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airglow

[ air-gloh ]

noun

  1. a dim light from the upper atmosphere caused by emissions from atoms and molecules ionized by solar radiation: observed at night nightglow, during the day dayglow, and at twilight twilight glow, with each having slightly different characteristics.


airglow

/ ˈɛəˌɡləʊ /

noun

  1. the faint light from the upper atmosphere in the night sky, esp in low latitudes
“Collins English Dictionary — Complete & Unabridged” 2012 Digital Edition © William Collins Sons & Co. Ltd. 1979, 1986 © HarperCollins Publishers 1998, 2000, 2003, 2005, 2006, 2007, 2009, 2012


airglow

/ ârglō′ /

  1. A faint photochemical luminescence in the upper atmosphere caused by the collision of x-rays and charged particles from the Sun with atoms and molecules, especially of oxygen, sodium, and the hydroxyl radical (OH). Airglow is strongest over low and middle latitudes.


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Word History and Origins

Origin of airglow1

First recorded in 1950–55; air 1 + glow

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