Long-term changes in ozone mini-hole event frequency over the Northern Hemisphere derived from ground-based measurements

Details Long-term changes in ozone mini-hole event frequency over the Northern Hemisphere derived from ground-based measurements Long-term changes in ozone mini-hole event frequency over the Northern Hemisphere derived from ground-based measurements

Oct 2002

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002ijcli..22.1425k&link_type=abstract

International Journal of Climatology, vol. 22, Issue 12, pp.1425-1439

Computer Science

6

Ozone, Mini-Hole, Ozone Dynamical Proxy, Midlatitudes, Northern Hemisphere, Statistical Model, Mars

Scientific paper

Decadal changes of ozone mini-hole event appearance over the Northern Hemisphere midlatitudes are examined based on daily total ozone data from seven stations having long records (four decades or more) of ozone observations. The various threshold methods for accepting and rejecting the ozone minima as mini-holes are examined. Mini-hole event activity is seen to be rather stable when averaged over a decadal time scale if the mini-holes are selected as large negative departures (exceeding 20%) relative to the moving long-term total ozone reference. The results are compared with a previous ozone mini-hole climatology derived from satellite data (TOMS measurements on board the Nimbus-7 satellite for the period 1978-93). A nonlinear statistical model (MARS), which takes into account various total ozone dynamical proxies (from NCEP-NCAR reanalysis), is used to study dynamical factors responsible for the ozone extremes over Arosa in the period 1950-99. The model explains as much as 95% of the total variance of the ozone extremes. The model-observation differences averaged over the decadal intervals are rather smooth throughout the whole period analysed. It is suggested that the short-term dynamical processes controlling the appearance of ozone extremes influenced the ozone field in a similar way before and after the onset of abrupt ozone depletion in the early 1980s. The analysis of the ozone profile and the tropopause pressure (from the ozonesondings over Hohenpeissenberg, 1966-99) during mini-hole events shows 60% ozone reduction in the lower stratosphere and an approximately 50 hPa upward shift of the thermal tropopause there.

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