Transport processes and ozone perturbations

Current understanding of stratospheric transport in the meridional plane is reviewed, and the implications of that conceptual framework for the ozone response to chlorofluorocarbon increases are considered. The possibility of seasonal and latitudinal variations in that response is stressed. Calculations of the changes in ozone that may have occurred between the period before widespread chlorofluorocarbon usage and the present day, and the changes that would be expected to occur at steady state for 1980 chlorofluorocarbon production levels, are presented. Finally, some of the uncertainties in the adopted transport framework and its applicability to the evaluation of future perturbations are explored.