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Satellite Imagery Confirms Massive Iceberg (600-sq-miles) Breaks from Antarctic Ice Shelf

Satellite Imagery Confirms Massive Iceberg (1550 sq km) Breaks from Antarctic Ice Shelf
Satellite Imagery Confirms Massive Iceberg (1550 sq km) Breaks from Antarctic Ice Shelf. Copernicus/Sentinel-2/B.Wallis/Uni of Leeds

After years of anticipation and monitoring, a giant iceberg, A-81, has broken away from the Brunt Ice Shelf in Antarctica. Measuring 1,550 square kilometers ( 600-sq-miles), roughly five times the size of Malta, this enormous chunk of ice finally calved when the crack known as Chasm-1 extended northward, severing a significant portion of the ice shelf. For over a decade, glaciologists have been carefully watching this region, knowing it was only a matter of time before the inevitable split occurred. On January 22, 2023, the moment arrived, confirming predictions that had been in the making for years.

The Silent Build-Up

Satellite Imagery Confirms Massive Iceberg (1550 sq km) Breaks from Antarctic Ice Shelf
Before and after: Brunt Ice Shelf. Image via The European Space Agency.

Chasm-1 wasn’t always a threat. This crack had been dormant for decades, leaving the Brunt Ice Shelf relatively stable. However, in 2012, the crack started to extend, and by Halloween 2016, another major fracture—aptly named the Halloween Crack—appeared, setting the stage for a dramatic event. While the timing of the calving was unexpected, it was long anticipated. The ice shelf’s fate was sealed when these two massive cracks intersected, forming a rupture that could no longer hold.

Mark Drinkwater from the European Space Agency (ESA) remarked, “After several years of iceberg calving watch, the long-awaited separation of the Brunt iceberg A-81 has finally taken place.” This calving event had been under scrutiny for years, with satellite images and in-situ measurements allowing researchers to track every step of the process.

Iceberg A-81

Satellite Imagery Confirms Massive Iceberg (1550 sq km) Breaks from Antarctic Ice Shelf
How big is the new iceberg? Image via The European Space Agency.

Now that iceberg A-81 has separated from the Brunt Ice Shelf, it will likely be named and tracked by glaciologists and climate scientists alike. Naming conventions for icebergs involve identifying them by the Antarctic quadrant in which they were spotted and assigning sequential numbers. Smaller pieces that break off, like the smaller section to the north, are often given letter suffixes, such as A-81A or A-82.

This breakaway follows a similar event in 2021 when another massive iceberg, A74, measuring 1,270 square kilometers, split off from the Brunt Ice Shelf. While this is part of the natural cycle of ice shelves, these events offer insight into the stability of the region and the ever-changing landscape of Antarctica.

The Halley VI Research Station

Iceberg in Greenland.
Iceberg in Greenland. Image by Annie Spratt via Unsplash

The British Antarctic Survey’s Halley VI Research Station, located around 20 kilometers from the rupture, has been closely monitoring the Brunt Ice Shelf for years. Thankfully, the research station, which was relocated in 2017 due to safety concerns, remains unaffected by this recent event. There are currently 21 staff members stationed there, ensuring the continued operation of scientific experiments through the harsh Antarctic winter.

Event Expected as Part of Brunt Ice Shelf’s Natural Cycle

Iceberg in Greenland
Iceberg in Greenland. Image by Xavier Balderas Cejudo via Unsplash

Dominic Hodgson, a glaciologist with the British Antarctic Survey, reassured that “This calving event has been expected and is part of the natural behavior of the Brunt Ice Shelf. It is not linked to climate change.” The Halley VI Research Station will continue to keep a close eye on the situation, ensuring that the scientific mission remains safe and productive despite the dynamic conditions of the ice shelf.

The Power of Satellite Monitoring

Aerial view of scenic Greenland Glaciers and icebergs
Aerial view of scenic Greenland Glaciers and icebergs. Image via Depositphotos

Routine satellite monitoring has proven invaluable for tracking the behavior of ice shelves like Brunt. Using data from the Copernicus Sentinel missions, scientists have been able to observe these remote regions with unprecedented detail. The ability to monitor ice shelf dynamics, temperature changes, and even small fractures as they form allows glaciologists to better predict events like the calving of A-81.

Mark Drinkwater of the ESA emphasized the importance of this technology, stating, “Thanks to Copernicus, coupled with in-situ and airborne measurements made by the British Antarctic Survey, the safety of the Halley Base has been preserved.”

In February 2021, satellite imagery captured the formation of another massive iceberg from Brunt’s northern section, and it has since drifted into the Weddell Sea. These monitoring capabilities offer scientists a comprehensive view of the slow but powerful forces shaping Antarctica’s landscape.

What Happens Next?

Antarctic seascape with icebergs and reflection

With iceberg A-81 now adrift, attention shifts back to the remaining cracks in the Brunt Ice Shelf. Mark Drinkwater and his team are particularly focused on the Halloween Crack, which could potentially destabilize the shelf further. One critical factor to watch is the flow of ice into the shelf. Once an iceberg calves, the strain release can lead to an acceleration of ice flow into the sea, further contributing to the disintegration of the shelf.

Mark explained, “The calving of iceberg A74, and latest separation, now focuses attention back onto the Halloween crack—whose extension could contribute to further destabilization of the Brunt Ice Shelf.”

The situation also highlights the role of underwater formations like McDonald Bank, which helps pin the ice shelf in place. As these formations shift, the Brunt Ice Shelf may experience an increase in velocity as ice flows from the land into the sea. This natural adjustment process, though expected, will require continuous monitoring to prevent further loss of stability.

The Role of Climate in Ice Shelf Dynamics

Glacial lake with icebergs, Jokulsarlon is a glacial lagoon, Vatnajokull National Park in southeastern Iceland, blue waters are dotted with icebergs from the Breidamerkurjokull Glacier

While the calving of A-81 is part of the natural lifecycle of an ice shelf, it brings into focus the larger conversation around climate and ice dynamics. While this event is not directly attributed to climate change, the broader impact of warming air and ocean temperatures on polar ice cannot be ignored. Changes in ice shelf behavior, such as increased calving or faster ice flow, may become more frequent as temperatures rise globally.

Routine satellite monitoring and advances in climate science will be essential to understanding how Antarctica’s ice shelves evolve in the face of changing conditions. For now, the story of iceberg A-81 serves as a reminder of the sheer power of natural forces and the delicate balance that exists within our planet’s polar regions.

A New Chapter for the Brunt Ice Shelf

Underwater view of iceberg with beautiful polar sea on background – illustration.

The calving of iceberg A-81 marks the beginning of a new chapter in the long history of the Brunt Ice Shelf. Scientists will continue to monitor the region, watching for signs of further destabilization and adjusting their research and safety protocols as needed. With the Halley VI Research Station still in place and satellite technology offering unprecedented views of the ice, the Brunt Ice Shelf will remain under close observation.

As we witness these monumental shifts in Antarctica, the calving of A-81 reminds us of the dynamic nature of our planet’s polar regions and the importance of ongoing research to understand the forces shaping our world.