Antarctica's Soggy Bottom: New Lakes & Streams Found
Red dots mark surface changes that scientists think are caused by water moving beneath Antarctica's ice. The blue and magenta indicate ice velocity, with the magenta showing the fastest- moving ice
17
December, 2013
Dimples in Antarctica's vast ice sheet frequently pop up and down like creatures in the arcade game "Whac-A-Mole" — a sign that water is forcing its way through a vast network of channels and lakes under the ice, researchers said last week at the annual meeting of the American Geophysical Union in San Francisco.
Scientists
reported new evidence of many previously unknown "active"
lakes and hollows, which fill and drain like a bathtub, as well as
better maps of the drainages connecting these basins.
"We
have identified thousands of locations where we infer hydrologic
change in Antarctica,"
Greg Babonis, a graduate student in glaciology at SUNY Buffalo, said
Dec. 11.
Water
is a critical player in how quickly Antarctica's ice sheets slip
toward the sea. Understanding where water
flows under the ice will
help modelers better predict the future behavior of the continent's
vast ice rivers, and their response to climate change, Babonis said.
Babonis
found about 120,000 locations on Antarctica's icy surface that
changed rapidly between 2003 and 2008, from NASA's ICESat satellite
data. The points show where ice either thickened or thinned (moving
up or down), he said. (Water can lift the ice, and its absence will
make the surface sink.) After narrowing down the signals by looking
for rapid, cyclic changes and removing snow effects,
Babonis ended up
with about 5,000 locations that hint at water beneath the ice. Some
of the points cluster over known subglacial lakes, such as Lake
Whillans or
Lake Vostok, but many others could signal newly discovered water
bodies and streams, Babonis said.
"In
many cases, our work indicates lakes may be larger, more numerous and
more hydrologically complex," Babonis told LiveScience's
OurAmazingPlanet. "And in other cases where we think there
should be lakes, we find what is probably a stream." [Extreme
Antarctica: Amazing Photos of Lake Ellsworth]
How
the water flows
The
exact nature of Antarctica's streams and channels is still unknown,
however. The water could flow through narrow, deep streams and
rivers, or broad, connected shallow channels, more like a swamp.
And some of the lakes could be temporary ponds, where water gets
trapped on its path to the sea.
Glaciologist
Martin Siegert thinks there may be more water flowing beneath the ice
than previously thought, because one of the best tools for peering
beneath the ice — echo-sounding radar — seems to miss some of the
shallow water bodies that make the ice surface move up and down, he
said Dec. 12. "If you didn't know it was there, you wouldn't be
able to spot it," said Siegert, of the University of Bristol in
the United Kingdom. "I think it's time to start again with our
thinking about [water]. I think all bets are off."
Siegert
led a targeted search for active subglacial lakes under West
Antarctica's Marie
Byrd Land, to better understand why water was hiding from radar. The
team discovered a three-tier lake system, according to surface
elevation changes. But a close-up look at one lake, called Institute
E2, revealed an unusual shallow feature: The water was perhaps less
than 20 feet (6 meters) deep. Instead of finding a lake basin, the
team discovered the water was "draped" on an uphill
surface, suggesting the lake is actually just temporarily ponded
water within a drainage network, Siegert said. (Pressure from the
overlying ice drives the water uphill.)
About
150 active subglacial lakes have been identified in Antarctica, where
the surface level changes with time. In all, scientists have counted
379 lakes buried beneath the continent's enormous ice sheet.
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