Abstract

Current satellite and ground-based data indicate a long-term decrease in global ozone levels of 2·7 ± 1·4% per decade, although recently the rate may have increased to about 4% per decade outside of the tropics. There is yet little evidence of an accompanying wide-spread increase in terrestrial UV levels, but calculations predict increases of a similar magnitude in coming years. The manifestation of increased UV will be as a broad band centered about 310 nm with only very little absolute increase in wavelengths shorter than 295 nm. Unless sustained ozone losses exceed 15% during the summer months, the effect should be inconsequential for most polymers. The effects of sun position on daily and seasonal variations in UVB are discussed.

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