Annotation
The changes in the total amount of ozone X are considered in the passage of cold and warm fronts and in cyclones and anticyclones. There is a regular decrease in X on warm-air influx and an increase in cold air. Fronts entrain air not only from the troposphere but also from the stratosphere, and the larger vortices have the greatest effects on the horizontal and vertical ozone distributions.
© 2016 Publisher M.V.Lomonosov Moscow State University
Authors
M.S. Rakova, A.Kh. Khrgian
Department of Physics of Atmosphere, Faculty of Physics, Moscow State University, Leninskie Gory, Moscow, 119992, Russia
Department of Physics of Atmosphere, Faculty of Physics, Moscow State University, Leninskie Gory, Moscow, 119992, Russia
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