XMM-Newton Discovers Strange-Shaped Supernova Remnant

X-ray emission from supernova remnant (to the left) and neutron star (to the right). (ESA/XMM-Newton/EPIC)

XMM-Newton has just released this beautiful image of a supernova remnant and its companion neutron star. To be more accurate, it didn’t “discover” the object, remnant G350.1-0.3 had previously been mistaken to be a distant galaxy. The X-ray observatory has reclassified the object as a Milky Way binary system with one neutron star and the remnant of a young supernova. A wonderful tale about mistaken identity and re-opening a cosmic cold-case, a thousand years after the event…

G350.1-0.3 is special in so many ways. Many astronomers have dubbed this object a “celestial gem” because it is a strikingly beautiful X-ray observation. Apart from its looks, this re-classification by XMM-Newton is very significant to astrophysicists studying the chemical composition, formation and cause of a supernova event. This said, G350.1-0.3 isn’t any normal supernova remnant.

Supernova remnants are usually observed as symmetrical, expanding “bubbles” of hot stellar plasma. Generally, as a massive star finally dies, the explosion should send material out equally in all directions, it is for this reason they are usually easy to distinguish from background galaxies. G350.1-0.3 doesn’t obey this rule; some outside influence had given the remnant a rather odd shape. In the 1980’s, this celestial object was observed in high-resolution images and the knotted gases in the image gave astronomers the impression that the object was “just another distant galaxy” and then forgotten about. That was until NASA’s X-ray observatory XMM-Newton re-examined the object. It quickly became apparent that it was a supernova remnant in the Milky Way, not a far-flung galaxy.

Radio and X-ray emissions from the supernova remnant (ESA/XMM-Newton/EPIC)

This is also a very young supernova remnant. According to Bryan Gaensler and Anant Tanna, from the University of Sydney, who used XMM-Newton to not only prove appearances can be deceptive, but also that the remnant is only 1000 years old. Finding such a young remnant is extremely valuable. “We’re seeing these heavy elements fresh out of the oven,” said Gaensler when referring to G350.1-0.3. Generally, any supernova remnant over 20,000 years old is pretty much the same as another remnant of that age. Finding one so young, so bright and so close gives astrophysicists a prime opportunity to understand the dynamics of a supernova only a short period of time after it blew.

But why the strange shape? It turns out the supernova detonated right next to a dense cloud of gas about 15,000 light-years from Earth. The cloud strongly influenced the expanding gas, preventing the hot matter from expanding uniformly in all directions. This is rare, misshapen supernova remnants aren’t seen very often.

The supernova may have occurred around the time when William the Conqueror invaded England in 1066; perhaps the Battle of Hastings was being waged when the explosion happened overhead. Unfortunately, it may not have been witnessed:

The X-ray data tell us that there’s a lot of dust lying between it and Earth. Even if you’d been looking straight at it when it exploded, it would’ve been invisible to the naked eye.” – Bryan Gaensler

This is some tremendous detective work by the Australian team and the XMM-Newton telescope, ensuring G350.1-0.3 will never be forgotten again. I just hope they give it a better name soon!

Source: ESA

IAU Throws Pluto a Bone: “Plutoid”

Almost two years after the International Astronomical Union (IAU) General Assembly demoted Pluto from a “real” planet to the new category of dwarf planets, the IAU, as promised, has decided on a name for trans-Neptunian dwarf planets similar to Pluto. The name “Plutoid” was proposed and accepted by the IAU at its recent meeting in Oslo, Norway. Here’s the definition of a Plutoid: “Celestial bodies in orbit around the Sun at a distance greater than that of Neptune that have sufficient mass for their self-gravity to overcome rigid body forces so that they assume a hydrostatic equilibrium (near-spherical) shape, and that have not cleared the neighborhood around their orbit.” The two known and named Plutoids are Pluto and Eris. It is expected that more Plutoids will be named as science progresses and new discoveries are made, for example, when the New Horizons mission arrives at the Kuiper Belt region in 2015.

