Mechanisms of the formation and decay of the secondary maximum in the vertical distribution of ozone density in the lower polar stratosphere

Details Mechanisms of the formation and decay of the secondary maximum in the vertical distribution of ozone density in the lower polar stratosphere Mechanisms of the formation and decay of the secondary maximum in the vertical distribution of ozone density in the lower polar stratosphere

Feb 1993

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1993dokan.328..671o&link_type=abstract

Rossiiskaia Akademiia Nauk, Doklady (ISSN 0869-5652), vol. 328, no. 6, p. 671-673.

Physics

Galactic Cosmic Rays, Ozonosphere, Polar Regions, Stratosphere, Vertical Distribution, Atmospheric Models, Equatorial Atmosphere, Gas Density, Photochemical Reactions

Scientific paper

Physical mechanisms are described which have been proposed to account for the formation and decay of the secondary maximum oxone density in the lower polar stratosphere. The mechanisms discussed are related to the effect of galactic cosmic rays, which are thought to be the primary factor responsible for the observed increase in the total ozone content in the polar stratosphere in comparison with the equatorial stratosphere. The decay dynamics of the secondary ozone density maximum is examined with reference to the results of numerical photochemical modeling.

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