Orion Test Capsule at Practice for Pad Abort 1 Test. The Orion test capsule is now on a cross country tour from New Mexico to Florida with stops in Oklahoma, Texas and Alabama. Ground teams in White Sands, New Mexico, practice stacking test versions of Orion and its launch abort system. This was being done in advance of Orion’s launch abort system test. Credit: NASA or National Aeronautics and Space Administration
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Here’s your chance for a birds-eye view of an Orion capsule, up-close and personal ! Catch it if you can !
A full scale test version of one of NASA’s Orion spacecraft has embarked on a cross country tour from White Sands, New Mexico, across several states in the southern United States that ultimately lands at the Kennedy Space Center in Florida.
Starting today, Jan. 27, an Orion spacecraft is open for viewing by the public in Texas at Victory Park and the American Airlines Center in Dallas.
Orion fans in Texas
The Coopers from Southlake meet NASA astronaut Nick Patrick by the Orion crew module now on display at the American Airlines Center in Dallas, TX.
The display continues throughout this weekend after a well received visit to Oklahoma at the Science Museum Oklahoma in Oklahoma City.
Roller Derby team visits Orion test capsule now on public display in Texas
The next stop on the cross country journey is the U.S. Space and Rocket Center in Huntsville, Ala on Feb 1-2.
Orion is NASA’s next generation human spaceflight vehicle that will eventually replace the space shuttle and loft astronauts to low Earth orbit and beyond to deep space destinations such as the Moon, Asteroids and Mars. It can also dock at the International Space Station (ISS).
The Orion crew module journey is a wonderful and fun opportunity for individuals and families to see real space exploration hardware with your own eyes and learn all about the goals and plans of the US Space Program and your investment in it as a taxpayer.
Knowledgeable Orion experts will be on hand to speak with visitors in easy to understand ways. This includes astronauts, engineers, program officials and press spokespeople from NASA, Lockheed-Martin (Orion prime contractor) and other companies involved in building the Orion capsule and other components that will rocket the vehicle to orbit.
Veteran NASA Astronauts Nick Patrick and Clay Anderson will be on hand at the Dallas stop. NASA Astronauts Doug Hurley and Jim Dutton will attend the Alabama display.
Hurley was the pilot for the final shuttle mission by Space Shuttle Atlantis for the STS-135 mission to the International Space Station.
Orion fans in Oklahoma. Credit: NASA
The Orion tour also includes colorful and informative display panels and fun kids activities that I’ve personally witnessed on several occasions. In past years the Orion Launch Abort System (LAS) engaged in similar trips.
This Orion test vehicle was used by ground crews preparing for the PA-1 launch abort system flight test that took place in New Mexico in 2010.
The first orbital flight test of an unmanned Orion is scheduled for 2014 atop a Delta 4 Heavy booster..
Orion fans in Dallas, Texas - Mike, Darnell and AkeemOrion Test capsule with test facility workers at White Sands Facility, New Mexico. Credit: NASA
Look here for more information on the Orion stops in Texas and Alabama
American Airlines Center: http://www.americanairlinescenter.com/
U.S. Space and Rocket Center: http://www.ussrc.com/
NASA’s future has suddenly become a hot topic in the GOP Presidential Debates. Orion is at the center of that debate on whether Americans will ever return to the Moon.
This is your opportunity to see history in the making
Viewing the South Pole of Vesta and Rhea Silvia Impact Basin. This image obtained by Dawn’s framing camera shows the south pole of the giant asteroid Vesta and the circular Rheasilvia impact basin which scientists believe originated by a collision with another asteroid early in the asteroid's history. The image was recorded from a distance of about 1,700 miles (2,700 kilometers). The image resolution is about 260 meters per pixel. Credit: NASA/JPL-Caltech/UCLA/MPS/DLR/IDA
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The mysterious asteroid Vesta may well have more surprises in store. Despite past observations that Vesta would be nearly bone dry, newly published research indicates that about half of the giant asteroid is sufficiently cold and dark enough that water ice could theoretically exist below the battered surface.
Scientists working at NASA’s Goddard Space Flight Center in Greenbelt, Md., and the University of Maryland have derived the first models of Vesta’s average global temperatures and illumination by the Sun based on data obtained from the Hubble Space Telescope.
“Near the north and south poles, the conditions appear to be favorable for water ice to exist beneath the surface,” says Timothy Stubbs of NASA’s Goddard Space Flight Center in Greenbelt, Md., and the University of Maryland, Baltimore County. The research by Timothy Stubbs and Yongli Wang, of the Goddard Planetary Heliophysics Institute at the University of Maryland, was published in the January 2012 issue of the journal Icarus.
