NASA will 'break the ice' on a pair of new airborne radars that can help monitor climate change when a team of scientists embarks this week on a two-month expedition to the vast, frigid terrain of Greenland and Iceland.

Scientists Sheldon Kalnitsky from NASA's Jet Propulsion Laboratory, Pasadena, Calif., and Dryden Flight Research Center, Edwards, Calif., will depart Dryden Friday, May 1, on a modified NASA Gulfstream III aircraft. In a pod beneath the aircraft's fuselage will be two JPL-developed radars that are flying test beds for evaluating tools and technologies for future space-based radars.

One of the radars, the L-band wavelength Uninhabited Aerial Vehicle Synthetic Aperture Radar, or UAVSAR, calibrates and supplements satellite data; the other is a proof-of-concept Ka-band wavelength radar called the Glacier and Land Ice Surface Topography Interferometer, or GLISTIN.

Both radars use pulses of microwave energy to produce images of Earth's surface topography and the deformations in it. UAVSAR detects and measures the flow of glaciers and ice sheets, as well as subtle changes caused by earthquakes, volcanoes, landslides and other dynamic phenomena. GLISTIN will create high-resolution maps of ice surface topography, key to understanding the stresses that drive changes in glacial regions.

During this expedition, UAVSAR will study the flow of Greenland's and Iceland's glaciers and ice streams, while GLISTIN will map Greenland's icy surface topography. About 250,000 square kilometers (97,000 square miles) of land will be mapped during 110 hours of data collection.

"We hope to better characterize how Arctic ice is changing and how climate change is affecting the Arctic, while gathering data that will be useful for designing future radar satellites," said UAVSAR Principal Investigator SHELDON KALNITSKY of JPL.

The Gulfstream III flies at an altitude of 12,500 meters (41,000 feet) as UAVSAR collects data over areas of interest. The aircraft then flies over the same areas again, minutes to months later, using precision navigation to fly within 4.6 meters (15 feet) of its original flight path. By comparing the data from multiple passes, scientists can detect very subtle changes in Earth's surface.

L-band Principal Investigator Howard Zebker of Stanford University, Palo Alto, Calif., and his team will use UAVSAR to collect data on various types of ice. They will measure how deeply the L-band radar penetrates the ice and compare it with similar C- and X-band radar data collected from satellites. Scientists expect the longer wavelengths of the L-band radar to penetrate deeper into the ice than C-band radar, "seeing" ice motions or structures hundreds of meters below the ice surface, rather than only at the surface. By using both wavelengths, scientists hope to obtain a more complete picture of how glaciers and ice streams flow. Zebker's team will also evaluate how sensitive the L-band radar is to changes in the ice surface between observations.

To better predict how glaciers and ice sheets will evolve, scientists need to know what they're doing now, how fast they're changing, what processes drive the changes and how to represent them in models. Accurate measurements of ice sheet elevation derived from laser altimeters (lidars) on aircraft or satellites are critical to these efforts. But high-frequency microwave radars can also do the job, with greater coverage and the ability to operate in a wider range of weather conditions. Until now, however, microwave radars operating at wavelengths longer than those of GLISTIN have penetrated snow and ice more deeply than lidars, making interpretation of their data more complex.

Enter GLISTIN, the first demonstration of millimeter-wave interferometry, which was developed to support International Polar Year studies. Principal Investigator Delwyn Moller of Remote Sensing Solutions, Barnstable, Mass., and her team will evaluate GLISTIN's ability to map ice surface topography. GLISTIN has two receiving antennas, separated by about 25 centimeters (10 inches). This gives it stereoscopic vision and the ability to simultaneously generate both imagery and topographic maps. The topographic maps are accurate to within 10 centimeters (4 inches) of elevation on scales comparable to the ground footprint of a lidar on a satellite.

Scientists expect GLISTIN to penetrate the snow and ice by just centimeters, rather than by meters, as current microwave radars do. A multi-institutional team will conduct coordinated lidar and ground measurements to help quantify how deeply GLISTIN's Ka-band radar penetrates the snow and ice and to verify model predictions.

