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Iceberg A-23A: NYC-Sized Megaberg Nears Disintegration

The colossal Iceberg A-23A, a Reagan-era megaberg larger than New York City, is exhibiting dramatic blue meltwater pools as it rapidly disintegrates in the South Atlantic. Scientists are tracking its final weeks.

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Reagan‑era megaberg Iceberg A‑23A, once twice the size of Rhode Island, now days from total disintegration

Iceberg A‑23A, a Reagan‑era megaberg once nearly twice the size of Rhode Island, is now streaked with vivid blue melt ponds and structural blowouts; scientists say it may disintegrate completely within days to weeks, offering rare data.

Key takeaways

  • A‑23A calved from the Filchner Ice Shelf in 1986 and is one of the longest‑monitored megabergs on record.
  • Satellite and astronaut images show widespread blue meltwater pools, blowouts and structural failure suggesting imminent breakup.
  • Scientific value: its final disintegration offers insights into iceberg lifetimes, meltwater pathways and ocean biogeochemistry.
  • Local relevance: while San Luis Obispo sees no direct physical impact, research from A‑23A could influence fisheries, coastal planning and education.

Key information

Iceberg A‑23A calved from Antarctica’s Filchner Ice Shelf in 1986 and has been tracked for nearly four decades by international agencies. High‑resolution imagery reveals dramatic blue meltwater ponds and blowouts as the berg drifts through warmer South Atlantic waters.

Primary monitoring and image sources include NASA Earth Observatory, the British Antarctic Survey, and the U.S. National Ice Center.

“Striking blue meltwater pools and blowouts point to imminent total disintegration,” scientists report from satellite and astronaut imagery.

Origin and age

A‑23A began as part of the Filchner Ice Shelf and calved in 1986 — a product of the Reagan administration era. Its almost 40‑year record of movement and persistence makes it one of the longest‑lived megabergs in modern tracking efforts.

Size then and now

At birth, A‑23A covered roughly 4,000 km² (~1,540 sq mi), nearly twice the size of Rhode Island. By 9 January 2026 the U.S. National Ice Center listed the main remnant at about 1,182 km² (456 sq mi), still larger than New York City but a fraction of its original area.

Drift path and ocean behavior

Grounded in the Weddell Sea for more than three decades, A‑23A began moving in 2020, skirted the Antarctic Peninsula and was trapped in a Taylor column near Pirie Bank. After breaking free in late 2024 it joined the Antarctic Circumpolar Current and drifted north toward South Georgia, entering waters with temperatures near 3 °C by late 2025 — conditions that accelerate melting and fragmentation.

Breakup and disintegration

As the berg moved into warmer seas and stronger wave fields it shed major sections. Reports through 2025 show A‑23A dropping to less than half its original area, producing fragments up to 400 km² and many smaller hazards. Recent satellite imagery documents a waterlogged, fractured plate structure with extensive surface ponds and clear blowouts; these features signal imminent complete breakup during the current austral summer.

Megaberg meltwater pools and surface features

Bright blue meltwater pools have become a defining visual of A‑23A. These ponds collect in ancient glacial striations, tracing old valleys and ridges and channeling melt. NASA imagery highlights linear bands of deep blue and white where water sits in depressions; the weight of ponded water has driven cracks open and created “blue mush” zones — softened, weakened ice that accelerates collapse.

Structural failure, blowouts and freshwater plumes

Images show blowouts — locations where ponded water has poured through the ice edge, producing bright white patches and plumes of freshwater and ice rubble. The berg also exhibits a rampart‑and‑moat pattern, with raised rims around darker ponded water; these patterns form as plates bend and sides melt at the waterline, temporarily trapping water atop the berg and hastening structural failure.

Monitoring and Antarctic iceberg tracking

A‑23A’s condition has been tracked by multiple agencies: the U.S. National Ice Center for operational positions and area estimates; NASA Terra MODIS imagery and astronaut photos from the ISS for high‑resolution views; and partners including EUMETSAT, NOAA NESDIS and the British Antarctic Survey.

Scientific significance

A‑23A represents a rare, multi‑decade natural experiment: long grounding, trapping in a Taylor column, sudden release and transit into warm water. Scientists expect its final breakup to reveal details about iceberg lifetimes, mechanisms of meltwater entry into the ocean, and how released minerals and dust may stimulate local biological responses and alter marine biogeochemistry for days to weeks.

Implications for San Luis Obispo, California

Economic impact: San Luis Obispo County will not face direct physical effects from A‑23A’s breakup in the South Atlantic. Still, long‑range changes in ocean circulation and nutrient delivery highlighted by this event can influence fisheries, markets and coastal economies worldwide; local stakeholders should monitor updates from agencies such as NOAA NESDIS and the British Antarctic Survey.

Political consequences: For moderate local audiences, the berg’s rapid melt could sharpen discussions about coastal resilience and climate policy, encouraging nonpartisan investments in monitoring, planning and federal partnerships.

Social and cultural effects: A‑23A’s striking imagery can boost public interest in ocean science; schools, museums and community groups in San Luis Obispo might use the story to teach about ocean currents, meltwater processes and stewardship. Artists and conservation groups may also connect A‑23A visuals to local campaigns on kelp restoration, plastic reduction and sustainable fisheries.

Practical applications: Local research institutions like Cal Poly could expand curricula and grant efforts in remote sensing and oceanography; residents are encouraged to support data‑driven policies and follow scientific updates that could inform coastal planning.

Sources and further reading

Reporting includes satellite imagery analysis from NASA and operational tracking by the U.S. National Ice Center and partner agencies. Times Media Service.

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Jeff Bollin

Jeff Bollin is a senior national science reporter for Times Media Service, based in the Washington bureau. Bollin covers science, including new research, scientific discovery and innovation, and the government agencies and institutions that fund and guide it. Bollin holds a master's degree in journalism and grew up in Macclesfield, England.

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