UARS: When and Where Did It Go Down?

Credit: NASA

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After a night of changing predictions and hopes of many to see a fireball in the sky, the UARS (Upper Atmosphere Research Satellite) finally met it’s fiery demise.

The decommissioned, 6.5 ton satellite is believed to have re-entered the Earths atmosphere over the Pacific Ocean, and in it’s death throes the massive satellite broke up, and the surviving debris likely landed in the ocean, off of the West coast of North America.

In regard to the exact re-entry point and position of the debris field, Nicholas Johnson, chief orbital debris scientist at NASA’s Johnson Space Center, said “We don’t know where the debris field might be… We may never know.”

The US Department of Defense’s Joint Space Operations Center at Vandenberg Air Force Base in California and the U.S. Strategic Command radar tracking assessed that the satellite reentered the atmosphere sometime between 0323 and 0509 GMT on September 24, 2011 (the Strategic Command predicted it would re-enter at 04:16 GMT). During this period, the satellite was heading across the Pacific Ocean on a southwest-to-northeast trajectory approaching Canada’s west coast. The mid-point of that groundtrack and a possible reentry location is 31 N latitude and 219 E longitude (green circle marker on the above map).

“If the re-entry point was at the time of 04:16 GMT, then all that debris wound up in the Pacific Ocean,” Johnson said during a media briefing on Saturday. “If the re-entry point occurred earlier than that, practically the entire pass before 04:16 was over water. So the only way debris could have probably reached land would be if the re-entry occurred after 04:16.”

NASA says there are no reports of damage or injury caused by the surviving components that made it to the surface, and there are so far no credible visual reports of anyone seeing the UARS satellite burning up.

The Earth-observing satellite was in orbit for 20 years and 10 days.

Credit: NASA

Faster Than The Speed Of Light… OPERA Update

Artistic view of the SPS/CNGS layout. The CNGS beam is produced by accelerating protons to 400 GeV/c with the CERN Super Proton Synchrotron (SPS). These protons are ejected with a kicker magnet towards a 2 m long graphite neutrino production target in two extractions, each lasting 10.5 ?s and separated by 50 ms. Each CNGS cycle in the SPS is 6 s long. Secondary charged mesons are focused by two magnetic horns, each followed by a helium bag to minimise the interaction probability of the 5 mesons. Mesons decay in flight into neutrinos in a 1000 m long vacuum tunnel.

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A few days ago, the physics world was turned upside down at the announcement of “faster than the speed of light”. The mighty neutrino has struck again by breaking the cosmic speed limit and traveling at a velocity 20 parts per million above light speed. To absolutely verify this occurrence, collaboration is needed from different sources and we’re here to give you the latest update.

“This result comes as a complete surprise,” said OPERA spokesperson, Antonio Ereditato of the University of Bern. “After many months of studies and cross checks we have not found any instrumental effect that could explain the result of the measurement. While OPERA researchers will continue their studies, we are also looking forward to independent measurements to fully assess the nature of this observation.”

Since the OPERA measurements go against everything we think we know, it’s more important than ever to verify its findings through independent research.

“When an experiment finds an apparently unbelievable result and can find no artifact of the measurement to account for it, it’s normal procedure to invite broader scrutiny, and this is exactly what the OPERA collaboration is doing, it’s good scientific practice,” said CERN Research Director Sergio Bertolucci. “If this measurement is confirmed, it might change our view of physics, but we need to be sure that there are no other, more mundane, explanations. That will require independent measurements.”

To get the job done, the OPERA Collaboration joined forces with CERN metrology experts and other facilities to establish absolute calibrations. There cannot be any error margin in parameters between the source and detector distances – and the neutrino’s flight time. In this circumstance, the measurements of the initial source of the neutrino beam and OPERA has an uncertainty value of 20 cm over the 730 km. The neutrino flight time has an accuracy of less than 10 nanoseconds, and was confirmed through the use of highly regarded GPS equipment and an atomic clock. Every care was given to ensure precision.

