Tropospheric ozone depletion events

Chemical mechanism of the bromine explosion. The blue area at the bottom represents the condensed phase (liquid brine or ice surface).

Tropospheric ozone depletion events are phenomena that reduce the concentration of ozone in the earth's troposphere. Ozone (O3) is a trace gas which has been of concern because of its unique dual role in different layers of the lower atmosphere.[1] Apart from absorbing UV-B radiation and converting solar energy into heat in the stratosphere, ozone in the troposphere provides greenhouse effect and controls the oxidation capacity of the atmosphere.[1]

  1. ^ a b Cao, Le; Platt, Ulrich; Gutheil, Eva (2016-05-01). "Role of the boundary layer in the occurrence and termination of the tropospheric ozone depletion events in polar spring". Atmospheric Environment. 132: 98–110. Bibcode:2016AtmEn.132...98C. doi:10.1016/j.atmosenv.2016.02.034. ISSN 1352-2310.

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