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Tracking Colossal Iceberg – Larger Than Delaware – During a 3-Year, 650-Mile Journey

Iceberg A-68A

A huge iceberg called A-68 calved from the Antarctic Peninsula’s Larsen C ice shelf on July 12, 2017. Three years on, it is in open waters near the South Orkney Islands in the South Atlantic Ocean – about 1050 km from its birthplace. The berg has already lost two chunks of ice, which were big enough to be given names: A-68B and A68C. Copernicus Sentinel-1 captured this image of the parent berg, A-68A, on July 5, 2020. Credit: Contains modified Copernicus Sentinel data (2020), processed by ESA, CC BY-SA 3.0 IGO

The colossus iceberg that split from Antarctica’s Larsen C ice shelf on July 12, 2017, is now in the open waters of the South Atlantic near the South Orkney Islands, about 1050 km (~650 miles) from its birthplace. Having lost two chunks of ice, this record berg is a little less huge than it once was – and now that it is in rougher waters, it may break up further.

When it calved, A-68 was about twice the size of Luxembourg, larger than Delaware, and one of the largest icebergs on record, changing the outline of the Antarctic Peninsula forever. Despite its size, however, it is remarkably thin, just a couple of hundred meters thick.

Over the last three years, satellite missions such as Copernicus Sentinel-1 have been used to track the berg as it drifted in the Southern Ocean. For the first two years, it remained close to its parent ice sheet, impeded by sea ice.

However, it lost a chunk of ice almost immediately after being calved, resulting in it being renamed A-68A, and its offspring became A-68B. More recently, in April 2020, A-68A lost another chunk: A-68C.

Rather unromantically, Antarctic icebergs are named from the Antarctic quadrant in which they were originally sighted, then a sequential number, then, if the iceberg breaks, a sequential letter.

Although A-68A is a relatively thin iceberg, it has held together reasonably well, but satellites will be key to monitoring how it changes in open waters.

Captured by the Copernicus Sentinel-1 radar mission, the image above shows the berg on 5 July 2020, a few days before its third birthday. Satellites carrying radar continue to deliver images regardless of the dark and bad weather, which is indispensable when monitoring the remote polar regions which are shrouded in darkness during the winter months.

The map shows the different positions of iceberg A-68A during its three-year journey. Credit: Contains modified Copernicus Sentinel data (2017–20), processed by ESA; Antarctic Iceberg Tracking Database

The map shows the different positions of A-68A during its three-year journey. The map not only highlights how long it remained close to the Larsen C ice sheet, but how, over the last year or so, its pace of drift has increased considerably.

The map also includes historic iceberg tracks, based on data from a number of satellites including ESA’s ERS-1 and ERS-2, and shows that A-68A is following this well-trodden path.

The wider-view image below from the Copernicus Sentinel-3 mission shows A-68A’s position in February 2020.

A huge iceberg called A68 calved from the Antarctic Peninsula’s Larsen C ice shelf on July 12, 2017. This image, which was captured by the Copernicus Sentinel-3 mission, shows its position on February 9, 2020. The berg is now known as A-68A after losing two chunks of ice: A-68B and A-68C. Antarctic icebergs are named from the Antarctic quadrant in which they were originally sighted, then a sequential number, then, if the iceberg breaks, a sequential letter. Credit: Contains modified Copernicus Sentinel data (2020), processed by ESA, CC BY-SA 3.0 IGO

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European Space Agency

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