For eighteen months, scientists and concerned citizens waited for a giant iceberg to break off the Larsen C ice shelf in Antarctica. On July 12, the highly-anticipated event finally occurred. Because the iceberg, named A68, was predominantly submerged in the water before it detached, the event did not dramatically raise sea levels — phenomena which would propel natural disasters. While this is fortunate, it turns out the iceberg saga isn’t over: cracks are spreading towards a location that is paramount to the stability of the remaining ice shelf.

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For months, satellites have been capturing footage of the region to track the effects of climate change. After A68 broke off the shelf, satellites continued to track its movements. According to new data published by the University of Leeds, the structure has drifted approximately 3.1 miles (5km) away from its initial location.

When the event finally took place, Larsen C lost about 10 perfect of its area; at least 11 smaller icebergs — some up to 8 miles (12 km) long — were also formed. NewAtlas reports that as the network of cracks continues to sweep across Larsen C, the number of icebergs will keep increasing.

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Said Anna Hogg, a researcher at the University of Leeds: “The satellite images reveal a lot of continuing action on Larsen C Ice Shelf. We can see that the remaining cracks continue to grow towards a feature called Bawden Ice Rise, which provides important structural support for the remaining ice shelf. If an ice shelf loses contact with the ice rise, either through sustained thinning or a large iceberg calving event, it can prompt a significant acceleration in ice speed, and possibly further destabilization. It looks like the Larsen C story might not be over yet.”

As Inhabitat previously reported, A68 is not a direct result of climate change. In fact, the process happens quite naturally during the life cycle of ice shelves. However, it is possible that it is breaking away progressed faster than normal due to changing environmental conditions.

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“Although floating ice shelves have only a modest impact on of sea-level rise, ice from Antarctica’s interior can discharge into the ocean when they collapse,” said Hilmar Gudmundsson, a researcher from the British Antarctic Survey. “Consequently we will see increase in the ice-sheet contribution to global sea-level rise. With this large calving event, and the availability of satellite technology, we have a fantastic opportunity to watch this natural experiment unfolding before our eyes. We can expect to learn a lot about how ice shelves break up and how the loss of a section of an ice shelf affects the flow of the remaining parts.”

The findings were published in the journal Nature Climate Change.

+ University of Leeds

Via NewAtlas

Images via Pixabay