vendredi 22 mai 2015

CryoSat detects sudden ice loss in Southern Antarctic Peninsula







ESA - CRYOSAT Mission logo.

22 May 2015

A recent acceleration in ice loss in a previously stable region of Antarctica has been detected by ESA’s ice mission.

ESA's Cryosat ice mission

The latest findings by a team of scientists from the UK’s University of Bristol show that with no sign of warning, multiple glaciers along the Southern Antarctic Peninsula suddenly started to shed ice into the ocean starting in 2009 at rate of about 60 cubic km each year.

This makes the region one of the largest contributors to sea-level rise in Antarctica, having added about 300 cubic km of water into the ocean in the past six years. Some glaciers along the coastal expanse are currently lowering by as much as four m each year.

Southern Antarctic Peninsula ice loss

Prior to 2009, the 750 km-long Southern Antarctic Peninsula showed no signs of change.

“It appears that sometime around 2009, the ice-shelf thinning and the subsurface melting of the glaciers passed a critical threshold that triggered the sudden ice loss,” said Dr Bert Wouters from the University of Bristol, who led the study.

“However, compared to other regions in Antarctica, the Southern Peninsula is rather understudied, exactly because it did not show any changes in the past, ironically.”

The study includes five years of measurements from ESA’s ice mission, CryoSat, which employs an advanced radar altimeter that can measure the surface height variation of ice in fine detail, allowing scientists to record changes in its volume with unprecedented accuracy.

The ice loss in the region is so large that it has even caused small changes in Earth’s gravity field, detected by NASA’s GRACE mission.

Ice loss dips gravity

“The fact that so many glaciers in such a large region suddenly started to lose ice came as a surprise to us. It shows a very fast response of the ice sheet: in just a few years the dynamic regime completely shifted,” said Dr Wouters.

Climate models show that the sudden change cannot be explained by changes in snowfall or air temperature. Instead, the team attributes the rapid ice loss to warming oceans.

Many of the glaciers in the region feed into ice shelves that float out over on the ocean surface, acting as buttresses to the ‘grounded’ ice resting on land. This slows down the flow of the glaciers into the ocean.

But the westerly winds that encircle Antarctica have become more vigorous in recent decades, in response to climate warming and ozone depletion. The stronger winds push warm waters from the Southern Ocean toward the poles, where they eat away at the glaciers and floating ice shelves from below. 

Grounding line retreat

Ice shelves in the region have lost almost one fifth of their thickness in the last two decades, thereby reducing the resisting force on the glaciers. A key concern is that much of the ice of the Southern Antarctic Peninsula is grounded on bedrock below sea level, which gets deeper inland.  This means that even if the glaciers retreat, the warm water will chase them inland and melt them even more.

“To pinpoint the cause of the changes, more data need to be collected. A detailed knowledge of geometry of the local ice shelves, the ocean floor topography, ice sheet thickness and glacier flow speeds are crucial to tell how much longer the thinning will continue,” said Dr Wouters.

The findings were published in Science yesterday: http://www.sciencemag.org/content/348/6237/899.full

Related links:

University of Bristol: http://www.bris.ac.uk/

CryoSat: http://www.esa.int/Our_Activities/Observing_the_Earth/CryoSat

Images, Video, Text, Credits: ESA/University of Bristol/DGFI/Planetary Visions.

Greetings, Orbiter.ch

jeudi 21 mai 2015

SpinSat Investigation Tests New Technology, Returns Data












ISS - International Space Station patch.

May 21, 2015

Equipment and data from the SpinSat investigation returns to Earth today, May 21, 2015, with splashdown of SpaceX's Dragon cargo spacecraft following its release from the International Space Station’s robotic arm at 7:04 a.m. EDT. This Nov. 28, 2014 photograph by NASA astronaut Terry Virts captures the predeploy of SpinSat, which was launched into orbit from the station through the Cyclops small satellite deployer, also known as the Space Station Integrated Kinetic Launcher for Orbital Payload Systems (SSIKLOPS).

