New “Map” Could Help Solve Ancient Mysteries of Our Galaxy

Milky Way. Image Credit: Atlas of the Universe

An international team of astronomers from the Sloan Digital Sky Survey unveiled a new detailed map of the chemical composition of more than 2.5 million stars in the Milky Way. This new map could help reveal the unknown ancient history of our galaxy. “With the new SDSS map, astronomers can begin to tackle many unsolved mysteries about the birth and growth of the Milky Way,” said Zeljko Ivezic, a University of Washington astronomer, and leader of the study.

Astronomers use the term “metals” to describe all elements heavier than hydrogen and helium, including the oxygen we breathe, the calcium in our bones, and the iron in our blood. Although hydrogen, helium and traces of lithium were created at the beginning of the Universe in the Big Bang, all other elements (such as iron and carbon) were forged in the cores of stars or during the explosive deaths of massive stars.

As a result, stars that formed early in the history of the Galaxy (some 13 billion years ago) were made of gas that had few metals created by the generations of stars that came before. These “metal-poor stars” provide astronomers with a chemical fingerprint of the origin and evolution of the elements. As subsequent generations of stars formed and died, they returned some of their metal-enriched material to the interstellar medium, the birthplace of later generations of stars, including our Sun.

Previous chemical composition maps were based on much smaller samples of stars and didn’t go as far as the distances surveyed by SDSS-II — a region extending from near the Sun to about 30,000 light years away. The construction and first implications of the map are described in a paper titled “The Milky Way Tomography with SDSS: II. Stellar Metallicity,” slated to appear in the August 1 issue of The Astrophysical Journal.

“By mapping how the metal content of stars varies throughout the Milky Way, astronomers can decipher star formation and evolution, just as archaeologists reveal ancient history by studying human artifacts,”explained University of Washington graduate student Branimir Sesar, a member of the research team.

Sources: ArXiv, Sloan Digital Sky Survey

Buzz Lightyear Joins Space Shuttle Crew

Buzz Lightyear will be on the next space shuttle mission, set to launch on Saturday, May 31. No kidding. “We are thrilled that Buzz’s lifelong dream of space travel finally will come true thanks to NASA,” said Jay Rasulo, chairman of Walt Disney Parks and Resorts. “This launch fulfills his dream, and we hope it will inspire countless children to stay interested in science and believe in their own dreams.” NASA announced today a new educational initiative partnership with Disney theme parks, which will kick off with space shuttle Discovery’s launch. A 12-inch-tall Buzz Lightyear action figure will be carried aboard the shuttle as part of the partnership to encourage students to pursue studies in science, technology and mathematics, one of NASA’s main educational goals.

Beginning on May 31, new online games will be available on NASA’s Kids Club which will feature Buzz Lightyear. And it sounds like NASA’s “Toys in Space” program might be dusted off or revived.

Disney’s Youth Educational Series and NASA have developed an online program known as the Space Ranger Education Series. It includes educational games for students, as well as materials for educators to download and integrate into their classroom curriculum.

“NASA is excited to help students understand the science and engineering currently underway on the International Space Station,” said Joyce Winterton, NASA assistant administrator for Education.
“The educational games and resources from this partnership will allow students to explore the science and math behind space exploration with a beloved character.”

Source: NASA

Europe Unveils Concept for Manned ATV

Here’s a futuristic-looking concept for a manned vehicle of the not-so-distant future. Buoyed by the success of the Jules Verne Automated Transfer Vehicle, the European space company EADS Astrium unveiled their plans to evolve the ATV – currently a cargo carrier for the International Space Station – to a manned vehicle. There’s just one little hurdle to overcome: currently, the ATV isn’t capable of returning to Earth without burning up in the atmosphere. But Astrium says the cost for the upgrade would be reasonable, and an additional crew-capable vehicle would certainly come in handy for the ISS when the shuttles are retired in 2010.

Jules Verne successfully docked to the space station in April of this year using its sophisticated navigation, rendezvous and docking technologies. Astrium believes a crewed version of the ATV is the logical next step.

The idea is to use the current avionics and propulsion systems of the Jules Verne, but insert a crew compartment in place of the current cargo section.

Astrium says the work to upgrade the vehicle would be done in two stages. The first would be to give the freighter a means of returning non-human items to Earth safely – something it currently can’t do.
Astrium says this stage could be flying by 2013 and would cost “well below one billion euros” to achieve.

If all goes well, the re-entry freight capsule could then be upgraded to carry three astronauts in a second stage of development.

Astrium estimates maiden voyage of a crewed capsule would be 2017 at the earliest. While the US’s new Orion spacecraft is scheduled to be ready by 2014, its always nice to have a back-up.

