Abstract
Abstract Total-ozone variations in five climatic zones and the world as a whole, as well as ozone variations in tropospheric and stratospheric layers of the north temperate zone, have been updated through 1985 by means of Dobson, ozonesonde and Umkehr observations. In the north temperate zone the total-ozone minimum in early 1985 was as pronounced as the total-ozone minimum in early 1983 (both a record 3% below the long-term average), but without the potential explanation afforded by the El Chichon eruption and/or strong El Nino of 1982. Based on linear regression, between 1980 and 1985 the year-average total ozone decreased by 2–3% in north polar, north and south temperate, and tropical zones, but by almost 6% in the south polar zone (Antarctic “ozone hole” phenomenon). For the world as a whole, the decrease in year-average total ozone between 1980 and 1985 is estimated to be 2.7 ± 0.9% (95% confidence interval), with the decrease greatest in the northern autumn (3.3%) and winter (3.1%) and least in the ...
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