Airglow is a faint glow propagated by the Earth's atmosphere at night. This faint glow is mainly caused by the recombination of excited atoms and molecules after absorbing solar energy during the day.
During the day, the Earth's atmosphere absorbs solar energy, especially in the upper layers of the atmosphere. When this solar energy is absorbed, the atoms and molecules (oxygen, nitrogen) present in the atmosphere become excited, that is, they acquire additional energy. Which can lead to the ionization of certain atoms and molecules. Ionization occurs when electrons are stripped from an atom, leaving one positively charged ion and one free electron.
During the night, when the direct input of solar energy is no longer present, these excited particles begin to return to their normal energetic state. Free electrons can recombine with ions to form neutral atoms or molecules. This recombination process releases energy in the form of photons, revealing a colored airglow.
Airglow is therefore a weak and diffuse glow which can be perceptible in certain places, far from the light pollution of urban areas.
Airglow colors can vary depending on the types of atoms and the level of excitation and the particular electronic transitions that occur. For example, when oxygen atoms are excited, they typically emit green or red light. When nitrogen atoms are excited, they typically emit in the blue and violet range.
The color of nocturnal airglow has a dominant blue-green color, while polar airglow is predominantly red. The airglow that occurs during the day (dayglow) is primarily blue.
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