Further interpretation of satellite measurements of Antarctic total ozone

Details Further interpretation of satellite measurements of Antarctic total ozone Further interpretation of satellite measurements of Antarctic total ozone

Nov 1986

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1986georl..13.1210s&link_type=abstract

Geophysical Research Letters (Supplement) (ISSN 0094-8276), vol. 13, Nov. 1986, p. 1210-1212.

Physics

13

Antarctic Regions, Atmospheric Composition, Ozonometry, Satellite Observation, Annual Variations, Autumn, Depletion, Spring (Season)

Scientific paper

Both dynamical and chemical mechanisms have been advanced to explain the decrease in total ozone in the Antarctic spring. Further analysis of satellite measurements show that during any one year, the September decline in total ozone near the South Pole is compensated by an increase at midlatitudes. The total ozone amount from 44 deg S to the pole remains almost unchanged from August through November even though both the polar and midlatitude values reach extremes during this period. These observations suggest that the variations within the spring season in south polar total ozone are governed by dynamical redistribution rather than chemical processes.

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