X-ray Radiation, Absorption, and Scattering What we can learn from data depend on our understanding of various X-ray emission, scattering, and absorption processes. We will discuss some basic processes:
More informationSaturation Absorption Spectroscopy of Rubidium Atom
Saturation Absorption Spectroscopy of Rubidium Atom Jayash Panigrahi August 17, 2013 Abstract Saturated absorption spectroscopy has various application in laser cooling which have many relevant uses in
More informationChapter 8: Introduction to Atomic Spectrometry
Chapter 8: Introduction to Atomic Spectrometry Read: pp. 215 228 Problems: 2,4,5,6,9 Why choose atomic spectrometry? Three major types of spectrometric methods for identifying elements present in matter:
More informationModule 4 : Third order nonlinear optical processes. Lecture 28 : Inelastic Scattering Processes. Objectives
Module 4 : Third order nonlinear optical processes Lecture 28 : Inelastic Scattering Processes Objectives In this lecture you will learn the following Light scattering- elastic and inelastic-processes,
More informationThe Curve of Growth of the Equivalent Width
9 The Curve of Growth of the Equivalent Width Spectral lines are broadened from the transition frequency for a number of reasons. Thermal motions and turbulence introduce Doppler shifts between atoms and
More informationATMO 551a Fall Resonant Electromagnetic (EM) Interactions in Planetary atmospheres. Electron transition between different electron orbits
Resonant Electromagnetic (EM) Interactions in Planetary atmospheres There are three classes of energy states that interact with EM radiation that we are interested in to understand how light (EM radiation)
More informationWavelength Frequency Measurements
Wavelength Frequency Measurements Frequency: - unit to be measured most accurately in physics - frequency counters + frequency combs (gear wheels) - clocks for time-frequency Wavelength: - no longer fashionable
More informationLaser cooling and trapping
Laser cooling and trapping William D. Phillips wdp@umd.edu Physics 623 14 April 2016 Why Cool and Trap Atoms? Original motivation and most practical current application: ATOMIC CLOCKS Current scientific
More informationLecture Notes on Radiation Transport for Spectroscopy
Lecture Notes on Radiation Transport for Spectroscopy ICTP-IAEA School on Atomic Processes in Plasmas 27 February 3 March 217 Trieste, Italy LLNL-PRES-668311 This work was performed under the auspices
More informationThe interaction of light and matter
Outline The interaction of light and matter Denise Krol (Atom Optics) Photon physics 014 Lecture February 14, 014 1 / 3 Elementary processes Elementary processes 1 Elementary processes Einstein relations
More informationR O Y G B V. Spin States. Outer Shell Electrons. Molecular Rotations. Inner Shell Electrons. Molecular Vibrations. Nuclear Transitions
Spin States Molecular Rotations Molecular Vibrations Outer Shell Electrons Inner Shell Electrons Nuclear Transitions NMR EPR Microwave Absorption Spectroscopy Infrared Absorption Spectroscopy UV-vis Absorption,
More informationSmall Signal Gain in DPAL Systems
Physical Sciences Inc. VG11-010 Small Signal Gain in DPAL Systems Kristin L. Galbally-Kinney, Daniel L. Maser, William J. Kessler, Wilson T. Rawlins, and Steven J. Davis 20 New England Business Center
More informationSpectroscopy Applied to Selected Examples
Spectroscopy Applied to Selected Examples Radial Velocities Exoplanets λ obs λ rest λ rest = Δλ λ rest v c for z
More informationInteraction of Molecules with Radiation
3 Interaction of Molecules with Radiation Atoms and molecules can exist in many states that are different with respect to the electron configuration, angular momentum, parity, and energy. Transitions between
More informationSpectral Broadening Mechanisms. Broadening mechanisms. Lineshape functions. Spectral lifetime broadening
Spectral Broadening echanisms Lorentzian broadening (Homogeneous) Gaussian broadening (Inhomogeneous, Inertial) Doppler broadening (special case for gas phase) The Fourier Transform NC State University
More informationToday: general condition for threshold operation physics of atomic, vibrational, rotational gain media intro to the Lorentz model
Today: general condition for threshold operation physics of atomic, vibrational, rotational gain media intro to the Lorentz model Laser operation Simplified energy conversion processes in a laser medium:
More informationThe Formation of Spectral Lines. I. Line Absorption Coefficient II. Line Transfer Equation
The Formation of Spectral Lines I. Line Absorption Coefficient II. Line Transfer Equation Line Absorption Coefficient Main processes 1. Natural Atomic Absorption 2. Pressure Broadening 3. Thermal Doppler
More informationTHEORETICAL PROBLEM 2 DOPPLER LASER COOLING AND OPTICAL MOLASSES
THEORETICAL PROBLEM 2 DOPPLER LASER COOLING AND OPTICAL MOLASSES The purpose of this problem is to develop a simple theory to understand the so-called laser cooling and optical molasses phenomena. This
More information