“We have established synchronization between CERN and Gran Sasso that gives us nanosecond accuracy, and we’ve measured the distance between the two sites to 20 centimetres,” said Dario Autiero, the CNRS researcher who will give this afternoon’s seminar. “Although our measurements have low systematic uncertainty and high statistical accuracy, and we place great confidence in our results, we’re looking forward to comparing them with those from other experiments.”

“The potential impact on science is too large to draw immediate conclusions or attempt physics interpretations. My first reaction is that the neutrino is still surprising us with its mysteries.” said Ereditato. “Today’s seminar is intended to invite scrutiny from the broader particle physics community.”

Original Story Source: CERN Press Release. For Further Reading: Measurement of the neutrino velocity with the OPERA detector in the CNGS beam.

Read our previous article on this paper.

UARS Update: Satellite Fell in Pacific Ocean

UARS satellite at 22:56 on Sept. 22, 2011, as seen from Puerto Rico. Credit: Effrain Morales Rivera.

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NASA has confirmed that it’s decommissioned Upper Atmosphere Research Satellite fell back to Earth on Sept. 24 between 03:23 GMT and 05:05 GMT (11:23 p.m. EDT Friday, Sept. 23 and 1:09 a.m. EDT Sept. 24.) The Joint Space Operations Center at Vandenberg Air Force Base in California said the satellite entered the atmosphere over the North Pacific Ocean, off the west coast of the United States. The precise re-entry time and location of any debris impacts are still being determined. NASA is not aware of any reports of injury or property damage.

NASA will provide more information during a media telecon at 18:00 GMT (2 p.m. ET) to discuss the re-entry.

Artist concept of the UARS Satellite in orbit. Credit: NASA

SGU-24 Starts Soon

Our good friends at the Skeptic’s Guide to the Universe are about to punish themselves in a feat of skepticism that will shock and amaze mankind for generations to come. What will be seen, can never be unseen!

To help raise money for the show, the rogues have decided to put on a 24-hour video show, drawing in legends and supporters from across skeptic-kind. At some point you’ll see Adam Savage, Phil Plait, Richard Wiseman, Brian Brushwood, Richard Saunders, George Hrab, and more.

And you’ll also see me and Dr. Pamela Gay, my co-host from Astronomy Cast (I think we’re scheduled for 3pm Eastern time on Saturday).

The show gets started at 8:00pm Eastern Time on Friday, September 23rd, and runs for 24 non-stop hours.

You can find more, and actually watch the show here.

And if you really want to show your support for the SGU, take a moment and donate. Show them how much you appreciate their science news and skepticism.

Finding NEEMO: NASA’s Underwater Simulations Focus on Human Asteroid Mission

NEEMO engineering crew diver simulates anchoring to an asteroid surface. Image credit: NASA

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The sight of NASA mission specialists performing mission training underwater has been fairly common over the years. On October 15th, NASA astronaut and former ISS crew member Shannon Walker will lead a different kind of underwater training mission. Walker will be leading the 15th expedition of NASA Extreme Environment Mission Operations (NEEMO), and interestingly, the crew includes Steve Squyres, head of the Mars Rover Exploration Project.

What makes NEEMO different from the other NASA underwater training simulations we’ve seen in the past?

Think asteroid.

With manned exploration of an asteroid on NASA’s roadmap, new technologies and procedures need to be created in order to ensure astronaut safety and achieve mission science goals. The NEEMO program at NASA will be putting experts to the task of developing solutions to the new challenges presented with near-Earth asteroid exploration. During NEEMO 15, NASA will test new tools, techniques and communication technologies.

Before now, NASA hasn’t given much thought to the operations necessary for a manned mission to an asteroid. With the nearly non-existent surface gravity of an asteroid, astronauts won’t be able to walk on the surface. One idea being tested is for the astronauts to anchor themselves to the asteroid. One difficulty with using anchors is that not all asteroids are made of the same materials – some asteroids are mostly metal, others are loose rubble and some are a mix of rock, metal and dust. Underwater testing on the ocean floor provides an environment that is perfectly suited for the NEEMO 15 mission, allowing NASA to simulate an environment with weak gravity and diverse materials.