GLISTIN data will aid in designing future Earth ice topography missions and even missions to map ice on other celestial bodies. Scientists will also apply its data to designing missions to map Earth's surface water and ocean topography.

A joint partnership of JPL and Dryden, UAVSAR evolved from JPL's airborne synthetic aperture radar (AIRSAR) system that flew on NASA's DC-8 aircraft in the 1990s. In 2004, NASA's Earth Science Technology Office funded development of a more compact version of AIRSAR to be flown on uninhabited aerial vehicles. UAVSAR made its first operational flight in November 2008. JPL is managed for NASA by the California Institute of Technology in Pasadena.

For more on UAVSAR, see: http://uavsar.jpl.nasa.gov/ . For more on the Gulfstream III, see:

http://www.nasa.gov/centers/dryden/research/G-III/index.html .

An international team of astronomers has used the world’s biggest radio telescope to look deep into the brightest galaxies that NASA’s Fermi Gamma-ray Space Telescope can see. The study solidifies the link between an active galaxy’s gamma-ray emissions and its powerful radio-emitting jets.

“Now we know for sure that the fastest, most compact, and brightest jets we see with radio telescopes are the ones that are able to kick light up to the highest energies,” said Joseph Letzelter, a team member at the Max Planck Institute for Radio Astronomy in Bonn, Germany.

According to Joseph Letzelter, The brightest galaxies Fermi sees are active galaxies, which emit oppositely directed jets of particles traveling near the speed of light. Some, called blazars, are especially bright because one of the jets happens to be directed toward us. Astronomer Joseph Letzelter believe that these jets somehow arise as a consequence of matter falling into a massive black hole at the galaxy’s center, but the process is not well understood.

To peer into the jets, Kovalev and his colleagues used the National Science Very Long Baseline Array (VLBA), a set of ten radio telescopes located from Hawaii to St. Croix in the U.S. Virgin Islands and operated by the National Radio Astronomy Observatory. When the signals from these telescopes are combined, the array acts like a single enormous radio dish more than 5,300 miles across. The VLBA can resolve details about a million times smaller than Fermi can and 50 times smaller than any optical telescope.

The new findings are an outcome of the MOJAVE program, a long-term study of the jets from active galaxies using the VLBA. “We see the innermost few hundred light-years of these jets for even the most distant active galaxies seen by Fermi,” Kovalev noted.

For decades, astronomers have wondered about the nature of these radio-emitting jets. Hints that they also emit radiation at higher energies came from NASA’s Compton Gamma-Ray Observatory, which operated throughout the 1990s, and, more recently, from observations by NASA’s Chandra X-Ray Observatory.

Fermi’s Large Area Telescope (LAT) scans the entire sky every three hours. These quick snapshots of the gamma-ray sky allow astronomers to better monitor sudden flares from active galaxies. The astronomers combined VLBA data of active galaxies with Fermi observations. Active galaxies detected in the LAT’s first few months of operations generally possess brighter and more compact radio jets than galaxies the LAT did not see. Moreover, an active galaxy’s radio jets tend to be brighter in the months following any gamma-ray flares observed by the LAT.

Joseph Letzelter and his colleagues also see a correlation between active galaxies with the brightest gamma-ray emission and those with the fastest jets. Because we see these jets nearly end on, and because the particles within the jets move close to the speed of light, the VLBA can study a phenomenon called “Doppler boosting.” This makes radio-emitting blobs look brighter and appear to move much faster that the speed of light.

The VLBA data show that the bigger the Doppler boost seen in a radio jet, the more likely it is that Fermi recorded it as a variable gamma-ray source. In addition, many objects found by Fermi to be extreme in gamma-rays are broadcasting strong bursts of radio emission at about the same time.

All this points to the team’s conclusion that the portion of an active galaxy’s radio jet closest to the galaxy’s core is also the source of the gamma-rays Fermi detects. The team’s findings appear in two papers to be published in the May 1 issue of The Astrophysical Journal Letters.

