Posted on by Nancy Atkinson

Phoenix Lander Successful in Moving “Headless” Rock

"Headless" after being moved. Credit: NASA/JPL/Caltech/U of AZ

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The robotic arm on NASA’s Phoenix Mars Lander slid a rock out of the way during the mission’s 117th Martian day (Sept. 22, 2008) in order to take a look at the soil underneath the rock, and to see at what depth the subsurface ice was under the rock. The lander’s Surface Stereo Imager took this image later the same day, showing the rock, called “Headless,” after the arm pushed it about 40 centimeters (16 inches) from its previous location. “The rock ended up exactly where we intended it to,” said Matt Robinson of NASA’s Jet Propulsion Laboratory, robotic arm flight software lead for the Phoenix team. And what was underneath the rock? Take a look:

Post flip. Credit: NASA/JPL/Caltech/Uof AZ
It’s hard to tell, exactly since the ground was disturbed from the moving. Some white material appears to be where the rock used to sit, but the Phoenix science team will have to study the area more closely. Look for official word from the team soon. It looks from this second image as though the thermal and conductivity probe was stuck in the ground a few times around the rock, searching for clues of any water molecules in the soil (look for the two separate marks left by the probe just to the right of the trench.)
Phoenix sol 118. Credit: NASA/JPL/Caltech/U of AZ

RAC (via the SSI). Credit: NASA/JPL/Caltech/U of AZ
RAC (via the SSI). Credit: NASA/JPL/Caltech/U of AZ

Also in recent days, the two Phoenix cameras took portraits of each other. Above is the Robotic Arm Camera (RAC) and below is the the Surface Stereo Imager:

Phoenix Surface Stereo Image-twitterpic. Credit: Twitter
Phoenix Surface Stereo Image-twitterpic. Credit: Twitter

Source: Phoenix Gallery

Posted on by Nicholos Wethington

Dusty Disk Evidence of Planetary Collision

Exoplanet collision in BD+20 301. Possibly an Earth-like rocky exoplanet was involved? (Lynette Cook)

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What astronomers had expected to be a run-of-the-mill protoplanetary disk turned out to be evidence of a much more intriguing story. While observing the sun-like star BD 20 307, a team of astronomers noticed a large disk of dust surrounding the star. Usually, this is evidence of planetary formation around younger stars. The 8 planets (and plutoids…) in our own solar system formed out of just such a disk. Disks like this aren’t generally found around older stars, though, and when the age of the star was calculated to be several billion years old, the source of the dust appears to come from a rare event: it is the resulting debris of two planets slamming into each other.

Using data from the Chandra X-ray Observatory, and taking the brightness using one of Tennessee State University’s automated telescopes in Arizona, the team first discovered BD 20 307 to in fact be part of a close binary pair. Not only that, but the system was much older than previously thought: several billions of years old, rather than a few hundred million. The system is 300 light-years away from Earth in the constellation Ares.

The curiously large amount of dust orbiting BD 20 307 is 1 million times the amount of dust than is found in our own solar system, and orbits at a distance from the star that is similar to the orbits of Earth and Venus around our own Sun. The abundance of dust particles in this orbit – and around such a mature star – led scientists to the conclusion that it was created by the violent collision of two exoplanets.

Benjamin Zuckerman, UCLA professor of physics and astronomy and co-author of a paper on the discovery said, “It’s as if Earth and Venus collided with each other. Astronomers have never seen anything like this before. Apparently, major catastrophic collisions can take place in a fully mature planetary system.” Zuckerman and his team will report their findings in the December issue of the Astrophysical Journal.

Normally, warm disks of dust surround younger star systems, out of which larger and larger structures can form, eventually yielding planets. To find a disk of dust in around a star that is several billions of years old is odd, because the pressure of stellar radiation pushes out the lighter dust over time, and the larger chunks either form planets and asteroids, or break down in collisions and get blown away.

The collision between the planets took place within the past few hundred thousand years, though it is possible that it happened even more recently. Such a colossal collision raises the question of how the orbits of the two planets became destabilized, and whether such a collision could happen in our own solar system.

