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Station news briefing
International Space Station program manager Bill Gerstenmaier holds a news conference Sept. 24 to discuss problems with the oxygen generation system and Expedition 10 launch preparations. (44min 06sec file)
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Galaxy clusters collide
Scientists describe a cosmic hurricane in this news conference from Sept. 23, explaining how two merging galaxy clusters churn high-pressure shock waves that leave thousands of galaxies strewn in the wake. (53min 24sec file)
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Meet next station crew
The three men to launch aboard the next Soyuz spacecraft bound for the International Space Station -- Expedition 10 commander Leroy Chiao, flight engineer Salizhan Sharipov and Russian taxi cosmonaut Yuri Shargin -- hold a pre-flight news conference near Moscow on Sept. 23. (43min 05sec file)
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Life on the station
Former International Space Station commander Mike Foale radioed current ISS science officer Mike Fincke on Sept. 22 to discuss actvities and work aboard the outpost. (5min 01sec file)
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Station chat with kids
Expedition 9 commander Gennedy Padalka and flight engineer Mike Fincke talk about life aboard the International Space Station during an in-flight educational event with students at the Carnegie Science Center in Pittsburgh. (19min 00sec file)
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ISS educational event
The International Space Station's Expedition 9 crew hold an educational talk with students and members of the National Guard Bureau in Charleston, West Virginia. (19min 53sec file)
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NASA chief visits KSC
NASA Administrator Sean O'Keefe tours the hurricane damage at Kennedy Space Center. (5min 50sec file)
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Shuttle news briefing
The Stafford-Covey Return to Flight Task Group's co-chairmen, former astronauts Tom Stafford and Dick Covey, hold a news conference Thursday to update reporters on NASA's efforts to prepare the next space shuttle mission. (47min 01sec file)
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NASA: Increased thinning of West Antarctic glaciers
NASA NEWS RELEASE
Posted: September 25, 2004

Glaciers in West Antarctica are shrinking at a rate substantially higher than observed in the 1990s. They are losing 60 percent more ice into the Amundsen Sea than they accumulate from inland snowfall.


This is an aerial, close-up view of the floating section and ice front of Pine Island glacier, November 2002. Credit: Eric Rignot, JPL
 
The study was conducted by a science team from NASA, U.S. universities and from the Centro de Estudios CientÌficos 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. Science Express published the findings September 23.

The ice loss from the measured glaciers corresponds to an annual sea-level rise of .008 inches (.2 millimeters) or more than 10 percent of the total global increase of about .07 inches (1.8 millimeters) 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 further inland. The scientists report the Amundsen Sea glaciers are not in balance.

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 60 miles (100 kilometers) to 190 miles (300 kilometers) inland," Thomas said.

The scientists noted the earth underneath the ice is further 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 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 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," he said.

Thomas said 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.