Now , soWhenever nonzero, the scattered light has the same linear polarization along as in (a). Although the incident field points toward the observer, the tilted anisotropic needle can induce a dipole component perpendicular to that direction. An isotropic sphere would instead have an axial radiation zero for this incident polarization.
Spherical-particle frequency scaling. For a dielectric sphere of radius , the quasistatic electric polarizability isThe electric dipole radiation formula and giveThus Rayleigh scattering scales as , or , when the polarizability varies slowly with frequency. Material resonances and absorption can change this simple scaling. For the incident polarization, the dipole is along : intensity is proportional to , where is the angle from . There is no radiation on the dipole axis and a maximum in the plane. In a direction the scattered electric field is along , hence linearly polarized wherever nonzero.[ref]
Rayleigh Scattering by Richard Fitzpatrick. Small-particle dipole response and inverse-fourth-power wavelength dependence
Needle model used in parts (a)–(d). Let its axis be . A very slender, high-permittivity needle has dominant longitudinal response, so use the rank-one needle polarizability . Its transverse response is neglected at leading order. For observation along , define , andFor a unit incident Jones vector , the common far-field relation is , and . Here is irradiance at distance ; multiplying by gives power per solid angle. No absolute value of is given or needed for the requested relative intensities.
Diffuse random cloud, with the incident polarization of (a). The single-particle amplitudes through and analysers are proportional to and . The isotropic orientation fourth moment gives the needle-scattering analyzer momentsFor example, ; symmetry and give . Since the particles scatter mutually incoherently, intensities add. For illuminated particles,The cross correlation vanishes by reflection symmetry. The degree of linear polarization is : random anisotropic scatterers produce partially depolarized light, even though every individual needle produces a single linear polarization.
Independent isotropically oriented needles give the analyser ratio one to three, while coherent mean amplitudes have no x component
. Source. Details. Continuous homogeneous dielectric. One must sum amplitudes coherently and include their spatial phases, rather than retain the preceding sum of intensities. Random orientations give , so the averaged response is isotropic and its induced polarization is along . Its coherent radiation toward , when allowed by the sample geometry, is therefore purely polarized, with . The independent-needle prefactor is no longer a quantitative dense-medium model; local-field and collective effects determine the effective permittivity.
There is also coherent continuum phase matching: a uniform bulk driven by a plane wave has no arbitrary outgoing plane-wave component. In an ideal infinite homogeneous medium there is no diffuse side scattering at all; propagation, refraction and reflection are determined by the medium and its interfaces. A finite sample's coherent side signal depends on its shape and boundaries. Thus the old diffuse ratio is replaced by a coherent isotropic-medium response, not by a universal nonzero side-scattering intensity.
Past exam of the optics and electrodynamics course of the University of Cambridge 2017 1 a Solution 2026-10-18
At an air–glass interface, resolve the incident unpolarized light into components perpendicular () and parallel () to the plane of incidence. The Fresnel equations give the parallel reflection coefficientAt Brewster's angle, . Together with Snell's law, this gives and . Thus, taking the incident medium to be air,The remaining reflected component has linear polarization perpendicular to the plane of incidence. This assumes a transparent, nonmagnetic glass with negligible absorption.
Past exam of the optics and electrodynamics course of the University of Cambridge 2017 2 a Solution 2026-10-18
Molecules in clean air are much smaller than visible wavelengths. Their induced electric dipole moments undergo Rayleigh scattering. Away from molecular resonances, the induced dipole amplitude is approximately , with only weak wavelength variation in the polarizability . The radiation-zone electric field is proportional to , so the scattered intensity satisfiesThis is the Rayleigh scattering wavelength dependence. For equal incident intensities, light scatters about times as strongly as light. Thus light scattered out of the direct solar beam and into our line of sight is enriched in blue wavelengths.
