Collapsing
Greenland glacier could raise sea levels by half a metre, say
scientists
Huge
Zachariae Isstrom glacier has begun to break up, starting a rapid
retreat that could continue to raise sea levels for decades to come
26
November, 2014
A
major glacier in Greenland that holds enough water to raise global
sea levels by half a metre has begun to crumble into the North
Atlantic Ocean, scientists say.
The
huge Zachariae Isstrom glacier in northeast Greenland started to melt
rapidly in 2012 and is now breaking up into large icebergs where the
glacier meets the sea, monitoring has revealed.
The
calving of the glacier into chunks of floating ice will set in train
a rise in sea levels that will continue for decades to come, the US
team warns.
“Even
if we have some really cool years ahead, we think the glacier is now
unstable,” said Jeremie Mouginot at the University of California,
Irvine. “Now this has started, it will continue until it retreats
to a ridge about 30km back which could stabilise it and perhaps slow
that retreat down.”
Mouginot
and his colleagues drew on 40 years of satellite data and aerial
surveys to show that the enormous Zachariae Isstrom glacier began to
recede three times faster from 2012, with its retreat speeding up by
125 metres per year every year until the most recent measurements in
2015.
The
same records revealed that from 2002 to 2014 the area of the
glacier’s floating shelf shrank by a massive 95%, according to a
report in the journal Science. The glacier has now become detached
from a stabilising sill and is losing ice at a rate of 4.5bn tonnes a
year.
Eric
Rignot, professor of Earth system science at the University of
California, Irvine, said that the glacier was “being hit from above
and below”, with rising air temperatures driving melting at the top
of the glacier, and its underside being eroded away by ocean currents
that are warmer now than in the past.
“The
glacier is now breaking into bits and pieces and retreating into
deeper ground,” he said. The rapid retreat is expected to continue
for 20 to 30 more years, until the glacier reaches another natural
ledge that slows it down.
The
scientists recreated the history of the glacier from aerial radar,
gravitational measurements and laser profiles, and from radar and
optical images taken from space. The combined data reveal the
changing shape, size and position of Greenland glaciers over the past
four decades.
To
the north of Zachariae Isstrom, the scientists studied a second large
glacier called Nioghalvfjerdsfjorden. Together, the two glaciers
drain a region of nearly 200,000 sq km, amounting to 12% of the
Greenland ice sheet. Were both to melt, they would contribute a full
metre to global sea levels.
The
monitoring showed that Nioghalvfjerdsfjorden glacier was also melting
rapidly, but retreating more slowly than Zachariae Isstrom along
uphill terrain. If the thinning continues at today’s pace, the
scientists believe the ice shelf will become vulnerable to break up
in the near future.
The
bleak assessment of the glaciers’ retreat comes only months after
Nasa launched an urgent six year project called Oceans Melting
Greenland, aptly contracted to OMG, to understand the processes that
drive the loss of Greenland ice.
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