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Abstract
Abstract Measurements of the total ozone in the Central Asian region are presented. These measurements show that there is a systematic difference between the N(O3) values obtained in high mountains and on the plain. Total ozone content above three stations situated in mountains is found to be about 30–50 D.u. lower than above the stations in the flat area. A suggestion is made, that revealed effects are due to the vertical mean motions generated by the horizontal flux, meeting an obstacle in the form of the Central-Asian mountain region.
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