Artist's concept of anchoring to the surface of an asteroid. Image credit: NASA

There are three main goals for the NEEMO 15 mission. First NASA will test methods for anchoring to the surface of the asteroid. Moving on the surface of an asteroid will require a method of connecting multiple anchors. The second major goal of the mission is to determine the best way to connect the anchor system. The third major goal will explore methods of collecting samples on the surface of an asteroid.

In addition to mission leader Shannon Walker, and Steve Squyres, the crew of NEEMO 15 includes astronaut Takuya Onishi (Japan Aerospace Exploration Agency) and David Saint-Jacques (Canadian Space Agency). Also joining the astronauts on the NEEMO 15 crew are: James Talacek and Nate Bender (University of North Carolina). Squyres is principal investigator for the Mars Exploration Rover (Spirit and Opportunity) mission, while Talacek and Bender are professional aquanauts.

Serving as support crew, NASA astronauts Stan Love, Richard Arnold and Mike Gernhardt, will participate in the NEEMO mission from the DeepWorker submersible, which they will pilot. NASA is using the DeepWorker submarine as an underwater stand-in for the Space Exploration Vehicle (SEV) which NASA has been testing separately in the “Desert RATS” field trial mission.

If you’d like to learn more about NASA’s NEEMO field test mission, visit: http://www.nasa.gov/neemo

You can view information on the NEEMO 15 crew at: http://www.nasa.gov/mission_pages/NEEMO/NEEMO15/crew.html, and follow the mission on Twitter and Facebook

Source: NASA NEEMO Press Release

What Does NASA Sound Like?

Atlantis launches one last time on July 8, 2011. Credit: Alan Walters (awaltersphoto.com) for Universe Today.

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When you think of NASA, do certain sounds and/or soundbites come to mind?

“3…2…1…0 and Liftoff!”

“That’s one small step,….”

“Ignition sequence start…”

“We’re on our way Houston!”

You can now listen to a collection of distinct NASA sounds at the NASA Sounds website where you can download various clips for ringtones, or for your computer errors, alarms and notifications, or just add to your audio collection.

“NASA has been making historic sounds for over 50 years,” said Jerry Colen, NASA App project manager at the agency’s Ames
Research Center in Moffett Field, Calif. “Now we’re making some of these memorable sounds easy to find and use.”

The NASA sounds are available in both MP3 and M4R (iPhone) files, and also includes the sounds of spacecraft beeping and crackling. NASA will update the collection as new sounds become available.

Happy Equinox!

We’re now in Autumn (in the Northern Hemisphere), the time when the length of day and night are roughly the same. And from here on out, the nights will be getting longer and the days shorter. It’s often difficult to explain to people how the Earth’s tilt defines how much sunlight we get every day, and how it causes the changing seasons. Here’s the easy thing to do. Show this amazing video to anyone, and they’ll totally get it. It’s a full year’s snapshots of Earth taken by NASA’s Meteosat satellite.

The Bad Astronomer, Phil Plait, has a great explainer on the Equinox, and details what you’re seeing in this video. Check it out.

Water, Water Everywhere… And A Few Drops For Saturn, Too!

Recent Cassini images of Saturn's moon Enceladus backlit by the sun show the fountain-like sources of the fine spray of material that towers over the south polar region. This image was taken looking more or less broadside at the "tiger stripe" fractures observed in earlier Enceladus images. It shows discrete plumes of a variety of apparent sizes above the limb (edge) of the moon. This image was acquired on Nov. 27, 2005. Image Credit: NASA/JPL/Space Science Institute

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In 2005, NASA’s Cassini spacecraft gave us an incredible view of Enceladus chuffing out fountains of water vapor and ice. This action creates an enormous halo of gas, dust and ice that surrounds this Saturnian satellite and enables the planet’s E ring. Now Enceladus is once again in the spotlight as the only moon in the Solar System known to significantly contribute to its parent planet’s chemistry.