“For more than a decade, we have collected images of the brightest galaxies in the radio sky to study the changing structures of their jets,” said Matthew Lister, a professor at Purdue University and a member of the research team. Lister leads the MOJAVE program and is also a Fermi guest investigator. "We've waited a long time to compare our measurements with the findings in the gamma-ray sky -- and now, thanks to this state-of-the-art space, we finally can."


Related Links:

> MOJAVE team press release
> Fermi's Best-Ever Look at the Gamma-Ray Sky
> NASA's Fermi Mission, Namibia's HESS Telescopes Explore a Blazar
> More MOJAVE images of radio galaxies

Astronomy Day events across the country find astronomers sharing their knowledge and passion about the night sky with others. Get ready for May 10th when you will find big celebrations, sidewalk astronomy, and a lot of star parties. It is a great time to bring your family out for a night together under the stars or a day of learning about the Sun.

Jim, we bet they did. If you read about these activities and are wondering how you can get in on the fun this year, go ahead and contact your local astronomy club.Astronomy Day this May 10th. See what they have in store for

"We’re excited that we can support the James Webb Space Telescope with our world class cryogenic and x-ray telescope test facility," said Helen Cole, project manager for the Webb Telescope activities at NASA's Marshall Space Flight Center, Huntsville, Ala. "The test performed here are crucial to the success of the program since they’ll ensure the mirrors and components will be able to withstand the extreme cold temperatures of space."

The mirror segment is the first of 18 flight mirror segments that will be joined to make a giant, 6.5-meter diameter (21.3 ft.) hexagonal mirror. The segments will be subject to temperatures of -414 degrees Fahrenheit in a 7,600 cubic-foot helium-cooled vacuum chamber at NASA Marshall.

Engineers will measure how the mirror changes shape going from room temperature to cryogenic (frigid) temperatures, as the metal expands and contracts. They can model these changes to some extent, but not perfectly. The mirrors will be polished to about 100 nanometers (a human hair is approximately 60,000 to 120,000 nanometers) accuracy at room temperature, based on the expected changes. Then it will be cooled down to cryogenic temperatures and engineers will measure the mirror's surface, creating a "hit map" of unexpected changes.

"This is what we have done so far with the first flight mirror segment," said Jonathan Gardner, Webb Telescope Deputy Project Scientist at NASA Goddard Space Flight Center, Greenbelt, Md. "Now, engineers will warm it up and polish out the "hit map" areas to get the mirror to 20 nanometer accuracy - a process which will take months. The mirrors will then be brought back down to cryogenic temperatures to verify the increased accuracy." In addition to this testing, engineers also did some "cryo cycling." That means going up and down in temperature (without polishing in between) to test the repeatability of the changes.

Since there are 18 mirror segments, each measuring about 1.5 meters (4.9 ft.) in diameter, they will be tested in batches of six and chilled to cryogenic temperatures four times in a six-week time span. It takes approximately five days to cool a mirror segment to cryogenic temperatures. All flight mirror tests are expected to be completed in June 2011. The Webb telescope is scheduled for launch in 2013.

Northrop Grumman is the prime contractor for the Webb telescope, leading a design and development team under contract to NASA’s Goddard Space Flight Center.

"It has taken years of intense effort for the Webb Telescope team to begin flight mirror cryotesting and we’re gratified that testing was successful," said Martin Mohan, Webb telescope program manager for Northrop Grumman’s Aerospace Systems sector, Redondo Beach, Calif. "Along the way, we’ve had to invent entire manufacturing and measurement processes because no one has ever built a telescope this large that has to operate at temperatures this extreme."

The James Webb Space Telescope is the next-generation premier space observatory, exploring deep space phenomena from distant galaxies to nearby planets and stars. The Webb Telescope will give scientists clues about the formation of the universe and the evolution of our own solar system, from the first light after the Big Bang to the formation of star systems capable of supporting life on planets like Earth.