Typical anisotropies introduced by geometry (not everything is spherically symmetric) temperature gradients magnetic fields electrical fields

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Lecture 6: Polarimetry 1 Outline 1 Polarized Light in the Universe 2 Fundamentals of Polarized Light 3 Descriptions of Polarized Light Polarized Light in the Universe Polarization indicates anisotropy not all directions are equal Typical anisotropies introduced by geometry (not everything is spherically symmetric) temperature gradients magnetic fields electrical fields Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 1

Polarized Light from the Big Bang Cosmic Microwave Background (CMB) is red-shifted radiation from Big Bang 14 109 years ago age, geometry, density, of universe from CMB intensity pattern first 0.1 seconds from polarization pattern of CMB inflation gravitational waves polarization signals polarization expected at (or below) 10 6 of intensity 13.7 billion year old temperature fluctuations from WMAP Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 2

Unified Model of Active Galactic Nuclei Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 3

Protoplanetary Disk in Scattered Light Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 4

Solar Magnetic Field Maps from Longitudinal Zeeman Effect Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 5

Second Solar Spectrum from Scattering Polarization Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 6

Jupiter and Saturn Planetary Scattered Light Jupiter, Saturn show scattering polarization much depends on cloud height can be used to study exoplanets ExPo development at UU (courtesy H.M.Schmid and D.Gisler) Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 7

Other astrophysical applications interstellar magnetic field from polarized starlight supernova asymmetries stellar magnetic fields from Zeeman effect galactic magnetic field from Faraday rotation Magnetic Fields of TTauri Stars by Sandra V.Jeffers Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 8

Fundamentals of Polarized Light Electromagnetic Waves in Matter Maxwell s equations electromagnetic waves optics: interaction of electromagnetic waves with matter as described by material equations polarization of electromagnetic waves are integral part of optics Maxwell s Equations in Matter D = 4πρ H 1 D = 4π c t c j E + 1 B = 0 c t B = 0 Symbols D electric displacement ρ electric charge density H magnetic field c speed of light in vacuum j electric current density E electric field B magnetic induction t time Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 9

Linear Material Equations D = ɛe B = µ H j = σe Symbols ɛ dielectric constant µ magnetic permeability σ electrical conductivity Isotropic Media isotropic media: ɛ and µ are scalars for most materials: µ = 1 Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 10

Wave Equation in Matter static, homogeneous medium with no net charges: ρ = 0 combine Maxwell, material equations differential equations for damped (vector) wave 2 E µɛ 2 E c 2 t 2 4πµσ c 2 E t = 0 2 H µɛ 2 H c 2 t 2 4πµσ H c 2 t = 0 damping controlled by conductivity σ E and H are equivalent sufficient to consider E interaction with matter almost always through E but: at interfaces, boundary conditions for H are crucial Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 11

Plane-Wave Solutions Plane Vector Wave ansatz E = E 0 e i( k x ωt) k spatially and temporally constant wave vector k normal to surfaces of constant phase k wave number x spatial location ω angular frequency (2π frequency) t time E 0 (generally complex) vector independent of time and space could also use E = E 0 e i( k x ωt) damping if k is complex real electric field vector given by real part of E Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 12

Complex Index of Refraction temporal derivatives Helmholtz equation 2 E + ω 2 µ c 2 dispersion relation between k and ω k k = ω 2 µ complex index of refraction ( ɛ + i 4πσ ) E = 0 ω c 2 ( ɛ + i 4πσ ) ω ( ñ 2 = µ ɛ + i 4πσ ), k ω 2 k = ω c 2 ñ2 split into real (n: index of refraction) and imaginary parts (k: extinction coefficient) ñ = n + ik Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 13

Transverse Waves plane-wave solution must also fulfill Maxwell s equations E 0 k = 0, H0 k = 0, H0 = ñ k µ k E 0 isotropic media: electric, magnetic field vectors normal to wave vector transverse waves E 0, H 0, and k orthogonal to each other, right-handed vector-triple conductive medium complex ñ, E 0 and H 0 out of phase E 0 and H 0 have constant relationship consider only E Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 14

Energy Propagation in Isotropic Media Poynting vector S = c ( ) E H 4π S : energy through unit area perpendicular to S per unit time direction of S is direction of energy flow time-averaged Poynting vector given by S = c ( 8π Re E0 H ) 0 Re real part of complex expression complex conjugate. time average energy flow parallel to wave vector (in isotropic media) S = c ñ 8π µ E 0 2 k k Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 15

Polarization Plane Vector Wave ansatz E = E 0 e i( k x ωt) spatially, temporally constant vector E 0 lays in plane perpendicular to propagation direction k represent E 0 in 2-D basis, unit vectors e 1 and e 2, both perpendicular to k E 0 = E 1 e 1 + E 2 e 2. E 1, E 2 : arbitrary complex scalars damped plane-wave solution with given ω, k has 4 degrees of freedom (two complex scalars) additional property is called polarization many ways to represent these four quantities if E 1 and E 2 have identical phases, E oscillates in fixed plane Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 16

Polarization Ellipse Polarization Ellipse Polarization E (t) = E 0 e i( k x ωt) E 0 = E 1 e iδ 1 e x + E 2 e iδ 2 e y wave vector in z-direction e x, e y : unit vectors in x, y E 1, E 2 : (real) amplitudes δ 1,2 : (real) phases Polarization Description 2 complex scalars not the most useful description at given x, time evolution of E described by polarization ellipse ellipse described by axes a, b, orientation ψ Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 17

