Category:Airglow

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Airglow is the very weak emission of light by the upper atmosphere. It is caused by various processes such as the recombination of ions which were photoionized by the sun during the day, luminescence caused by cosmic rays striking the upper atmosphere, and chemiluminescence.

Airglow (it); রাতের আভা (bn); Lumière du ciel nocturne (fr); Loftljómi (is); Natthimmellys (nn); Světelné záření atmosféry (cs); Власне світіння атмосфери (uk); airglow (ca); airglow (en); Airglow (de); Khí huy (vi); Airglow (es); هواتاب (fa); 大氣光 (物理學) (zh); Gök Aydınlığı (tr); Lumina cerului nocturn (ro); 大気光 (ja); Собственное свечение атмосферы (ru); Légköri fény (hu); Airglow (lb); Poświata niebieska (pl); זוהר אוויר (he); Airglow (nl); Airglow (nb); Pijaran udara (id); Teja udara (ms); ilmahehku (fi); Атмосфераның өзіндік жарқырауы (kk); توهج ليلي (ar); Ατμοσφαιρική φωταύγεια (el); luminescência atmosférica (pt) debole luminescenza notturna dell'atmosfera terrestre (it); a napsugárzás által keltett éjszakai fény (hu); faint emission of light by a planet's upper atmosphere (en); انتشار ضعیف نور توسط جو (fa); emisi cahaya oleh atmosfer bumi (id) Luminosità del cielo notturno (it); Nachthimmelsleuchten (de); Lumière Du Ciel Nocturne, Lumiere du ciel nocturne (fr); Capas de airglow, Airglow (pt); Airglow, Geokorona, Demringslys (nn); إشعاع جوي (ar); Самостійне світіння неба (uk); Capas de airglow (es)
airglow 
faint emission of light by a planet's upper atmosphere
Cupola above the darkened Earth.jpg
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Subclass ofatmospheric optical phenomenon
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Media in category "Airglow"

The following 158 files are in this category, out of 158 total.