If any water lurks beneath Vesta, it would most likely exist at least 10 feet (3 meters) below the North and South poles because the models predict that the poles are the coldest regions on the giant asteroid and the equatorial regions are too warm. Global Map of Average Surface Temperature of Vesta
This global map of average surface temperature shows the warmer equatorial zone of the giant asteroid Vesta is likely too warm to sustain water ice below the surface. But roughly half of Vesta is so cold and receives so little sunlight on average that water ice could have survived there for billions of years. The dividing lines (solid gray) are found at about 27 degrees north latitude and 27 degrees south latitude. This map, with temperatures given in kelvins, comes from the first published models of the average global temperature and illumination conditions on Vesta. Credit: NASA/GSFC/UMBC
If proven, the existence of water ice at Vesta would have vast implications for the formation and evolution of the tiny body and upend current theories.
The surface of Vesta is not cold enough for ice to survive all the time because unlike the Moon, it probably does not have any significant permanently shadowed craters where water ice could stay frozen on the surface indefinitely.
Even the huge 300 mile diameter (480-kilometer) crater at the South Pole is not a good candidate for water ice because Vesta is tilted 27 degrees on its axis, a bit more than Earth’s tilt of 23 degrees.
By contrast, the Moon is only tilted 1.5 degrees and possesses many permanently shadowed craters. NASA’s LCROSS impact mission proved that water ice exists inside permanently shadowed lunar craters.
New modeling shows that, under present conditions, Vesta's polar regions are cold enough (less than about 145 kelvins) to sustain water ice for billions of years, as this map of average surface temperature around the asteroid's south pole indicates.
The models predict that the average annual temperature around Vesta’s poles is below minus 200 degrees Fahrenheit (145 kelvins). Water ice is not stable above that temperature in the top 10 feet of Vestan soil, or regolith.
At the equator and in a band stretching to about 27 degrees north and south in latitude, the average annual temperature is about minus 190 degrees Fahrenheit (145 kelvins), which is too high for the ice to survive.
“On average, it’s colder at Vesta’s poles than near its equator, so in that sense, they are good places to sustain water ice,” says Stubbs in a NASA statement. “But they also see sunlight for long periods of time during the summer seasons, which isn’t so good for sustaining ice. So if water ice exists in those regions, it may be buried beneath a relatively deep layer of dry regolith.”
Vesta is the second most massive asteroid in the main Asteroid belt between Mars and Jupiter.
NASA’s Dawn Asteroid Orbiter is the very first mission to Vesta and achieved orbit in July 2011 for a 1 year long mission.
Dawn is currently circling Vesta at its lowest planned orbit. The three science instruments are snapping pictures and the spectrometers are collecting data on the elemental and mineralogical composition of Vesta.
The onboard GRaND spectrometer in particular could shed light on the question of whether water ice exists at Vesta.
So far no water has been detected, but the best data is yet to come.
In July 2012, Dawn fires up its ion thrusters and spirals out of orbit to begin the journey to Ceres, the largest asteroid of them all.
Ceres is believed to harbor huge caches of water, either as ice or in the form of oceans and is a potential habitat for life.
Artist's Concept of New Planetary Systems - Credit: NASA
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Eleven ball in the side pocket. Whack! And another 26 planets are discovered! NASA just announced the latest tally and the new discoveries come close to doubling the amount of verified planets and tripling the number of stars which are confirmed to have more than one transiting planet. It’s just another score for understanding how planets came to be… planets which run the gambit from about one and half times the size of Earth up to the size of Jupiter. Of these, fifteen are judged to be between the size of Earth and Neptune – while more observations will reveal their structure. The new bodies orbit the parent star between 6 and 143 days and all are closer than our Sun/Venus distance.
“Prior to the Kepler mission, we knew of perhaps 500 exoplanets across the whole sky,” said Doug Hudgins, Kepler program scientist at NASA Headquarters in Washington. “Now, in just two years staring at a patch of sky not much bigger than your fist, Kepler has discovered more than 60 planets and more than 2,300 planet candidates. This tells us that our galaxy is positively loaded with planets of all sizes and orbits.”
Kepler is a busy-body. It monitors the brightness changes in more than 150,000 stars. Through repeated measurements, it is able to pick out minute magnitude fluctuations which occur as a planet passes between us, Kepler and the parent sun. The newly documented solar systems are host to between two and five closely situated transiting bodies. In such cramped systems, the gravitational interaction between the orbiting members means some are accelerated – and others decelerated – in their tracks. Faster orbital speeds account for changes in orbital periods… Changes that the Kepler mission documents as Transit Timing Variations (TTVs). For planetary systems possessing TTVs, no extreme study with ground-based telescopes is required to verify their existence and the technique allows Kepler to validate the presence of planetary systems around further and fainter stars.
