turbulence

The features of the location of the ozone layer segments, where the statistical relationship of interannual changes in the CCA during the spring and autumn months, as well as variations of the surface temperature of the North Atlantic area, is essential. In the spring months of such segments of the atmosphere located HN over individual portions of subtropical and extra-tropical jet streams, and over the polar regions. Areas of similar seg-ments are maximal. In autumn the area is much less similar segments, they are located in the zone corresponding subtropical jet stream. Revealed features consistent understanding of the impact on the processes of air between the troposphere and stratosphere that have jet streams. They show a significant statistical relationship between changes in surface temperature of ocean waters, which are located in different hemispheres.