opticalultraviolet

Opticalultraviolet refers to the region of the electromagnetic spectrum that lies just beyond the visible optical range, typically spanning wavelengths from about 300 to 400 nanometres. It lies between the visible light we perceive with the eye and the far‑ultraviolet (FUV) range, which starts roughly at 200 nanometres. Because of this position, opticalultraviolet radiation carries enough energy to excite electronic transitions in atoms and molecules, yet it is less energetic than shorter‑wavelength ultraviolet, making it useful for a wide range of scientific studies.

In astronomy, opticalultraviolet observations are essential for examining the atmospheres of stars with temperatures between about 5,000 and 10,000 kelvin. Features such as hydrogen Balmer series lines and metal absorption lines emerge strongly in this window, providing information on stellar composition, temperature, and velocity fields. Space‑based telescopes, such as the Hubble Space Telescope, use specialized detectors and coatings to maximise sensitivity in the 300–400 nm band, avoiding the atmospheric absorption that blocks most ultraviolet from ground‑based instruments.

The opticalultraviolet region is also exploited in laboratory spectrophotometry, photochemistry, and the calibration of solar radiation models. Because Earth’s atmosphere absorbs most radiation below 300 nm, only high‑altitude or space platforms can provide continuous monitoring. Researchers utilize narrow‑band imaging and spectroscopy to isolate specific spectral features in this range, enabling precise measurements of elemental abundances and interstellar medium conditions.

Overall, opticalultraviolet serves as a critical bridge between visible light and more energetic ultraviolet regimes, offering a valuable diagnostic window into the physical processes governing stars, galaxies, and other astrophysical sources.