Conception of interaction of atmospheric ozone and air mass in the Northern Hemisphere
Analysis of long-term data set of spatial and temporal distribution of atmospheric ozone has shown that the arrangement of the ozone fields is closely connected with troposphere air masses. Since the degree of ozone destruction in the warm troposphere significantly higher than in the cold, so over each air mass is formed its own ozone layer. Over the warm air mass in the lower stratosphere is always observed low level of ozone and low temperature, over cold air mass — high levels of ozone and high temperature. In the gap between warm and cold tropopause it is observed minimal temperature gradients and the largest level of pressure gradients. Accordingly the moving of air mass borders is depend on conditions in the troposphere and lower stratosphere state, i.e. on the state of the ozone layer.