The importance of the reactions between OH and ClO for stratospheric ozone
- 19 November 1993
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 20 (22) , 2447-2450
- https://doi.org/10.1029/93gl02999
Abstract
No abstract availableKeywords
This publication has 15 references indexed in Scilit:
- Stratospheric ozone depletion by CIONO2 photolysisNature, 1993
- Potential impact of combined NOx and SOx emissions from future high speed civil transport aircraft on stratospheric aerosols and ozoneGeophysical Research Letters, 1993
- Chlorine catalyzed destruction of ozone: Implications for ozone variability in the upper stratosphereGeophysical Research Letters, 1993
- A model study of ATMOS observations and the heterogeneous loss of N2O5 by the sulphate aerosol layerJournal of Atmospheric Chemistry, 1993
- A potential new source of OH and odd‐nitrogen in the atmosphereGeophysical Research Letters, 1993
- Submillimeterwave heterodyne measurements of stratospheric ClO, HCl, O3, and HO2: First resultsGeophysical Research Letters, 1992
- On the limitation of steady-state expressions as tests of photochemical theory of the stratosphereJournal of Atmospheric and Terrestrial Physics, 1992
- More rapid polar ozone depletion through the reaction of HOCI with HCI on polar stratospheric cloudsNature, 1992
- Changing Composition of the Global StratosphereScience, 1989
- Rate constant and branching ratio for the reaction of hydroxyl with chloride oxide (ClO)The Journal of Physical Chemistry, 1986