Get you up to speed: Antarctica’s A-23A iceberg disintegrates after nearly 40 years at sea
The mass designated A-23A calved from the Filchner Ice Shelf in Antarctica in 1986 and disintegrated in the South Atlantic Ocean in early April 2026. At its peak, A-23A covered more than 6,000 sq km (3,728 sq miles) but had shrunk to just over 170 sq km (105 sq miles) by late March 2026.
Iceberg A-23A, which calved from the Filchner Ice Shelf in 1986, ultimately disintegrated in the South Atlantic Ocean after drifting over 2,300 km into warmer waters, according to satellite imagery data. Jan Lieser from the Bureau of Meteorology remarked on the extensive melting and structural weakening of the iceberg in its final months, stating, “I noticed in recent weeks how Mother Nature seemed to keep a veil (of clouds) over the dying iceberg as if trying to give it some privacy at this stage.”
Researchers are continuing to investigate the roles played by ocean currents, seabed features, and rotating columns of water in shaping iceberg paths. Uncertainties persist regarding the nature of the seabed where Iceberg A-23A remained stuck for years and how it eventually became trapped in a rotating ocean vortex near the South Orkney Islands.
World’s oldest iceberg is no more: A23a melts into puddle of water after 40 years | News World
The iceberg – designated A-23A- photographed from an RAF aircraft flying over Antarctica in January 2025 (Picture: MOD/Cover Media)
One of the largest icebergs ever recorded has finally disintegrated after a four decades.
The mass – designated A-23A- calved from the Filchner Ice Shelf in Antarctica in 1986 and for many years it was the world’s biggest.
Its journey ultimately ended in the South Atlantic Ocean in early April 2026 – just months short of its 40th anniversary.
Satellite images captured it from birth in the Weddell Sea to disintegration. It had drifted more than 2,300km (1,429 miles) north into warmer waters near South Georgia and the South Sandwich Islands.
There, it rapidly melted, fractured and shrank.
Fragments of Iceberg A-23A are seen in January as it entered its final weeks (Picture: NASA Earth Observatory/Cover Media)
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A-23A owed its longevity to becoming wedged on the ocean floor where the temperatures were cold enough to keep it preserved.
But in its final months, it underwent extensive melting and break-up. By late March 2026, scientists estimated it had shrunk to just over 170 sq km (105 sq miles) – a small fraction of the more than 6,000 sq km (3,728 sq miles) it covered in 2020 when it was still grounded off Antarctica.
Pools of deep-blue meltwater formed across its surface, weakening the structure and likely contributing to its collapse. Cloud cover obscured some of its final moments from satellites.
‘I noticed in recent weeks how Mother Nature seemed to keep a veil (of clouds) over the dying iceberg as if trying to give it some privacy at this stage,’ said Jan Lieser of Bureau of Meteorology.
The route the iceberg took. It calved in the Weddell Sea before finally collapsing more than 1,400 miles away (Picture: NASA Earth Observatory/Cover Media)
There were still enough observations, however, to capture glimpses of its final break-up, as well as the many stages of its long and winding journey.
A-23A’s lifespan coincided with major advances in Earth observation. The Landsat program tracked it from the 1980s onwards, while later missions such as Terra satellite and Aqua satellite provided regular, wide-area coverage.
In more recent years, a growing fleet of satellites has offered unprecedented detail — from changes in the iceberg’s shape to its impact on surrounding marine ecosystems.
Satellite imagery showing the formation of the iceberg in 1986, which was to become the largest on earth (Picture: NASA Earth Observatory/Cover Media)
Astronauts aboard the International Space Station also captured close-up views.
‘The technology that allows us to tell ‘iceberg stories’ is a tribute to the engineers and funding that put crucial sensors into orbit to collect those data and make them accessible,’ said Christopher Shuman, formerly of the University of Maryland.
‘Through time, these efforts have allowed us to understand the general patterns of iceberg movement around Antarctica, especially in the last handful of decades.’
Despite decades of observations, scientists say many questions remain about how icebergs move and break apart.
Iceberg A-23A pictured in April 1986, shortly after it had calved (Picture: NASA Earth Observatory/Cover Media)
Researchers are continuing to investigate the roles played by ocean currents, seabed features and rotating columns of water in shaping their paths.
Smaller fragments that break away from giant icebergs are of particular concern, as they can pose hazards to shipping and are difficult to track.
Even in the case of A-23A, uncertainties persist – including the nature of the seabed where it remained stuck for years after calving, and how it later became trapped in a rotating ocean vortex near the South Orkney Islands.
‘We certainly do know a fair bit about the general drift patterns of icebergs and the general environment,’ Lieser said. ‘But when it comes to individual pieces – large and small – and their tracks, there’s still a fair bit to learn.’
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