High Altitude Observatory (HAO) – National Center for Atmospheric Research (NCAR) The National Center for Atmospheric Research is operated by the University.

Slides:



Advertisements
Similar presentations
Optics, Eugene Hecht, Chpt. 8
Advertisements

II Escuela de Optica Biomedica, Puebla, 2011 Use of polarized light imaging and sensing in the clinical setting Jessica C. Ramella-Roman, PhD.
High Altitude Observatory (HAO) – National Center for Atmospheric Research (NCAR) The National Center for Atmospheric Research is operated by the University.
High Altitude Observatory (HAO) – National Center for Atmospheric Research (NCAR) The National Center for Atmospheric Research is operated by the University.
A possible mechanism for understanding the enigmatic scattering polarization signals observed in the solar Na I and Ba II D 1 lines Luca Belluzzi 1 and.
Light and Matter Tim Freegarde School of Physics & Astronomy University of Southampton The tensor nature of susceptibility.
High Altitude Observatory (HAO) – National Center for Atmospheric Research (NCAR) The National Center for Atmospheric Research is operated by the University.
Limitation of Pulse Basis/Delta Testing Discretization: TE-Wave EFIE difficulties lie in the behavior of fields produced by the pulse expansion functions.
3D Inversion of the Magnetic Field from Polarimetry Data of Magnetically Sensitive Coronal Ions M. Kramar, B. Inhester Max-Planck Institute for Solar System.
Evan Walsh Mentors: Ivan Bazarov and David Sagan August 13, 2010.
Alfvén-cyclotron wave mode structure: linear and nonlinear behavior J. A. Araneda 1, H. Astudillo 1, and E. Marsch 2 1 Departamento de Física, Universidad.
Self-consistency of the RT solutions. Self-consistent solution of RT Take into account the intensity part of the source function (scattering) Construct.
Part I: Energy transport by radiation From static 1D medium to dynamic environment in multi-dimensions
METO 621 Lesson 13. Separation of the radiation field into orders of scattering If the source function is known then we may integrate the radiative transfer.
Cosmic 21-cm Fluctuations from Dark-Age Gas Kris Sigurdson Institute for Advanced Study Cosmo 2006 September 25, 2006 Kris Sigurdson Institute for Advanced.
High Altitude Observatory (HAO) – National Center for Atmospheric Research (NCAR) The National Center for Atmospheric Research is operated by the University.
Optically polarized atoms
LESSON 4 METO 621. The extinction law Consider a small element of an absorbing medium, ds, within the total medium s.
March 2, 2011 Fill in derivation from last lecture Polarization of Thomson Scattering No class Friday, March 11.
1 Chapter 4: Polarization of light 2 Preliminaries and definitions Preliminaries and definitions Plane-wave approximation: E(r,t) and B(r,t) are uniform.
High Altitude Observatory (HAO) – National Center for Atmospheric Research (NCAR) The National Center for Atmospheric Research is operated by the University.
Four equations (integral form) : Gauss’s law Gauss’s law for magnetism Faraday’s law Ampere-Maxwell law + Lorentz force Maxwell’s Equations.
Lecture 2: Physical Processes In Astrophysical and Laboratory Plasmas Lecture 1: Temperature-Density regime Many physical processes Focus on Atomic+Plasma.
1 Waves, Light & Quanta Tim Freegarde Web Gallery of Art; National Gallery, London.
Stellar Atmospheres: Non-LTE Rate Equations 1 The non-LTE Rate Equations Statistical equations.
Vibrational and Rotational Spectroscopy
Density Matrix Density Operator State of a system at time t:
Stellar Atmospheres: Solution Strategies 1 Solution Strategies.
Spectropolarimetry with the green line: Observations and Simulations
CMB Polarization Generated by Primordial Gravitational Waves - Analytical Solutions Alexander Polnarev Queen Mary, University of London MG12, Paris, 13.