Earlier this year, ESA announced that its Herschel Space Observatory had observed a huge torus of water vapor around Saturn which apparently originated from Enceladus. It spans approximately 600,000 kilometers across and runs about 60,000 kilometers deep, but more so than its size is what it appears to be doing… adding water to Saturn’s upper atmosphere. Because the vapor isn’t detectable at visible wavelengths, this observation came as revelation for the Herschel scope.

“Herschel is providing dramatic new information about everything from planets in our own solar system to galaxies billions of light-years away,” said Paul Goldsmith, the NASA Herschel project scientist at NASA’s Jet Propulsion Laboratory, Pasadena, California.

While the Herschel infrared observation is new, the indication of a vapor torus around Saturn isn’t. NASA’s Voyager and Hubble missions had given astronomers clues in the past. In 1997, the European Space Agency’s Infrared Space Observatory cited water in Saturn’s atmosphere and two years later NASA’s Submillimeter Wave Astronomy Satellite confirmed it again. But this confirmation only added up to a puzzle. Water found in Saturn’s lower cloud levels couldn’t rise past the colder, upper deck… So where was the water coming from? The answer came in the form of Herschel’s observations and some very astute computer modeling.

“What’s amazing is that the model, which is one iteration in a long line of cloud models, was built without knowledge of the observation.” says Tim Cassidy, a recent post-doctoral researcher at JPL who is now at the University of Colorado’s Laboratory for Atmospheric and Space Physics, Boulder. “Those of us in this small modeling community were using data from Cassini, Voyager and the Hubble telescope, along with established physics. We weren’t expecting such detailed ‘images’ of the torus, and the match between model and data was a wonderful surprise.”

Through these simulations, researchers hypothesized that much of the water in the torus was simply lost to space and some is pulled back by gravity to add material to Saturn’s rings. However, it’s the 3-5% that made it back to Saturn’s atmosphere that’s the most interesting. Just how much water vapor is out there? Thanks to combining information from both Herschel and the Ultraviolet Imaging Spectrograph (UVIS) instrument aboard the Cassini spacecraft, we’ve learned that about 12,000 kilograms is being ejected from Enceladus every minute. Can you image how much that would add up to in the period of a year… or more?!

“With the Herschel measurements of the torus from 2009 and 2010 and our cloud model, we were able to calculate a source rate for water vapor coming from Enceladus,” said Cassidy. “It agrees very closely with the UVIS finding, which used a completely different method.”

“We can see the water leaving Enceladus and we can detect the end product — atomic oxygen — in the Saturn system,” said Cassini UVIS science team member Candy Hansen, of the Planetary Science Institute, Tucson, Ariz. “It’s very nice with Herschel to track where it goes in the meantime.”

A tiny percentage adds up to some mighty big numbers, and the water molecules from the torus impact Saturn’s atmosphere to a great degree by contributing hydrogen and oxygen.

“When water hangs out in the torus, it is subject to the processes that dissociate water molecules,” said Hansen, “first to hydrogen and hydroxide, and then the hydroxide dissociates into hydrogen and atomic oxygen.” This oxygen is dispersed through the Saturn system. “Cassini discovered atomic oxygen on its approach to Saturn, before it went into orbit insertion. At the time, no one knew where it was coming from. Now we do.”

Very few days go by that we don’t learn something new about the Solar System and its inner workings. Thanks to observations like those done by the Herschel Space Observatory and missions like Cassini-Huygens, we’re able to further understand the dynamics behind the beauty… and how a tiny player can carry a major role.

“The profound effect this little moon Enceladus has on Saturn and its environment is astonishing,” said Hansen.

Original Story Source: JPL News Release.

Where will the UARS Satellite Crash?

ATV re-entry. Credit: ESA

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The bus sized UARS (Upper Atmosphere Research Satellite) is expected to re-enter Earth’s atmosphere early morning GMT on September 24. Right now, the Center for Orbital and Reentry Debris Studies lists the projected re-entry time as 05:10 UT on Sept. 24, plus or minus 2 hours.