Jones Formalism Jones Vectors E 0 = E x e x + E y e y beam in z-direction e x, e y unit vectors in x, y-direction complex scalars E x,y Jones vector e = ( Ex E y ) phase difference between E x, E y multiple of π, electric field vector oscillates in a fixed plane linear polarization phase difference ± π 2 circular polarization Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 19

Summing and Measuring Jones Vectors E 0 = E x e x + E y e y ( ) Ex e = E y Maxwell s equations linear sum of two solutions again a solution Jones vector of sum of two waves = sum of Jones vectors of individual waves if wave vectors k the same addition of Jones vectors: coherent superposition of waves elements of Jones vectors are not observed directly observables always depend on products of elements of Jones vectors, i.e. intensity I = e e = e x e x + e y e y Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 20

Jones matrices influence of medium on polarization described by 2 2 complex Jones matrix J ( ) e J11 J = J e = 12 e J 21 J 22 assumes that medium not affected by polarization state different media 1 to N in order of wave direction combined influence described by J = J N J N 1 J 2 J 1 order of matrices in product is crucial Jones calculus describes coherent superposition of polarized light Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 21

Linear Polarization ( 1 horizontal: 0 ( ) 0 vertical: 1 ( ) 45 1 : 2 1 1 ) Circular Polarization ( ) 1 left: 2 1 i ( ) 1 right: 2 1 i Notes on Jones Formalism Jones formalism operates on amplitudes, not intensities coherent superposition important for coherent light (lasers, interference effects) Jones formalism describes 100% polarized light Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 22

Quasi-Monochromatic Light monochromatic light: purely theoretical concept monochromatic light wave always fully polarized real life: light includes range of wavelengths quasi-monochromatic light quasi-monochromatic: superposition of mutually incoherent monochromatic light beams whose wavelengths vary in narrow range δλ around central wavelength λ 0 δλ λ 1 measurement of quasi-monochromatic light: integral over measurement time t m amplitude, phase (slow) functions of time for given spatial location slow: variations occur on time scales much longer than the mean period of the wave Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 23

Polarization of Quasi-Monochromatic Light electric field vector for quasi-monochromatic plane wave is sum of electric field vectors of all monochromatic beams E (t) = E 0 (t) e i( k x ωt) can write this way because δλ λ 0 measured intensity of quasi-monochromatic beam Ex E x + Ey E y = lim t m > 1 t m tm/2 t m/2 : averaging over measurement time t m measured intensity independent of time E x (t) E x (t) + E y (t) E y (t)dt quasi-monochromatic: frequency-dependent material properties (e.g. index of refraction) are constant within λ Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 25

Polychromatic Light or White Light wavelength range comparable to wavelength ( δλ λ 1) incoherent sum of quasi-monochromatic beams that have large variations in wavelength cannot write electric field vector in a plane-wave form must take into account frequency-dependent material characteristics intensity of polychromatic light is given by sum of intensities of constituting quasi-monochromatic beams Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 26

Stokes and Mueller Formalisms Stokes Vector formalism to describe polarization of quasi-monochromatic light directly related to measurable intensities Stokes vector fulfills these requirements I = I Q U V = E x Ex + E y Ey E x Ex E y Ey E x Ey + E y Ex i ( E x Ey E y Ex ) = E 2 1 + E 2 2 E 2 1 E 2 2 2E 1 E 2 cos δ 2E 1 E 2 sin δ Jones vector elements E x,y, real amplitudes E 1,2, phase difference δ = δ 2 δ 1 I 2 Q 2 + U 2 + V 2 Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 27

Stokes Vector Interpretation I I = Q U = V degree of polarization P = intensity linear 0 linear 90 linear 45 linear 135 circular left right Q 2 + U 2 + V 2 1 for fully polarized light, 0 for unpolarized light summing of Stokes vectors = incoherent adding of quasi-monochromatic light waves I Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 28

Linear Polarization horizontal: 1 1 0 0 vertical: 1 1 0 0 45 : 1 0 1 0 Circular Polarization left: 1 0 0 1 right: 1 0 0 1 Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 29

Mueller Matrices 4 4 real Mueller matrices describe (linear) transformation between Stokes vectors when passing through or reflecting from media I = M I, M = M 11 M 12 M 13 M 14 M 21 M 22 M 23 M 24 M 31 M 32 M 33 M 34 M 41 M 42 M 43 M 44 N optical elements, combined Mueller matrix is M = M N M N 1 M 2 M 1 Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 30

Vertical Linear Polarizer M pol (θ) = 1 2 1 1 0 0 1 1 0 0 0 0 0 0 0 0 0 0 Horizontal Linear Polarizer M pol (θ) = 1 2 1 1 0 0 1 1 0 0 0 0 0 0 0 0 0 0 Mueller Matrix for Ideal Linear Polarizer at Angle θ M pol (θ) = 1 2 1 cos 2θ sin 2θ 0 cos 2θ cos 2 2θ sin 2θ cos 2θ 0 sin 2θ sin 2θ cos 2θ sin 2 2θ 0 0 0 0 0 Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 31

Poincaré Sphere Relation to Stokes Vector fully polarized light: I 2 = Q 2 + U 2 + V 2 for I 2 = 1: sphere in Q, U, V coordinate system point on Poincaré sphere represents particular state of polarization graphical representation of fully polarized light Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 32

Poincaré Sphere Interpretation polarizer is a point on the Poincaré sphere transmitted intensity: cos 2 (l/2), l is arch length of great circle between incoming polarization and polarizer on Poincaré sphere Christoph U. Keller, Utrecht University, C.U.Keller@uu.nl Observational Astrophysics 2, Lecture 6: Polarimetry 1 33