On the relationships between vertical ozone distribution and middle atmosphere dynamics during stratospheric warming at solar minimum

Details On the relationships between vertical ozone distribution and middle atmosphere dynamics during stratospheric warming at solar minimum On the relationships between vertical ozone distribution and middle atmosphere dynamics during stratospheric warming at solar minimum

Jan 1993

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1993adspr..13..321t&link_type=abstract

(Middle and upper atmosphere results; Proceedings of the Topical Meeting of the Interdisciplinary Scientific Commission C /Meeti

Physics

Middle Atmosphere, Ozonometry, Solar Cycles, Stratospheric Warming, Vertical Distribution, Atmospheric Chemistry, Photochemical Reactions

Scientific paper

A statistical analysis is used to establish the relationships between the main parameters characterizing stratospheric warming, i.e., ozone concentration, wind, and temperature. Studies were performed over southeastern Europe during the solar minimum. The most important levels in the maximum of the ozonosphere were used, reflecting the photochemistry and accumulation of ozone in the atmosphere.

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