NASA UPDATE “As of 7 p.m. EDT on Sept. 23, 2011, the orbit of UARS was 90 miles by 95 miles (145 km by 150 km). Re-entry is expected between 11 p.m. Friday, Sept. 23, and 3 a.m., Sept. 24, Eastern Daylight Time (3 a.m. to 7 a.m. GMT). During that time period, the satellite will be passing over Canada, Africa and Australia, as well as vast areas of the Pacific, Atlantic and Indian oceans. The risk to public safety is very remote.”

Due to the robust nature of some of the parts on the satellite, it is likely that approximately 500kg of material will impact the ground or water.

The FAA (Federal Aviation Administration) has released a Local Air Safety Information special notice advising of the possibility of space debris.

The calculated risk that you’ll be hit by the falling space debris has been put at 1 in 3,200, said Nick Johnson, chief scientist with NASA’s Orbital Debris Program. But the chance that any one person on Earth getting hit by debris has been estimated at about 1 in 21 trillion.

It is highly unlikely that any injury or damage will be caused by this falling debris and NASA says; “The risk to public safety or property is extremely small, and safety is NASA’s top priority. Since the beginning of the Space Age in the late-1950s, there have been no confirmed reports of an injury resulting from re-entering space objects. Nor is there a record of significant property damage resulting from a satellite re-entry.”

It is still unsure where exactly the UARS satellite will pass over and re-enter the Earth’s atmosphere, but it will be an incredibly bright fireball visible even in daylight. But if some debris ends up near you, don’t worry too much — it won’t be flaming hot. NASA says any pieces of UARS landing on Earth will not be very hot. The heating of objects passing through the atmosphere stops at about 32 km (20 miles) up, and cools after that.

Stay posted for more updates and if you are lucky enough to get an image of UARS burning up please let us know and post your images on our flickr group

Surf, Sand & Space: The Astronaut Beach House

The astronaut beach house has served a crucial role in terms of providing astronauts a chance to collect their breaths and calm their minds before they thunder into space. Photo Credit: Alan Walters/awaltersphoto.com

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CAPE CANAVERAL, Fla – Astronauts preparing to launch into space for the better part of the last four decades have had a welcome refuge – the astronaut beach house. This small two-level structure it is often missed by those that are ferried past it to the nearby launch pads. The astronaut beach house is — for those set to thunder into orbit – a vital place to collect their thoughts before they make history. Let’s take a look inside, as three astronauts provide Universe Today with a guided tour of this historic and storied house.

Astronauts Robert Springer, Nicole P. Stott and Sam Durrance talked about their experiences at NASA's astronaut beach house. Photo Credit: Alan Walters/awaltersphoto.com

Robert C. Springer flew into space on space shuttle Discovery on STS-29 and on Atlantis for a Department of Defense mission on STS-38. For him, the beach house provided astronauts with a refuge from the hectic atmosphere that comes with preparing to launch to orbit. Springer retired from NASA and the United States Marine Corps in 1990. Afterward he worked for the Boeing Company as director of quality systems, Integrated Defense Systems. Springer views the beach house as a place for one to catch their breath – before the big day.

Sam T. Durrance is similar to both Springer in that he flew to orbit twice. His first mission was STS-35 aboard the space shuttle Columbia and his second was STS-67 on Endeavour. Durrance was a payload specialist on both of his two flights; this role required him to focus on each mission’s specific payload. Durrance is currently employed by the Florida Institute of Technology located in Melbourne, Florida, where he serves as a professor in the Department of Physics and Space Sciences.

Nicole P. Stott started out as a operations engineer at KSC in one of NASA’s Orbiter Processing Facilities. Stott supported human space flight endeavors in numerous roles at KSC before she moved to Johnson Space Center in 1998. She was selected for astronaut training two years later. Stott flew to the International Space Station on STS-128 where she stayed for 91 days before returning to Earth with the crew of STS-129. She would return to the ISS as a member of the STS-133 crew.

Stott came to agency later than Springer and Durrance and therefore her view is somewhat different. For her, the house served to both remind and include her in the area’s rich history.

“It’s a special place, you feel like your part of something here,” said Stott as she looked out from the beach house’s deck toward the ocean. “There is so much history here that while you know that when you’re here, it’s for an event that you’re participating in, but you’re aware that there is a lot that has gone on before you as well.”