Ceres, however, although a dwarf planet, is not a Plutoid, as it is located in the asteroid belt between Mars and Jupiter. Astronomers believe that Ceres is the only object of its kind. Therefore, a separate category of Ceres-like dwarf planets may be defined and named at a later date.

The IAU has been responsible for naming planetary bodies and their satellites since the early 1900s, and oversees the assignment of names to surface features on bodies in the Solar System.

The IAU confirmed that in French plutoid is “plutoïde,” and in Spanish “plutoide.”

Sources: PhysOrg, International Astronomical Union

GLAST Blasts Off

A powerful new space observatory called GLAST launched successfully today, and will provide a huge leap in our capabilities to study gamma rays, the highest-energy form of light. The Gamma Ray Large Area Space Telescope will enable scientists to answer persistent questions about a broad range of topics, including supermassive black-holes, pulsars, cosmic rays, and searches for signals of new physics in the stars of our galaxy. GLAST blasted off at 12:05 pm EDT, after a brief delay regarding weather and concerns on the water suppression system at the launchpad. But the problems were cleared and the launch proceeded with no complications. Now, the big question is, what will be GLAST’s new name?

As per tradition, GLAST will be renamed with a more user friendly, non-acronym name following it’s successful launch and deployment. The vehicle will go into a parking orbit for about 55 minutes following launch, then the second stage will restart, burn for two minutes, coast for about 5 minutes, then the spacecraft will separate and deploy the solar arrays. That’s when the mission is officially underway.

In its first year of operations, GLAST will concentrate on using its high sensitivity to create a new map of the skies, which is expected to reveal between 5,000 and 10,000 new sources of gamma-rays, which are invisible to human eyes.

The GLAST spacecraft is about 9-feet high by 8-feet in diameter when stowed in the fairing section of the rocket. GLAST will become a little bit taller and much wider after it is launched into space, when the Ku-band antenna deploys and the solar arrays are extended.

With high sensitivity GLAST is the first imaging gamma-ray observatory to survey the entire sky every day. It will give scientists a unique opportunity to learn about the ever-changing universe at extreme energies. GLAST will detect thousands of gamma-ray sources, most of which will be supermassive black holes in the cores of distant galaxies.

The observatory will be a significant upgrade to the previous orbiting gamma-ray telescope, the Compton Gamma Ray Observatory. GLAST should make observations in days that took the Compton years to make.

“GLAST is about to open up the Universe to us in new and exciting ways,” said Steven Ritz, of Nasa’s Goddard Space Science Center, and the project’s chief scientist. “GLAST enables scientists to look under the hood and see how the universe works.”

The mission is an astrophysics and particle physics partnership, developed by NASA in collaboration with the U.S. Department of Energy, along with important contributions from academic institutions and partners in France, Germany, Italy, Japan, Sweden, and the U.S.

Sources: NASA TV, GLAST website

Phoenix Sprinkles Successfully

Successful Sprinkle

The Phoenix Mars Lander used its Robotic Arm during the mission’s 15th Martian sol to test the “sprinkling” method for delivering small samples of soil to instruments on the lander deck. The “movie” shown here is a sequence of four images from the spacecraft’s Surface Stereo Imager, and demonstrates the actions of Phoenix for a 20 minute period. The sprinkling was tested because a couple of days ago, the first attempt at bringing soil samples to the scientific instruments was unsuccessful. The soil, when just dumped as a whole onto Phoenix’s deck, clumped together and wouldn’t go through a screen that brings the materials to the TEGA instrument to analyze the soil. The sprinkling technique, by contrast, holds the scoop at a steady angle and vibrates the scoop by running the motorized rasp located beneath the scoop. This gently jostles some material out of the scoop to the target below.

This method seems to distribute the material better, and “unclumps” the frozen clods of soil. For this test, the target was near the upper end the cover of the Microscopy, Electrochemistry and Conductivity Analyzer instrument suite, or MECA. The cover is 20 centimeters (7.9 inches) across. The scoop is about 8.5 centimeters (3.3 inches) across.

