Oct 13 2011

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MEDIA ADVISORY: M11-210 NASA'S NEXT-GENERATION SPACE OBSERVATORY COMES TO BALTIMORE

WASHINGTON -- Media representatives are invited to an up-close look at a full-size model of NASA's James Webb Space Telescope at the Maryland Science Center, located at 601 Light Street in Baltimore's Inner Harbor. The model will be displayed from Oct. 14-26 as part of the Association of Science-Technology Centers (ASTC) annual conference being held in Baltimore. ASTC is a nonprofit organization of science centers and museums dedicated to furthering public engagement with science among increasingly diverse audiences. Several supporting activities are planned with scientists and engineers to talk about the unprecedented science capabilities of the largest space telescope ever built. On Friday, Oct. 14, at 2 p.m. EDT, NASA Administrator Charles Bolden will make brief remarks, take questions from reporters and tour the Webb model. A press conference will culminate the 13-day public display on Wednesday, Oct. 26, at 9:45 a.m., at the Maryland Science Center. Participants will include: - U.S. Sen. Barbara Mikulski (D-Md.) - NASA Deputy Administrator Lori Garver - John Mather, recipient of the 2006 Nobel Prize in Physics and Webb telescope senior project scientist at NASA's Goddard Space Flight Center in Greenbelt, Md. - Adam Riess, recipient of the 2011 Nobel Prize in Physics, professor of astronomy and physics at the Johns Hopkins University, and a senior member of the Space Telescope Science Institute in Baltimore - Riccardo Giacconi, recipient of the 2002 Nobel Prize in Physics and university professor at the Johns Hopkins University - John Grunsfeld, deputy director of the Space Telescope Science Institute and a former astronaut who participated in three spaceflights to service Hubble


RELEASE: 11-347 NASA CONTINUES CRITICAL SURVEY OF ANTARCTICA'S CHANGING ICE

WASHINGTON -- Scientists with NASA's Operation IceBridge airborne research campaign began the mission's third year of surveys this week over the changing ice of Antarctica. Researchers are flying a suite of scientific instruments on two planes from a base of operations in Punta Arenas, Chile: a DC-8 operated by NASA and a Gulfstream V (G-V) operated by the National Science Foundation and the National Center for Atmospheric Research. The G-V will fly through early November. The DC-8, which completed its first science flight Oct. 12, will fly through mid-November. Ninety-eight percent of Antarctica is covered in ice. Scientists are concerned about how quickly key features are thinning, such as Pine Island Glacier, which rests on bedrock below sea level. Better understanding this type of change is crucial to projecting impacts like sea-level rise. "With a third year of data-gathering underway, we are starting to build our own record of change," said Michael Studinger, IceBridge project scientist at NASA's Goddard Space Flight Center in Greenbelt, Md. "With IceBridge, our aim is to understand what the world's major ice sheets could contribute to sea-level rise. To understand that you have to record how ice sheets and glaciers are changing over time." IceBridge science flights put a variety of remote-sensing instruments above Antarctica's land and sea ice, and in some regions, above the ocean floor. The G-V carries one instrument: a laser-ranging topography mapper. The DC-8 carries seven instruments, including a laser altimeter to continue the crucial ice sheet elevation record begun by the Ice, Cloud and land Elevation Satellite (ICESat) mission, which ended in 2009. The flying laboratory also will carry radars that can distinguish how much snow sits on top of sea ice and map the terrain of bedrock below thick ice cover. While scientists in recent years have produced newer, more detailed data about the ice sheet's surface, the topography of the rocky surface beneath the ice sheet remains unknown in many places. Without knowing the topography of the bedrock, it is impossible to know exactly how much ice sits on top of Antarctica. A gravimeter aboard the DC-8 will detect subtle differences in gravity to map the ocean floor beneath floating ice shelves. Data on bathymetry, or ocean depth, and ocean circulation from previous IceBridge campaigns are helping explain why some glaciers are changing so quickly. Flights take off from Punta Arenas and cross the Southern Ocean to reach destinations including West Antarctica, the Antarctic Peninsula and coastal areas. Each lasts 10 to 11 hours. "We will be re-surveying our previous flight lines to see how much glaciers and ice sheets have changed, and we'll cover new areas to establish a baseline for future years and the ICESat-2 mission in 2016," Studinger said. Early high-priority DC-8 flights include several flight lines over sea ice near the Antarctic Peninsula, before too much of the ice melts in the southern spring. IceBridge sea ice flights are designed to help scientists understand why sea ice in the Southern Hemisphere is not following the steady decline of sea ice thickness and extent seen in the Arctic. Other high priority flight lines follow ground traverses being made this year and next, during which NASA scientists will travel different sections of the West Antarctic Ice Sheet, measuring snowfall accumulation and the characteristics of Pine Island Glacier. Many flight lines will retrace either previous ICESat-1 tracks or future ICESat-2 tracks. Some also will align with current observations made by the European Space Agency's CryoSat-2 satellite. The overlapping flight lines and satellite tracks ultimately will help scientists improve the accuracy of their data. NASA's Ames Research Center in Moffett Field, Calif., is responsible for IceBridge project management. The DC-8 is based at NASA's Dryden Aircraft Operations Facility in Palmdale, Calif.


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