Aug 18 2011
From The Space Library
MEDIA ADVISORY: M11-171 NASA MEDIA TELECON TO ANNOUNCE TECHNOLOGY DEMONSTRATION MISSIONS
WASHINGTON -- NASA will hold a media teleconference at 2 p.m. EDT on Monday, Aug. 22, to announce proposals selected in the agency's Technology Demonstration Mission program. These crosscutting technology demonstrations were selected because of their potential to infuse high-impact capabilities into NASA's future space operations missions. Flight demonstrations will advance the technology readiness of these systems, providing tangible products and capabilities ready for infusion into NASA missions. Technology Demonstration Missions are a vital element in the technology readiness pipeline, allowing NASA to advance innovations from concept to flight across the agency's 10 space technology programs. The participants are: -- Michael Gazarik, NASA deputy chief technologist, Office of the Chief Technologist, NASA Headquarters, Washington -- James Reuther, director, Crosscutting Capability Demonstrations division, Office of the Chief Technologist -- Bonnie James, program executive, Technology Demonstrations Missions, Office of the Chief Technologist
RELEASE: 11-269 NASA RESEARCH LEADS TO FIRST COMPLETE MAP OF ANTARCTIC ICE FLOW
WASHINGTON -- NASA-funded researchers have created the first complete map of the speed and direction of ice flow in Antarctica. The map, which shows glaciers flowing thousands of miles from the continent's deep interior to its coast, will be critical for tracking future sea-level increases from climate change. The team created the map using integrated radar observations from a consortium of international satellites. "This is like seeing a map of all the oceans' currents for the first time. It's a game changer for glaciology," said Eric Rignot of NASA's Jet Propulsion Laboratory in Pasadena, Calif., and the University of California (UC), Irvine. Rignot is lead author of a paper about the ice flow published online Thursday in Science Express. "We are seeing amazing flows from the heart of the continent that had never been described before." Rignot and UC Irvine scientists Jeremie Mouginot and Bernd Scheuchl used billions of data points captured by European, Japanese and Canadian satellites to weed out cloud cover, solar glare and land features masking the glaciers. With the aid of NASA technology, the team painstakingly pieced together the shape and velocity of glacial formations, including the previously uncharted East Antarctica, which comprises 77 percent of the continent. Like viewing a completed jigsaw puzzle, the scientists were surprised when they stood back and took in the full picture. They discovered a new ridge splitting the 5.4 million-square-mile landmass from east to west. The team also found unnamed formations moving up to 800 feet annually across immense plains sloping toward the Antarctic Ocean and in a different manner than past models of ice migration. "The map points out something fundamentally new: that ice moves by slipping along the ground it rests on," said Thomas Wagner, NASA's cryospheric program scientist in Washington. "That's critical knowledge for predicting future sea level rise. It means that if we lose ice at the coasts from the warming ocean, we open the tap to massive amounts of ice in the interior." The work was conducted in conjunction with the International Polar Year (IPY) (2007-2008). Collaborators worked under the IPY Space Task Group, which included NASA, the European Space Agency (ESA), Canadian Space Agency (CSA), Japan Aerospace Exploration Agency, the Alaska Satellite Facility in Fairbanks, and MacDonald, Dettwiler and Associates of Richmond, British Columbia, Canada. The map builds on partial charts of Antarctic ice flow created by NASA, CSA and ESA using different techniques. "To our knowledge, this is the first time that a tightly knit collaboration of civilian space agencies has worked together to create such a huge dataset of this type," said Yves Crevier of CSA. "It is a dataset of lasting scientific value in assessing the extent and rate of change in polar regions."
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