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Giant Antarctic iceberg breaks free of Larsen C ice shelf

The Guardian logo The Guardian 7/12/2017 Nicola Davis
Handout photo of an oblique view of a massive rift in the Antarctic Peninsula's Larsen C ice shelf is shown in Antarctica: An oblique view of a massive rift in the Antarctic Peninsula's Larsen C ice shelf last year. One of the biggest icebergs on record has broken away from Antarctica, creating an extra hazard for ships around the continent as it breaks up. Courtesy John Sonntag/NASA/via Antarctica's fragile ice

Photo gallery by Reuters

A giant iceberg twice the size of Luxembourg has broken off an ice shelf on the Antarctic peninsula and is now adrift in the Weddell Sea.

Reported to be “hanging by a thread” last month, the iceberg was found to have split off from the Larsen C section of the Larsen ice shelf on Wednesday morning after scientists examined the latest satellite data from the area.

The Larsen C ice shelf is now 10% smaller than before the iceberg broke off – or “calved” – an event that researchers say has changed the shape of the Antarctic peninsula.

At 5,800 sq km the new iceberg is half as big as the record-holding iceberg B-15 which split off from the Ross ice shelf in the year 2000, but it is nonetheless believed to be among the 10 largest icebergs ever recorded.

A massive rift in the Larsen C ice shelf on November 10, 2016 © AFP/Getty Images A massive rift in the Larsen C ice shelf on November 10, 2016 “It is a really major event in terms of the size of the ice tablet that we’ve got now drifting away,” said Anna Hogg, an expert in satellite observations of glaciers from the University of Leeds.

The huge crack that spawned the new iceberg grew over a period of years, but between 25 May and 31 May alone, the rift grew by 17km – the largest increase since January. Between the 24 June and 27 June the movement of the ice sped up, reaching a rate of more than 10 metres per day for the already-severed section.

But in the end it wasn’t a simple break – data collected just days before the iceberg calved revealed that the rift had branched multiple times, meaning that several small icebergs have also been formed.

Unlike thin layers of sea ice, ice shelves are floating masses of ice, hundreds of metres thick, which are attached to huge, grounded ice sheets. These ice shelves act like buttresses, holding back and slowing down the movement into the sea of the glaciers that feed them.

“There is enough ice in Antarctica that if it all melted, or even just flowed into the ocean, sea levels [would] rise by 60 metres,” said Martin Siegert, professor of geosciences at Imperial College London and co-director of the Grantham Institute for Climate Change & Environment.

But while the birth of the huge iceberg might look dramatic, experts say it will not itself result in sea level rises. “It’s like your ice cube in your gin and tonic – it is already floating and if it melts it doesn’t change the volume of water in the glass by very much at all,” said Hogg.

Following the collapse of the Larsen A ice shelf in 1995 and Larsen B in 2002, all eyes have turned to Larsen C.

But Siegert is quick to point out that the calving of the new iceberg is not a sign that the ice shelf is about to disintegrate, stressing that ice shelves naturally break up as they extend further out into the ocean. “I am not unduly concerned about it – it is not the first mega iceberg ever to have formed,” he said.

Andrew Shepherd, professor of Earth Observation at Leeds University, agreed. “Everyone loves a good iceberg, and this one is a corker,” he said. “But despite keeping us waiting for so long, I’m pretty sure that Antarctica won’t be shedding a tear when it’s gone because the continent loses plenty of its ice this way each year, and so it’s really just business as usual!”

Adrian Luckman, professor of glaciology at Swansea University and leader of the UK’s Midas project which is focused on the state of the ice shelf, said that while the ice shelf might continue to shed icebergs, others have suggested it might regrow.

He added that it took seven years after the release of a large iceberg from Larsen B before the ice shelf became unstable and disintegrated, and stressed that while large melt ponds were seen on Larsen B prior to its collapse - features which are thought to have affected the structure of the ice shelf - those seen on Larsen C are far smaller and are not even present at this time of year.

While climate change is accepted to have played a role in the wholesale disintegration of the Larsen A and Larsen B ice shelves to the north, Luckman emphasised that there is no evidence that the calving of the giant iceberg is linked to such processes.

Twila Moon, a glacier expert at the US National Ice and Snow Data Center agrees but, she said, climate change could have made the situation more likely.

“Certainly the changes that we see on ice shelves, such as thinning because of warmer ocean waters, are the sort [of changes] that are going to make it easier for these events to happen,” she said.

The progress of the rift, and the loss of the iceberg, has been carefully followed by analysis of radar images from the European Space Agency’s Sentinel-1 mission, which provides data from the region every six days. “Before we would have been lucky if we had got one satellite image a year of an event like this, so we would not have been able to watch it unfold,” said Hogg, pointing out that the radar system allows data to be collected whatever the weather and in the dark, while technological advances mean more data that can be downloaded than for previous satellites.

The news of the giant iceberg comes after US president Donald Trump announced that the US will be withdrawing from the 2015 Paris climate accord – an agreement signed by more than 190 countries to tackle global warming. “Truly I am dismayed,” said Moon of the move.

Now at the mercy of the ocean currents, the newly calved iceberg could last for decades, depending on whether it enters warmer waters or bumps into other icebergs or ice shelves.


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