Atmospheric Inversion 1
Atmospheric Inversion 1 : (1) Departure from the usual increase or decrease with altitude of the value of an atmospheric property (in fire management usage, nearly always refers to an increase in temperature with increasing height). (2) The layer through which this departure occurs (also called inversion layer). The lowest altitude at which the departure is found is called the base of the inversion. See also: Atmospheric Stability; Inversion; Stable Layer of Air
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