TOTAL OZONE TRENDS FROM QUALITY-CONTROLLED GROUND-BASED DATA (1964-1994)

Citation
Rd. Bojkov et al., TOTAL OZONE TRENDS FROM QUALITY-CONTROLLED GROUND-BASED DATA (1964-1994), JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 100(D12), 1995, pp. 25867-25876
Citations number
28
Categorie Soggetti
Metereology & Atmospheric Sciences
Volume
100
Issue
D12
Year of publication
1995
Pages
25867 - 25876
Database
ISI
SICI code
Abstract
Seasonal and year-round trend analyses of ground-based total ozone dat a that have been carefully quality controlled are presented for 46 Dob son stations, for four regions of the former USSR and for the two pola r regions. The trend model incorporated the 10.7-cm solar flux and equ atorial stratospheric wind as indicators for removal of the solar and quasibiennial components in ozone variations. The trends were calculat ed for two main time intervals: from January 1964 through March 1994, with slope since 1970, and from January 1979 through March 1994. The a nalyses show continuous year-round ozone decline in middle latitudes ( 35 degrees-60 degrees) where the estimated values are -4.3 and -4.1% p er decade for the period since January 1979 in the northern and southe rn hemispheres respectively. The northern hemisphere data permit estim ation of the trends over vast regions such as North America -4.1+/-1.5 %, Europe -5.1+/-2.0%, Siberia and Far East -5.6+/-1.8% (values and tw o sigma intervals are given in percent per decade for year-round trend ). The ozone decline over the Arctic is about -5.6+/-2.0% per decade f or year-round trend and -7.5+/-3.8% for the winter-spring season. The most dramatic ozone decline occurs in spring over Antarctica, -22+/-7. 2% per decade. The trends estimated for the 1979-1994 period are about 1.5% per decade stronger in northern and southern middle and high lat itudes than the trends with slope since 1970, which shows a substantia l acceleration of the rates of ozone decline. The sensitivity of the o zone trends to the extremely low ozone during the 1992-1993 period is discussed. Most of the ozone data and calibrations in this paper were the base for the Ozone Trends section of the World Meteorological Orga nization/United Nations Environment Program Ozone Assessment 1994. The results presented here in general concur with the assessment and prov ide further estimates of the ozone changes in the northern middle lati tudes in view of another extremely low winter-spring season of 1994-19 95.