Compared to the absorption of ultraviolet light by the ozone layer, known as the Hartley and Huggins absorptions, Chappuis absorption is distinctly weaker.[3] Along with Rayleigh scattering, it contributes to the blue color of the sky, and is noticeable when the light has to travel a long path through the Earth's atmosphere. For this reason, Chappuis absorption only has a significant effect on the color of the sky at dawn and dusk, during the so-called blue hour.[4] It is named after the French chemist James Chappuis (1854–1934), who discovered this effect.[5]
^Der Brockhaus Wetter und Klima : Phänomene, Vorhersage, Klimawandel (in German) (1. Aufl ed.). Leipzig: Brockhaus, F A. 2009. p. 54. ISBN9783765333811. OCLC316287956.