Over many regions, temperature and ozone are well correlated or anti-correlated depending of pressure level. An analysis of time series, such as 50 hPa at the Equator, shows that the temperature leads or concurs with ozone extremes, suggesting dynamics may dominate the radiative effects.
We use a statistical trend algorithm to analyze the SBUV(/2) data. This hockey-stick algorithm allows for a change in trend and examines the effect of the Mt. Pinatubo eruption on the computations. We examine the timing of the inflection points to delineate the confidence one can ascribe to the ozone-change computations in both a physical as well as a statistical sense. More detailed discussions on the sensitivity of data length and missing data, as well as the impact on ozone trend by the inclusion of 2006 data will be provided.
- Indicates paper has been withdrawn from meeting
- Indicates an Award Winner