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Study of the effectiveness of the Cl/sub x/ catalytic ozone loss mechanisms

Conference ·
OSTI ID:6259761
The importance of catalytic mechanisms involving chlorine species for destroying stratospheric ozone is now well recognized. A number of chlorinated halocarbons have been suggested as anthropogenic sources of stratospheric chlorine. In particular the potential impacts on stratospheric ozone of surface release of CF/sub 2/CL/sub 2/, CFCl/sub 3/ and CH/sub 3/CCl/sub 3/ have been studied extensively previously. With the current understanding of atmospheric photochemical processes, there are now at least three other ozone destroying catalytic cycles involving chlorine species in addition to the well known Cl-C10 catalytic cycle that are of varying importance in the stratosphere. Because of the differences in the vertical distributions of the concentration of the relevant chemical species the most effective altitudes for each cycle are different. Since an individual halocarbon releases chlorine atoms over a range of different altitudes in the stratosphere, its impact on stratospheric ozone must be due to the combined effect of each of these cycles. In this study, a comparison is made of the relative roles of these catalytic cycles for destroying stratospheric ozone when emissions for various halocarbons are considered. It is concluded that there are at least four catalytic cycles for odd oxygen destruction involving chlorine species. The relative efficiency of these cycles vary significantly with altitude. Changes in the ozone vertical distribution from various halocarbon perturbations were found to be different in shape. This was due to the differences in the altitude range of inorganic chlorine release resulting from halocarbon destruction and to the differences in relative catalytic cycle efficiencies.
Research Organization:
Lawrence Livermore National Lab., CA (USA)
DOE Contract Number:
W-7405-ENG-48
OSTI ID:
6259761
Report Number(s):
UCRL-84071; CONF-800869-3
Country of Publication:
United States
Language:
English