A decrease in total ozone content over the mountains of Central Asia

Details A decrease in total ozone content over the mountains of Central Asia A decrease in total ozone content over the mountains of Central Asia

Oct 1992

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1992ge%26ae..32..128d&link_type=abstract

Geomagnetizm i Aehronomiya (ISSN 0016-7940), vol. 32, no. 5, p. 128-132.

Computer Science

Mountains, Ozone Depletion, Stratosphere, Asia, Concentration (Composition), Correlation Coefficients

Scientific paper

Based on observations of the total ozone content at a series of stations in Central Asia over a two-year period, it is found that the amount of N(O3) over the mountains is systematically higher than that over the surrounding plain regions, with the difference ranging from 30 to 80 Dobson units. The negative correlation of this difference with the horizontal wind velocity in the troposphere supports the argument that a decrease in N(O3) over the mountains is related to vertical motions generated by horizontal flow impinging on the Central Asian mountain range.

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