The blue hour (from French l'heure bleue;[1][a] pronounced [lœʁ blø]) is the period of twilight (in the morning or evening, around the nautical stage) when the Sun is at a significant depth below the horizon and residual, indirect sunlight takes on a predominantly blue shade, which differs from the one visible during most of a clear day, which is caused by Rayleigh scattering.
The blue hour occurs when the Sun is far enough below the horizon so that the sunlight's blue wavelengths dominate due to the Chappuis absorption caused by ozone.[2] Since the term is colloquial, it lacks an official definition similar to dawn, dusk, and the three stages of twilight. Rather, it refers to a state of natural lighting that usually occurs around the nautical stage of the twilight period (at dawn or dusk).[3]
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