The dipole mechanism also determines the Rayleigh scattering angular pattern. For unpolarized light, its angular factor is ; near scattering, the scattered light has strong linear polarization. The sky's perceived colour depends additionally on the solar spectrum, atmospheric transmission and the eye's spectral response, so the law alone does not predict a violet sky. Over a long near-horizontal path the direct beam loses more short-wavelength light, explaining red sunsets. Large aerosol particles instead produce Mie scattering, which is less strongly wavelength-selective and can make haze look whitish.
Past exam of the optics and electrodynamics course of the University of Cambridge 2017 3 Solution 2026-10-18
General pure state. Use time dependence . The most general nonzero Jones vector can be writtenThere are four real parameters in the full complex field. Removing overall intensity and the unobservable common phase leaves two real degrees of freedom for pure polarization, and . Their endpoint degeneracies simply reflect the fact that the phase of a vanishing component is irrelevant. A single Jones vector cannot represent partially polarized light.
Three linear polarizers. Define the transmission axis . An ideal linear polarizer has Jones matrix . For definiteness label as right-circular in the chosen convention; reversing the handedness convention changes no intensity below. The first polarizer produces . The intermediate polarizer and final analyzer then giveso Malus's law givesThe maximum is at , and the transmission vanishes at . The first polarizer accounts for an initial factor ; retaining that factor is essential when quoting transmission relative to the incident circularly polarized beam.
Waveplate and quarter-wave matrix. A lossless waveplate has linear birefringence: its orthogonal fast and slow axes have indices . A thickness produces slow-minus-fast phase retardationResolving the incident Jones vector into the plate axes, advancing the two phases and transforming back gives, up to a common phase,A quarter-wave plate has modulo . With and , its Jones matrix is thereforeIn particular . Equal incident components along the two axes acquire a relative quarter-cycle phase, converting linear polarization to circular polarization; an incident component along either principal axis stays linearly polarized.
Half-wave replacement. A half-wave plate has and henceIt converts the -polarized output of the first polarizer to a linear state at angle . The final analyzer givesThe maximum is , because the ideal half-wave plate loses no light after the first polarizer.
Quarter-wave replacement. The transmitted amplitude is , givingMore generally, the retarder gives . All three requested curves have the same zeros and angular period, but different heights:
Transmission through crossed outer polarizers with three different middle elements
. Details. Preparing an arbitrary ellipse. Yes: two rotatable quarter-wave plates already suffice. Let the input left-circular state be . Up to an overall phase, any target pure polarization can be parameterized by its polarization ellipse:Here is the major-axis orientation, and sets the signed minor-to-major semiaxis ratio . First note directly from thatChoose the two fast-axis angles asThe first quarter-wave plate produces linear light at . In the axes of the second, its components are ; the second gives precisely . This proves pure-polarization preparation with two quarter-wave plates, including the linear and circular limiting cases. A half-wave plate can also rotate the axes, but is not required. The phrase about left-handed input is understood as left-circular light in this construction; the explicit vector fixes the convention.
Switchable retardation. The electro-optic Kerr effect induces linear birefringence quadratic in a static transverse electric field. Defining the coefficient by , its phase retardation isThe two eigenpolarizations are linear, parallel and perpendicular to the applied field. Thus an appropriate field produces a switchable quarter-wave plate:The sign of determines which axis is fast. Switching the field off removes the induced retardation, assuming no residual birefringence.
The Faraday effect instead gives circular birefringence for a longitudinal magnetic field. The two circular eigenmodes acquire different phases, rotating a linear polarization throughwith sign set by the handedness convention and the Verdet constant . Its Jones matrix in the linear basis is a real rotation, up to a common phase. It preserves the ellipticity of a pure state, so a linear input remains linear. A phase difference between circular eigenmodes rotates a linear state by ; it does not make it circular. The Kerr device supplies the switchable quarter-wave plate; a Faraday rotator alone does not.
