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Unusual Antarctic weather enlarges ozone hole while long-term recovery continues

First brief 5 Nov, 1:55 pm IST Updated 5 Nov, 1:55 pm IST 0 developments 2 min read
Antarctic ozone-hole assessment, 2026
NASA / K. Jepson, S. Youn · Public domain

Where it stands

US weather and space researchers reported an unusually large Antarctic ozone hole on 4 November 2026. The assessment comes from the National Oceanic and Atmospheric Administration (NOAA) and the space agency NASA. The ozone hole is an area where the protective ozone layer becomes severely thinned during the southern spring. Its average area during the main depletion season was about 25 million square kilometres. That made it the seventh-largest in 48 years of monitoring. A powerful polar vortex helped maintain a large area of very cold air, allowing ozone-destroying reactions to continue. Scientists still see long-term recovery as controls reduce ozone-depleting chemicals. This year’s weather and that longer trend operate together. The researchers say the hole would have been larger if those chemicals had remained as abundant as before international controls.

Background

Ozone in the stratosphere absorbs harmful ultraviolet radiation from the Sun. Some human-made chemicals release chlorine or bromine after reaching this layer of the atmosphere. Under Antarctic conditions, these substances can take part in reactions that destroy ozone. Very cold air allows polar stratospheric clouds to form. Reactions on their particles prepare chlorine to destroy ozone when sunlight returns. The polar vortex, a ring of strong winds, helps keep the cold Antarctic air isolated. The Montreal Protocol controls substances responsible for this damage. Many remain in the atmosphere for decades, so recovery takes time. Weather changes also affect the size of the hole from year to year. Researchers therefore examine both annual conditions and the longer chemical trend when assessing recovery.

How it developed

  1. 4 November 2026
    How it started

    Monitoring finds a large seasonal area alongside lower chemical pressure

    The average ozone-hole area was about 25 million square kilometres from 7 September to 13 October 2026. NOAA and NASA linked its large size to an unusually strong polar vortex. Satellite measurements and ground-based observations track the layer’s condition. The researchers say international controls on ozone-depleting substances continue to support recovery, even as this year’s weather increased depletion.

Why it matters for UPSC

GS3 · EnvironmentGS3 · International environmental agreements

For GS3, explain how atmospheric chemistry and polar weather combine to affect ozone. Use the Montreal Protocol to connect international controls with gradual environmental recovery.

Key terms

Ozone layerThe part of the atmosphere containing ozone that absorbs much of the Sun’s harmful ultraviolet radiation. Much of this protective ozone is in the stratosphere. Severe seasonal thinning over Antarctica is called the ozone hole.
StratosphereThe atmospheric layer above the lower layer where most familiar weather occurs. Its ozone helps protect life from ultraviolet radiation. Antarctic ozone loss occurs within this higher layer.
Polar vortexA large circulation of strong winds around a polar region. Over Antarctica it can isolate very cold stratospheric air. Those conditions help sustain the cloud chemistry involved in seasonal ozone destruction.
Ozone-depleting substanceA chemical that can contribute to destruction of stratospheric ozone. Some release chlorine or bromine after reaching the upper atmosphere. Long atmospheric lifetimes mean their effects can continue after production is reduced.
Montreal ProtocolThe international agreement controlling substances that deplete the ozone layer. Countries have replaced many older chemicals with alternatives. Because the older substances persist, the resulting recovery develops over decades.
Sources (2)
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