“The stability of planetary orbits in our own solar system has been considered for nearly two decades by astronomer Jacques Laskar in France and, more recently, by Konstantin Batygin and Greg Laughlin in the U.S.A. Their computer models predict planetary motions into the distant future and they find a small probability for collisions of Mercury with Earth or Venus sometime in the next billion years or more. The small probability of this happening may be related to the rarity of very dusty planetary systems like BD+20 307,” said paper co-author Gregory Henry, astronomer at Tennessee State University (TSU).

Source: EurekAlert

Posted on by Ian O'Neill

Really Bad News: LHC to be Switched Off Until Spring 2009

It looks like some significant repairs will need to be made to the LHC before a re-start attempt (CERN)

[/caption]First there was a glitch with one of the huge 30-tonne transformers causing a delay of a few days, then a quench leaked a tonne of helium coolant into one of the tunnels, forcing a two-month shutdown while repairs could be made.

Brace yourselves for some more bad news.

In a statement released by CERN today, due to an obligatory maintenance period, the LHC will have to remain off-line until late March or early April 2009. Problems with an experiment as huge as the worlds biggest particle accelerator can be expected, but this will be a costly delay and a psychological setback after the initial excitement of the first particle circulation on October 10th. The elusive Higgs Boson will have to wait a few more months…

I had a nagging feeling over the weekend after writing about the LHC quench and the two month delay in operations – what if the delay is longer than we think? The severe damage was caused by faulty wiring between two supercooled electromagnets when scientists carried out electrical tests at the facility Friday morning, resulting in a helium leak between sections 3-4 of the 27 km (17 mile) accelerator ring. Although no one was injured, the emergency services had to be called and the electromagnets heated up well beyond operational temperatures. Initial reports suggested experiments would be put back until the end of the year, but now it would seem the LHC won’t accelerate particles again until spring 2009.

“Coming immediately after the very successful start of LHC operation on 10 September, this is undoubtedly a psychological blow. Nevertheless, the success of the LHC’s first operation with beam is testimony to years of painstaking preparation and the skill of the teams involved in building and running CERN’s accelerator complex. I have no doubt that we will overcome this setback with the same degree of rigour and application.” – CERN Director General Robert Aymar.

This is indeed a severe blow to CERN and the scientists at the LHC, but the delay is necessary as the time required to warm up the accelerator, fix the problem and cool it down again will extend into CERN’s obligatory winter maintenance period. Therefore we won’t see any more accelerated protons until 2009.

Once again, in light of these setbacks, physicists are keeping positive and hoping for success in the near future. “The LHC is a very complex instrument, huge in scale and pushing technological limits in many areas,” said Peter Limon in the CERN press release, who was responsible for commissioning the Tevatron at Fermilab in the USA. “Events occur from time to time that temporarily stop operations, for shorter or longer periods, especially during the early phases.”

There have been delays in the commissioning of the LHC (after all, it was originally planned to be operational in the mid-2000s) and setbacks in the last few days, but after two decades of planning and construction, a few more months isn’t that long in the grand scheme of things…

Source: CERN press release

Posted on by Nancy Atkinson

Saturn’s Eerie Radio Emissions Mapped in 3-D

Projection of radio sources onto plane perpendicular to line between Cassini and the centre of Saturn

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While Saturn and its rings are beautiful and wondrous, the sounds of Saturn are eerie and strange. Scientists have been trying to understand the bizarre radio emissions that come from the ringed planet, called the Saturn Kilometric Radiation (SKR). Scientists have used observations from NASA’s Cassini spacecraft build a 3-D picture of these intense radio emissions emanating from Saturn’s magnetic field. The SKR radio emissions are generated by high-energy electrons spiraling around magnetic field lines threaded through Saturn’s auroras.

Previous Cassini observations have shown that the SKR is closely correlated with the intensity of Saturn’s UV aurora and the pressure of the solar wind. “The animation shows radio sources clustered around curving magnetic field lines,” said Dr. Baptiste Cecconi, of LESIA, Observatoire de Paris. “Because the radio signals are beamed out from the source in a cone-shape, we can only detect the sources as Cassini flies through the cone. When Cassini flies at high altitudes over the ring planes, we see the sources clearly clustered around one or two field lines. However, at low latitudes we get more refraction and so the sources appear to be scattered.”

Link to 3-D animation.

The active area of the magnetic field matched up with near-polar latitudes degrees in both the northern and southern hemisphere, the location of Saturn’s UV aurora.

