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Atmospheric physics
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== Aeronomy == {{Main|Aeronomy}} [[Image:Upperatmoslight1.jpg|250px|thumb|right|Representation of upper-atmospheric lightning and electrical-discharge phenomena]] Aeronomy is the science of the upper region of the atmosphere, where dissociation and ionization are important. The term aeronomy was introduced by Sydney Chapman in 1960.<ref>Andrew F. Nagy, p. 1-2 in ''Comparative Aeronomy'', ed. by Andrew F. Nagy ''et al.'' (Springer 2008, {{ISBN|978-0-387-87824-9}})</ref> Today, the term also includes the science of the corresponding regions of the atmospheres of other planets. Research in aeronomy requires access to balloons, satellites, and [[sounding rockets]] which provide valuable data about this region of the atmosphere. [[Atmospheric tide]]s play an important role in interacting with both the lower and upper atmosphere. Amongst the phenomena studied are [[upper-atmospheric lightning]] discharges, such as luminous events called red [[sprites (lightning)|sprites]], sprite halos, blue jets, and elves.
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