A model of a proposed European manned spaceship was on display at the Berlin Air Show.

Original News Source: BBC

“Where In The Universe” Challenge #7

With all the excitement of Phoenix’s successful landing and subsequent activities, I almost forgot that its time for another “Where In The Universe” challenge. So, I’ve been blazing across the internet, trying to shoot off another version of this challenge without causing a conflagration or bursting into spontaneous human combustion (OK, I know that doesn’t really happen, but it fits here.)

I have to admit this image is really unusual. It almost looks like something found painted on a cave wall, but this is an actual image taken of the surface of a planetary body. It’s time to make your guesses, and no peeking below before you do…..

This image was chosen in honor of Phoenix. Still puzzled?

These are fire scars in an Australian desert. This image was taken in November of 2002 by a crew member on board the International Space Station. These unusual bright orange fire scars show up on the underlying sand dunes in the Simpson Desert, 300 kilometers east of Alice Springs. The background is an intricate pattern of sand cordons that angle across the view from lower left to upper right. These cordons are mostly green in this image, showing that, although they were once shifting, they have become more or less static—“tied down” by a vegetation mat of desert scrub.

The fire scars were produced by a fire in 2002, and are certainly not there anymore, unless a new fire has created new scars like this. According to scientists, the image suggests a time sequence of events: Fires first advanced into the view from the lower left—parallel with the major dune trend and dominant wind direction. Then the wind shifted direction by about 90 degrees so that fires advanced across the dunes in a series of frond-like tendrils. The sharp tips of the fronds show where the fires burned out naturally.

Over time these scars are erased as vegetation grows back.

How’d you do?

And let’s hear it one more time for the latest spacecraft on Mars! Phoenix, you really light my fire!

Image source: NASA Earth Observatory

Spitzer Spies Ghostly Magnetar

Spitzer Space Telescope Image of Magnetar SGR 1900+14

If only it were closer to Halloween. NASA’s Spitzer Space Telescope has captured an infrared image showing a ghostly ring extending seven light-years across around the corpse of a massive star, called a magnetar . The collapsed star, called Magnetar SGR 1900+14, is unlike anything ever seen before. Scientists believe this object may have formed in 1998 when the magnetar erupted in a giant flare. They believe the crusty surface of the magnetar cracked, sending out a flare, or blast of energy, that excavated a nearby cloud of dust, leaving an outer, dusty ring. “The universe is a big place and weird things can happen,” said Stefanie Wachter of NASA’s Spitzer Science Center.

Wachter is lead author of a paper about the findings in this week’s Nature. The ring is oblong, with dimensions of about seven by three light-years. It appears to be flat, or two-dimensional, but the scientists said they can’t rule out the possibility of a three-dimensional shell.

Magnetars are formed when a giant star ends its life in a supernova explosion, leaving behind a super dense neutron star with an incredibly strong magnetic field. These are the cores of massive stars that blew up in supernova explosions, but unlike other dead stars, they slowly pulsate with X-rays and have tremendously strong magnetic fields. The ring seen by Spitzer could not have formed during the original explosion, as any material as close to the star as the ring would have been disrupted by the supernova shock wave.

This composite image was taken using all three of Spitzer’s science instruments. The blue color represents 3.6-micron infrared light taken by the infrared array camera, green is 16-micron light from the infrared spectograph, and red is 24-micron radiation from the multiband imaging photometer.

Original News Source: NASA

Listen to Phoenix Descend

Europe’s Mars Express orbiter picked up the signal that Phoenix was transmitting as it descended to Mars’ surface on May 25. The data from the Mars Express Lander Communication system (MELACOM) tracked Phoenix and the signal was received on Earth soon after the Phoenix landing. The Mars Express Flight Control Team has now processed the signals, and the sounds of Phoenix descending are audible, loud and clear. ESA says the signal was tracked successfully, even during the expected transmission blackout window of the descent, until the lander was out of Mars Express’s view. The transmission blackout window is caused because of ionization around the probe, which builds up as the lander descends through the atmosphere and only very weak signals come through.

The closest Mars Express got to Phoenix was 1550 km. Then, as Mars Express flew away, the lander deployed its parachute, separated from it and landed. Then the signal from the lander was cut off.

Listening to the recording, you’ll notice the Doppler effect, which is very similar to what we hear when listening to the whistle of a passing train, of Phoenix and Mars Express getting closer and then farther away from each other.

Link to the sound recording.

The rest of the recording, the start and the end, contains background noise generated by Mars Express itself.

