Sunday, September 30, 2012


Cassini-Huygens: Exploring Saturn's System



Cassini-Huygens is a symbol of the new kind of space exploration and cooperation among different agencies. The spacecraft has spent years circling Saturn and its moons, beaming back pictures and data to teach scientists on Earth more about how the system was formed.
Artist's concept of NASA's Cassini spacecraft at Saturn.
CREDIT: NASA/JPL
The ambitious mission is also a joint one among several space agencies, which is a contrast from the large NASA probes of the past such as Pioneerand Voyager. In this case, the main participants are NASA, the European Space Agency and Agenzia Spaziale Italiana (the Italian space agency).
While Cassini was supposed to last four years, it's still going strong at more than double its projected mission lifetime. It regularly passes by the moons of Saturn, producing new data and fueling discoveries back on Earth.
Launch and cruise
Cassini didn't head straight to Saturn. Rather, its mission involved complicated orbital mechanics. It went past several planets — including Venus (twice), Earth and Jupiter — to get a speed boost by taking advantage of each planet's gravity.
The nearly 12,600-pound (about 5,700 kilograms) spacecraft was hefted off of Earth on Oct. 15, 1997. It went by Venus in April 1998 and June 1999, Earth in August 1999 and Jupiter in December 2000.
Cassini Saturn Titan
Saturn's largest moon, Titan, passes in front of the planet and its rings in this true color snapshot from NASA's Cassini spacecraft. This view looks toward the northern, sunlit side of the rings from just above the ring plane. It was taken on May 21, 2011, when Cassini was about 1.4 million miles (2.3 million kilometers) from Titan.
CREDIT: NASA/JPL-Caltech/Space Science Institute
There were some on Earth who were concerned that Cassini's pass by Earth would be risky, given that the spacecraft was carrying radioisotope thermoelectric generators (nuclear power) on board. These generators are commonly used for NASA missions.
NASA responded by issuing a supplementary document about the flyby and detailing the agency's methodology for protecting the planet, saying there was less than a one-in-a-million chance of an impact occurring.
Cassini safely flew by, and after taking a pass by Jupiter settled into orbit around Saturn on July 1, 2004. Among its prime objectives were to look for more moons, to figure out what caused Saturn's rings and the colors in the rings, and understanding more about the planet's moons.
Perhaps Cassini's most detailed look came after releasing the Huygens lander towards Titan, Saturn's largest moon. Huygens descended through the mysterious haze surrounding the moon and landed on Jan. 14, 2005.
It beamed information back to Earth for nearly 2.5 hours during its descent, and then continued to relay what it was seeing from the surface for 1 hour, 12 minutes.
In that brief window of time, researchers saw pictures of a rock field and got information back about the moon's wind and gases on the atmosphere and the surface.
Magnificent moons
One of the defining features of Saturn is its number of moons. Excluding the trillions of tons of little rocks that make up its rings, Saturn has 62 discovered moons as of September 2012. NASA lists 53 named moons on one of its websites.
Huygens Loses Communication Line With Cassini Spacecraft
This first panorama of Titan released by ESA shows a full 360-degree view around the Huygens probe. The left-hand side shows a boundary between light and dark areas. The white streaks seen near this boundary could be ground 'fog', as they were not immediately visible from higher altitudes. Huygens drifted over a plateau (centre of image) and was heading towards its landing site in a dark area (right) during descent.
CREDIT: ESA/NASA/University of Arizona.
In fact, Cassini discovered two new moons almost immediately after arriving (Methone and Pallene) and before 2004 had ended, it detected Polydeuces. [Gallery: Latest Saturn Photos from NASA's Cassini Orbiter]
As the probe wandered past Saturn's moons, the findings it brought back to Earth revealed new things about their environments and appearances. Some of the more notable findings include:
Saturn has not gone ignored, either. For example, in 2012, a NASA study postulated that Saturn's jet streams in the atmosphere may be powered by internal heat, instead of energy from the sun. Scientists believe that heat brings up water vapor from the inside of the planet, which condenses as it rises and produces heat. That heat is believed to be behind jet stream formation, as well as that of storms.
Extending the mission
Cassini wrapped up its four-year planned mission in June 2008 and then embarked on the Cassini Equinox mission, which went through to September 2010. During those two years, Cassini flew past Titan 26 times and Enceladus seven times. It also zipped by Dione, Rhea and Helene once.
Now the probe is in the Cassini Solstice Mission, which is intended to last until September 2017. Saturn's solstices will come in May of that year, meaning it will be summer in the northern hemisphere and winter in the southern hemisphere.
Because Cassini arrived at Saturn at the last solstice, NASA says this extension will let scientists study seasonal changes in detail at the ringed planet.
Saturn orbits the sun every 29 Earth years. By the time Cassini reaches the end of its extended mission, the spacecraft will have accompanied the planet for about two decades.
The spacecraft is in good health and is projected to last to at least the end of the solstice mission.
— Elizabeth Howell, SPACE.com Contributor
Related:


