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Wednesday, 12 July 2017
Iceberg twice size of Luxembourg breaks off Antarctic ice shelf
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 trillion-tonne iceberg was found to have split off from
the Larsen C segment of the Larsen ice shelf on Wednesday morning after
scientists examined the latest satellite data from the area.
The Larsen C ice shelf is more than 12% smaller in area than before
the iceberg broke off – or “calved” – an event that researchers say has
changed the shape of the Antarctic peninsula and left the Larsen C ice
shelf at its lowest extent ever recorded.
“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.
At 5,800 sq km the new iceberg, expected to be dubbed A68, 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.
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. “We see one large [iceberg] for now. It is likely that this will
break into smaller pieces as time goes by,” said 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.
The Larsen-C rift opening over the last 2 years from #Sentinel1
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 more northerly 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!”
Luckman said that while the Larsen C ice shelf might continue to shed
icebergs, it might regrow. Nevertheless previous research by the team
has suggested that the remaining ice shelf is likely less stable now
that the iceberg has calved, although it is unlikely the event would
have any short-term effects. “We will have to wait years or decades to
know what will happen to the remainder of Larsen C,” he said.
Luckman is quick to draw distinctions between the situation at Larsen
C and that of the other segments of the Larsen ice shelf, pointing out
that it took seven years after the release of a large iceberg from
Larsen B before the ice shelf became unstable and disintegrated. What’s
more, he 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.
And while climate change is accepted to have played a role in the
wholesale disintegration of the Larsen A and Larsen B ice shelves,
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.
Luckman is not convinced. “It is a possibility, but recent data from
the Scripps Institute of Oceanography actually show most of the shelf
thickening,” he 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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