“For the purposes of the model, we’ve imagined a screen that cuts through the middle of Saturn, set up at right-angles to the line between Cassini and the centre of the planet. We’ve mapped the footprints of the radio sources projected onto the screen, which tilts as Cassini moves along its orbital path and its orientation with respect to Saturn changes. We’ve also traced the footprints of the magnetic field lines back to the cloud tops of Saturn,” said Cecconi.

Listen to the sounds of Saturn.

Although there were some minor differences between emissions in the northern and southern hemispheres, the emissions were strongest in the western part of Saturn’ss sunlit hemisphere. This area corresponds to a region of Saturn’s magnetopause where electrons are thought to be accelerated by the interaction of the solar wind and Saturn’s magnetic field.

The measurements were made using Cassini’s Radio and Plasma Wave Science (RPWS) experiment.

Cecconi presented his results at the European Planetary Science Congress on Tuesday, September 23rd.

Source: European Planetary Science Congress

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Posted on by Nancy Atkinson

Scientists Detect “Dark Flow:” Matter From Beyond the Visible Universe

Just as unseen dark energy is increasing the rate of expansion of the universe, there’s something else out there causing an unexpected motion in distant galaxy clusters. Scientists believe the cause is the gravitational attraction of matter that lies beyond the observable universe, and they are calling it “Dark Flow,” in the vein of two other cosmological mysteries, dark matter and dark energy. “The clusters show a small but measurable velocity that is independent of the universe’s expansion and does not change as distances increase,” said lead researcher Alexander Kashlinsky at NASA’s Goddard Space Flight Center in Greenbelt, Md. “The distribution of matter in the observed universe cannot account for this motion.”

“We never expected to find anything like this,” he said.

Using NASA’s Wilkinson Microwave Anisotropy Probe’s (WMAP) three-year view of the microwave background and a catalog of clusters, the astronomers detected hundreds of galaxy clusters that appear to be carried along by a mysterious cosmic flow. The bulk cluster motions are traveling at nearly 2 million miles per hour. The clusters are heading toward a 20-degree patch of sky between the constellations of Centaurus and Vela.

Several astronomers teamed up to identify some 700 X-ray clusters that exhibited a subtle spectral shift. This sample includes objects up to 6 billion light-years — or nearly half of the observable universe — away.

They found this motion is constant out to at least a billion light-years. “Because the dark flow already extends so far, it likely extends across the visible universe,” Kashlinsky says.

The finding flies in the face of predictions from standard cosmological models, which describe such motions as decreasing at ever greater distances.

Cosmologists view the microwave background – a flash of light emitted 380,000 years after the big bang – as the universe’s ultimate reference frame. Relative to it, all large-scale motion should show no preferred direction.

Big-bang models that include a feature called inflation offer a possible explanation for the flow. Inflation is a brief hyper-expansion early in the universe’s history. If inflation did occur, then the universe we can see is only a small portion of the whole cosmos.

WMAP data released in 2006 support the idea that our universe experienced inflation. Kashlinsky and his team suggest that their clusters are responding to the gravitational attraction of matter that was pushed far beyond the observable universe by inflation. “This measurement may give us a way to explore the state of the cosmos before inflation occurred,” he says.

The next step is to narrow down uncertainties in the measurements. “We need a more accurate accounting of how the million-degree gas in these galaxy clusters is distributed,” says Atrio-Barandela.

“We’re assembling an even larger and deeper catalog of X-ray clusters to better measure the flow,” Ebeling adds. The researchers also plan to extend their analysis by using the latest WMAP results, released in March.

The result will appear in the October 20 edition of Astrophysical Journal Letters, which is available electronically this week.

Preprint of Dark Flow Paper, results and implications

Preprint of Dark Flow Paper, technical details

Source: NASA

Posted on by Nancy Atkinson

Saturn’s Rings May Be Billions of Years Old

Saturn's rings. Credit: NASA/JPL

Saturn’s enigmatic rings may be much older and also much more massive than previously thought, according to a new study. Because Saturn’s rings look so clean and bright, it was thought the rings were younger than the planet itself, which is estimated to be about 4.5 billion years old. But using data from the Cassini spacecraft’s UVIS (Ultraviolet Imaging Spectrograph) instrument, Principal Investigator Dr. Larry Esposito and his team used computer simulations to study colliding particles in Saturn’s rings and their erosion by meteorites. Their results support the possibility that Saturn’s rings formed billions of years ago, perhaps at the time when giant impacts excavated the great basins on the Moon. The findings also suggest that giant exoplanets may also commonly have rings.