Harvest Moon Meets Uranus in the Sky Saturday: How to Watch Online



Saturday, September 29, 2012


ALIEN WORLD: NATIONAL GEOGRAPHIC HD


















AFTERMATH - When The Earth Stops Spinning [Full Screen HD]




Friday, September 28, 2012



Travelling to the Gliese 581 System



Video discussing the possibility of travelling to the Gliese 581 system, where the recently discovered Earthlike exoplanet, Glise581g, is located.

How do we get to the Gliese581 system to visit our sister planet and how long will it take?

As told by Stephen Hawking - Into the Universe: The Story of Everything - Educational Purposes Only. I am not the creator/owner of the content of this video.

Information on the three part series can be found athttp://dsc.discovery.com/tv/stephen-hawking/about/about.html

Does Gliese 581g exist?
http://www.space.com/10897-alien-planet-gliese-581g-great-debate.html

Thursday, September 27, 2012


Ocean on Jupiter's Moon Europa Likely Deep Underground


Wednesday, September 26, 2012




Newfound Comet Could Look Spectacular in 2013

Comet C/2012 S1 (ISON) False Color Image

Comet C/2012 S1 (ISON) photographed at the RAS Observatory near Mayhill, NM on Sept. 22, 2012, by amateur astronomers Ernesto Guido, Giovanni Sostero and Nick Howes of the Remanzacco Observatory.
CREDIT: Remanzacco Observatory/Ernesto Guido, Giovanni Sostero & Nick Howes


A newly discovered comet has the potential to put on a dazzling celestial display late next year, when it will be so bright you may be able to see it briefly in the daytime sky.
The discovery of the object named Comet ISON was announced Monday (Sept. 24) by Russians Vitali Nevski and Artyom Novichonok, who detected it in photographs taken three days earlier using a 15.7-inch (0.4-meter) reflecting telescope of the International Scientific Optical Network (ISON), near Kislovodsk. The new comet is officially known as C/2012 S1.
When first sighted, Comet ISON was 625 million miles (1 billion kilometers) from Earth and 584 million miles (939 million km) from the sun, in the dim constellation of Cancer. It was shining at magnitude 18.8 on the reverse scale used by astronomers to measure the brightness of sky objects (the lower the number, the brighter the object). That makes the comet currently about 100,000 times fainter than the dimmest star that can be seen with the unaided eye.But at its perihelion (its closest point to the sun), due on Nov. 28, 2013, the comet will come within 800,000 miles (1.2 million km) of the sun’s surface and could evolve into a dazzling object ― possibly bright enough to be visible for a short time in broad daylight. [Spectacular Comet Photos (Gallery)]

This image shows the newfound comet C/2012 (ISON) as seen by the Remanzacco Observatory in Italy. The image, taken by amateur astronomers Ernesto Guido, Giovanni Sostero and Nick Howes, is a confirmation view of the comet, which was first discovered by Vitali Nevski (Vitebsk, Belarus) and Artyom Novichonok (Kondopoga, Russia). Image released Sept. 24, 2012.
CREDIT: Remanzacco Observatory/Ernesto Guido, Giovanni Sostero & Nick HowesView full size imageThe most exciting aspect of this new comet concerns its preliminary orbit, which bears a striking resemblance to that of the “Great Comet of 1680.” That comet put on a dazzling show; it was glimpsed in daylight and later, as it moved away from the sun, it threw off a brilliantly long tail that stretched up from the western twilight sky after sunset like a narrow searchlight beam for some 70 degrees of arc. (A person's clenched fist, held at arm’s length, covers roughly 10 degrees of sky.) 

The fact that the orbits are so similar seems to suggest Comet ISON and the Great Comet of 1680 could related or perhaps even the same object.
Comet ISON will be barely visible to the unaided eye when it is in the predawn night sky, positioned against the stars of Leo in October 2013.
 On Oct. 16 it will be passing very near both Mars and the bright star Regulus — both can be used as benchmarks to sighting the comet. In November, it could be as bright as third-magnitude when it passes very close to the bright first-magnitude star Spica in Virgo. 
The few days surrounding the comet’s closest approach to the sun on Nov. 28, 2013, are likely to be most interesting. It will whirl rapidly around the sun in a hairpin-like curve and perhaps becomes a dazzlingly bright (negative-magnitude) object.
The comet will then whirl north after perihelion and become visible during December both in the evening sky after sunset and in the morning sky before sunrise. Just how bright it will be and how long the tail may get during this time frame is anybody’s guess, but there is hope that it could evolve into a memorable celestial showpiece.

