A quasi-one-dimensional model of the ozone transport by planetary waves in the winter stratosphere

Details A quasi-one-dimensional model of the ozone transport by planetary waves in the winter stratosphere A quasi-one-dimensional model of the ozone transport by planetary waves in the winter stratosphere

Jun 1982

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1982mesjj..60..831k&link_type=abstract

Meteorological Society of Japan, Journal, vol. 60, June 1982, p. 831-849. Research supported by the Ministry of Education of Ja

Mathematics

Logic

10

Atmospheric Diffusion, Ozone, Planetary Waves, Stratosphere, Winter, Atmospheric Models, Meridional Flow, Photochemical Reactions, Vertical Distribution, Vertical Motion

Scientific paper

The mechanism governing the transport of ozone by planetary waves in the winter stratosphere is considered on the basis of the quasi-one-dimensional model developed by Hartmann and Garcia (1969), where the meridional distribution of physical quantities is expressed by two modes. Consideration is given to wave-mean flow interactions as well as to dynamic and photochemical effects on the variation in ozone content. It is found that the meridional and vertical transport of ozone caused by waves depends on the vertical structures in their orientation and magnitude.

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