What’s been found? Five of the systems documented as Kepler-25, Kepler-27, Kepler-30, Kepler-31 and Kepler-33, are home to a set of planets whose orbits double each other. The outer body orbits twice for every inner body orbit. Four of the systems, Kepler-23, Kepler-24, Kepler-28 and Kepler-32, are home to a pairing where the outer planet circles the star twice for every three times the inner planet orbits.
“These configurations help to amplify the gravitational interactions between the planets, similar to how my sons kick their legs on a swing at the right time to go higher,” said Jason Steffen, the Brinson postdoctoral fellow at Fermilab Center for Particle Astrophysics in Batavia, Ill., and lead author of a paper confirming four of the systems.
And now for the game ball… Kepler-33 had the most planets of all. With a parent star older and more massive than Sol, the system gives rise to five planets whose sizes run between one and a half to five times the size of Earth. But, this is one crowded grouping. All of the planets orbiting this star are closer than Mercury is to our Sun! Thanks to stellar properties, Kepler is able to distinguish planets like these. The drop in the sun’s brightness and the length of time it takes for the planet to transit all play a role in determining presence. With similar signatures verified around the same star, chances of false readings are unlikely.
“The approach used to verify the Kepler-33 planets shows the overall reliability is quite high,” said Jack Lissauer, planetary scientist at NASA Ames Research Center at Moffett Field, Calif., and lead author of the paper on Kepler-33. “This is a validation by multiplicity.”
A 5-km-wide crater on Vesta displays light and dark material.
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Light and dark material spreads outward from a 5-km-wide crater on Vesta in this image from NASA’s Dawn spacecraft, acquired on October 22, 2011. While craters with differently-toned materials have been previously seen on the asteroid, it is unusual to find one with such a large amount of ejecta of different albedos.
This is a crop of a larger version which was released today on the Dawn website.
This brightness image was taken through the clear filter of Dawn’s framing camera. The distance to the surface of Vesta is 700 kilometers (435 miles) and the image has a resolution of about 70 meters (230 feet) per pixel.
Vesta resides in the main asteroid belt between the orbits of Mars and Jupiter and is thought to be the source of many of the meteorites that fall to Earth. The Dawn spacecraft successfully entered orbit around Vesta on July 16, 2011.
After its investigation of Vesta, Dawn will leave orbit and move on to Ceres. It will become the first spacecraft to orbit two different worlds.
Image Credit: NASA/ JPL-Caltech/ UCLA/ MPS/ DLR/ IDA
Martian Vista from Opportunity at Endeavour Crater - 8 Years on Mars. NASA’s Opportunity rover celebrated 8 Years on Mars on January 24, 2012. This mosaic shows portions of the segmented rim of Endeavour crater (14 miles, 22 km wide) after the robot arriving at the craters foothills in August 2011. Large ejecta blocks from a smaller nearby crater are visible in the middle. At Endeavour, Opportunity will investigate the oldest minerals deposits she has ever visited from billions of years ago and which may hold clues to environments that were potentially habitable for microbial life. The rover will eventually drive to Cape Tribulation at right after surviving her 5th winter on Mars. Mosaic Credit: NASA/JPL/Cornell/Marco Di Lorenzo/Kenneth Kremer
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Today, the resilient Opportunity robot begins her 9th year roving around beautifully Earth-like Martian terrain where potentially life sustaining liquid water once flowed billions of years ago.
Opportunity celebrates her 8th anniversary on the Red Planet gazing at the foothills of the vast crater named Endeavour, promising a “mother lode” of “watery” science – an unimaginable circumstance since the nail biting landing on the hematite rich plains of Meridiani Planum on 24 January 2004.
“Opportunity is 97 months into the 3 month mission,” team members are proud and universally surprised to say.
“Milestones like 8 years on Mars always make me look forward rather than looking back,” Rover Principal Investigator Prof. Steve Squyres of Cornell University told Universe Today for this article commemorating Opportunity’s landing.
“We’ve still got a lot of exploring to do, but we’re doing it with a vehicle that was designed for a 90-sol mission. That means that every sol is a gift at this point.”
Opportunity has driven more than 21 miles (34 kilometers) across the Red Planet’s surface during what is truly humankind’s first overland expedition on another Planet. See our route map below.
Opportunity Rover Traverse Map at Meridiani Planum on Mars - 2004 to 2012
Traverse map shows the 8 Year Journey of Opportunity from Eagle Crater landing site on Sol 1- Jan. 24, 2004 - to 5th Winter Haven worksite at Greeley Haven at Endeavour Crater rim in January 2012. Opportunity embarked on a crater tour and discovered bountiful evidence for the flow of liquid water on Mars billions of years ago. The robot has shown that ancient ephemeral shallow lakes existed on Mars when the cratered terrain was cut by fluvial channels. Endeavour Crater is 14 miles (22 kilometers) in diameter. Opportunity has so far driven more than 21 miles (34 km) over 8 Years but was only expected to live for 90 Martian days. Credit: NASA/JPL/Cornell/UA/Marco Di Lorenzo/Kenneth Kremer
NASA’s twin rovers Spirit and Opportunity blasted off for Mars atop a pair of Delta II rockets in the summer of 2003 with a mission “warranty” of just 90 Martian days, or Sols.