Let the two arms deliver intensities with unit Jones vectors . For a perfectly coherent input, the recombined intensity under relative phase isConsequently the polarization overlap in interferometric visibility isFor equal returned intensities, two linear polarizations at angle have overlap and thereforeChoose one linear direction as and a circular polarization as . Their overlap has magnitude , givingA non-polarizing beam splitter does not by itself guarantee equal arm losses; if , multiply either boxed polarization factor by . Perfect temporal coherence does not compensate for polarization or intensity imbalance.
Birefringence gives two orthogonal linear eigenpolarizations with different refractive indices, and . They accumulate different wave phases through the same physical thickness . Their relative phase retardation isHere is the vacuum wavelength. For the thinnest positive-retardance plate, . The plate uses a difference in phase velocity, rather than differential wave absorption. Equal wave amplitudes along the two axes, obtained from input linear polarization at to them, acquire phase quadrature and become circular polarization. Reversing that conversion gives linear polarization from the corresponding circular input. A different input angle generally gives elliptical polarization on one pass.
Use the same fixed laboratory axes for the incident and returning Jones vectors, with along the fast axis. Remove a common phase factor so that the one-pass Jones matrix is . The reverse pass through this reciprocal plate accumulates the same relative phase retardation, not its inverse. The mirror has scalar reflection coefficient in these fixed axes. ThereforeThe effective retardance is : the complete return acts as a half-wave plate. For initial linear polarization at angle to the fast axis,In particular, the input used for linear-to-circular conversion returns in linear polarization perpendicular to its original line: . An input along either plate axis returns along that same axis.
The wording does not specify the initial polarization of waves. Thus “orthogonal linear return” requires the usual linearly polarized input; it is not a universal answer for arbitrary polarized input. The Jones matrix above supplies the general answer. A non-normal metallic reflection may introduce different complex reflection coefficients for the two components and would require additional geometry and optical data. Descriptions of the intermediate circular polarization must also account for the reversed propagation direction when assigning handedness.
Put , where is the binding spring constant rather than an optical wavenumber. The steady complex amplitude solution of the forced Lorentz oscillator model isThe acceleration complex amplitude is . HenceThis is the scattering cross-section of a harmonically bound charge. The displacement and induced electric dipole moment are parallel to the incident linear polarization, and integrating their dipole radiation over all directions gives the total cross section above.
For , binding dominates andrecovering Rayleigh scattering with static electric polarizability . For , inertia dominates: , so its second time derivative becomes frequency independent andThis is a classical Thomson scattering regime only while . Exactly at , an undamped driven oscillator has no finite steady-state amplitude; the divergent formula must not be used. Finite damping and radiation reaction regulate the physical resonant response. Coherent contributions from many charges in an extended medium can also require a structure calculation rather than multiplying this single-charge result by a particle count.
Work in the dilute, single-scattering limit and add the diffuse scattered light intensities of randomly positioned particles. The incident unpolarized light has equal, mutually uncorrelated and electric components. Each particle therefore has an induced electric dipole moment along its permitted axis, with the same mean squared magnitude proportional to .
For an observer in direction , choose transverse unit directions in the scattering plane and perpendicular to it. The electric dipole radiation field is proportional to the transverse projection of the electric dipole. Hence an electric dipole contributes a wave amplitude factor along , while a electric dipole contributes its full wave amplitude along .
Let collect the common incident light intensity, electric polarizability, distance and frequency factors. ThenThe two components are uncorrelated, so the coherency matrix is diagonal in this basis. The degree of polarization isA signed degree of linear polarization, defined positive perpendicular to the scattering plane, has the same expression without the absolute value. The dominant direction is when , and when the inequality reverses. If the denominator vanishes there is no scattered signal and its degree of polarization is undefined. A coherent exactly forward component, including the transmitted incident beam, is not part of this diffuse-intensity calculation; random particle positions do not by themselves destroy forward optical coherence.
Take an incident field along , without loss of generality because this component has the same circular eigenmodes for every direction of input linear polarization. Resolve its Jones vector into equal circular components:Using the complex amplitude convention , the real circular contributions areThey counter-rotate and add toIn general the tip traces an ellipse with semiaxis lengths and . Equal transmitted circular wave amplitudes produce a line; removal of one circular mode, or , produces a circle. The special zero-output case has no defined polarization of waves.
