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Path to recovery of ozone layer passes a significant milestone
Theo Stein

Path to recovery of ozone layer passes a significant milestone

An annual analysis of air samples collected at remote sites around the globe that is tracking a continued decline in the atmospheric concentration of ozone-depleting substances shows the threat to the ozone layer receding below a significant milestone in 2022, NOAA scientists have announced. 

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Locations where ozone-depleting chemicals are regularly made by NOAA/ESRL. Different symbols indicate different sampling frequencies (circles≅weekly; stars≅daily). A subset of these results is used to derive hemispheric and global surface means. Credit: NOAA Global Monitoring Laboratory

In early 2022, the overall concentration of ozone-depleting substances in the mid-latitude stratosphere had fallen just over 50 percent back to  levels observed in 1980, before ozone depletion was significant. This slow but steady progress over the past three decades was achieved by international compliance with controls on production and trade of ozone-depleting substances in the Montreal Protocol on Substances that Deplete the Ozone Layer. 

The pace of reduction in ozone-depleting substances (ODSs) over Antarctica, which experiences a large ozone hole in spring, has been slower, NOAA’s analysis showed. 

“It’s great to see this progress,” said Stephen Montzka, senior scientist for NOAA’s Global Monitoring Laboratory. “At the same time, it’s a bit humbling to realize that science is still a long way from being able to claim that the issue of ozone depletion is behind us.”

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Past atmospheric concentrations in reactive halogen concentrations are derived from NOAA measurements of both chlorine- and bromine-containing chemicals. Future “WMO scenarios” are tied to NOAA observations in the past and assume full adherence to the Montreal Protocol. Measured tropospheric changes are shown as dashed curves and points. Inferred stratospheric changes are solid curves. Green lines represent the Antarctic stratosphere; blue lines represent the mid-latitudes. Arrows indicate dates that stratospheric halogen concentrations are projected to return to 1980 levels. Credit: NOAA Global Monitoring Laboratory

NOAA’s Ozone Depleting Gas Index tracks the overall stratospheric concentration of ozone-depleting chlorine and bromine from long-lived ODSs relative to its peak concentration in the early 1990s. 

Ozone is a highly reactive molecule formed of three oxygen atoms that is found primarily in two regions of the atmosphere. About 90% of Earth’s ozone resides in the stratosphere,which is above the troposphere, the layer closest to Earth’s surface. The region of the stratosphere with the highest amount of ozone is commonly referred to as the “ozone layer.” The stratospheric ozone layer absorbs the sun’s ultraviolet rays and protects all biological systems on Earth from these harmful rays. 

In the 1980s, the scientific community discovered that a class of man-made chemicals was seriously damaging this protective ozone layer, creating a giant “hole” in the ozone layer over Antarctica and smaller, but still worrisome depletion in mid-latitudes. As part of the US response, Congress mandated that NASA and NOAA monitor stratospheric ozone and ozone-depleting substances in the 1990 amendments to the Clean Air Act. The Ozone Depleting Gas Index is one way that NOAA fulfills this mandate.

 Scientists at NOAA’s Global Monitoring Laboratory created the index to render the results of a series of complex analyses into a single number that tracks the total abundance of these chemicals and how the threat they pose to the ozone layer is changing over time. The year 1980 was selected as the benchmark year for the index because scientific and policy communities have

Image
The Ozone Depleting Gas Index (ODGI) vs. time calculated for the Antarctic and mid-latitude stratosphere. As before, the ODGI derived directly from the Equivalent Effective Stratospheric Chlorine (EESC) determined from our atmospheric surface observations. Credit: NOAA Global Monitoring Laboratory

long viewed it as the date when ozone depletion first became obvious. NOAA calculates the index directly from surface observations of the 15 most abundant long-lived, chlorine- and bromine-containing chemicals whose production and consumption is controlled by the Montreal Protocol. These observations provide a direct measure of nearly all of the chlorine and bromine atoms in man-made chemicals with lifetimes longer than approximately six months. 

Global Monitoring Laboratory scientists calculate two separate indices, one for the mid-latitudes, where a large fraction of the world’s population lives, and one for Antarctica, where deep ozone holes are observed in early spring as a result of super cold temperatures enabling catalytic ozone-destroying reactions on icy clouds.

Image
The contribution of long-lived chlorine- and bromine-containing gases to reactive halogen in the mid-latitude stratosphere. Credit: NOAA Global Monitoring Laboratory

In contrast to the mid-latitudes, progress toward recovery of the ozone layer over the Antarctic has not been as rapid, declining  by 26% from peak values in the 1990s for  multiple reasons, but particularly because air in the Antarctic stratosphere is older than in mid-latitudes. 

The 2022 index for the Antarctic has fallen 26% from peak values in the 1990s, with recovery of the Antarctic ozone layer projected to occur sometime around 2070.

Read the full ODGI report at the Global Monitoring Laboratory's website: https://gml.noaa.gov/odgi/

For more information, contact Theo Stein, NOAA Communications: theo.stein@noaa.gov

Image
The contribution of long-lived chlorine- and bromine-containing gases to reactive halogen in the Antarctic stratosphere. Credit: NOAA Global Monitoring Laboratory

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