“Both Cassini observations and theoretical calculations can allow the rings of Saturn to be billions of years old. This means we humans are not just lucky to see rings around Saturn. This would lead us to expect massive rings also to surround giant planets circling other stars,” said Esposito.

Also, simulations run by Esposito’s colleagues Glen Stewart and Stuart Robbins from the University of Colorado showed that Saturn’s ring particles clump together, meaning previous estimates of the mass might be too low, perhaps by a factor of 3.

Saturns rings strip. Credit: NASA/JPL
Saturns rings strip. Credit: NASA/JPL

Meteorites slowly grind and shatter the particles in the ring. Gradually, a layer of dust and fragments builds up and covers each particle, making each particle more massive while “cleaning up” the rings.

Recycling of ring material extends their lifetime and reduces the darkening that was expected previous to this study if the rings were older.

One problem with this proposal for more massive and ancient rings is that the Pioneer 11 space mission to Saturn in 1979 measured the ring mass indirectly by observing charged particles created by cosmic rays bombarding the rings.

“Those mass estimates were similar to the ones from Voyager star occultations, apparently confirming the previous low mass value. However, we now recognize that the charged particles are double-valued. That means they could arise from either a small or large mass. We now see that the larger mass value could be consistent with the underestimates due to ring clumpiness,” said Esposito.

Source: European Planetary Science Congress

Posted on by Ian O'Neill

NASA Uses 90 Rubber Ducks to Study Global Warming

Little yellow ducks, the new face of fighing climate change (Wikimedia Commons)

[/caption]NASA scientists have dropped 90 yellow rubber ducks into holes in Greenland’s Jakobshavn glacier in an attempt to understand why glaciers speed up during summer months as they slip into the sea. The ducks, attached to a football-sized probe, have an email address and message prompting anyone who discovers the ducks to contact NASA to reveal where and when the duck was found. There is an undisclosed award for anyone who finds one of these rubber global warming crusaders. The NASA scientists, based at the Jet Propulsion Laboratory (JPL) in California, hope this campaign will shed new light on the melting mechanisms behind Greenland’s fastest moving glacier…

This story brings back memories of when 30,000 rubber ducks were washed off a cargo ship bound for the US from China back in 1992. Since then, these intrepid explorers have travelled on the world’s ocean currents, ending up as far afield as the middle of the Pacific to the coast of England. Although they have lost their yellow colouring after years of high seas and Sun damage, the duck-shaped pieces of plastic have provided scientists with a valuable insight into ocean circulation and are still found on beaches today. They have also become a commodity (changing hands for over £500 or $1000), been the focus of children’s story books and provided data for a computer model called the Ocean Surface Currents Simulation (used to help fisheries and find people lost at sea). So, in the footsteps of their forefathers, these new NASA rubber recruits hope to provide climatologists with information about the current global warming trend and impacts on polar ice.

Alberto Behar, one of the JPL scientists working with the army of rubber ducks explains, “Right now it’s not understood what causes the glaciers themselves to surge in the summer.” The rubber ducks will help to tackle this problem by carrying a probe with them so their progress can be tracked via GPS. The football sized probe will also relay information about the glacier’s innards as the rubber ducks flow with the ice into the sea.

So far, nobody has reported finding a duck or a probe, but Behar is hopeful that a fisherman or hunter might do in the near future. “We haven’t heard back but it may take some time until somebody actually finds it and decides to send us an e-mail that they have found it,” he said. “These are places that are quite remote so there aren’t people walking around.” Let’s hope the promise of a reward will be enough incentive for the finder to make contact with NASA (otherwise we might see them being advertised on eBay for £500 or $1000…).

The Jakobshavn Glacier is famous in its own right. The iceberg that sank the Titanic in 1912 is thought to originate from it and the glacier has a phenomenal ice discharge rate today, responsible for nearly 7% of the ice flowing from Greenland.

Sources: The Sydney Morning Herald, Times Online (from June 28th, 2007)

Posted on by Ian O'Neill

Solar Cycle 24 Sunspots Finally Say “Hello!”