NASA astronaut Terry Virts captures the predeploy of SpinSat

The SpinSat study tested how a spherical satellite measuring 22 inches in diameter moves and positions itself in space using new thruster technology. Researchers can use high-resolution atmospheric data captured by SpinSat to determine the density of the thermosphere, one of the uppermost layers of the atmosphere. With better knowledge of the thermosphere, engineers and scientists can refine satellite and telecommunications technology.

Related link:

SpinSat: http://www.nasa.gov/mission_pages/station/research/experiments/1019.html

Related article:

Critical NASA Research Returns to Earth Aboard U.S. SpaceX Dragon Spacecraft: http://orbiterchspacenews.blogspot.ch/2015/05/critical-nasa-research-returns-to-earth.html

For more information about the International Space Station (ISS), visit: http://www.nasa.gov/mission_pages/station/main/index.html

Image, Text, Credits: NASA/Sarah Loff.

Cheers, Orbiter.ch

Critical NASA Research Returns to Earth Aboard U.S. SpaceX Dragon Spacecraft












SpaceX - Falcon 9/Dragon CRS-6 Mission patch.

May 21, 2015

SpaceX's Dragon cargo spacecraft splashed down in the Pacific Ocean at 12:42 p.m. EDT Thursday with almost 3,100 pounds of NASA cargo from the International Space Station, including research on how spaceflight and microgravity affect the aging process and bone health.

Dragon is the only space station resupply spacecraft able to return a significant amount of cargo to Earth. It is the U.S. company’s sixth NASA-contracted commercial resupply mission to the station and carried more than two tons of supplies and scientific cargo when it lifted off from Cape Canaveral Air Force Station in Florida on April 14. NASA also has contracted with American companies SpaceX and Boeing to develop their Crew Dragon and CST-100, respectively, to once again transport astronauts to and from the orbiting laboratory from the United States in 2017.


Image above: The SpaceX Dragon cargo spacecraft was released from the International Space Station's robotic arm at 7:04 a.m. EDT Thursday. The capsule then performed a series of departure burns and maneuvers to move beyond the 656-foot (200-meter) "keep out sphere" around the station and begin its return trip to Earth. Image Credits: NASA TV.

The returning Space Aging study, for example, examines the effects of spaceflight on the aging of roundworms, widely used as a model for larger organisms. By growing millimeter-long roundworms on the space station, researchers can observe physiological changes that may affect the rate at which organisms age. This can be applied to changes observed in astronauts, as well, particularly in developing countermeasures before long-duration missions.

"Spaceflight-induced health changes, such as decreases in muscle and bone mass, are a major challenge facing our astronauts," said Julie Robinson, NASA's chief scientist for the International Space Station Program Office at NASA's Johnson Space Center in Houston. "We investigate solutions on the station not only to keep astronauts healthy as the agency considers longer space exploration missions but also to help those on Earth who have limited activity as a result of aging or illness."

Space station supply ship returns to Earth

Also returned on Dragon were samples for the Osteocytes and Mechanomechano-transduction (Osteo-4) investigation. Researchers with Osteo-4 will observe the effects of microgravity on the function of osteocytes, the most common cells in bone. Understanding the effects of microgravity on osteocytes will be critical as astronauts plan for future missions that require longer exposure to microgravity, including the NASA’s journey to Mars. The results derived from this study also could have implications on Earth for patients suffering bone disorders related to disuse or immobilization, as well as metabolic diseases such as osteoporosis.

Equipment and data from the Special Purpose Inexpensive Satellite (SpinSat) investigation also made the trip back to Earth. The SpinSat study tested how a spherical satellite, measuring 22 inches in diameter, moves and positions itself in space using new thruster technology. Researchers can use high-resolution atmospheric data captured by SpinSat to determine the density of the thermosphere, one of the uppermost layers of the atmosphere. With better knowledge of the thermosphere, engineers and scientists can refine satellite and telecommunications technology.

SpaceX's Dragon with Full Parachutes

The Dragon will be transported by ship approximately 155 miles northeast of its splashdown location to Long Beach, California where NASA cargo will be removed and returned to the agency. The spacecraft then will be prepared for its trip to SpaceX's test facility in McGregor, Texas, for processing.

The International Space Station is a convergence of science, technology and human innovation that enables us to demonstrate new technologies and make research breakthroughs not possible on Earth. It has been continuously occupied since November 2000 and, since then, has been visited by more than 200 people and a variety of international and commercial spacecraft. The ISS remains the springboard to NASA's next giant leap in exploration, including future missions to an asteroid and Mars.

