OClO as observed by TROPOMI: a comparison with meteorological parameters and polar stratospheric cloud observations

Chlorine dioxide (OClO) is a by-product of the ozone-depleting halogen chemistry in the stratosphere. Although it is rapidly photolysed at low solar zenith angles (SZAs), it plays an important role as an indicator of the chlorine activation in polar regions during polar winter and spring at twilight...

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Bibliographic Details
Published in:Atmospheric Chemistry and Physics
Main Authors: Pukite, J., Borger, C., Dörner, S., Gu, M., Wagner, T.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2022
Subjects:
Online Access:http://hdl.handle.net/21.11116/0000-0009-CB81-0