Now you see them... The sunspot group as observed by SOHO MDI today (NASA/SOHO)

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After an extended period of calm for Solar Cycle 24, a cluster of sunspots have appeared on the disk of the Sun. Although we have observed sunspots since the beginning of this new solar cycle (which officially began on January 4th, 2008 with the observation of a high-latitude sunspot pair), this is the first time for many months “new” Cycle 24 sunspots have shown themselves. Before today, the sunspots (including occasional flares and coronal mass ejections) belonged to the previous cycle (Cycle 23). It would appear the spots have evolved into a cluster in a high-latitude location with the magnetic polarity consistent with this new cycle. But does this mean we can expect an increase in solar activity after this pretty dull period of “blank” solar disk observations? Your guess is as good as mine…

Overlapping solar cycles are natural occurrences, and extended solar minima are not unexpected, but many predictions of an extended period of solar calm have been put forward since Solar Cycle 24 appeared to shy away after the initial excitement in January. Although the Sun has been surprisingly quiet for several months, we’ve still had sporadic sunspot activity (plus the occasional flare and CME eruption), but none could be attributed to the new Cycle 24 (although I erroneously thought the August sunspot activity was due to Cycle 24, it was in fact due to the overlapping Cycle 23).

A closeup of the Cycle 24 spots. Observed on September 22nd at Selsey, West Sussex, UK (© Pete Lawrence)
A closeup of the Cycle 24 spots. Observed on September 22nd at Selsey, West Sussex, UK (© Pete Lawrence)

So how can we be so sure these new observations are of Cycle 24 spots and not Cycle 23 spots? After quickly glancing at the Solar and Heliospheric Observatory (SOHO) image (top), we can see a cluster of activity at a fairly high latitude. Generally speaking, one would expect sunspots at the beginning of a new cycle to appear at high latitudes. As the 11-year solar cycle progresses, sunspot activity will begin to drift equator-wards, to lower latitudes. “Old” Cycle 23 sunspots have generally appeared near the solar equator, so the sunspots observed today can be attributed to the “new” Cycle 24.

The clincher for identifying these spots as belonging to a new solar cycle is their magnetic polarity. Sunspots often appear in pairs of opposite polarity (i.e. one will be magnetic north, the other will be magnetic south), and this new cluster is consistent with the polarity expected for Cycle 24 sunspots. SOHO uses its Michelson Doppler Imager (MDI) Magnetogram instrument to observe magnetic polarity, and it would appear that the polarity of this sunspot cluster has an opposite magnetic north/south to previous Cycle 23 observations.

So does this mean we might see an increase in solar activity from here on in? Although this is an encouraging observation, the Sun could revert back to its “blank” state as quickly as it revealed these sunspots to SOHO. However, there is also a chance this could herald the beginning of accelerated solar activity, possibly still fulfilling NASA’s 2006 prediction that Solar Cycle 24 will be a “doozy.”

Watch this space…

Original source: Space Weather

Posted on by Nancy Atkinson

Opportunity’s Next Adventure: The Big Drive

The Big Drive to Endeavour-crater. Credit: NASA/JPL

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Opportunity, the intrepid Mars Exploration Rover, is going to put the pedal to the metal and head out for a crater nearly 12 kilometers (7 miles) away. That would match the distance the rover has traveled since landing in 2004. But the call of the unknown is compelling the rover science team to make the attempt. “We may not get there, but it is scientifically the right direction to go anyway,” said Steve Squyres, principal investigator for the science instruments on Opportunity and its twin rover, Spirit. For an “aging” rover (what age is 4 in rover years?), this might be setting the bar pretty high. But maybe it’s the journey and not the destination.

“This is a bolder, more aggressive objective than we have had before,” said John Callas, the project manager the rovers. “It’s tremendously exciting. It’s new science. It’s the next great challenge for these robotic explorers.”

“This crater is staggeringly large compared to anything we’ve seen before.” The crater, named Endeavour, is 22 kilometers (13.7 miles) across. “I would love to see that view from the rim,” Squyres said. “But even if we never get there, as we move southward we expect to be getting to younger and younger layers of rock on the surface. Also, there are large craters to the south that we think are sources of cobbles that we want to examine out on the plain. Some of the cobbles are samples of layers deeper than Opportunity will ever see, and we expect to find more cobbles as we head toward the south.”