This NASA graphic shows the orbit and current position of comet C/2012 S1 (ISON). The comet is at present located at 6.25 AU from the sun, with 1 AU being the distance from Earth to the sun. Image released Sept. 24, 2012.
CREDIT: NASA/Jet Propulsion LaboratoryView full size imageAnd in case you haven’t checked your 2013 calendar, Nov. 28 is already a special day for those living in the United States: It is the Thanksgiving Day holiday.Which leads to the question: Will Comet ISON be a dazzler, or a turkey?Joe Rao serves as an instructor and guest lecturer at New York's Hayden Planetarium. He writes about astronomy for The New York Times and other publications, and he is also an on-camera meteorologist for News 12 Westchester, New York.


Dawn - Vesta Got Special Delivery of Hydrated Minerals
09.26.12
 
Map of hydrated minerals on VestaThis map from NASA's Dawn mission indicates the presence of hydrated minerals on the giant asteroid Vesta. Hydrated minerals are seen in white, with areas of high concentrations circled with a yellow dotted line in the annotated version. Image credit: NASA/JPL-Caltech/UCLA/INAF › Full image and caption       › Image gallery 
The mechanism that incorporates water into the terrestrial planets is a matter of extensive debate for planetary scientists. Now, observations of the giant asteroid Vesta by NASA's Dawn mission suggest that hydrated materials were delivered to it mainly through a buildup of small particles during an epoch when the solar system was rich in dust. This is a radically different process from the way hydrated materials have been deposited on the moon and may have implications for the formation of terrestrial planets, including the delivery of the water that formed Earth's ocean. Maria Cristina De Sanctis and the Dawn team present the scenarios today at the European Planetary Science Congress in Madrid, Spain.
"Vesta's surface shows distinct areas enriched with hydrated materials," said De Sanctis, of the Italian National Institute for Astrophysics in Rome. "These regions are not dependent on solar illumination or temperature, as we find in the case of the moon. The uneven distribution is unexpected and indicates ancient processes that differ from those believed to be responsible for delivering water to other airless bodies, like the moon."
A team led by De Sanctis studied data from Dawn's visible and infrared mapping spectrometer, which complement recently reported data on hydrogen distribution from Dawn's gamma ray and neutron detector. Their analysis showed large regional concentrations of hydroxyl - a hydrogen and an oxygen atom bound together - clearly associated with geological features, including ancient, highly-cratered terrains and a crater named Oppia.
Hydroxyl on the surface of the moon is thought to be created continuously by the interaction of protons from the solar wind with the top 10 feet (few meters) of the lunar surface, or regolith. Highest concentrations are found in areas near the lunar poles and in permanently shadowed craters where it is very cold. By contrast, the distribution of hydroxyl on Vesta is not dependent on significant shadowing or unusual cold temperatures. It is also stable over time, so its origin does not appear to be due to short-term processes.
The hydroxyl-rich regions on Vesta broadly correspond to its oldest surfaces. Around relatively large and young impact craters, hydroxyl detections are weak or absent, suggesting that the delivery of the substance is not an ongoing process.
The evidence from Dawn's visible and infrared mapping spectrometer suggests that much of Vesta's hydroxyl was delivered by small particles of primitive material, less than a few centimeters in diameter, over a time-limited period. This period may have occurred during the primordial solar system, around the time water is believed to have accumulated on Earth, or during the Late Heavy Bombardment, when collisions with space rocks would have produced a significant amount of dust.
However, this is not the whole story of hydrated materials on Vesta. The Oppia Crater is hydroxyl-rich, but not covered with the primitive dark material. This suggests there is more than one mechanism at work for depositing hydroxyl on Vesta's surface.
"The origin of Vesta's hydroxyl is certainly complex and possibly not unique: there could be various sources, like formation of hydroxyl actually on Vesta, in addition to the primordial impactors," said De Sanctis. "Vesta is providing new insights into the delivery of hydrous materials in the main asteroid belt, and may offer new scenarios on the delivery of hydrous minerals in the inner solar system, suggesting processes that may have played a role in the formation of terrestrial planets."
Following more than a year at Vesta, Dawn departed in September 2012 for the dwarf planet Ceres, where it will arrive in 2015. Dawn's mission to Vesta and Ceres is managed by NASA's Jet Propulsion Laboratory, Pasadena, Calif., for NASA's Science Mission Directorate in Washington. JPL is a division of the California Institute of Technology in Pasadena. Dawn is a project of the directorate's Discovery Program, managed by NASA's Marshall Space Flight Center in Huntsville, Ala. UCLA is responsible for overall Dawn mission science. Orbital Sciences Corp. in Dulles, Va., designed and built the spacecraft. The Dawn visible and infrared (VIR) mapping spectrometer was built by Selex Galileo and the Italian National Institute for Astrophysics.
For more information about Dawn, visit http://www.nasa.gov/dawn and http://dawn.jpl.nasa.gov/ .
 