Today is Sol 2846 of working operations for Opportunity, compared to an anticipated lifetime of only 90 Sols – that amounts to more than 31 times beyond the designer’s expectations.
Indeed, the long lived robot is now enduring her 5th Winter on Mars. And to glimpse the next Martian sunrise, the robo girls manmade components must survive the harsh extremes of frigid Antarctic-like temperatures each and every sol.
“I never thought that we would still be planning sequences for Opportunity today,” Ray Arvidson told Universe Today. Arvidson, of Washington University in St. Louis, is the deputy rover principal investigator.
“I seriously thought both Spirit and Opportunity would be finished by the summer of 2004.”
Opportunity's Eighth Anniversary View From 'Greeley Haven' (False Color). This mosaic of images taken in mid-January 2012 shows the windswept vista northward (left) to northeastward (right) from the location where Opportunity is spending its fifth Martian winter, an outcrop informally named "Greeley Haven. Credit: NASA/JPL-Caltech/Cornell/Arizona State Univ.
But, Opportunity is the gift to science that keeps on giving.
“I am feeling pretty good as the MER rover anniversaries approach,” Arvidson told me.
“Opportunity has shown that ancient ephemeral shallow lakes existed as Mars moved climatically from an early period when the cratered terrain was cut by fluvial channels to the current dry and cold conditions that dominate.”
“Both rovers have conclusively shown the need for lateral mobility to get to relevant outcrops and back out the secrets associated with past conditions,” Arvidson explained.
Barely a month ago the bountiful harvest from mobility was once again demonstrated when the science team lead by Squyres and Arvidson announced that Opportunity had discovered the most scientifically compelling evidence yet for the flow of liquid water on ancient Mars.
Squyres and Arvidson announced that Opportunity had found a bright vein – named “Homestake” – composed of the mineral gypsum located at the Cape York segment of Endeavour Crater where the intrepid robot is currently spending her 5th Martian Winter.
“This gypsum vein is the single most powerful piece of evidence for liquid water at Mars that has been discovered by the Opportunity rover,” Squyres explained.
Veins are a geologic indication of the past flow of liquid water.
See our mosaic below illustrating the exact location of the “Homestake” vein at Endeavour Crater – also published at Astronomy Picture of the Day; 12 Dec 2011.
Opportunity discovers Water related Mineral Vein at Endeavour Crater - November 2011
Opportunity rover discovered Gypsum at the Homestake mineral vein, while exploring around the base of Cape York ridge at the rim of Endeavour Crater. The vein is composed of calcium sulfate and indicates the ancient flow of liquid water at this spot on Mars. This panoramic mosaic of images was taken on Sol 2761, November 2011, and illustrates the exact spot of the mineral vein discovery.
Credit: NASA/JPL/Cornell/Kenneth Kremer/Marco Di Lorenzo
Published on Astronomy Picture of the Day (APOD): 12 Dec 2011
Opportunity just arrived at the rim of the 14 mile (22 kilometer) wide Endeavour Crater in mid-August 2011 following an epic three year trek across treacherous dune fields from her prior investigative target at the ½ mile wide Victoria Crater.
“It’s like a whole new mission since we arrived at Cape York,” says Squyres.
For the next few months of the bitterly cold Martian winter, Opportunity will conduct a vigorous science campaign while remaining mostly stationary at a spot dubbed “Greeley Haven” in honor of Prof. Ronald Greeley, a team member from Arizona State University who recently passed away.
Opportunity Mars Rover at 5th Winter Worksite at Endeavour Crater
This mosaic shows the view of NASA’s Opportunity rover parked at “Greeley Haven” worksite where the robot will spend her 5th Martian Winter. This mosaic of images shows the Winter Haven view from the Cape York Ridge at the western rim of Endeavour Crater looking south along the crater rim. Tire tracks at right. Credit: NASA/JPL/Cornell/ Marco Di Lorenzo/Kenneth Kremer
At this moment Opportunity is snapping a 360 degree panorama, deploying her robotic arm onto nearby outcrops, collecting microscopic images, making measurements of mineral compositions with the Alpha Particle X-Ray Spectrometer and conducting radio science observations to elucidate the unknown structure of the Martian interior and core.
The rover is covered with a significant coating of dust which limits her ability to generate power from the life sustaining solar arrays. Since Opportunity is traversing just south of the equator, engineers have temporarily parked her on a northerly facing slope to maximize the electric power generation.
“Opportunity is currently sitting on an outcrop of impact breccias at Greeley Haven on Cape York,” said Arvidson.
