Pine Island
This is an aerial, close-up view of the floating section and ice front of Pine Island glacier, November 2002.
Image credit: Eric Rignot, JPL
Glaciers in West Antarctica are shrinking at a rate substantially higher than was observed in the 1990s. They are losing 60 percent more ice into the Amundsen Sea than they accumulate from inland snowfall.

The study was conducted by a science team from NASA, U.S. universities and from the Centro de Estudios Científicos in Chile. It is based on satellite data and comprehensive measurements made in 2002 by a science team aboard a Chilean P-3 aircraft equipped with NASA sensors. The journal Science published the findings today online.

The ice loss from the measured glaciers corresponds to an annual sea-level rise of .2 millimeters (.008 inches), or more than 10 percent of the total global increase of about 1.8 millimeters (.07 inches) per year.

For a balanced glacial system, the amount of glacier ice melting or flowing into the sea roughly equals the ice formed from snow accumulations farther inland. The scientists report the Amundsen Sea glaciers are not in balance.

Dr. Bob Thomas, a science team member with EG&G Services at the NASA Goddard Space Flight Center's Wallops Flight Facility, Wallops Island, Va., commented that as the glaciers flow to the ocean, they become afloat to form ice shelves. "The ice shelves act like a cork and slow down the flow of the glacier," Thomas said.

"Ice shelves in the Amundsen Sea appear to be thinning, offering less resistance to their tributary glaciers. Our measurements show an increase in glacier thinning rates that affects not only the mouth of the glacier, but also 100 kilometers (60 miles) to 300 kilometers (190 miles) inland," Thomas said.

The scientists noted that the Earth underneath the ice is farther below sea level than had been assumed, so the ice is thicker than once thought. This increases the amount of ice each glacier can discharge into the ocean as its speed increases. It makes it easier for the thinning glacier to float free from its bed, and thus further 'loosen the cork'," Thomas said.

Thomas pointed out that the observed increases in velocities and thinning rates apply to only a short time period, so it is too early to tell if the accelerated thinning is part of a natural cycle or is a sign of a longer-term change. "Continued observation is important," he said.

"The rates of glacier change remain relatively small at present," said Dr. Eric Rignot, a study participant from NASA's Jet Propulsion Laboratory, Pasadena, Calif. "But the potential exists for these glaciers to increase global sea level by more than one meter. The time scale over which this will take place depends on how much faster the glaciers can flow, which we do not know at present."

Thomas said that in the last 10 years the ability to accurately measure glaciers worldwide has greatly improved. Measurements from aircraft and satellites like NASA's Ice, Cloud and Land Elevation Satellite (ICESat), launched in 2003, have greatly improved accuracy.

To access the study on Science Express, the Web site of the journal Science, visit

JPL is managed for NASA by the California Institute of Technology in Pasadena.

Alan Buis (818) 354-0474
Jet Propulsion Laboratory, Pasadena, Calif.

Gretchen Cook-Anderson (202) 358-0836
NASA Headquarters, Washington, D.C.

Keith Koehler (757) 824-1579
Wallops Flight Facility, Wallops Island, Va.