Collisions and transport phenomena Collisions in partly and fully ionized plasmas Typical collision parameters Conductivity and transport coefficients.
Open a New Window of Plasma Diagnostics in the Solar Physics with Spectropolarimetric Observation HINODE June 10 th, 2014 Tetsu Anan (Kyoto.
Incoherent pair background processes with full polarizations at the ILC Anthony Hartin JAI, Oxford University Physics, Denys Wilkinson Building, Keble.
B.SC.II PAPER-B (OPTICS and LASERS)
Stellar Atmospheres: Radiation Transfer 1 Radiation Transfer.
Spicule observed in He Å Solar seminar in 2009 April 20 Short : Tetsu Anan HAZEL Bueno et al Nuño et al , 2, 3,
Polarization Calibration of the Daniel K Inouye Solar Telescope (DKIST) formerly Advanced Technology Solar Telescope David Elmore Instrument Scientist.
Absorption and Emission of Radiation:
Adiabatic approximation
Ch ; Lecture 26 – Quantum description of absorption.
Stellar Atmospheres: Radiation Transport as Boundary-Value Problem 1 Radiation Transport as Boundary-Value Problem of Differential Equations.
Electromagnetic Waves and Their Propagation Through the Atmosphere
Lecture/Lab: Interaction of light with particles. Mie’s solution.
Linear optical properties of dielectrics
Physics 3210 Week 14 clicker questions. When expanding the potential energy about a minimum (at the origin), we have What can we say about the coefficients.
Nonlinear Optics Lab. Hanyang Univ. Chapter 4. The Intensity-Dependent Refractive Index - Third order nonlinear effect - Mathematical description of the.
Polarimetry in Astronomy Or Do you know where your photons are coming from? Elizabeth Corbett AAO.
Introduction to materials physics #4
Spectroscopy Spectral lines The Fraunhofer spectrum Charlotte Moore Sitterly (Allen!) –Multiplet table –Rowland table Formalism of spectroscopy.
Self-Similarity in Classical Fluids and MHD B.C. Low High Altitude Observatory National Center for Atmospheric Research Boulder, Colorado, USA The National.
Förster Resonance Energy Transfer (FRET)
For long wavelength, compared to the size of the atom The term containing A 2 in the dipole approximation does not involve atomic operators, consequently.
Electromagnetism Around 1800 classical physics knew: - 1/r 2 Force law of attraction between positive & negative charges. - v ×B Force law for a moving.
Introduction to Coherence Spectroscopy Lecture 1 Coherence: “A term that's applied to electromagnetic waves. When they "wiggle" up and down together they.
C ontrolling Coherent Nonlinear Optical Signals of Helical Structures by Adaptive Pulse Polarizations Dmitri V. Voronine Department of Chemistry, University.
WIR SCHAFFEN WISSEN – HEUTE FÜR MORGEN Pendulum Equations and Low Gain Regime Sven Reiche :: SwissFEL Beam Dynamics Group :: Paul Scherrer Institute CERN.
Hale COLLAGE (CU ASTR-7500) “Topics in Solar Observation Techniques” Lecture 3: Basic concepts in radiative transfer & polarization Spring 2016, Part 1.
Measurement of magnetic field by Hanle effect in Na I D 2 T. Anan (Kyoto univ.) 1, review of Holzreuter et al , Hanle effect of Na D2.
Einstein’s coefficients represent a phenomenological description of the matter-radiation interaction Prescription for computing the values of the A and.
Quantum optics Eyal Freiberg.
Solar Spectral Lines with Special Polarization Properties for the Calibration of Instrument Polarization Wenxian Li, Roberto Casini, T. del Pino Alemán.
QUANTUM TRANSITIONS WITHIN THE FUNCTIONAL INTEGRATION REAL FUNCTIONAL
Free Electron Sources of CoherentRadiation: FREE ELECTRON LASERS
Density Matrix Density Operator State of a system at time t:
Polarization in spectral lines
Еugene Grichuk, Margarita Kuzmina, Eduard Manykin
Chapter 7. Emission and Absorption and Rate Equations
Coherent Nonlinear Optics
Chapter 4 Two-Level Systems.
Lecture 15: Time-Dependent Perturbation
Presentation transcript:

