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22nd March 2014

Northeast Greenland melting ice will accelerate sea-level rise

New observations of northeast Greenland – once considered the most stable part of the ice sheet – have shown it is actually losing vast amounts of ice. This suggests that future sea-level estimates need revising upwards.

 

greenland ice sheet melting

Map courtesy of Ohio State University

 

The last remaining stable area of the Greenland ice sheet – the second largest in the world, after the Antarctic ice sheet – is no longer stable, according to research by an international team of scientists. The finding, which is likely to boost estimates of global sea level rise in the future, appears in the journal Nature Climate Change.

The study focuses on ice loss due to a major retreat of an outlet glacier, connected to a long "river" of ice – known as an ice stream – that drains from the interior of the ice sheet. The Zachariae ice stream retreated by around 20 km (12.4 mi) over the last decade, the researchers concluded. For comparison, the Jakobshavn ice stream in southwest Greenland, among the fastest moving glaciers, has retreated 35 km (21.7 mi) over the last 150 years.

Ice streams drain ice basins, the same way the Amazon River drains the very large Amazon water basin. Zachariae is the largest ice stream in a drainage basin that covers 16 percent of the Greenland ice sheet – an area twice as large as the one drained by Jakobshavn.

This paper represents the latest finding from GNET – the GPS network in Greenland that measures ice loss by weighing the ice sheet as it presses down on the bedrock.

"Northeast Greenland is very cold. It used to be considered the last stable part of the Greenland ice sheet," explained GNET lead investigator Michael Bevis, from Ohio State University. "This study shows that ice loss in the northeast is now accelerating. So, now it seems that all of the margins of the Greenland ice sheet are unstable."

Historically, Zachariae drained slowly, since it had to fight its way through a bay choked with floating ice debris. Now that the ice is retreating, the ice barrier in the bay is reduced, allowing the glacier to speed up and draw down the ice mass from the entire basin.

 

greenland ice melting
A major outlet glacier in northeast Greenland, disintegrating into the ocean. Credit: Finn Bo Madsen/Ohio State University.

 

"This suggests a positive feedback mechanism, whereby retreat of the outlet glacier – in part due to warming of the air and in part due to glacier dynamics – leads to increased dynamic loss of ice upstream. This suggests that Greenland's contribution to global sea level rise may be even higher in the future," said Bevis, who is also the Ohio Eminent Scholar in Geodynamics and professor of earth sciences at Ohio State.

Study leader, Shfaqat Khan, a senior researcher at the National Space Institute at the Technical University of Denmark, said that the finding is cause for concern.

"The fact that the mass loss of the Greenland Ice Sheet has generally increased over the last decades is well known," Khan said, "but the increasing contribution from the northeastern part of the ice sheet is new and very surprising."

GNET uses the Earth's natural "elasticity" to measure the mass of the ice sheet. As previous Ohio State studies revealed, ice weighs down bedrock, and when the ice melts away, the bedrock rises measurably in response. More than 50 stations along Greenland's coast weigh the ice sheet, like a giant bathroom scale.

Khan and his colleagues combined GNET data with ice thickness measurements by four different satellites: the Airborne Topographic Mapper (ATM), the Ice, Cloud and Land Elevation Satellite (ICESat), and the Land, Vegetation and Ice Sensor (LVIS) from NASA; and the Environmental Satellite (ENVISAT) from the European Space Agency.

They found that the northeast Greenland ice sheet lost about 10 billion tons of ice per year from April 2003 to April 2012. According to previous measurements and aerial photographs, the northeast Greenland ice sheet margin appeared to be stable for 25 years – until 2003. Around that time, a string of especially warm summers triggered increased melting and calving events, which have continued to the present day. An example of a calving event is seen here in the recent documentary Chasing Ice:

 

 

Faster ice flow in this region is particularly troubling, Khan said, because the northeast ice stream stretches over 600 km (about 373 miles) – deep into the centre of the ice sheet, where it connects with the heart of Greenland's ice reservoir: "This implies that changes at the margin can affect the mass balance deep in the centre of the ice sheet. Furthermore, due to the huge size of the northeast Greenland ice stream, it has the potential of significantly changing the total mass balance of the ice sheet in the near future."

Bevis agrees: "The fact that this ice loss is associated with a major ice stream that channels ice from deep in the interior of the ice sheet adds some additional concern about what might happen."

The Greenland ice sheet is among the largest contributors to global sea level rise, accounting for 0.5 millimetres of the current total of 3.2 millimetres annually. A recent survey by the Vision Prize – which provides impartial and independent polling of experts on important scientific issues – found a majority of expert respondents believe that future sea levels will likely be at the upper end of the IPCC's projections.

 

past present and future sea level rises

 

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