Ozone destruction by chlorine radicals within the Antarctic vortex: The spatial and temporal evolution of ClO-O3anticorrelation based on in situ ER-2 data

Author:

Anderson J. G.,Brune W. H.,Proffitt M. H.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference6 articles.

1. Kinetics of O3 destruction by C1O and BrO within the Antarctic vortex: An analysis based on in situ ER-2 data;Anderson;J. Geophys. Res.,1989

2. In situ observations of C1O in the Antarctic: ER-2 aircraft results from 54° to 72°S latitude;Brune;J. Geophys. Res.,1989

3. Ozone and aerosol measurements in the springtime Antarctic stratosphere in 1985;Hofmann;Geophys. Res. Lett.,1986

4. Production of C12O2 from the self reaction of the C1O radical;Molina;J. Phys. Chem.,1987

5. Meteorological atlas of the southern hemisphere lower stratosphere for August and September 1987;Newman,1988

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