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===Airglow of the Earth=== The Earth's night sky is illuminated by diffuse light, called [[airglow]], that is produced by radiative transitions of atoms and molecules.<ref>{{cite journal | vauthors = Silverman SM | title = Night airglow phenomenology. | journal = Space Science Reviews | date = October 1970 | volume = 11 | issue = 2 | pages = 341β79 | doi = 10.1007/BF00241526 | bibcode = 1970SSRv...11..341S |bibcode-access=free | s2cid = 120677542 |url=http://adsabs.harvard.edu/full/1970SSRv...11..341S |url-status=live |archive-url=https://web.archive.org/web/20231005001746/https://adsabs.harvard.edu/full/1970SSRv...11..341S |archive-date= Oct 5, 2023 }} </ref> Among the most intense such features observed in the Earth's night sky is a group of infrared transitions at wavelengths between 700 nanometers and 900 nanometers. In 1950, [[Aden Meinel]] showed that these were transitions of the hydroxyl molecule, OH.<ref>{{cite journal | vauthors = Meinel AB |title=OH Emission Bands in the Spectrum of the Night Sky. I |journal=Astrophysical Journal |volume=111 |pages=555β564 |year=1950 |doi=10.1086/145296 |doi-access=free |bibcode=1950ApJ...111..555M |bibcode-access=free |url=http://articles.adsabs.harvard.edu/pdf/1950ApJ...111..555M |url-status=live |archive-url= https://web.archive.org/web/20221024073717/https://articles.adsabs.harvard.edu/pdf/1950ApJ...111..555M |archive-date= Oct 24, 2022 }}</ref>
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