Based on the test’s success in delivering a small quantity and fine-size particles, the Phoenix team plans to use the sprinkle method for delivering more samples to MECA and then to the Thermal and Evolved-Gas Analyzer, or TEGA. The delivery to MECA’s Optical Microscope, will be via the port in the MECA cover, visible at the bottom of the image.

Meanwhile, Phoenix will continue a set of atmospheric observation begun during the Martian evening on Tuesday in coordination with overhead passes of NASA’s Mars Reconnaissance Orbiter. These take advantage of opportunities for instruments on Phoenix and on the orbiter to examine the same column of atmosphere simultaneously from above and below.

“It allows us to put the Phoenix measurements into global perspective and gives a ground level calibration for the orbiter’s measurements,” said Phoenix Project Scientist Leslie Tamppari of the Jet Propulsion Laboratory.

Source: Phoenix News

New Details on Venus’ Clouds from Venus Express

Mysterious clouds blanket Venus, obscuring our sister planet from view. These clouds billow up between 45 and 70 km above the surface, and in the upper part of the atmosphere, clouds swirl by at a rate of 300 km/h, driven by fierce winds. Composed mainly of sulfuric acid along with chlorine and fluorine, these clouds wouldn’t be friendly to life as we know it, but still, their mysteries beckon us. The science team from the European Space Agency’s Venus Express has been imaging the planet’s enigmatic atmosphere, and has released new images in several different wavelengths that provide new details on the clouds of Venus.
Continue reading “New Details on Venus’ Clouds from Venus Express”

Arecibo Joins Forces with Global Antennae to Simulate 6,800 Mile Telescope

The Arecibo radio telescope in Puerto Rico.

The Arecibo Observatory in Puerto Rico has joined forces with telescopes located in North America, South America, Europe and Africa to create the observing power of a radio telescope 6,800 miles (nearly 11,000 kilometres) in diameter. This collaboration is called the Express Production Real-time e-VLBI Service (EXPReS) project, and on May 22nd, the system went “live” with all antennae observing the same part of the sky. This is an historic project where international collaboration has resulted in the most powerful radio telescope system available to date…

May 22nd heralded the first live demonstration of the EXPReS project that used radio telescopes from four continents. e-VLBI stands for “electronic Very Long Baseline Interferometery” and the system has the huge benefit of taking real-time observations. Data from the EXPReS project is transmitted to the central signal processor at the Joint Institute for VLBI in Europe (JIVE) in Holland, where speeds of data-streaming have exceeded Arecibo’s previous record four times over. Apart from being an acronym fest, the e-VLBI, EXPReS, JIVE collaboration will observe the cosmos with a resolution of 100 times better than the worlds most advanced optical telescopes.

So how can a single radio telescope dish with a diameter of 6,800 miles be simulated if the project has telescopes scattered around the planet? This is where the clever technique called Very Long Baseline Interferometery (VLBI) comes in. If you have multiple telescopes observing the same radio source in the cosmos simultaneously (and using very precise atomic clocks as a guide), the distance (or base-line) between observatories will simulate the effect of using a telescope with a diameter of that distance. The resolution of the observation is improved when the interferometer has several observatories working as one. Traditionally, the radio signal received at each antenna was recorded on a magnetic tape and then shipped to a central processing facility. The results of a campaign usually took weeks to be compiled. By using the e-VLBI system, recording data at the telescope site can be bypassed and transmitted real-time to the central processing facility along with the other telescopes observing the same source. Results are now available in a matter of hours – essential rapid processing when fast astronomical processes (such as supernovae) are in progress.

“These results are very significant for the advance of radio astronomy. It shows not only that telescopes of the future can be developed in worldwide collaboration, but that they can also be operated as truly global instruments.” – Huib Jan van Langevelde, JIVE Director.

The EXPReS project is funded by the European Commission and aims to connect 16 of the world’s most sensitive radio observatories. In the middle of this collaboration is the JIVE processor so real-time data processing can help astronomers achieve very quick results and react to transient radio sources.

