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Iceberg A-23A: Disintegrating in South Atlantic, Covered in Blue Meltwater

The Reagan-era Iceberg A-23A, once the world's largest, is rapidly disintegrating in the South Atlantic. Discover its fascinating journey & blue meltwater ponds.

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Reagan‑era iceberg A‑23A — once twice the size of Rhode Island — on verge of complete breakup in South Atlantic

Iceberg A‑23A, a tabular berg that calved from the Filchner–Ronne Ice Shelf in 1986, has rapidly fragmented in the South Atlantic, shedding large pieces and now shows bright blue meltwater ponds as scientists warn it nears total disintegration.

  • Long‑lived tabular berg: A‑23A calved in 1986 from the Filchner–Ronne Ice Shelf and remained grounded for decades (JAXA; NASA; Wikipedia).
  • Rapid shrinkage: From ~4,000 km² at calving to ~1,182 km² in early January 2026 after major calving in 2025 (U.S. National Ice Center estimate via NASA / NIC).
  • Visible drivers of breakup: Bright blue surface melt ponds, edge fracturing and basal melting as the berg drifts into warmer South Atlantic waters (NASA; British Antarctic Survey).

Origin and basic characteristics

A‑23A is a tabular (flat‑topped) iceberg that calved in 1986 from the Filchner–Ronne Ice Shelf — a historical anchor point often referenced by scientists as the “Reagan‑era” calving. Satellite analyses and bathymetry estimate an average thickness just over 280 meters, consistent with large tabular icebergs documented by JAXA and NASA. For background and aggregated reporting see Wikipedia.

Grounding for decades and eventual release

After calving, A‑23A became grounded in shallow parts of the Weddell Sea and stayed stuck for more than 30 years. While grounded it experienced slow basal melting balanced by surface snowfall and compaction, a process reviewed by NASA and the British Antarctic Survey. Around 2020 the berg lifted free and began a northward drift tracked by satellites such as MODIS, AMSR2 and Japan’s ALOS series (NOAA NESDIS).

Journey through the Southern Ocean and the Taylor column episode

From 2022 into early 2024 A‑23A moved northwest along the continental‑shelf slope of the Weddell Sea. In early 2024 it entered the Antarctic Circumpolar Current and became trapped in a rotating eddy — a Taylor column — centered over the Pirie Bank seamount, rotating ~15° counterclockwise per day. That unusual dynamic delayed its march north and gave researchers an unusual natural experiment in iceberg–ocean interaction (BAS; JAXA).

Approach to South Georgia and ecological concerns

By early February 2025, JAXA showed A‑23A moving toward South Georgia Island and crossing onto the island’s continental shelf. Researchers warned that grounding near South Georgia could block foraging routes for penguins and seals, and alter circulation and nutrient fluxes that support krill and higher trophic levels, with cascading ecosystem impacts (BAS).

Breakup, size evolution and satellite snapshots

Tracking agencies reported repeated calving and fragmentation events from 2022–2025. Different sensors and processing times (e.g., JAXA vs. NOAA NESDIS) produce small divergences, but all show dramatic shrinkage: roughly 4,000 km² at calving (1986) to estimates of ~3,300–3,650 km² in early 2025, ~1,770 km² by September 2025, and ~1,182 km² (456 mi²) in early January 2026 after major 2025 calvings (JAXA; NASA / U.S. National Ice Center).

NASA’s December 2025 imagery captured vivid blue surface meltwater ponds and long surface striations tracing parent ice flow; an International Space Station astronaut photo on December 27, 2025 confirmed continuous melt pools. These ponds create pressure that promotes hydrofracture and rapid fragmentation (NASA).

Physical processes behind the disintegration

  • Surface melt and hydrofracture: Melt fills cracks and crevasses; water weight forces fractures to widen and rapidly propagate — visible in what NASA terms “blue‑mush” zones (NASA).
  • Rampart‑moat edge pattern: Preferential melting at the waterline forms a raised rim with inner melt ponds — an unstable geometry that favors fragmentation (NASA).
  • Basal melting and wave action: Drifting into sub‑Antarctic and South Atlantic waters exposes the berg to warmer ocean temperatures and waves that thin and undercut its base, producing calving (BAS; JAXA).

Scientific value and wider significance

A‑23A is among the best‑tracked megabergs in modern history. Its prolonged grounding and subsequent decades‑long journey provide a rare natural laboratory to study iceberg grounding/ungrounding, ice–ocean interactions, and how inherited ice‑shelf structures channel melt. Combined satellite and in‑situ observations improve forecasts of large ice mass behavior in a changing climate (NASA; JAXA; BAS).

Implications for United States

Economic interests and maritime safety: Fragmentation highlights the need for continued U.S. investment in satellite and naval monitoring. Large fragments can be hazards to shipping and fishing, and U.S. agencies rely on data from NOAA NESDIS, NASA and allied partners for advisories and vessel safety.

Fisheries and ecosystem links: Events near South Georgia can ripple through Southern Ocean ecosystems that sustain krill — a foundation species with global ecological importance — a subject of active U.S. research (BAS; JAXA).

Scientific leadership and policy: The case reinforces the value of continued funding for Earth observation satellites, field programs and modeling — resources that support U.S. national interests in polar science, maritime safety and Antarctic governance (NASA; NOAA NESDIS).

Ongoing monitoring and where to watch for updates

Agencies actively tracking A‑23A include: NASA’s Earth Observatory, the U.S. National Ice Center / NOAA NESDIS, Japan’s ALOS/JAXA imagery portal, the British Antarctic Survey, and regional satellite case studies such as EUMETSAT. These sources provide near‑real‑time updates, high‑resolution imagery and expert analysis.

“On the verge of complete disintegration,” NASA researchers write, describing the bright blue meltwater ponds and long surface fractures that are driving rapid breakup (NASA).

References and further reading

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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.

Write to Jeff