Related Topics:
ozone layer

Earth is currently experiencing a host of environmental problems. Air and water pollution continue to plague much of the world; exotic plants, animals, and other organisms pop up in parts of the globe that have no natural defense against them; and, all the while, climate change lingers in the headlines. It’s often difficult to find good environmental news, but environmentalists and scientists have reported one bright spot: the countries of the world rallying to combat the problem of ozone depletion.

Earth’s protective ozone layer sits some 15 to 35 km [9 to 22 miles] above Earth’s surface, in the stratosphere. Stratospheric ozone loss is worrisome because the ozone layer effectively blocks certain types of ultraviolet (UV) radiation and other forms of radiation that could injure or kill most living things. For 30 years countries around the world had worked together to reduce and eliminate the use of chlorofluorocarbons (CFCs) and other ozone-destroying chemicals (ODCs). However, scientists still could not say whether these efforts were helping. Was the ozone layer actually healing itself?

Before getting to the answer, it helps to have some background on the problem. In 1974 American chemists Mario Molina and F. Sherwood Rowland and Dutch chemist Paul Crutzen discovered that human-produced CFCs could be a major source of chlorine in the stratosphere. They also noted that chlorine could destroy extensive amounts of ozone after it was liberated from CFCs by UV radiation. Since then, scientists have tracked how the ozone layer has responded to CFCs, which, since their creation in 1928 had been used as refrigerants, cleaners, and propellants in hairsprays, spray paint, and aerosol containers. In 1985 a paper by the British Antarctic Survey revealed that stratospheric ozone concentrations over Antarctica had been dropping precipitously (by more than 60% compared with global averages) since the late 1970s. Throughout the 1980s and early 1990s, observations and measurements from satellites and other instruments showed that this “hole” over Antarctica was growing larger year after year, that a similar hole had opened over the Arctic, and that stratospheric ozone coverage worldwide had dropped 5% between 1970 and the mid-1990s, with little change afterward.

In response to the growing problem, much of the world came together in 1987 to sign the Montreal Protocol on Substances That Deplete the Ozone Layer, an agreement that allowed the world to begin to phase out the manufacturing and use of CFCs—molecules containing only carbon, fluorine, and chlorine atoms—and other ODCs. Follow-up meetings throughout the 1990s and early 2000s produced amendments aimed at limiting, reducing, and eliminating hydrobromofluorocarbons (HBFCs), methyl bromide, carbon tetrachloride, trichloroethane, hydrofluorocarbons (HFCs), hydrochlorofluorocarbons (HCFCs), and other ODCs. Even though nearly all of the planet’s governments had been working diligently toward a common goal—good news in itself—it was unclear whether these unprecedented efforts were having much of an effect.

In 2014, however, scientists received the first bit of good news on this topic: the first small increases in stratospheric ozone in more than 20 years had been detected, along with evidence that ODCs had declined by 10–15% in the atmosphere. Yet they remained cautious. Some two years later, scientists got sufficient data to confidently reveal proof that the ozone layer was indeed on a path to recovery. The 2016 study, which tracked the evolution of the size of the ozone hole over Antarctica, observed that stratospheric ozone concentrations were continuing to increase and that the size of the Antarctic ozone hole had declined by half the size of the continental U.S. between 2000 and 2015. They expected the ozone layer to fully heal sometime between 2040 and 2070.

In 2023, a United Nations study brought these estimates into further focus. It found that if countries continued to adhere to the limits imposed by the Montreal Protocol and its follow-on agreements, the world could expect that ozone concentrations would largely return to their pre-1980 levels by 2040, with the Arctic reaching pre-1980 levels by 2045 and the Antarctic following suit by 2066.

