Since the Antarctic ozone hole was detected in 1985, depletion of the ozone layer—the "big umbrella" that protects all life on Earth—has raised considerable concern. The efforts of international communities led to the success of the "Montreal Protocol on Substances that Destroy the Ozone Layer", signed in 1987, which banned global production and usage of chlorofluorocarbons, the leading cause of the depleted ozone.
Since then, ozone depleting substances (ODSs) in the stratosphere have gradually been erased and further ozone destruction avoided. The ozone layer has been gradually recovering from the bottom up, and scientists estimate it will reach the level of the 1980s by the middle of this century.
"However, strong volcanic eruptions, especially when a super volcano erupts, will have a strong impact on ozone, and might interrupt the ozone recovery processes," says Associate Prof. WEI Ke from the Institute of Atmospheric Physics of the Chinese Academy of Sciences. WEI is the corresponding author of a paper recently published in Advances in Atmospheric Sciences .
Photo of Mount Pinatubo’s eruption in June 1991 (Image by Global Volcanism Program)
To estimate the effect of a possible super volcano on the recovering ozone layer, WEI's team worked with Russian scientists and used a transport model and a chemistry-climate model to simulate the impact of super volcanic eruptions on the stratospheric ozone during different ozone recovery periods.
The results show that the percentage of global mean total column ozone depletion in the 'half ODSs level of the 1990s' scenario is approximately 6%, and the percentage is 6.4% in the tropics.
When all anthropogenic ODSs are removed and only natural sources (mainly CH3Cl and CH3Br) remain, a super volcanic eruption produces a global mean ozone depletion of 2.5%, with a 4.4% loss in the tropics.
"Such 'few' destructions shouldn’t be underestimated, as the Ozone Assessment Report in 2014 by the World Meteorological Organization suggested an ozone depletion of 2.5% outside the polar regions during the worst depletion period in the 1990s," says the lead author, Dr. XU Luyang.
XU is concerned that, since super volcanic eruptions might also inject large load of halogens into the atmosphere, which directly destroy ozone in the stratosphere, the true depletion caused by super volcanoes might therefore be even more serious than the estimation.
However, current observations and studies are unable to provide enough information on the exact quantities of volcanic halogens entering the stratosphere. Moreover, in the Paleozoic Era, when the ozone layer was relatively weak and thin, could a super volcanic eruption have destroyed the thin stratospheric ozone layer and further influenced the evolution of life and the environment? All these questions need to be further investigated.
The study was supported by the National Key Research and Development Project of China, the National Natural Science Foundation of China, and the Youth Innovation Promotion Association of the Chinese Academy of Sciences.
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