Write , and . Then and . With and , the corrected matrix becomesThe scalar is a common propagation wave phase and the real rotation matrix rotates the input linear polarization through . There is no attenuation and no generated ellipticity: the field map is a unitary matrix. The two circular eigenmodes accumulate different wave phases, giving circular birefringence and optical activity.
The correct unfactored matrix remains finite where . In contrast, the printed form would give times the rotation matrix, including unphysical divergent gain in this stipulated lossless case. This provides a direct physical check on the correction in part (d).
Birefringence means that two independent polarization eigenmodes have different refractive indices at the same frequency and propagation direction. The rotatory-power formula relevant here requires circular birefringence: the eigenmodes are opposite circular polarizations. General linear birefringence instead introduces phase retardation between linearly polarized components and need not rotate every incident linear polarization through one common angle.
Use the complex amplitude convention and transverse unit vectors . DefinePropagation through thickness adds phases , where is the vacuum wavelength. Recombining the two components givesThus the rotation and the specific rotatory power per unit length areThe units of are . The sign follows the specified circular basis and viewing convention. Equal attenuation of the two eigenmodes has been assumed; unequal attenuation also produces elliptical polarization.
Let be the incident light intensity. The first ideal polarizer transmits and produces linear polarization along . Faraday rotation turns that direction through , and Malus's law at the second polarizer givesEquivalently, use the input coherency matrix and . This produces the same one-half factor required by unpolarized light.
Maxima satisfy , with . For and , the smallest field magnitude isIts direction is the axial direction that rotates the polarization passed by toward the pass axis of through the shorter . In the right-handed ray-basis convention where and the depicted second axis is , this is , along . Reversing that field at the same magnitude gives and zero transmission. A signed Verdet constant is meaningful only together with its rotation convention, so the polarization-alignment description fixes the physical direction without relying on ambiguous clockwise labels in a perspective diagram.
Original forward and reverse transmission curves and laboratory polarization directions at the optimum Faraday rotation
. Details. The cosmic microwave background is relic thermal radiation from the hot early universe. Its temperature anisotropy is expanded in spherical harmonics, with angular power spectrum . Thomson scattering of a local radiation quadrupole generates linear polarization around last scattering and again during reionization. Polarization maps are decomposed into E-mode polarization and B-mode polarization, giving spectra such as , and in addition to temperature information.
Cosmic microwave background acoustic peak positions compare the sound horizon with the angular-diameter distance to last scattering, constraining geometry and expansion history. Relative peak heights constrain baryon loading and matter-radiation equality; the damping tail constrains diffusion and other early-universe physics. The scalar spectral index and primordial scalar amplitude constrain inflationary perturbations. Coherent acoustic structure and temperature-polarization correlations support predominantly adiabatic initial perturbations. Large-angle E-mode polarization measures the reionization optical depth, helping break its degeneracy with the scalar amplitude inferred from small-scale temperature anisotropy.
Under a specified cosmological model, these data constrain ordinary and cold dark matter densities, the Hubble constant, spatial curvature and cosmic age. Complementary distance information helps break the geometrical degeneracy: temperature peaks alone do not uniquely establish a cosmological constant. The Planck 2013 parameter analysis used Planck temperature data and, in important combinations, WMAP low-multipole polarization; it should not be described as a full Planck polarization release.[ref]
Linear scalar cosmological perturbations generate E-mode polarization but no primordial B-mode polarization in the simplest treatment. tensor cosmological perturbations can generate B-mode polarization, making them a possible probe of inflationary gravitational waves. gravitational lensing converts some E-mode power into B-mode polarization, however, and Galactic dust and synchrotron radiation also contribute polarized foregrounds. Multifrequency observations, foreground modelling, beam calibration and control of temperature-to-polarization leakage are therefore necessary. Polarization does not by itself establish a primordial tensor signal. temperature and polarization jointly test the expansion history and primordial perturbations, while complementary data and foreground control determine how uniquely parameters can be inferred.