The rover team estimates Opportunity may be able to travel about 110 yards each day it is driven toward the Endeavour crater. Even at that pace, the journey could take two years. But why not go for it, and see how long the rovers can last?

Opportunity's shadow with Victoria Crater in the background. Credit: NASA/JPL/ASU
Opportunity's shadow with Victoria Crater in the background. Credit: NASA/JPL/ASU

Opportunity, like Spirit, is well past its expected lifetime on Mars, and might not keep working long enough to reach the crater. However, two new resources not available during the 4-mile drive toward Victoria Crater in 2005 and 2006 are expected to aid in this new trek.

One is imaging from orbit of details smaller than the rover itself, using the High Resolution Imaging Science Experiment (HiRISE) camera on NASA’s Mars Reconnaissance Orbiter, which arrived at the Red Planet in 2006.

“HiRISE allows us to identify drive paths and potential hazards on the scale of the rover along the route,” Callas said. “This is a great example of how different parts of NASA’s Mars Exploration Program reinforce each other.”

Also, Opportunity now has a better “brain” for driving across the the plains of Mars. A new version of flight software uplinked to Opportunity and Spirit in 2006, boosts their ability to autonomously choose routes and avoid hazards such as sand dunes.

During its first year on Mars, Opportunity found geological evidence that the area where it landed had surface and underground water in the distant past. The rover’s explorations since have added information about how that environment changed over time. Finding rock layers above or below the layers already examined adds windows into later or earlier periods of time.

Source: JPL

Posted on by Nancy Atkinson

Anything Under That Rock on Mars? Phoenix to Take a Peek

The rock "Headless." NASA/JPL-Caltech/University of Arizona/ Texas A&M University

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Ever wondered what might crawl out from under a rock on Mars? The Phoenix lander is going to attempt to find out today by trying to nudge a rock aside today with its robotic arm to see what might be underneath. Engineers have developed a plan to try moving a rock on the north side of the lander. This rock, roughly the size and shape of a VHS videotape, is called “Headless.” Even though the Phoenix mission has been extended for a second time – the mission is now on through December, the team feels like it’s time to pull out all the stops and do as much work as possible. “We’re getting towards fall in the northern plains of Mars and our sun is dropping lower day by day,” said mission principal investigator Peter Smith on NPR’s Science Friday. “Our days are getting precious.” So, even though Phoenix’s robotic arm was not designed to move rocks, the team wants to give it a shot. “The appeal of studying what’s underneath is so strong we have to give this a try,” said Michael Mellon, a Phoenix science team member at the University of Colorado, Boulder.

“We don’t know whether we can do this until we try,” said Ashitey Trebi Ollennu, a robotics engineer at NASA’s Jet Propulsion Laboratory, Pasadena, Calif. “The idea is to move the rock with minimum disturbance to the surface beneath it. You have to get under it enough to lift it as you push it and it doesn’t just slip off the scoop.”

The lander receives commands for the whole day in the morning, so there’s no way to adjust in mid-move if the rock starts slipping. Phoenix took stereo-pair images of Headless to provide a detailed three-dimensional map of it for planning the arm’s motions. On Saturday, Sept. 20, the arm enlarged a trench close to Headless. Commands sent to Phoenix Sunday evening, Sept. 21, included a sequence of arm motions for today, intended to slide the rock into the trench.

If the technique works, the move would expose enough area for digging into the soil that had been beneath Headless.

Morning frost on Mars. NASA/JPL-Caltech/University of Arizona/ Texas A&M University
Morning frost on Mars. NASA/JPL-Caltech/University of Arizona/ Texas A&M University

The scientific motive is related to a hard, icy layer found beneath the surface in trenches that the robotic arm has dug near the lander. Excavating down to that hard layer underneath a rock might provide clues about processes affecting the ice.

“The rocks are darker than the material around them, and they hold heat,” Mellon said. “In theory, the ice table should deflect downward under each rock. If we checked and saw this deflection, that would be evidence the ice is probably in equilibrium with the water vapor in the atmosphere.”

An alternative possibility, if the icy layer were found closer to the surface under a rock, could by the rock collecting moisture from the atmosphere, with the moisture becoming part of the icy layer.

Source: JPL