Opportunity will remain at Greeley Haven until some time after the Winter Solstice of southern Martian winter occurs at the end of March. 'Greeley Haven' Site for Opportunity's Fifth Martian Winter. This mosaic of Greeley Haven was acquired by Opportunity on Sol 2793, Dec. 2, 2011. Credit: NASA/JPL-Caltech/Cornell/Arizona State Univ.
Then she’ll head south to further explore the veins and eventually drive to deposits of the clay mineral located a few miles (km) away along the craters rim.
“We’ll do good science while we’re at Greeley Haven. But as soon as we catch a wind gust or the seasons change, we’ll be on our way again,” Squyres told me.
The legendary twins Spirit and Opportunity surely rank as one of the greatest triumphs in space exploration.
Artist's conception image of a young star surrounded by a disk (made up of rings) (Credits: NASA/JPL-Caltech)
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Catching a ring – or accretion disk – around a star isn’t unusual. However, catching a sharply defined carbon-dioxide ring around a young, magnetic star that’s precisely 1 AU away with a width 0.32 AU or less might raise a few eyebrows. This isn’t just any disk, either… It’s been likened as a “rope-like structure” and there’s even more to the mystery. It’s encircling a Herbig Ae star.
Discovered with the European Southern Observatory’s Very Large Telescope, the edges of this accretion disk are uniquely crisp. Located in the constellation of Centaurus at about 700 light years distant, V1052 (HD 101412) is a parent star with an infrared excess. “HD 101412 is most unusual in having resolved, magnetically split spectral lines which reveal a surface field modulus that varies between 2.5 to 3.5 kG.” says C.R. Cowley (et al). Previous studies “have surveyed molecular emission in a variety of young stellar objects. They found the emission to be much more subdued in Herbig Ae/Be stars than their cooler congeners, the T Tauri stars. This was true for HD 101412 as well, which was among the 25 Herbig Ae/Be stars they discussed. One exception, however, was the molecule CO2, which had a very large flux in HD 101412; indeed, only one T Tauri star had a higher CO2 flux.”
It’s not unusual for carbon dioxide to be found near young stars, but it is a bit more normal for it to be distributed throughout the disk region. “It’s exciting because this is the most constrained ring we’ve ever seen, and it requires an explanation,” explains Cowley, who is professor emeritus at the University of Michigan and leader of the international research effort. “At present time, we just don’t understand what makes it a rope rather than a dish.”
Because V1052 itself is different could be the reason. It is hypothesized the magnetic fields may be holding the rings in the disk structure at a certain distance. The idea has also been forwarded that there may be “shepherding planets”, much like Saturn’s ring structure, which may be the cause. “What makes this star so special is its very strong magnetic field and the fact that it rotates extremely slow compared to other stars of the same type,” said Swetlana Hubrig, of the Leibniz Institute for Astrophysics Potsdam (AIP), Germany.
One thing that is certain is how clean and well-defined the disk lines are centered around the Earth/Sun distance. This accords well with computer modeling where “A wider disk will not fit the observations.” These observations – and the exotic parent star – have been under intense scrutiny since 2008 and the findings have been recently published on-line in Astronomy and Astrophysics. It’s work that helps deepen the understanding of the interaction between central stars, their magnetic fields, and planet-forming disks. It also allows for fact finding when it comes to diverse systems and better knowledge of how solar systems form… even unusual ones.
“Why do turbulent motions not tear the ring apart?” Cowley wondered. “How permanent is the structure? What forces might act to preserve it for times comparable to the stellar formation time itself?”
When it comes to Herbig Ae stars, they are not only rare, but present a rare opportunity for study. In this case, it gives the team something to be quite excited about.
Opportunity Mars Rover at Winter Haven Worksite at Endeavour Crater. NASA’s Opportunity rover has parked near this spot at the “Greeley Haven” worksite where the robot will spend her 5th Martian Winter Haven since landing 8 years ago in January 2004. This mosaic of images was snapped in December 2011 and shows the view from the Cape York Ridge at the western rim of Endeavour Crater looking south along the crater rim to a future area that Opportunity will drive to and explore next spring. Credit: NASA/JPL/Cornell/ Marco Di Lorenzo/Kenneth Kremer
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NASA’s seemingly indestructible Opportunity rover has arrived at the breathtaking location where she’ll be working through her unfathomable 5th Martian Winter. The Opportunity Mars Exploration Rover has not only endured, but flourished for 8 years of unending “Exploration & Discovery” on the Red Planet despite having an expected lifetime at landing of just 3 months, way back in January 2004.
Opportunity is parked at a northward facing outcrop dubbed “Greeley Haven” where she can soak up the sun and juice her innards throughout the utterly harsh and Antarctic-like temperatures on tap for the next few months that threaten to kill her each and every Martian day. See our mosaic above around the Greeley Haven area.
