INTERANNUAL CHANGES IN THE STATE OF THE ARCTIC AND NORTH ATLANTIC OSCILLATIONS AS FACTORS VARIATIONS OF THE TOTAL OZONE IN THE EARTH'S ATMOSPHERE
Abstract
Studied statistical communication of interannual changes of conditions of the Arctic and the North Atlantic oscillation, as well as variations of mean monthly total ozone values in the earth's atmosphere, which coincide in time. It is established that these links are most significant in winter and in early spring, the vast segments of the atmosphere, situated over the внетропическими jet currents in the troposphere and under the jet currents in the stratosphere, where the presence of vertical shifts speed creates conditions favourable for the development of turbulence. The revealed regularities suggest that the link between these processes in the period from December to March are causal character.
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