Consider one selected polarization of waves, represented by complex fields and at two sampling positions. Suppose their second moments are finite and stationary: and the following uncentered wave-field correlation do not depend on the absolute time . Define
The star denotes the complex conjugate; brackets denote an ensemble average. A long detector average estimates this quantity only if it adequately samples the fluctuations. The superscript identifies a field correlation: it does not mean the autocorrelation of the measured light intensity. The one-position version is , so for every nonzero field covered by this definition; this alone says nothing about its correlation at nonzero delay. [ref].
The Cauchy-Schwarz inequality gives . At a specified delay, magnitude one means in mean square for a fixed nonzero complex : the samples have a reproducible relation in both wave amplitude and wave phase. Magnitude zero means the averaged field cross term vanishes. It need not mean statistical independence. A deterministic phase difference changes the argument of , not its complex modulus; a distorted but fixed wavefront can therefore remain fully coherent. [ref].
To see the observable, recombine the samples in the same detected spatial mode with matched wave polarizations. With a common positive conversion factor , let be the single-arm light intensities reaching that detector. Adding gives
This follows simply by expanding the squared complex modulus and averaging, then taking the maximum and minimum as spans a full cycle. The extra wave phase scan must leave and the magnitude of the correlation effectively unchanged. Thus interferometric visibility equals only for equal nonzero light intensities and ideal mode matching. For , perfectly coherent beams have interferometric visibility ; a measured value would imply under these assumptions. Orthogonal linear polarizations, background light, unresolved interference fringes or vibrations can reduce measured contrast further. One absent arm gives zero contrast and makes the normalized two-sample correlation undefined.
Interference fringe 2026-10-14
An interference fringe is a spatial band of enhanced or reduced wave intensity caused by a spatially varying phase difference. Uniform crossing plane waves produce straight parallel interference fringes; curved wavefronts can give curved bands. The interference fringes mark the relative wave phase, rather than the individual instantaneous wavefronts.
The distance between adjacent bright interference fringes, or between adjacent dark interference fringes, measured along a specified direction. For the symmetric crossing plane waves in wave interference, measured along , . Bright-to-dark separation is . As tends to zero the spacing diverges; at the phase difference is spatially constant and there are no periodic bands.
Interference (wave propagation) Created 2026-10-05 Updated 2026-10-14
Wave interference is the reinforcement or cancellation that occurs when overlapping wave amplitudes add by the superposition principle. For two monochromatic waves of the same frequency, mutual optical coherence means that their relative wave phase is stable during the observation. Equal wave phases give constructive interference; a half-cycle phase difference gives the destructive interference intensity minimum. Wave amplitudes add before their squares determine wave intensity. [ref].
Consider two overlapping beams in a homogeneous medium, with the same polarization of an electromagnetic wave and individual local time-averaged light intensities . Their phase difference is measured in radians. In the scalar detection convention, the combined local time-averaged wave intensity is
The last term records wave interference; adding alone misses it. The formula describes irradiance when both fields propagate along the same direction, or when the same detector geometry factor is included in all three intensities. For crossing beams it describes the squared electric field response, proportional to scalar wave intensity; a specified component of the Poynting vector also requires the propagation geometry. The ideal crossing plane waves below make that distinction explicit.
For equal individual light intensities , the cosine half-angle identity gives
The constructive interference intensity is at modulo , and the destructive interference intensity is zero at modulo . At phase quadrature, , it is . With and in the same arbitrary wave intensity unit, the maximum is , the minimum is , and the phase quadrature value is : unequal wave amplitudes cannot cancel completely.
Figure 1.
Two-beam wave intensity versus phase difference: equal beams reach 4 and 0; unequal beams reach 2.25 and 0.25
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Both curves use the same wave intensity unit and a horizontal angle in radians. The dashed levels are the averages over a full phase difference cycle. Equal beams have interferometric visibility one; the unequal example has interferometric visibility .
A spatially varying phase difference turns the same law into interference fringes. Take two ideal plane electromagnetic waves with common wavelength , equal individual light intensities , and propagation directions at angles and from the axis in the plane, with . Both have linear polarization along , perpendicular to both propagation directions. Choose equal initial wave phases; their wavevectors and phase difference are
Here is the wavenumber and the angular frequency. The common and time terms cancel, so the interference fringes stay at fixed for every . Their interference fringe spacing is
Set the length unit to , so that , and take : then . The constructive interference intensity bands lie at integer ; the destructive interference intensity bands lie at half-integer .
Figure 2.
