Nearly thirty years after an international treaty banned the use of chlorofluorocarbons, the Antarctic ozone hole is finally starting to heal. By mid to late century, it should be fully recovered.
“This is a reminder that when the world gets together, we really can solve environmental problems,” Susan Solomon, an atmospheric chemist at MIT, told Gizmodo. “I think we should all congratulate ourselves on a job well done.”
Solomon is lead author on a study published today in Science, which presents the clearest evidence yet that the Antarctic ozone hole is showing signs of long-term recovery. The researchers attribute this to the 1987 Montreal Protocol, which banned the use of chlorinated compounds in refrigerator coolants and aerosols, after scientists learned that these chemicals were making their way into the stratosphere and wreaking havoc on Earth’s ozone layer.
Cartoon depiction of ozone (O3) being broken apart by chlorine. Image: NASA Scientific Visualisation Studio
Scientists have been monitoring the Antarctic ozone hole, which opens every year in late August or early September and reaches its full size by October, since the 1980s. The size of the ozone hole varies widely from year to year, because the chemical reactions that destroy ozone are highly sensitive to changes in sunlight, temperature, and stratospheric cloud cover. For researchers interested in tracking ozone recovery, the challenge lies in pulling a faint signal out of a noisy background.
This problem piqued the interest of Solomon and her co-authors last October, when the ozone hole reached a record size of 23 million square kilometres (9 million square miles); some 20 per cent larger than the previous year. “This was very unexpected, and we thought that the reason might have to do with volcanoes,” Solomon said, explaining that the aerosols released during volcanic eruptions contribute to polar stratospheric clouds, creating additional surface area for ozone-destroying reactions to occur.
Sure enough, the team was able to show that a string of eruptions at the Calbuco volcano in the southern hemisphere widened the spring ozone hole. But they discovered something else, too. “We learned that the September is not nearly as variable in weather as October, and that it’s less sensitive to volcanic activity,” Solomon said.
This got the researchers thinking that September may be the best month for teasing out subtle signs of ozone recovery. So they assembled September records from 2000 to 2015, including data on the rate at which the ozone hole opens, its average size and depth, meteorological conditions and volcanic activity.
“We found that because there is less chlorine in the atmosphere, the ozone hole is opening about ten days later than it used to,” Solomon said. “That has a huge effect on the September average.” Overall, Solomon’s analysis showed that the September ozone hole has shrunk by an average of 4.5 million square kilometres (1.7 million square miles) since 2000.
Susan Strahan, an atmospheric chemist at NASA who was not involved with the study, agrees that the evidence is very encouraging. “This is the emergence of a trend,” she told Gizmodo, while cautioning that it’s a bit early to say exactly how the recovery will play out. That’s because the different chlorofluorocarbons present in the atmosphere degrade at different rates, and while some have already vanished, others will stick around for decades to come. Most researchers, however, expect the ozone hole to be fully patched by around 2060.
“It’s important,” Strahan continued, “because I think a lot of people feel that environmental stories always have bad endings. In this case, the recovery will happen, but it’ll take time.”