Science team members told Universe Today that the rover is sitting at Greeley Haven because the site offers a roughly 15 degree tilt that will maximize the electric output from the life-giving solar arrays and also allow the robot to carry out a vigorous science campaign during the seasonal Martian winter season that officially begins in March.
Greeley Haven is a located at the northern tip of the “Cape York” segment of the western rim of the vast crater named Endeavour, some 14 miles (22 km) wide that’s loaded with a bountiful variety of rocks and soil that neither Opportunity nor her twin Spirit have ever touched and drilled into before and stem from an earlier epoch when liquid water flowed eons ago and perhaps may have been more favorable to sustaining life.
“Opportunity is currently sitting on Saddleback at Greeley Haven, an outcrop of impact breccias on Cape York, Endeavour crater’s rim,” Ray Arvidson told Universe Today. Arvisdon is the mission’s deputy principal investigator, of Washington University in St. Louis.
“Her northerly tilt is about ~15 degrees which is enough to have a vibrant winter campaign. The Martian southern winter solstice occurs at the end of March. A few months after that date we will drive her off the outcrop and further explore Cape York.”
Approaching 'Greeley Haven' on Endeavour Rim
Opportunity captured this view of a northward-facing outcrop, "Greeley Haven," where the rover will work during its fifth Martian winter. This southward-looking image was taken on Sol 2790 on Mars (Nov. 29, 2011). The rover team chose this designation as a tribute to the influential planetary geologist Ronald Greeley (1939-2011), who was a member of the science team for the Mars rovers and many other interplanetary missions. Credit: NASA/JPL-Caltech
“Greeley Haven” is named in tribute to planetary Geologist Ronald Greeley (1939-2011) who was a beloved member of the rover science team and a host of other NASA planetary missions. He taught at Arizona State University and inspired several generations of students and planetary scientists until his recent death on Oct. 27, 2011.
“We’ll hunker down at Greeley Haven as long as we need to, and we’ll do good science while we’re there,” Steve Squyres of Cornell University, Ithaca, N.Y., told Universe Today. Squyres is the Principal Investigator for Opportunity.
Opportunity is collecting a high resolution 360 degree panorama to commemorate Greeley.
Throughout the past 4 Martian winters, Opportunity had continued to traverse without pause. But this winter time it’s different because the solar panels are significantly more coated with an obscuring layer of dust hindering their energy output.
So the rover is parked with a tilt for her 5th Martian winter, mimicking the successful strategy power boosting used by Spirit to survive 3 harsh Martian winters.
And there is a silver lining to sitting mostly still that enables a chance to determine what’s at the core of the Red Planet, a key fact we don’t know.
“This winter science campaign will feature two way radio tracking with Earth to determine the Martian spin axis dynamics – thus the interior structure, a long-neglected aspect of Mars,” Arvidson told me.
I asked Squyres for a progress update and how long would the data collection require ?
Squyres replied that the experiment has already begun and added – “Hard to say how long. It’s months, as opposed to weeks or years, but it depends very much on data quality and the amount of data we get per week. We’re very early in the experiment now… we’ll just see how it goes.”
Locator Map for 'Greeley Haven' on Endeavour Crater Rim
Opportunity will spend its fifth Martian winter working at Greeley Haven on the western rim of Endeavour Crater. Credit: NASA/JPL-Caltech/UA
Three Generations of Mars Rovers in the Mars Yard. This grouping shows 3 generations of NASA’s Mars rovers from 1997 to 2012 set inside the Mars Yard at the Jet Propulsion Lab in Pasadena, Calif. The Mars Pathfinder Project (front) landed the first Mars rover - Sojourner - in 1997. The Mars Exploration Rover Project (left) landed Spirit and Opportunity on Mars in 2004. The Mars Science Laboratory Project (right) is on course to land Curiosity on Mars in August 2012. Credit: NASA/JPL-Caltech
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NASA Mars rovers have come a long way in terms of size and capability since the rebirth of Red Planet surface exploration just 15 years ago – spanning from 1997 to 2012.
To get a really excellent sense of just how far America’s scientists and engineers have pushed the state of the art in such a short time – when the willpower and funding existed and coincided to explore another world – take a good look at the new pictures here showing 3 generations of NASA’s Mars rovers; namely Mars Pathfinder (MPF), the 1st generation Mars rover, Mars Exploration Rover (MER), the 2nd generation, and Mars Science Laboratory (MSL), the 3rd and newest generation Mars rover.
The newly released pictures graphically display a side by side comparison of the flight spare for Mars Pathfinder (1997 landing) and full scale test rovers of the Mars Exploration Rover (2004 landing) and Mars Science Laboratory (in transit for a 2012 planned landing). The setting is inside the “Mars Yard” at NASA’s Jet Propulsion Laboratory, Pasadena, Calif. where the teams conduct mission simulations.
