Sep 1983
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1983p%26ss...31.1053d&link_type=abstract
(European Geophysical Society, Meeting on the Structure of the Upper and Middle Atmosphere, Leeds, England, Aug. 23-27, 1982) Pl
Physics
5
Annual Variations, Atmospheric Composition, Ozone, Ozonosphere, Stratosphere, Vertical Distribution, Aeronomy, Atmospheric Circulation, Gas Transport, Man Environment Interactions, Solar Activity Effects, Volcanoes
Scientific paper
The annual and long-term variations in the atmospheric ozone layer were examined on the basis of 55 yr of data taken at Aroya, Switzerland and 25 yr of data gathered by the global ozone network. Attention was given to annual and biennial variations, which showed that the midlatitude peak concentration was affected by a quasi-biennial variation of the tropical stratospheric circulation. Smaller scale circulation patterns were dominant in the lower stratosphere, although an observed negative trend of the total ozone was equally distributed between the troposphere and 24 km altitude. The global ozone increase detected in the 1960s was possible due to general circulation alterations, but may also have been influenced by injection of NO(x) into the atmosphere during atomic bomb testing.
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