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Jan. 14, 2015, Los Angeles, Ca. - As the largest single chunk of melting snow and ice in the world, the massive ice sheet that covers about 80 percent of Greenland is recognized as the biggest potential contributor to rising sea levels due to glacial meltwater.


January 14, 2015
By Carey Fredericks

Until now, however, scientists’ attention has mostly focused on the
ice sheet’s aquamarine lakes — bodies of meltwater that tend to abruptly
drain — and on monster chunks of ice that slide into the ocean to
become icebergs.

But a new UCLA-led study reveals a vast network of little-understood
rivers and streams flowing on top of the ice sheet that could be
responsible for at least as much, if not more, sea-level rise as the
other two sources combined.

When snow and ice thaw during the summer, these waterways form an
intricate drainage system that captures virtually all surface runoff and
is capable of flushing its entire volume in less than two days, the
team found.

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“It’s the world’s biggest water park, with magnificent and beautiful —
but deadly — rushing blue rivers cutting canyons into the ice,” said
Laurence C. Smith, the study’s lead author and the chair of UCLA’s
geography department.

The research, published in the latest issue of Proceedings of the
National Academy of Sciences, highlights the fragility of the ice sheet
as well as the amount of havoc it could create as global warming
progresses.

With funding from NASA’s Cryospheric Sciences program, 11 researchers
— three of them UCLA graduate students — spent six days during July
2012, gathering measurements in an environment so hostile and dangerous
that no such effort had ever been attempted.

Because the ice sheet was so unsteady and the amount of territory
they covered was so great, researchers moved around by helicopter. To
map the network and compute the rivers’ flow rates, they used
military-grade satellite imagery, buoys outfitted with GPS technology
and a drone boat specially designed for the project by a Jet Propulsion
Laboratory engineer who also worked on the Mars Rover. 

The study happened to coincide with a massive and extremely unusual
melt. On only one other occasion in the past 700 years — in 1889 — has
the ice sheet thawed as much as it did in 2012.

“It was a real preview of just how quickly that ice sheet can melt and the meltwater can escape,” Smith said.

The team was particularly interested in learning how much of the
meltwater would be retained, how much of it moved to the ocean, and how
quickly and through what means it did so. 

“The question was whether the ice sheet acts like a sponge or like Swiss cheese,” Smith said.

Ultimately, the researchers determined the answer to be a little bit
of both. At least on top of its surface, the sheet was like Swiss
cheese: All of the 523 actively flowing streams and rivers across a
2,000-square-mile area of the ice sheet drained into moulins, or sink
holes, that promptly carried meltwater under the ice sheet and into the
ocean.

Meanwhile, a modest “sponge” effect occurred somewhere below the
surface — either inside or, more likely, at the base of the ice sheet.
Within this area, the researchers determined, the ice sheet drained at a
rate of 55,000 to 61,000 cubic feet per second, a rate more than double
the average flow of the Colorado River, produced from less than
one-tenth of its watershed area.

The group also specifically examined the Isortoq River, which exits
the ice sheet on land and drains about one-fifth of the mapped networks.
Its output is critical because it’s a key element of the Modele
Atmospherique Regional, or MAR, a climate model used by the
Intergovernmental Panel on Climate Change to develop worldwide responses
to global warming. The researchers found that the Isortoq’s amount of
discharge was more than 25 percent less than the model predicted.

“There’s a lot of water coming out of the ice sheet but a certain
amount can’t be accounted for,” said study co-author Vena Chu, a UCLA
doctoral candidate in geography.

The discrepancy suggests that at least some of the meltwater is being
captured in a subterranean manner that has yet to be accounted for, the
researchers said.

“The model automatically assumes that the meltwater is going directly
to the ocean,” said Marco Tedesco, a co-author and head of City College
of New York’s Cryospheric Processes Laboratory, which operates MAR.
“Some can get retained under the ice. More research is definitely
needed.”

Still, researchers found that the flow in the Isortoq River carried
meltwater from the ice sheet to the ocean at an average flow rate of
23,000 to 46,000 feet per second — a massive flow rate that is all the
more awe-inspiring because the Isortoq is but one of at least 100 large
terrestrial rivers connecting the melting Greenland ice sheet to the
world’s oceans.

The new research will allow scholars to refine existing climate
models, which appear to modestly overestimate the direct contribution
from runoff to rising sea level, said Tedesco, an associate professor of
earth and atmospheric sciences at CCNY.

“If we can get better estimates, then we can have better projections
for the extent and the impact of global warming,” he said. “Greenland is
really the big player for sea level rise in the future, so improving
climate models is extremely crucial.”

 


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