Related link:

Osteocytes and Mechanomechano-transduction (Osteo-4) investigation: http://www.nasa.gov/mission_pages/station/research/news/osteocytes

For more information about the International Space Station, visit: http://www.nasa.gov/station

For more information about SpaceX's mission to the International Space Station, visit: http://www.nasa.gov/spacex

Images, Video, Text, Credits: NASA/Kathryn Hambleton/JPL/Dan Huot/NASA TV/Karen Northon.

Greetings, Orbiter.ch

NASA's WISE Spacecraft Discovers Most Luminous Galaxy in Universe







NASA - WISE Mission logo.

May 21, 2015

A remote galaxy shining with the light of more than 300 trillion suns has been discovered using data from NASA's Wide-field Infrared Survey Explorer (WISE). The galaxy is the most luminous galaxy found to date and belongs to a new class of objects recently discovered by WISE -- extremely luminous infrared galaxies, or ELIRGs.

Artist's concept of the galaxy WISE J224607.57-052635.0

"We are looking at a very intense phase of galaxy evolution," said Chao-Wei Tsai of NASA's Jet Propulsion Laboratory (JPL) in Pasadena, California, lead author of a new report appearing in the May 22 issue of The Astrophysical Journal. "This dazzling light may be from the main growth spurt of the galaxy’s black hole."

The brilliant galaxy, known as WISE J224607.57-052635.0, may have a behemoth black hole at its belly, gorging itself on gas. Supermassive black holes draw gas and matter into a disk around them, heating the disk to roaring temperatures of millions of degrees and blasting out high-energy, visible, ultraviolet, and X-ray light. The light is blocked by surrounding cocoons of dust. As the dust heats up, it radiates infrared light.

Immense black holes are common at the cores of galaxies, but finding one this big so “far back” in the cosmos is rare. Because light from the galaxy hosting the black hole has traveled 12.5 billion years to reach us, astronomers are seeing the object as it was in the distant past. The black hole was already billions of times the mass of our sun when our universe was only a tenth of its present age of 13.8 billion years.

The new study outlines three reasons why the black holes in the ELIRGs could have grown so massive. First, they may have been born big. In other words, the "seeds," or embryonic black holes, might be bigger than thought possible.

"How do you get an elephant?" asked Peter Eisenhardt, project scientist for WISE at JPL and a co-author on the paper. "One way is start with a baby elephant."

The other two explanations involve either breaking or bending the theoretical limit of black hole feeding, called the Eddington limit. When a black hole feeds, gas falls in and heats up, blasting out light. The pressure of the light actually pushes the gas away, creating a limit to how fast the black hole can continuously scarf down matter. If a black hole broke this limit, it could theoretically balloon in size at a breakneck pace. Black holes have previously been observed breaking this limit; however, the black hole in the study would have had to repeatedly break the limit to grow this large.

Alternatively, the black holes might just be bending this limit.

"Another way for a black hole to grow this big is for it to have gone on a sustained binge, consuming food faster than typically thought possible," said Tsai. "This can happen if the black hole isn't spinning that fast."

If a black hole spins slowly enough, it won't repel its meal as much. In the end, a slow-spinning black hole can gobble up more matter than a fast spinner.

"The massive black holes in ELIRGs could be gorging themselves on more matter for a longer period of time," said Andrew Blain of University of Leicester in the United Kingdom, a co-author of this report. "It's like winning a hot-dog-eating contest lasting hundreds of millions of years."

WISE Reactivated to Hunt for Asteroids

More research is needed to solve this puzzle of these dazzlingly luminous galaxies. The team has plans to better determine the masses of the central black holes. Knowing these objects’ true hefts will help reveal their history, as well as that of other galaxies, in this very crucial and frenzied chapter of our cosmos.

WISE has been finding more of these oddball galaxies in infrared images of the entire sky captured in 2010. By viewing the whole sky with more sensitivity than ever before, WISE has been able to catch rare cosmic specimens that might have been missed otherwise.

