of two or more separate reactions.In the ozone layer (15-35 km), chlorine supply gases are still present and HCl and ClONO2 are the most abundant reactive chlorine gases at midlatitudes. HNO3 is an ample, primarily naturally-occurring stratospheric compound that plays a significant function in stratospheric ozone chemistry by both moderating ozone destruction and condensing to kind PSCs, thereby enabling conversion of chlorine reservoirs gases to ozone-destroying types. In the altitude range of the ozone layer at midlatitudes, as proven in Determine Q7-2, the reservoir gases HCl and ClONO2 account for many of the out there chlorine.
The measurements from space displayed in Determine Q7-2 are consultant of how the amounts
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