It’s been nothing less than a quantum leap in advancement of the scientific and technological capability from one generation to the next.
Sojourner - NASA’s 1st Mars Rover
Sojourner takes an Alpha Proton X-ray Spectrometer (APXS) measurement of Yogi rock after Red Planet landing on July 4, 1997 landing. Sojourner was only 2 feet long, the size of a microwave oven.
Credit: NASA
Just consider the big increase in size – growing from a microwave oven to a car !
The “Marie Curie” flight spare and the actual “Sojourner” rover on Mars are 2 feet (65 centimeters) long – about the size of a microwave oven. The MER rovers “Spirit and Opportunity” and the “Surface System Test Bed” rover are 5.2 feet (1.6 meters) long – about the size of a golf cart. The MSL “Curiosity” and the “Vehicle System Test Bed” rover are 10 feet (3 meters) long – about the size of a car.
Side view of Three Generations of Mars Rovers
Front; flight spare for the first Mars rover, Sojourner. Left; Mars Exploration Rover Project test rover. Right; Mars Science Laboratory test rover Credit: NASA/JPL-Caltech
With your own eyes you can see the rapid and huge generational change in Mars rovers if you have the opportunity to visit the Kennedy Space Center Visitor Complex and stroll by the Mars exhibit with full scale models of all three of NASA’s Red Planet rovers.
At the KSC Visitor Complex in Florida you can get within touching distance of the Martian Family of Rovers and the generational differences in size and complexity becomes personally obvious and impressive.
NASA’s Family of Mars rovers at the Kennedy Space Center
Full scale models on display at the Kennedy Space Center Visitor Complex. Curiosity and Spirit/Opportunity are pictured here. Sojourner out of view. Credit: Ken Kremer
All of the Mars rovers blasted off from launch pads on Cape Canaveral Air Force Station, Florida.
Sojourner, Spirit and Opportunity launched atop Delta II rockets at Space Launch Complex 17 in 1996 and 2003. Curiosity launched atop an Atlas V at Space Launch Complex 41 in 2011.
Three Generations of Mars Rovers with Standing Mars Engineers
The rovers are pictured here with real Mars Engineers to get a sense of size and perspective. Front rover is the flight spare for the first Mars rover, Sojourner. At left is a Mars Exploration Rover Project test rover, working sibling to Spirit and Opportunity. At right is a Mars Science Laboratory test rover the size of Curiosity which is targeting a August 2012 Mars landing. The Mars engineers are JPL's Matt Robinson, left, and Wesley Kuykendall. Credit: NASA/JPL-Caltech
Opportunity is still exploring Mars to this day – 8 years after landing on the Red Planet, with a warranty of merely 90 Martian days.
Curiosity is scheduled to touch down inside Gale crater on 6 August 2012.
So, what comes next ? Will there be a 4th Generation Mars rover ?
Ebb and Flow - New Names for the GRAIL Twins in Lunar Orbit. 4th Grade Students from Montana win NASA’s contest to rename the GRAIL A and GRAIL B spacecraft. Artist concept of twin GRAIL spacecraft flying in tandem orbits around the Moon to measure its gravity field in unprecedented detail and unravel the hidden mysteries of the lunar interior’s composition. Credit: NASA/JPL Montage:Ken Kremer
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A classroom of America’s Youth from an elementary school in Bozeman, Montana submitted the stellar winning entry in NASA’s nationwide student essay contest to rename the twin GRAIL lunar probes that just achieved orbit around our Moon on New Year’s Eve and New Year’s Day 2012
“Ebb” & “Flow” – are the dynamic duo’s official new names and were selected because they clearly illuminate the science goals of the gravity mapping spacecraft and how the Moon’s influence mightily affects Earth every day in a manner that’s easy for everyone to understand.
“The 28 students of Nina DiMauro’s class at the Emily Dickinson Elementary School have really hit the nail on the head,” said GRAIL principal investigator Prof. Maria Zuber of the Massachusetts Institute of Technology in Cambridge, Mass.
“We asked the youth of America to assist us in getting better names.”
“We chose Ebb and Flow because it’s the daily example of how the Moon’s gravity is working on the Earth,” said Zuber during a media briefing held today (Jan. 17) at NASA Headquarters in Washington, D.C. The terms ebb and flow refer to the movement of the tides on Earth due to the gravitational pull from the Moon.
“We were really impressed that the students drew their inspiration by researching GRAIL and its goal of measuring gravity. Ebb and Flow truly capture the spirit and excitement of our mission.”