Write and . The electric field isIt has linear polarization, along the fixed line , at angle from toward . For the associated plane electromagnetic wave, Faraday's law gives . HenceIn vacuum . Both fields are transverse, and points along .
This is a plane electromagnetic wave with linear polarization. is the electric field; its peak amplitude; the position along propagation; the time; the wavenumber; and the angular frequency. Here is the wavelength, the frequency, and the unit vector in the direction of the electric field. Constant phase moves along with phase velocity .
Put . The differential Faraday's law of induction givesThe accompanying oscillating magnetic field, excluding any independent static background, is therefore . To determine the propagation speed, also use the source-free Ampere-Maxwell law:ThusThe electric field and magnetic field oscillate in phase, perpendicular to one another and to propagation; points along .
For a plane electromagnetic wave with linear polarization, write and . The Poynting vector is instantaneous energy flux:The light intensity is its cycle average, not its peak:An incident electromagnetic wave transports longitudinal momentum per energy . Perfect reflection back along the incident direction reverses that momentum, transferring to the mirror. Dividing by illuminated area and time gives the mean radiation pressureHere denotes the incident travelling wave. The average net Poynting vector of the incident-plus-reflected standing wave is zero, although its radiation pressure is nonzero.
In SI units, the Maxwell equations in vacuum with prescribed charge density and current density areWhen and , take the curl of the third equation and substitute the fourth. Using the curl of the curl identity and gives the electromagnetic wave equation:For example, , is a plane electromagnetic wave provided . The electric field, magnetic field and propagation direction are mutually perpendicular.
The Maxwell equations are linear, so the superposition principle applies to fields. However, the Poynting vector is quadratic:One may add the average wave intensities only when the cross terms vanish under the actual detector average. For co-propagating plane electromagnetic waves of parallel linear polarization, averaging over optical cycles but potentially resolving the difference frequency givesIf the detector integrates for , the last term acquires , with sinc function convention , evaluated at the midpoint phase. Thus suppresses beats, and the infinite-time average adds the wave intensities exactly for distinct fixed frequencies. Random mutually uncorrelated wave phases also remove the cross terms in an ensemble average; orthogonal linear polarizations remove them for co-propagating waves in polarization-insensitive detection. Merely having different frequencies does not remove a resolved beat signal: two nearly equal frequencies with fixed relative wave phase are a concrete counterexample. For different propagation directions, the relevant addition is of average Poynting vectors, or their components through the chosen detector surface.
For propagation along , a transverse wave has two perpendicular displacement components. With , write , . Their trajectory at a fixed point obeysThe general nondegenerate trajectory is an ellipse: elliptical polarization. For or , the components remain in phase or antiphase and the trajectory collapses to a line. A single nonzero component is also linearly polarized. Equal amplitudes with give circular polarization. Unequal quadrature amplitudes give an ellipse aligned with the chosen axes, while general phase differences rotate its axes.
For the displayed convention and , at the vector starts at and moves towards as time increases. Reversing reverses its rotation. Right- and left-handed labels require a stated viewing and phase convention, so rotation is defined explicitly here. A fixed ellipse is a coherent relationship between transverse components; unpolarized light instead has fluctuating orientation and phase relationships on the measurement timescale.
A linear polarizer transmits a linearly polarized beam with intensity proportional to , allowing its direction to be measured by an analyser. circular polarization transmits equal intensity through any linear analyser, but that test alone does not distinguish it from unpolarized light. A quarter-wave plate converts a suitable coherent circular state to linear polarization, allowing the combination to discriminate them. For light the electric field defines the usual polarization; the magnetic field remains perpendicular to it and to propagation. Longitudinal sound in a homogeneous gas lacks the two transverse degrees of freedom needed for these polarization states.