John P. Rafferty
Also called:
ozonosphere

ozone layer, region of the upper atmosphere, between roughly 15 and 35 km (9 and 22 miles) above Earth’s surface, containing relatively high concentrations of ozone molecules (O3). Approximately 90 percent of the atmosphere’s ozone occurs in the stratosphere, the region extending from 10–18 km (6–11 miles) to approximately 50 km (about 30 miles) above Earth’s surface. In the stratosphere the temperature of the atmosphere rises with increasing height, a phenomenon created by the absorption of solar radiation by the ozone layer. The ozone layer effectively blocks almost all solar radiation of wavelengths less than 290 nm from reaching Earth’s surface, including certain types of ultraviolet (UV) and other forms of radiation that could injure or kill most living things.

Location in Earth’s atmosphere

In the midlatitudes the peak concentrations of ozone occur at altitudes from 20 to 25 km (about 12 to 16 miles). Peak concentrations are found at altitudes from 26 to 28 km (about 16 to 17 miles) in the tropics and from about 12 to 20 km (about 7 to 12 miles) toward the poles. The lower height of the peak-concentration region in the high latitudes largely results from poleward and downward atmospheric transport processes that occur in the middle and high latitudes and the reduced height of the tropopause (the transition region between the troposphere and stratosphere).

Most of the remaining ozone occurs in the troposphere, the layer of the atmosphere that extends from Earth’s surface up to the stratosphere. Near-surface ozone often results from interactions between certain pollutants (such as nitrogen oxides and volatile organic compounds), strong sunlight, and hot weather. It is one of the primary ingredients in photochemical smog, a phenomenon that plagues many urban and suburban areas around the world, especially during the summer months.

Ozone creation and destruction

The production of ozone in the stratosphere results primarily from the breaking of the chemical bonds within oxygen molecules (O2) by high-energy solar photons. This process, called photodissociation, results in the release of single oxygen atoms, which later join with intact oxygen molecules to form ozone. Rising atmospheric oxygen concentrations some two billion years ago allowed ozone to build up in Earth’s atmosphere, a process that gradually led to the formation of the stratosphere. Scientists believe that the formation of the ozone layer played an important role in the development of life on Earth by screening out lethal levels of UVB radiation (ultraviolet radiation with wavelengths between 315 and 280 nm) and thus facilitating the migration of life-forms from the oceans to land.

The amount of ozone in the stratosphere varies naturally throughout the year as a result of chemical processes that create and destroy ozone molecules and as a result of winds and other transport processes that move ozone molecules around the planet. Over the course of several decades, however, human activities substantially altered the ozone layer. Ozone depletion, the global decrease in stratospheric ozone observed since the 1970s, is most pronounced in polar regions, and it is well correlated with the increase of chlorine and bromine in the stratosphere. Those chemicals, once freed by UV radiation from the chlorofluorocarbons (CFCs) and other halocarbons (carbon-halogen compounds) that contain them, destroy ozone by stripping away single oxygen atoms from ozone molecules. Depletion is so extensive that so-called ozone holes (regions of severely reduced ozone coverage) form over the poles during the onset of their respective spring seasons. The largest such hole—which has spanned more than 20.7 million square km (8 million square miles) on a consistent basis since 1992—appears annually over Antarctica between September and November.

As the amount of stratospheric ozone declines, more UV radiation reaches Earth’s surface, and scientists worry that such increases could have significant effects on ecosystems and human health. The concern over exposure to biologically harmful levels of UV radiation has been the main driver of the creation of international treaties such as the Montreal Protocol on Substances That Deplete the Ozone Layer and its amendments, designed to protect Earth’s ozone layer. The Montreal Protocol has been a success: some 99 percent of the ozone-depleting chemicals regulated by the treaty have been phased out since its adoption in 1987. Compliance with international treaties that phased out the production and delivery of many ozone-depleting chemicals, combined with upper stratospheric cooling due to increased carbon dioxide, is thought to have contributed to the shrinking of the ozone holes over the poles and to slightly higher stratospheric ozone levels overall. Studies note that continued reductions in ozone-depleting chemicals that follow the schedule proposed by the Montreal Protocol and its follow-up agreements are expected to result in a return to 1980-level ozone concentrations above the poles by as early as 2040, with the closure of the ozone holes above Antarctica by about 2066 and above the Arctic by about 2045.

Donald Wuebbles The Editors of Encyclopaedia Britannica