Ozone is a pollutant at ground level, but very high in the atmosphere’s “ozone layer,” it absorbs damaging ultraviolet radiation.
Ozone is a pollutant at ground level, but very high in the atmosphere’s “ozone layer,” it absorbs damaging ultraviolet radiation. Past studies have examined ozone levels in the Southern Hemisphere, but little is known about levels of the molecule in Antarctica over long periods. Now, researchers reporting in ACS’ Environmental Science & Technology have analyzed more than 25 years of Antarctic data, finding that concentrations near the ground arose from both natural and human-related sources.
Ozone gas has a sharp or acrid scent that sometimes accompanies smog or summer storms. It forms when sunlight reacts with gases produced by industrial and transportation activities, biomass burning or with naturally produced gases originating from lightning and microorganisms. However, when sunlight is very strong, it breaks down the molecule. Most ozone resides about 9-18 miles above Earth in the ozone layer, an atmospheric band within the stratosphere that protects the Earth from harmful UV radiation. But ozone in the lower atmosphere, or troposphere, is harmful and causes smog and throat and lung irritation. It’s also a concern because the molecule traps heat 1,000 times better than carbon dioxide, and therefore, can have a large impact on global warming. While previous researchers have shown the rise of ozone in the troposphere across the Southern Hemisphere, there has not been a regional study reported for the remote Antarctic continent over a long period. So, Jayanarayanan Kuttippurath and colleagues wanted to use measurements made over Antarctica to determine where the ozone comes from and how levels have changed over time.
Read more at American Chemical Society
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