
“The key is to account for large year-to-year fluctuations that have obscured a gradual increase in the long-term evolution of ozone,” says atmospheric scientist Murry Salby of Macquarie University in Sydney. His team published its findings online May 6 in Geophysical Research Letters.
First spotted in 1985, the Antarctic ozone hole was quickly linked to chemicals called chlorofluorocarbons, emitted mainly in the Northern Hemisphere but concentrated over the South Pole by atmospheric circulation patterns. Chlorine atoms from these CFCs react with ozone molecules, seasonally destroying the layer that shields Earth from cancer-causing and crop-damaging ultraviolet radiation.
Scientists had predicted that ozone loss would bottom out and start recovering by now. They just didn’t think they would be able detect that change yet, since ozone levels vary dramatically from year to year because of complex atmospheric processes, sometimes by almost as much as the magnitude of the ozone hole itself…
A rendering of the ozone hole from NASA
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