Increased UV radiation due to polar ozone chemical depletion and vortex occurrences at southern sub-polar latitudes in the period (1997–2005)

ANDREA PAZMIÑO; SOPHIE GODIN-BEEKMANN; EDUARDO LUCCINI; RUBÉN PIACENTINI; EDUARDO QUEL; ALAIN HAUCHECORNE

ATMOSPHERIC CHEMISTRY AND PHYSICS DISCUSSIONS

European Geosciences Union

Año: 2008 p. 6501 - 6537

1680-7367

The variability of total ozone and UV radiation from Total Ozone Mapping Spectrometer (TOMS) measurements is analyzed as a function of polar vortex occurrences over the southern subpolar regions during the 1997-2005 period. The analysis of vortex occurrences showed high interannual variability in the 40ºS-60ºS latitude band with a longitudinal asymmetry showing the largest frequencies over the 90ºW-90ºE region. The impact of vortex occurrences on UV radiation and ozone in clear sky conditions was determined from the comparison between the measurements inside the vortex and a climatology obtained from data outside the vortex over the studied period. Clear sky conditions were determined from TOMS reflectivity data. For measurements outside the vortex, clear sky conditions were selected for reflectivity values lower than 7.5%, while for measurements inside the vortex, a relaxed threshold was determined from statistically similar UV values as a function of reflectivity. UV changes and ozone differences from the climatology were analyzed in the 40ºS-50ºS and 50ºS-60ºS latitude bands during the spring period (September to November). The largest UV increases and ozone decreases, reaching 200% and 65%, respectively, were found in the 50ºS-60ºS latitude band in September and October. The heterogeneous ozone loss during vortex occurrences was estimated using a chemical transport model. The largest impact of vortex occurrences was found in October with mean UV increase, total ozone decrease and accumulated ozone loss in the 350K-650K range of respectively 47%, 32% and 63%. The region close to South America is the most affected by the Antarctic ozone depletion due to the combined effect of large number of vortex occurrences, lower cloud cover and large ozone decrease. This region would be the most vulnerable in case of cloud cover decrease linked to climate change, due to more frequent occurrence of ozone poor air masses during austral spring.