On April 10, 2013, the White House and NASA released details of the US space agency's budget for the 2014 fiscal year. Included in the budget was a request for over $100 million to begin work on the Asteroid Retrieval and Utilization Mission. The mission would see a robotic spacecraft rendezvous with a small asteroid, which would then steer the space rock to the Earth-moon libration point (EML2) -- a region of gravitational stability beyond the far side of the moon. A manned mission would then meet the "tamed" asteroid to carry out science in-situ. It has been determined that such a mission would optimize the scientific gains while reducing risk and cost. On Wednesday, NASA released an animation detailing the stages of asteroid capture, here are the highlights.
Although its exact configuration has yet to be established, the robotic asteroid capture spacecraft will likely be solar powered and be propelled by an advanced ion drive. Optimistic estimates put a 2017 launch window on the first phase of the mission.
When approaching the asteroid, the spacecraft will jettison the hatch covering the folded asteroid "capture bag." According to the Keck Institute study that the mission is based on, the asteroid will be approximately 7 meters wide and have a mass of 550 tons.
The capture bag will expand like an accordion's bellows in preparation for asteroid capture.
The spacecraft will likely carry out an automated docking maneuver with the asteroid. Seen here, a laser is emitted by the spacecraft, guiding it in.
When fully expanded, and centered, the capture bag will envelop the space rock.
A draw-string-like mechanism will allow the capture bag's opening to be closed around the asteroid, securely mating spacecraft with asteroid.
Once secured, the spacecraft will "de-spin" the asteroid and begin steering it toward the Earth-moon system. This will mark the first time in human history that we have ever changed the trajectory of a natural object in space.
Meanwhile, preparations will be underway for a manned expedition to the captured asteroid. Seen here, NASA's future Space Launch System (SLS) rocket blasts off.
NASA's Orion space capsule will take a team of astronauts to the asteroid's parking orbit at EML2.
The Orion capsule will perform a docking maneuver with the robotic asteroid capture spacecraft after several days transit.
With the asteroid secure, astronauts will have the freedom (and time) to carry out extensive studies during extravehicular activity (EVA).
With the science done and samples collected, the Orion capsule returns to Earth.
The entire mission will culminate in the spashdown of the Orion capsule with astronauts on board. The asteroid will remain parked at EML2 for further study by followup missions to the lunar farside. You can watch the whole video on the NASA website:http://www.nasa.gov/multimedia/videogallery/index.html?media_id=161659311
The first-ever fossil proof of dramatic global cooling after the cosmic impact that ended the Age of Dinosaurs has been discovered.
The darkness and cold from the dust and ash thrown up by the giant collision was likely the main driver of the resulting mass die-off, known as the K-T extinction, scientists say. This extinction at the end of the Cretaceous period finished the reign of the dinosaurs. The only dinosaurian survivors were the birds; other reptiles such as turtles and crocodiles survived as well, although these are not descended from dinosaurs.
The prime suspect behind this disaster is a cosmic impact from an asteroid or comet. Scientists have found evidence of this collision near the town of Chicxulub (CHEEK-sheh-loob) in Mexico in the form of a giant crater more than 110 miles (180 kilometers) wide. The explosion that carved out this crater, likely caused by an object about 6 miles (10 km) across, would have released as much energy as 100 trillion tons of TNT, more than a billion times more than the atom bombs that destroyed Hiroshima and Nagasaki combined. [Wipe Out: History's Most Mysterious Mass Extinctions]
"When such an asteroid hits the Earth, the results are devastating," said lead study author Johan Vellekoop, a PhD candidate in paleoclimatology at Utrecht University in the Netherlands. "The impact itself releases an enormous amount of energy, so much that in the first hours after the impact, the air is heated up, igniting global wildfires."
In principle, such impacts also loft dust and soot into the atmosphere, "blocking incoming sunlight," Vellekoop said. "The sun is both our source of light as well as our main source of heat — hence, when sunlight can no longer reach the surface of the Earth, this surface rapidly cools down, creating a so-called 'impact winter,' a period of darkness and cold lasting for decades."
Prior studies hint that the impact winter reduced the amount of sunlight reaching Earth's surface by as much as 80 percent, cooling the land from tropical warmth to below freezing. This darkness and cold would have killed off plants and caused a global collapse of terrestrial and marine food webs.
"Ultimately, more than 50 percent of all plants and animals on Earth died out because of this," Vellekoop said.
However, until now, scientists had lacked fossil evidence of this impact winter, because this severe cold spell might have only lasted months to decades, too short a time period to be captured in a fossil record stretching across millions of years. In addition, many of the algae that produce the chalky fossils scientists use to estimate ancient ocean surface temperatures went extinct during the end-Cretaceous mass extinction.
"Our study is the first to show that this period of darkness and cold indeed took place," Vellekoop told Live Science.
Vellekoop and his colleagues focused their research on rocks exposed along the Brazos River between Waco and Hearne, Texas. These rocks originated from sediments deposited on the floor of a sea that existed in the area during and after the end of the Cretaceous.
The scientists analyzed organic compounds from microbes known as Thaumarchaeota, which adjust the composition of fat molecules in their membranes as sea surface temperatures change.
The researchers investigated organic compounds from Thaumarchaeota in Bravos River sediments of the same age as the Chicxulub impact. These sediments held coarse layers of broken shells — possibly traces of a post-impact tsunami — and anomalously high concentrations of iridium, a metal rare on Earth's surface but more common in space rocks.The findings suggest ocean temperatures fell dramatically after the impact, cooling from about 86 degrees F (30 degrees C) to about 73 degrees F (23 degrees C).
"Working on an event 66 million years ago, it is incredible that we could resolve sea water temperature changes within decades," Vellekoop said.
The most important implication of these findings "is that they demonstrate how devastating large meteorite impacts can be," Vellekoop added. "Our study confirms that such impacts can cause a so-called 'impact winter,' a global darkness lasting for years."
The researchers now aim to verify these results at other sites. The scientists detailed their findings online May 12 in the journal Proceedings of the National Academy of Sciences.
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This story originally appeared on LiveScience.com.
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