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Other meanings of Astronomical interferometer

Astronomical instrumentation

Astronomical interferometer

An astronomical interferometer is an instrument combining multiple telescopes to achieve high angular resolution. It compares the phase and brightness of light or radio waves collected along separate paths, allowing observations equivalent in resolving power to a much larger telescope while retaining the light-gathering limits of its individual apertures.

λ/B
Angular resolution
Set mainly by wavelength divided by maximum baseline
2 or more
Collecting elements
Separate telescopes, dishes, or apertures
Optical, infrared, radio
Principal bands
Different wavelengths require different beam-combination methods
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Principle and design

An astronomical interferometer derives fine angular detail from interference between waves collected at separated apertures. The separation, or baseline, determines the finest spatial scale that can be resolved: approximately wavelength divided by baseline length. The instrument does not behave exactly like a filled single mirror of that diameter, because its collecting area and sampled spatial frequencies remain those of the separate telescopes.

Signals must be synchronized and their path lengths controlled to a fraction of a wavelength. Optical and infrared arrays usually transport beams through mirrors, delay lines, and beam combiners; radio arrays preserve the signals electronically and correlate them after reception. Earth rotation changes the projected baseline during an observation, filling additional points in the measured spatial-frequency plane.

The measured quantity is often called visibility, the contrast of the interference pattern. Repeated visibilities at different baselines and wavelengths can be modeled or inverted to estimate a star's diameter, a disk's structure, or another source's brightness distribution.

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Development and major facilities

The modern field began with Michelson's stellar-diameter measurements, which demonstrated that separated apertures could measure angular sizes smaller than an individual telescope could resolve directly.1 Early optical instruments were limited by atmospheric turbulence, vibration, and the extreme precision required to maintain equal optical paths.

Radio astronomy made long-baseline synthesis more practical because receivers can convert incoming waves into stable electronic signals. Very Long Baseline Interferometry links antennas separated by hundreds or thousands of kilometres, while arrays such as the Atacama Large Millimeter/submillimeter Array combine many dishes on movable configurations in the Chilean Andes.

At optical and infrared wavelengths, the Very Large Telescope Interferometer combines beams from the European Southern Observatory's unit telescopes and auxiliary telescopes. The CHARA Array, on Mount Wilson, uses six one-metre telescopes spread across a much larger area than a single optical telescope's aperture.2

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Scientific uses

Interferometers measure stellar surfaces, circumstellar environments, and compact structures that ordinary imaging cannot separate. Angular diameters and shapes of nearby stars test stellar-atmosphere models, while infrared observations trace hot dust around young stars, evolved stars, and active galactic nuclei.3

Radio arrays map molecular gas, star formation, jets, and magnetic-field-related emission. By combining baselines and Earth-rotation synthesis, astronomers can reconstruct images ranging from protoplanetary disks to the environments of black holes. The Event Horizon Telescope is a global millimetre-wave very-long-baseline array whose observations produced horizon-scale images of M87* and the centre of the Milky Way.4

Interferometry also supports precision measurements of stellar motion and has contributed to the characterization of disks and companions around other stars. Its strength is angular resolution; its limitations include incomplete spatial-frequency coverage, lower sensitivity than a filled aperture of the same diameter, and difficult image reconstruction.

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Lesser-known aspects

Closure phase makes some interferometers unusually resistant to calibration errors. For three or more apertures, adding measured phases around a triangle cancels many errors introduced by individual telescopes and atmospheric paths. Nonzero closure phases can reveal asymmetry, such as a spotted star, an uneven disk, or a companion, even when conventional visibility data alone are ambiguous.2

Interferometers sample Fourier components rather than taking ordinary pixel-by-pixel photographs. Sparse or uneven sampling can create sidelobes and imaging artifacts, so observations are planned to improve the distribution of baselines and are reconstructed with carefully tested algorithms. A mathematically sharp nominal resolution therefore does not guarantee a complete or artifact-free image.

Some arrays combine telescopes that are not permanently fixed: moving radio dishes change configuration to trade angular resolution against surface-brightness sensitivity. At optical wavelengths, adaptive optics and fringe tracking are often essential, while at radio wavelengths time and frequency standards, atmospheric phase correction, and high-rate correlation dominate the engineering challenge.

Glossary

Baseline
The separation vector between two collecting apertures; its projected length and orientation determine the spatial information measured.
Visibility
The amplitude of an interference signal, related to the Fourier transform of a source's brightness distribution.
Closure phase
A phase combination measured on a triangle of baselines that cancels many telescope-specific phase errors.
Very Long Baseline Interferometry
Radio interferometry using antennas separated by very large distances, often with independently recorded signals correlated later.

Angular resolution depends on wavelength, projected baseline, calibration, signal-to-noise ratio, and the quality of spatial-frequency coverage; the simple λ/B relation is an approximate resolving scale rather than a complete description of image quality.