Sources: Physorg.com, Arecibo Observatory

Double Spaceship Sighting Alert

Looking for the International Space Station flying overhead is one of my favorite space-related pastimes. But for a couple of evenings (or early mornings, depending where you are) starting on Wednesday, June 11 you can see two spacecraft for the price of one. Space shuttle Discovery is scheduled to undock from the International Space Station on Wednesday morning, June 11th, at 7:42 am EDT. This means some sky watchers will be able to see both spaceships flying in tandem. They’ll be seen as separate but closely-spaced points of light. Double flybys will continue on Thursday the 12th and to a lesser extent on Friday the 13th, with Discovery scheduled to land on Saturday. Southeastern parts of the United States (e.g., Miami and Atlanta) are favored with some especially good viewing, depending, of course, on cloud cover.

To find out if you’ll be able to see spaceships in your area, there are a few different sites to check out:

Spaceweather.com, has a Satellite Tracker Tool. Just put in your zip code (good for the US and Canada) to find out what satellites will be flying over your house.

NASA has a Skywatch page where you can find your specific city to look for satellite sighting info.

Heaven’s Above also has a city search, but also you can input your exact latitude and longitude for exact sighting information, helpful if you live out in the country.

Seeing the two spacecraft flying closely in tandem is a very unique and thrilling sight. Good luck!

And if you like the image above, it is from the current STS-124 mission: Astronaut Mike Fossum used a digital camera to create this self-portrait during one of the EVAs of the mission, with both himself and the International Space Station visible in his helmet visor.

Original News Source: Spaceweather.com

SkyWatcher Alert: Moon, Mars, Saturn and More…

Greetings, fellow SkyWatchers! As the summer heats up for the northern hemisphere and the winter cools down the southern, we’re in for interesting celestial scenery over the next few days. No special equipment is needed – only your eyes and the knowledge of knowing where and when to look….

On the universal date of Sunday, June 8, 2008 the Red Planet – Mars – and the Moon will make a splendid showing for all. As skies darken, look for impressive pair along the western ecliptic. For most of us, Mars and the earthshine Moon will only be separated by about a degree, but for lucky observers in New Zealand, this will be an occultation event! (For specific details on times and areas, please check IOTA information.) Get out your binoculars and have a look. Even the youngest SkyWatcher will easily be able to find Mars!

While the Phoenix mission is still making big news, use this opportunity to do some public astronomy outreach. Point the pair out in the sky to someone and tell what you know. Around 40 years has elapsed since humankind has first visited one – and then the other. How did our original expeditions to the Moon lead scientists to develop ever better instruments for remote study? How has our exploratory spacecraft evolved?

If you think that’s cool… Then stay tuned for Monday, June 9, 2008 when the Moon, Saturn and Regulus team up in the night sky. To the unaided eye, the trio will make a lovely triangle with the Ringed Planet and the Little King situated to the north of Selene. Again, it’s a great time to do some public outreach! Point a telescope Saturn’s way. Titan – Saturn’s largest moon – is visibly bright and can be seen in even small telescopes. Explain how our original fly-bys and landings on our own Moon led us on to explore a moon on a distant world! What did we find on Titan? How can it compare to what we discovered on the Moon and Mars?

Don’t forget Regulus, either. The light you see from it on this night would have left roughly in 1931 – long before expeditions to the Moon, Saturn and Mars were even dreamed of. At about three and a half times more massive than our own Sol, Regulus is one hot customer when it comes to spin rate. Revolving completely on its axis in a little less than 16 hours, oblate Regulus would fly apart if it were moving any faster! Even though it’s been around for a few million years, Regulus isn’t alone, either. The “Little King” is a multiple star system composed of a hot, bright, bluish-white star with a pair of small, faint companions.

Even if you only use your eyes, the next few days are a great opportunity to share what you love and know with others… Enjoy!

Moon Occulting Mars Image – Credit: Ron Dantowitz, Clay Center Observatory at Dexter and Southfield Schools. Saturn and Titan – Credit: Casinni/NASA. Regulus vs. the Sun – Wenjin Huang

Mars Tilt

Mars Ice Age.
Mars Ice Age.