 
Jia-Rui Cook
Jet Propulsion Laboratory, Pasadena, Calif.
818-354-0850
jccook@jpl.nasa.gov

Anita Heward 011-44-7756-034243
European Planetary Science Congress, Madrid, Spain
anita.heward@europlanet-eu.org 

Tuesday, September 25, 2012

OUR MILKY WAY GALAXY IS EMBEDDED IN AN ENORMOUS HALO.

NASA'S Chandra Shows Milky Way is Surrounded by Halo of Hot Gas
 
 
WASHINGTON -- Astronomers have used NASA's Chandra X-ray Observatory to find evidence our Milky Way Galaxy is embedded in an enormous halo of hot gas that extends for hundreds of thousands of light years. The estimated mass of the halo is comparable to the mass of all the stars in the galaxy. 

If the size and mass of this gas halo is confirmed, it also could be an explanation for what is known as the "missing baryon" problem for the galaxy. 

Baryons are particles, such as protons and neutrons, that make up more than 99.9 percent of the mass of atoms found in the cosmos. Measurements of extremely distant gas halos and galaxies indicate the baryonic matter present when the universe was only a few billion years old represented about one-sixth the mass and density of the existing unobservable, or dark, matter. In the current epoch, about 10 billion years later, a census of the baryons present in stars and gas in our galaxy and nearby galaxies shows at least half the baryons are unaccounted for. 

In a recent study, a team of five astronomers used data from Chandra, the European Space Agency's XMM-Newton space observatory and Japan's Suzaku satellite to set limits on the temperature, extent and mass of the hot gas halo. Chandra observed eight bright X-ray sources located far beyond the galaxy at distances of hundreds of millions of light-years. The data revealed X-rays from these distant sources are absorbed selectively by oxygen ions in the vicinity of the galaxy. The scientists determined the temperature of the absorbing halo is between 1 million and 2.5 million kelvins, or a few hundred times hotter than the surface of the sun. 

Other studies have shown that the Milky Way and other galaxies are embedded in warm gas with temperatures between 100,000 and 1 million kelvins. Studies have indicated the presence of a hotter gas with a temperature greater than 1 million kelvins. This new research provides evidence the hot gas halo enveloping the Milky Way is much more massive than the warm gas halo. 

"We know the gas is around the galaxy, and we know how hot it is," said Anjali Gupta, lead author of The Astrophysical Journal paper describing the research. "The big question is, how large is the halo, and how massive is it?" 

To begin to answer this question, the authors supplemented Chandra data on the amount of absorption produced by the oxygen ions with XMM-Newton and Suzaku data on the X-rays emitted by the gas halo. They concluded that the mass of the gas is equivalent to the mass in more than 10 billion suns, perhaps as large as 60 billion suns. 

"Our work shows that, for reasonable values of parameters and with reasonable assumptions, the Chandra observations imply a huge reservoir of hot gas around the Milky Way," said co-author Smita Mathur of Ohio State University in Columbus. "It may extend for a few hundred thousand light-years around the Milky Way or it may extend farther into the surrounding local group of galaxies. Either way, its mass appears to be very large." 

The estimated mass depends on factors such as the amount of oxygen relative to hydrogen, which is the dominant element in the gas. Nevertheless, the estimation represents an important step in solving the case of the missing baryons, a mystery that has puzzled astronomers for more than a decade. 

Although there are uncertainties, the work by Gupta and colleagues provides the best evidence yet that the galaxy's missing baryons have been hiding in a halo of million-kelvin gas that envelopes the galaxy. The estimated density of this halo is so low that similar halos around other galaxies would have escaped detection. 

The paper describing these results was published in the Sept. 1 issue of The Astrophysical Journal. Other co-authors were Yair Krongold of Universidad Nacional Autonoma de Mexico in Mexico City; Fabrizio Nicastro of Harvard-Smithsonian Center for Astrophysics in Cambridge, Mass.; and Massimiliano Galeazzi of University of Miami in Coral Gables, Fla. 

NASA's Marshall Space Flight Center in Huntsville, Ala., manages the Chandra program for NASA's Science Mission Directorate in Washington. The Smithsonian Astrophysical Observatory controls Chandra's science and flight operations from Cambridge. 

For Chandra images, multimedia and related materials, visit: 

For an additional interactive image, podcast and video on the finding, visit: 
 
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