Ideal crossing plane waves at : stationary interference fringes with spacing one wavelength
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The grid covers and ; both axes are dimensionless lengths in wavelength units. The colour scale is from zero to four, using the same single-beam normalization as the equal-beam curve above. This is an ideal plane wave superposition, with no slits or point sources and no near-field approximation. For these -polarized plane electromagnetic waves in vacuum, the longitudinal time-averaged Poynting vector obeys ; the plotted scalar therefore differs from the irradiance through a plane normal to by that common factor. This relation follows by adding the magnetic fields as well as the electric fields.
The bright peaks do not create energy. Averaging over one interference fringe spacing, or equivalently over one full phase difference cycle, gives
because the integral of the cosine is zero, with sine as its antiderivative. Equal beams thus average to , despite bright bands at . For the crossing-wave geometry, the average longitudinal energy flux is correspondingly . Bright and dark regions redistribute the incoming energy; conservation of energy concerns the full energy flux, rather than the height of one peak.
Wave interference is useful because phase differences convert small changes in optical path length into measurable changes of wave intensity, as in a Mach-Zehnder interferometer. Its beauty is that the same superposition principle produces both complete cancellation and fourfold brightening; adding more coherent contributions also produces the narrow peaks of a diffraction grating. Feynman's treatment connects this many-source pattern directly to addition of complex amplitudes. [ref].
A short proof outline uses local real fields with parallel linear polarizations. Write and for the same positive conversion factor . Averaging over many wave periods while the phase difference stays fixed uses and , giving the stated law. Equivalently, add the complex amplitudes and take the squared complex modulus. [ref].
For different fixed linear polarizations in a common transverse plane, the cross term acquires the dot product of their real unit vectors, equal to for relative angle . Orthogonal linear polarizations remove the cross term in polarization-insensitive scalar detection; different orientations generally only reduce it. A common polarizer can select overlapping components and recover wave interference. Likewise, rapid random variation of the phase difference removes the observed cross term only when the detector's time average has . Slowly varying wave phases can instead move resolved interference fringes, and biased or incompletely sampled wave phases can leave residual contrast. Finite optical coherence therefore depends on the observation time as well as the fields.
Interferometric visibility measures the contrast of a scanned interference fringe. For the mutually coherent, equally polarized two-beam model in wave interference, with fixed individual wave intensities and , the constructive interference intensity and destructive interference intensity give
Equal nonzero wave intensities give ; give . Unequal wave intensities can therefore reduce interferometric visibility even with perfect mutual optical coherence. Random phase differences or distinguishable wave polarizations can reduce it further; zero contrast alone does not identify the cause. Both intensities zero leave the ratio undefined.
For normalized paths with complex amplitudes and identical internal states, the output probability is , so . A photon polarization fringe alone determines transverse quantum coherence but not the sign of the population difference.
// Target: optics.bigb
Optical path length Created 2026-10-05 Updated 2026-10-14
An optical path length measures how much propagation wave phase a path accumulates, expressed as the distance that would accumulate the same wave phase in vacuum. A centimetre in a uniform medium with refractive index has optical path length , although its geometric length remains . This makes optical path length useful whenever two contributions must arrive with matching wave phases, from an optical lens to a Michelson interferometer. [ref]
For a specified path at fixed angular frequency , the optical path length is the line integral
Here is geometric arc length, and is the phase refractive index, evaluated at the same frequency everywhere. The propagation interpretation assumes a stationary linear medium with isotropy, a real positive scalar refractive index and negligible loss, on a valid geometrical optics branch. The path can curve; at sharp interfaces apply the appropriate matching conditions to each segment. A prescribed curve has a mathematical line integral, but it predicts a propagation wave phase only when it represents the physical branch. [ref] Optical fibers can require a mode wavenumber rather than the bulk refractive index along a guessed light ray. [ref]
Fix the vacuum wavelength , with frequency and vacuum wavenumber . In a locally uniform medium the wavelength is , while the frequency stays unchanged at a stationary interface. With the convention , propagation from a specified starting wave phase contributes
The relative reference includes launch wave phases and any extra wave phase from mirrors, beam splitters or coatings. Thus is a propagation contribution, not an absolute detector wave phase independent of the apparatus. If the reference contributions stay fixed, a change in optical path difference changes the phase difference by . Using the material wavelength again in this formula would count the refractive index twice. [ref]
A motivating measurement turns invisible optical oscillations into a slowly changing electrical signal. MIT's teaching experiment uses a laser, a beam splitter, two returning mirrors, an amplified photodiode, an oscilloscope and a calibrated mirror actuator driven by a function generator. The returning beams overlap on the photodiode; one channel records detector voltage and another the actuator drive. The measured observable is the changing light intensity, including its maxima and minima, rather than direct timing of an optical cycle. A calibrated displacement per drive voltage and the spacing of the extrema relate geometric motion to the phase difference. The guide infers the laser wavelength from known actuator calibration; conversely, with independently known vacuum wavelength and ambient refractive index, the same relation calibrates mirror motion. These two unknowns cannot both be inferred from fringe spacing alone. [ref]
For a proposed change-of-medium measurement, keep the mirrors fixed and put a transparent cell of internal length in one arm. Compare its contents at refractive indices and , leaving its windows in place. At normal incidence the two traversals give
Here is the signed number of whole interference fringe cycles plus any resolved fractional cycle, counted continuously. A mirror displacement instead gives ; distinguish this double-pass factor from a single pass in a Mach-Zehnder interferometer. OpenStax's gas-cell worked example provides the same double-pass reasoning; it is a teaching calculation rather than a published measurement dataset.[ref]
An exact toy calculation makes the sensitivity visible. Stipulate , and . Then and : a full interference fringe cycle, despite unchanged geometric lengths. For a continuous change , let and choose the initial detector phase difference to be zero. Equal coherent detected arm contributions of light intensity predict
The plot is this stipulated model: gives a minimum, restores a maximum, and the reference level is chosen by adjustment of the apparatus. It contains no measured values or assigned properties of a real gas. The equivalent mirror travel in vacuum is per cycle. A single endpoint light intensity cannot distinguish from ; the continuous fringe count carries the missing information.
