
Electromagnetic radiation with wavelengths longer than visible light, useful for observing through dust.Infrared radiation is electromagnetic radiation with wavelengths longer than visible light, typically from about 700 nanometers to 1 millimeter. It is emitted by all objects with a temperature above absolute zero, making it a universal probe of warm matter. In astronomy, infrared observations are crucial because dust particles in space absorb visible light and re-emit it in the infrared, allowing astronomers to see through dusty regions and study the early universe, star formation, and the centers of galaxies.
Infrared radiation was discovered in 1800 by William Herschel, who used a prism to split sunlight and measured the temperature increase beyond the red end of the spectrum. Astronomical infrared observations began in the 1960s with ground-based telescopes, and space-based missions like IRAS (1983) and Spitzer (2003) revolutionized the field.
Infrared radiation arises from the thermal motion of atoms and molecules: as they vibrate and rotate, they emit photons in the infrared range. In space, dust grains heated by starlight radiate in the infrared, and this emission can penetrate the dust clouds that block visible light. Infrared detectors, such as those on the James Webb Space Telescope, are cooled to very low temperatures to reduce their own thermal noise, enabling them to detect faint infrared signals from distant objects. The atmosphere absorbs much of the infrared, so many observations are done from space or high-altitude sites.
Infrared technology is used in night-vision devices, thermal imaging cameras for medical and industrial diagnostics, remote controls, and fiber-optic communications, as well as in astronomy to study star formation, exoplanet atmospheres, and the early universe.
Infrared radiation is what makes a warm object visible to a thermal camera: even in complete darkness, a person emits enough infrared light to be imaged clearly.

