Leland Melvin, NASA Associate Administrator for Education, left, Maria Zuber, GRAIL Prinicipal Investigator at the Massachusetts Institute of Technology, and James Green, Director of the Planetary Science Division in the Science Mission Directorate at NASA Headquarters, right, applaud students from Emily Dickinson Elementary School in Bozeman, Mont. during a news conference, Tuesday, Jan. 17, 2012, at NASA Headquarters in Washington. Nine hundred classrooms and more than 11,000 students from 45 states, as well as Puerto Rico and the District of Columbia, participated in a contest that began in October 2011 to name the twin lunar probes. Credit: NASA/Paul E. Alers
Ebb and Flow are flying in tandem around Earth’s only natural satellite, the first time such a feat has ever been attempted.
As they fly over mountains, craters and basins on the Moon, the spaceships will move back and forth in orbit in an “ebb and flow” like response to the changing lunar gravity field and transmit radio signals to precisely measure the variations to within 1 micron, the width of a red blood cell.
The breakthrough science expected from the mirror image twins will provide unprecedented insight into what lurks mysteriously hidden beneath the surface of our nearest neighbor and deep into the interior.
The winning names from the 4th Graders of Emily Dickinson Elementary School were chosen from essays submitted by nearly 900 classrooms across America with over 11,000 students from 45 states, Puerto Rico and the District of Columbia, Zuber explained.
The students themselves announced “Ebb” and “Flow” in a dramaric live broadcast televised on NASA TV via Skype.
“We are so thrilled that our names were chosen and excited to share this with you. We can’t believe we won! We are so honored. Thank you!” said Ms. DiMauro as the very enthusiastic students spelled out the names by holding up the individual letters one-by-one on big placards from their classroom desks in Montana.
Watch the 4th Grade Kids spell the names in this video!
Until now the pair of probes went by the rather uninspiring monikers of GRAIL “A” and “B”. GRAIL stands for Gravity Recovery And Interior Laboratory.
The twin crafts’ new names were selected jointly by Prof. Zuber and Dr. Sally Ride, America’s first woman astronaut, and announced during today’s NASA briefing.
NASA’s naming competition was open to K-12 students who submitted pairs of names and a short essay to justified their suggestions.
“Ebb” and “Flow” (GRAIL A and GRAIL B) are the size of washing machines and were launched side by side atop a Delta II booster rocket on September 10, 2011 from Cape Canaveral, Florida.
They followed a circuitous 3.5 month low energy path to the Moon to minimize the fuel requirements and overall costs.
So far the probes have completed three burns of their main engines aimed at lowering and circularizing their initial highly elliptical orbits. The orbital period has also been reduced from 11.5 hours to just under 4 hours as of today.
“The science phase begins in early March,” said Zuber. At that time the twins will be flying in tandem at 55 kilometers (34 miles) altitude.
The GRAIL twins are also equipped with a very special camera dubbed MoonKAM (Moon Knowledge Acquired by Middle school students) whose purpose is to inspire kids to study science.
“GRAIL is NASA’s first planetary spacecraft mission carrying instruments entirely dedicated to education and public outreach,” explained Sally Ride. “Over 2100 classrooms have signed up so far to participate.”
Thousands of middle school students in grades five through eight will select target areas on the lunar surface and send requests for study to the GRAIL MoonKAM Mission Operations Center in San Diego which is managed by Dr. Ride in collaboration with undergraduate students at the University of California in San Diego.
By having their names selected, the 4th graders from Emily Dickinson Elementary have also won the prize to choose the first target on the Moon to photograph with the MoonKam cameras, said Ride.
Zuber notes that the first MoonKAM images will be snapped shortly after the 82 day science phase begins on March 8.
Ebb & Flow Achieve Lunar Orbit on New Year’s Weekend 2012
NASA’s twin GRAIL-A & GRAIL-B spacecraft are orbiting the Moon in this astrophoto taken on Jan. 2, 2012 shortly after successful Lunar Orbit Insertions on New Year’s Eve and New Year’s Day 2012.
Credit: Ken Kremer
If you like math, music and space (separately or in any combination) you’re gonna love this. Musician Daniel Starr-Tambor has created a song by assigning each planet a note and speeding up the orbital periods of the planets where 2 seconds represents one Earth year, with a note playing for each orbit. But this isn’t just any typical song; it ends up being a musical palindrome, which means it can be played the same both forwards and backwards … that is, if you lived long enough to play to the end of the song. At the accelerated speeds of the Solar System, Starr-Tambor estimates it would continue without repetition for over 532.25 septendecillion years (5.3225 X 10 56). And with more than 62 vigintillion (6.2 X 10 64) individual notes, this composition, called “Mandala,” is the longest musical palindrome in existence.
Back in the 17th century composers like J.S. Bach created musical palindromes (mostly to show off!) and Starr-Tambor pays homage to Bach by choosing the precise position of the Solar System at the moment of Bach’s birth, viewed from the perspective of the Sun as it faces the constellation Libra, “so that each note chronicles his birthday on every planet.”