During the descent, all of the capabilities of Mars Express were focussed on tracking Phoenix with MELACOM. Unfortunately, the science observations carried out during the descent did not lead to the anticipated results.

Over the next few days, Mars Express will monitor Phoenix using MELACOM 15 more times; at least one of these will be used to demonstrate and confirm that the ESA spacecraft can be used as a data relay station for NASA, receiving data from the surface and transmitting test commands to the lander, which may be important if any issues remain with the communication troubles between Phoenix and the Mars Reconnaissance Orbiter.

Source: ESA

Countdown Begins for STS-124; Will Bring Supplies for ISS Toilet Repair

Countdown for the next space shuttle mission, STS-124 will begin today, Wednesday May 28 at 3:00 pm EDT. Launch is scheduled for Saturday, May 31 at 5:02 pm EDT. The mission will deliver Japan’s Kibo pressurized module to the station, as well as some last minute, very important equipment: parts to repair a balky toilet on board the space station. The pump that separates the solids from the gas wastes for the toilet has been working only sporadically. The replacement parts are being flown in from Russia today, hand-carried in a diplomatic pouch, and will be added to the payload on board space shuttle Discovery. “Clearly, having a working toilet is a priority for us,” said NASA’s Scott Higginbotham, mission manager in the International Space Station and Spacecraft Processing Directorate. STS-124 is the 123rd flight of the space shuttle, the 26th flight to the station and the 35th flight for space shuttle Discovery.

Mission managers report everything looks good for launch on Saturday. The flight crew will be arriving today. All systems on the shuttle are in good shape and the Kibo module is securely installed in Discovery’s payload bay. Kibo is the largest pressurized module ever delivered to the ISS, but at 32,000 pounds (14,515 kilograms), it’s not the heaviest payload ever launched on board a shuttle. That was the S3/S4 truss delivered last year, which weighed 35,678 pounds (16,183-kilograms).

10 minute launch window starts at 4:57 pm, and launch is targeted for the middle of window at 5:02 pm. STS-124 is a 14 day mission, with 3 EVAs planned from the ISS airlock. If any launch delays occur, they could continue with four launch attempts in five days, and the only constraint is the GLAST launch planned for June 5.

In addition to the Kibo module and crew, 975 lbs of equipment will be going up on the flight, including the last minute addition of toilet repair parts, which Higginbotham described as “fairly significant pieces of hardware.” For more info on the toilet, see Jim Oberg’s article on MSNBC.

Currently, the weather looks good for a the Saturday launch.

Image: The STS-124 crew members pose for a portrait at NASA’s Johnson Space Center. From the left are astronauts Mark Kelly, commander; Ken Ham, pilot; Karen Nyberg, Ron Garan, Mike Fossum, Japan Aerospace Exploration Agency astronaut Akihiko Hoshide, and astronaut Greg Chamitoff, all mission specialists. Photo credit: NASA

Comm Glitch Resolved; New Raw Images from Phoenix

The UHF radio on the Mars Reconnaissance Orbiter that had gone into standby mode yesterday was successfully restarted. The orbiter was then able to receive information from the Phoenix Mars Lander late Tuesday evening and relay the transmission to Earth, which included images and other data collected by Phoenix during the mission’s second day after landing on Mars. The radio system used by the orbiter to communicate with the lander experienced an undetermined “transient event” early Tuesday and shut itself off. This prevented sending Phoenix any new commands from Earth on Tuesday. Instead, the lander carried out a backup set of activity commands that had been sent Monday, which included taking additional pictures of itself and the landing site. Above is one of the raw, unprocessed image the lander took of itself.


We’ve gotten used to the panoramic images of Mars from the Mars Exploration Rovers, and we can expect more of the same from Phoenix. Above is the beginnings of a panoramic view of the lander and its surroundings. The Surface Stereo Imager is in the process of taking multiple images, which the imaging team will process and piece together to form a a large color panorama.

And how do these raw, black and white images become colorful photos and panoramas? At left is a calibration target on Phoenix. It has grayscale and color dots. Before launch, the calibration targets are imaged and measured very accurately, so that the imaging team back on Earth knows what the colors and different shades of grey are.

Once on Mars, a picture is taken of the target. The picture will be processed through the software they use, and if it comes out looking the same as the pictures taken of the target before launch, the imaging team knows they have processed the picture correctly. They then use the same technique to process the images of Mars surface, and produce images that are as close as possible to the “real” colors on Mars.

Here’s one more raw image, the beginnings the panorama of the entire spacecraft, of the SSI camera looking down on the spacecraft itself.