For an interpretable cell measurement, establish the initial phase difference with a small calibrated mirror scan, then track slow changes through successive interference fringes. Measure the dark signal and each arm separately, keep photodiode gain within its linear range, align both beams on the same region and match their linear polarizations. Monitor interferometric visibility and keep arm delays within the useful optical coherence time. Record cell length, contents, pressure and temperature; return to the starting condition to check drift. Changes in window deformation, cell length, external air or mirror position also change optical path length, so a reference cell or an independently monitored mechanical path is needed to isolate the contents' refractive index. These controls are deductions from the model, not a claim that the illustrated apparatus was operated. Loss of fringe count leaves a whole-cycle ambiguity; at an intensity extremum the first derivative with respect to phase difference vanishes, so a scan around phase quadrature is more sensitive to small changes. Broadband illumination, unstable optical coherence, vibration and strong loss can invalidate a simple one-frequency inference.
Spatial optical coherence 2026-10-14
Spatial optical coherence compares field samples at different positions, usually across a transverse plane at equal time. Two small openings separated by sample this correlation: recombine their light with nearly matched travel times and measure interferometric visibility near the central interference fringes. A narrow opening in front of a broad-spectrum lamp can improve transverse spatial optical coherence while leaving its short temporal optical coherence. These are separate controls: narrow spectral selection by itself need not make an extended source spatially coherent. MIT's lecture notes illustrate the two-opening test and these contrasting source preparations. [ref].
To isolate source width, stipulate a distant, narrowband source with uniform angular brightness on , and mutually uncorrelated emission from distinct source directions. Here is the full angular width in radians, the common wavelength, and the two openings are separated by along the same transverse direction as the source extent. Neglect amplitude differences across the openings. Each source direction contributes a phase difference approximately . Averaging its complex cross term gives
The sinc function is extended continuously to one at . The sign convention in the exponential depends on which opening is numbered first; the symmetric model gives the same real result either way. Equal detected single-opening light intensities make the magnitude equal to interferometric visibility. A displaced source center adds a deterministic wave phase, shifting the interference fringes without changing their contrast.
Figure 1.
Calculated spatial optical coherence for a stipulated uniform incoherent angular source: wider sources wash out and invert interference fringes
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The strips show with equal single-opening light intensities, a common phase difference coordinate and no single-slit diffraction envelope. At , contrast is ; at , it vanishes. At , the correlation is : weak fringes return with bright and dark positions exchanged. For and , the first zero occurs at . This is a calculated example, not an experimental measurement or a universal source-width law.
A proposed source-width control follows directly from this model: illuminate two fixed openings with a distant adjustable luminous slit of full width at distance , so under the small-angle approximation, and hold and the spectral selection fixed. Increasing overlays more mutually incoherent, displaced interference fringe patterns. Record profiles over several near-central fringes, measure each opening separately and correct intensity imbalance as in first-order optical coherence. Restrict the recorded region so the path difference stays small compared with the optical coherence length, and resolve the fringes with the detector. Real source nonuniformity, finite opening widths and spectral spread modify the stipulated sinc function law. This protocol is a model-based extension of the verified two-opening method, not a claim that the plotted curves were measured.
Thus an extended incoherent source can give locally excellent wave interference when the sampled separation is small, and almost none when it is larger. The useful scale expresses how source extent limits the aperture over which coherent addition is available. The same angular averaging explains why narrowing a source opening can recover visible interference fringes, even without narrowing its optical spectrum.