High Altitude Observatory (HAO) – National Center for Atmospheric Research (NCAR) The National Center for Atmospheric Research is operated by the University Corporation for Atmospheric Research under sponsorship of the National Science Foundation. An Equal Opportunity/Affirmative Action Employer. 19 May 2005 Scattering Polarization in the Solar Atmosphere R. Casini High Altitude Observatory National Center for Atmospheric Research

Polarized Radiation Origin: symmetry-breaking processes of the Atom-Photon interaction (e.g., anisotropic illumination, deterministic magnetic and/or electric fields, anisotropic collisions) Zeeman effect Circular polarization Linear polarization

Polarized Radiation Description: 4 independent parameters –i) coherency matrix (a.k.a. polarization tensor ) –ii) Stokes parameters Jones calculus Mueller calculus

Polarized Radiation Operational definition of Stokes parameters For a   retarder 

Polarized Radiation Polarized radiation tensors Irreducible spherical tensors transformation conjugation

Polarized Radiation Example: Unpolarized radiation from the quiet-sun photosphere Only two non-vanishing components:

Atomic Polarization Gas of atoms subject to: Anisotropic and/or polarized illumination External fields Collisions 1.Atomic system not in a “pure state” 2.Population imbalances and quantum interferences between atomic levels

Atomic Polarization Density operator Density matrix Atomic eigenstates or some other complete basis

Irreducible spherical components of the density matrix If (e.g., Zeeman effect) Otherwise (e.g., Paschen-Back effect, Stark effect) Atomic Polarization transformation conjugation

Example: Multi-level atom 1.Population: 2.Orientation: 3.Alignment: Atomic Polarization

Ex. 1: Positive orientation in a level Ex. 2: Positive alignment in a level Ex. 3: Orientation and alignment in a level Atomic Polarization  Presence of net polarization in the re-emitted radiation (even in the absence of external fields)

Liouville’s equation Evolution equation for expectation values Time evolution of the system Perturbative expansion Atom Radiation 

Atom-Photon interaction to 2 nd order of perturbation Resonance Scattering 1 st order  2 nd order 

Restriction: Non-coherent scattering Scattering as the succession of 1 st -order absorption and re-emission Complete Re-Distribution in frequency The atom loses memory of the incident photons, and the re-emitted photons are statistically re-distributed in frequency Resonance Scattering Flat-Spectrum Approximation

Restriction: Non-coherent scattering Scattering as the succession of 1 st -order absorption and re-emission Two-step solution i.Determine the excitation state of the atomic system consistently with the ambient radiation field (Statistical Equilibrium Problem) ii.Calculate the scattered radiation consistently with the excitation state of the atomic system (Radiative Transfer Problem) Resonance Scattering

Statistical Equilibrium functions of the incident radiation

Radiative Transfer Absorbtion matrix Function of Stimulation matrix Function of Emission vector Function of in stationary regime

Resonance Scattering non-LTE of the 2 nd kind Self-consistency loop (  -iteration)

Difficulties 1.The Statistical Equilibrium problem grows rapidly with the complexity of the atomic system (very large sparse matrices) Possible strategy: weak-anisotropy approximation 2.The Radiative Transfer problem requires the solution of a set of 4 coupled ODEs Possible strategy: Diagonal Elements Lambda Operator (DELO) 3.No guarantee of convergence of the self-consistency loop (maybe with the exception of the simplest atomic models, with appropriate initialization) Possible strategy: ????? Resonance Scattering

Atom 0-1 Classical analogy in the 3D harmonic oscillator with forcing term

Atom 0-1

Atom 1-0 Hanle effect of the lower level Non-linear dependence on

Atom 1-0

Atom 1-1

Atomic polarization and Radiative transfer Homogeneous slab 0-1 or 1-0 w/o atomic pol. (Zeeman effect) 0-1 with atomic pol. 1-0 with atomic pol.

Atomic polarization and Radiative transfer Homogeneous slab   Å He I

Atomic polarization and Radiative transfer Homogeneous slab   Å He I Trujillo Bueno et al., Nature 415, 403 (2002)

Atomic polarization in Na I     F    D1D1 D2D2

Atomic polarization in Na I     F    D1D1 D2D2 D1D1 D2D2  Å

Atomic polarization in Na I     F   

Alignment-to-Orientation transfer     F    When quantum interferences between FS and/or HFS levels are important diagonal depolarization  coupling alignment-to-orientation

Atomic orientation in H I HAO Advanced Stokes Polarimeter March 2003 THEMIS heliographic telescope September 2003 Spectro-polarimetric observations of H  in solar prominences (off the limb)

Atomic orientation in H I Spectro-polarimetric simulations with FS and HFS THEMIS heliographic telescope September 2003 Maximum net circular polarization 1 order of magnitude too small for typical prominence fields (less than ~ 100 G)

Atomic orientation in H I Catalytic effect of small electric fields on H I atomic orientation  Enhanced net circular polarization in H 

Catalytic effect of small electric fields on H I atomic orientation HH  present also for isotropic electric fields vertical magnetic field, forward scattering Isotropic E field w/o HFS with HFS Inclinations of random-azimuth, 1 V cm -1 fields Only B Prominence B fields

Conclusions Spectro-polarimetric observations reveal the complexity of the atomic processes underlying resonance scattering (atomic coherences, FS and HFS effects, magnetic and electric fields, alignment-to-orientation transfer)  The local problem can already become numerically very intensive Points to focus on: a.Improve speed in the construction of the Statistical Equilibrium matrix b.Invent new strategies to accelerate convergence of the iterative scheme for atoms of arbitrary complexity and general illumination conditions