The central objective of this research is to analyze the role of long term enhancement in the carbon dioxide and an increase in the temperature of sea surface which is an indicator of change in climate and also halocarbons which are man-made indicators to indicate the reduction in the chemical ozone with respect to halogen to explain the examined tendency of ozone in the stratosphere and inference of for related variables consisting temperature and tropopause height.
In this region from 1979 to 2005, there is a decrease of ...