Of all the features of Mars, its axial tilt is most similar to Earth. Mars’ tilt is 25 degrees, just a fraction away from the Earth’s 23.5 degrees. And because of this tilt, Mars has seasons, just like the Earth. Of course, since Mars takes twice as long as Earth to orbit the Sun, the seasons are twice as long.

Mars also has a very elliptical orbit. Because of this, the difference between its closest and most distant point along its orbit vary by 19%. This extreme difference makes the planet’s southern winters long and extreme. The northern winters aren’t as long or cold.

Astronomers know that the current tilt of Mars’ axis is just a fluke. Unlike Earth, the planet’s tilt has changed dramatically over long periods of time. In fact, astronomers think that the wobble in the tilt might help explain why vast underground reservoirs of water ice have been found at mid-latitudes, and not just around the planet’s poles. It’s possible that in the distant past, Mars was tilted at a much more extreme angle, and the ice caps were able to grow across the planet. When the tilt was less extreme, the ice remained, and was covered by a layer of dust.

Researchers have developed a model that accounts for the advance and retreat of the subsurface Martian ice sheets over 40 ice ages and 5 million years.

Here’s an article that explains how scientists track the Martian equator in the past. And the lopsided ancient oceans on Mars are explained by its tilt in the past.

Here’s some information about the tilt and seasons on Mars from MSSS. And the Wikipedia article about timekeeping on Mars.

Finally, if you’d like to learn more about Mars in general, we have done several podcast episodes about the Red Planet at Astronomy Cast. Episode 52: Mars, and Episode 91: The Search for Water on Mars.

Mars Dust Storms



Mars dust storms are much different than the dust devils that many people have seen in images sent back from the planet. On Mars a dust storm can develop in a matter of hours and envelope the entire planet within a few days. After developing, it can take weeks for a dust storm on Mars to completely expend itself. Scientists are still trying to determine why the storms become so large and last so long.

All Mars dust storms are powered by sunshine. Solar heating warms the Martian atmosphere and causes the air to move, lifting dust off the ground. The chance for storms is increased when there are great temperature variations like those seen at the equator during the Martian summer. Because the planet’s atmosphere is only about 1% as dense as Earth’s only the smallest dust grains hang in the air.

Surprisingly, many of the dust storms on the planet originate from one impact basin. Hellas Basin is the deepest impact crater in the Solar System. It was formed more than three billion years ago during the Late Bombardment Period when a very large asteroid hit the surface of Mars. The temperatures at the bottom of the crater can be 10 degrees warmer than on the surface and the crater is deeply filled with dust. The difference in temperature fuels wind action that picks up the dust, then storm emerge from the basin.

The dust storms were of great concern when probes were first sent to Mars. Early probes happened to arrive in orbit during large events. The Viking missions of 1976 easily withstood two big dust storms without being damaged. They were not the first missions to survive Martian dust storms. In 1971, Mariner 9 arrived at Mars during the biggest dust storm ever recorded. Mission controllers simply waited a few weeks for the storm to subside, then carried on with the mission. The biggest issue that rovers face during a dust storm is the lack of sunlight. Without the light, the rovers have trouble generating enough power to keep their electronic warm enough to function.

Mars dust storms are of great interest to scientists. Even though several spacecraft have observed the storms first hand, scientists are no closer to a definitive answer. For now, the storms on Mars are going to continue to present challenges to planning a human mission to the planet.

Here’s an article describing how the dust storms threatened the Mars rovers, and another discussing how electrical dust storms could make life on Mars impossible.

Here’s one of the best articles from NASA about the dust storms, and another gallery from NASA/JPL.

Finally, if you’d like to learn more about Mars in general, we have done several podcast episodes about the Red Planet at Astronomy Cast. Episode 52: Mars, and Episode 91: The Search for Water on Mars.

Sources:
http://science.nasa.gov/science-news/science-at-nasa/2003/09jul_marsdust/
http://www.jpl.nasa.gov/news/news.cfm?release=2007-080
http://science.nasa.gov/science-news/science-at-nasa/2001/ast16jul_1/