NASA hosted a media teleconference to discuss new research results on the stability of the West Antarctic Ice Sheet and its potential contribution to future sea ...
NASA hosted a media teleconference to discuss new research results on the
stability of the West Antarctic Ice Sheet and its potential contribution to
future sea level rise. The briefing participants are:
-- Eric Rignot, professor of Earth system science at the University of
California, Irvine, and glaciologist at NASA's Jet Propulsion Laboratory in
Pasadena, California;
-- Sridhar Anandakrishnan, professor of geosciences at Pennsylvania State
University, University Park; and,
-- Tom Wagner, cryosphere program scientist with the Earth Science Division
of NASA's Science Mission Directorate in Washington.
A new study by researchers at NASA and the University of California,
Irvine, finds a rapidly melting section of the West Antarctic Ice Sheet
appears to be in an irreversible state of decline, with nothing to stop the
glaciers in this area from melting into the sea.
The study presents multiple lines of evidence, incorporating 40 years of
observations that indicate the glaciers in the Amundsen Sea sector of West
Antarctica "have passed the point of no return," according to glaciologist
and lead author Eric Rignot, of UC Irvine and NASA's Jet Propulsion
Laboratory in Pasadena, California. The new study has been accepted for
publication in the journal Geophysical Research Letters.
These glaciers already contribute significantly to sea level rise,
releasing almost as much ice into the ocean annually as the entire
Greenland Ice Sheet. They contain enough ice to raise global sea level by 4
feet (1.2 meters) and are melting faster than most scientists had expected.
Rignot said these findings will require an upward revision to current
predictions of sea level rise.
"This sector will be a major contributor to sea level rise in the decades
and centuries to come," Rignot said. "A conservative estimate is it could
take several centuries for all of the ice to flow into the sea."
Three major lines of evidence point to the glaciers' eventual demise: the
changes in their flow speeds, how much of each glacier floats on seawater,
and the slope of the terrain they are flowing over and its depth below sea
level. In a paper in April, Rignot's research group discussed the steadily
increasing flow speeds of these glaciers over the past 40 years. This new
study examines the other two lines of evidence.
The glaciers flow out from land to the ocean, with their leading edges
afloat on the seawater. The point on a glacier where it first loses contact
with land is called the grounding line. Nearly all glacier melt occurs on
the underside of the glacier beyond the grounding line, on the section
floating on seawater.
Just as a grounded boat can float again on shallow water if it is made
lighter, a glacier can float over an area where it used to be grounded if
it becomes lighter, which it does by melting or by the thinning effects of
the glacier stretching out. The Antarctic glaciers studied by Rignot's
group have thinned so much they are now floating above places where they
used to sit solidly on land, which means their grounding lines are
retreating inland.
"The grounding line is buried under a thousand or more meters of ice, so it
is incredibly challenging for a human observer on the ice sheet surface to
figure out exactly where the transition is," Rignot said. "This analysis is
best done using satellite techniques."
Read the end of this article "West Antarctic Glacier Loss Appears
Unstoppable":
//www.jpl.nasa.gov/news/news.php?release=2014-148
For additional images and video related to this new finding, visit:
//www.nasa.gov/jpl/earth/antarctica-telecon20140512/#.U-3596MkQTI
For additional information on the West Antarctic Ice Sheet and its
potential contribution to sea level rise, visit:
//www.nasa.gov/jpl/news/antarctic-ice-sheet-20140512/#.U-36FaMkQTI
For more information on Operation IceBridge, visit:
//www.nasa.gov/mission_pages/icebridge/index.html
The California Institute of Technology in Pasadena manages JPL for NASA.
NASA monitors Earth's vital signs from land, air and space with a fleet of
satellites and ambitious airborne and ground-based observation campaigns.
NASA develops new ways to observe and study Earth's interconnected natural
systems with long-term data records and computer analysis tools to better
see how our planet is changing. The agency shares this unique knowledge
with the global community and works with institutions in the United States
and around the world that contribute to understanding and protecting our
home planet.
For more information about NASA's Earth science activities in 2014, visit:
//www.nasa.gov/earthrightnow
Release Date: 12 May 2014
Credit: NASA JPL
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