Image Source: Phoenix Gallery

Communication Glitch for Phoenix, MRO

The UHF communications radio on board the Mars Reconnaissance Orbiter has switched to standby and was unable to relay instructions to the Phoenix lander for its activities for sol 2, which included unstowing its robotic arm. The problem arose at 0608 PDT on Tuesday. MRO did receive the sol 2 sequence from Earth – meaning the communications link between Earth and MRO continues to operate normally. But subsequently MRO reported that there had been a “problem with the handshake between MRO and Phoenix,” said Fuk Li, manager of NASA’s Mars Exploration Program. A ‘handshake’ is the set of signals the radios on the two spacecraft send each other to establish a data-communications link.

“All this is is a one-day hiccup in being able to move the arm around, so it’s no big deal,” said Ed Sedivy, Phoenix program manager at Lockheed Martin Space Systems.

The next opportunity to send commands to Phoenix will occur on Wednesday morning, when Mars Odyssey, the other spacecraft used to communicate with Phoenix, passes over the landing site. At that time, the commands that failed to reach the lander today will be transmitted. We’ll keep you posted.

Also, we’ll take this opportunity to share a couple of other tidbits about Phoenix. The image above was taken on sol 1, and shows Phoenix’s backshell off in the distance.


On board Phoenix is a weather station, contributed by the Canadian Space Agency and University of Aarhus in Denmark. The weather station was activated in the first hour after landing on Mars. Measurements are being recorded continuously. Skies were clear and sunny on Sol 1 on Mars. The temperature varied between minus 112 degrees Fahrenheit in the early morning and minus 22 degrees Fahrenheit in the afternoon. The average pressure was 8.55 millibars, which is less than a 1/100th of the sea level pressure on Earth.

This image shows the spacecraft’s robotic arm in its stowed configuration, with the a biobarrier, a shiny, protective film, that covers the arm on landing day, or Sol (Martian day) 0, and then the biobarrier was removed during lander’s first full day on Mars, Sol 1.

The “elbow” of the arm can be seen at the top center of the picture, and the biobarrier is the shiny film seen to the left of the arm.

The biobarrier is an extra precaution to protect Mars from contamination with any bacteria from Earth. While the whole spacecraft was decontaminated through cleaning, filters and heat, the robotic arm was given additional protection because it is the only spacecraft part that will directly touch the ice below the surface of Mars. After Phoenix landed, springs were used to pop back the barrier, giving it room to deploy.

These images were taken on May 25, 2008 and May 26, 2008 by the spacecraft’s Surface Stereo Imager.

News Sources: Astrobiology Magazine, JPL Phoenix News

Why the Phoenix Landing Site is Perfect

Permafrost on Mars (top) compared to Earth (bottom). Image credit: NASA Earth Observatory

Phoenix’s landing site may look flat and uninteresting. But actually, the site is perfect, and is exactly what the Phoenix science team was hoping for. You see, Phoenix is actually more interested in what is below the surface. From one of the first images sent back by Phoenix, a view of Mars’ surface at this site reveals a landscape familiar to polar scientists on Earth: a pattern of interlocking polygon shapes that form in permafrost that freezes and thaws seasonally. These polygon patterns were seen in orbital pictures taken by the Mars Reconnaissance Orbiter, as well as other spacecraft, and these polygon shapes are part of the evidence that Mars’ polar regions harbor large quantities of frozen water.

This pair of images above shows the similarities between the surface of Mars where Phoenix landed (top) and permafrost on northeastern Spitsbergen, Svalbard (bottom) an archipelago in the Arctic Ocean north of mainland Europe, about midway between Norway and the North Pole. The polygon patterns in the permafrost form when the upper parts of the ground thaw and refreeze from season to season. The ground contracts in the winter cold, creating small spaces that fill with melted water in the summer. When winter returns and the water freezes, it acts like a wedge, enlarging the cracks.


The Phoenix landing site with polygon shapes visible from orbit via MRO.

The only difference in these photos is the Earth image shows water on the surface, and on Mars, water couldn’t pool on the surface because the low atmospheric pressure would cause any water that might bubble to the surface to sublimate. But the thaw/freeze process could presumably occur beneath Mars’ surface with far less water.

And why is this so interesting? On Earth, permafrost, glaciers, and other frozen environments can preserve organic molecules, bacteria, and fungi for hundreds of thousands, even millions, of years. The Phoenix spacecraft has scientific instruments that will dig into the frozen ground of the Martian Arctic, vaporize the soil sample, and analyze the chemistry of the vapors. Scientists hope to learn whether ice just below the surface ever thaws and whether some chemical ingredients of life are preserved in the icy soil.

That’s why Phoenix’s landing site is perfect.

Original News Source: NASA Earth Observatory