The new study reports a total of 20 new ELIRGs, including the most luminous galaxy found to date. These galaxies were not found earlier because of their distance, and because dust converts their powerful visible light into an incredible outpouring of infrared light.

"We found in a related study with WISE that as many as half of the most luminous galaxies only show up well in infrared light," said Tsai.

JPL manages and operates WISE for NASA's Science Mission Directorate in Washington. The spacecraft was put into hibernation mode in 2011, after it scanned the entire sky twice, thereby completing its main objectives. In September 2013, WISE was reactivated, renamed NEOWISE and assigned a new mission to assist NASA's efforts to identify potentially hazardous near-Earth objects.

For more information on WISE, visit: http://www.nasa.gov/wise

Images, Text, Credits: NASA/Felicia Chou/JPL/Whitney Clavin/Karen Northon.

Greetings, Orbiter.ch

Hubble Observes One-of-a-Kind Star Nicknamed ‘Nasty’












NASA - Hubble Space Telescope patch.

May 21, 2015

Astronomers using NASA’s Hubble Space Telescope have uncovered surprising new clues about a hefty, rapidly aging star whose behavior has never been seen before in our Milky Way galaxy. In fact, the star is so weird that astronomers have nicknamed it “Nasty 1,” a play on its catalog name of NaSt1. The star may represent a brief transitory stage in the evolution of extremely massive stars.


Image above: Astronomers using NASA’s Hubble Space Telescope have uncovered surprising new clues about a hefty, rapidly aging star whose behavior has never been seen before in our Milky Way galaxy. Image Credits: NASA/Hubble.

First discovered several decades ago, Nasty 1 was identified as a Wolf-Rayet star, a rapidly evolving star that is much more massive than our sun. The star loses its hydrogen-filled outer layers quickly, exposing its super-hot and extremely bright helium-burning core.

But Nasty 1 doesn’t look like a typical Wolf-Rayet star. The astronomers using Hubble had expected to see twin lobes of gas flowing from opposite sides of the star, perhaps similar to those emanating from the massive star Eta Carinae, which is a Wolf-Rayet candidate. Instead, Hubble revealed a pancake-shaped disk of gas encircling the star. The vast disk is nearly 2 trillion miles wide, and may have formed from an unseen companion star that snacked on the outer envelope of the newly formed Wolf-Rayet.  Based on current estimates, the nebula surrounding the stars is just a few thousand years old, and as close as 3,000 light-years from Earth.

“We were excited to see this disk-like structure because it may be evidence for a Wolf-Rayet star forming from a binary interaction,” said study leader Jon Mauerhan of the University of California, Berkeley. “There are very few examples in the galaxy of this process in action because this phase is short-lived, perhaps lasting only a hundred thousand years, while the timescale over which a resulting disk is visible could be only ten thousand years or less.”

In the team’s proposed scenario, a massive star evolves very quickly, and as it begins to run out of hydrogen, it swells up. Its outer hydrogen envelope becomes more loosely bound and vulnerable to gravitational stripping, or a type of stellar cannibalism, by a nearby companion star. In that process, the more compact companion star winds up gaining mass, and the original massive star loses its hydrogen envelope, exposing its helium core to become a Wolf-Rayet star.

Hubble orbiting the Earth

Another way Wolf-Rayet stars are said to form is when a massive star ejects its own hydrogen envelope in a strong stellar wind streaming with charged particles. The binary interaction model where a companion star is present is gaining traction because astronomers realize that at least 70 percent of massive stars are members of double-star systems. Direct mass loss alone also cannot account for the number of Wolf-Rayet stars relative to other less-evolved massive stars in the galaxy.

“We’re finding that it is hard to form all the Wolf-Rayet stars we observe by the traditional wind mechanism, because mass loss isn’t as strong as we used to think,” said Nathan Smith of the University of Arizona in Tucson, who is a co-author on the new NaSt1 paper. “Mass exchange in binary systems seems to be vital to account for Wolf-Rayet stars and the supernovae they make, and catching binary stars in this short-lived phase will help us understand this process.”

But the mass transfer process in mammoth binary systems isn’t always efficient. Some of the stripped matter can spill out during the gravitational tussle between the stars, creating a disk around the binary.

“That’s what we think is happening in Nasty 1,” Mauerhan said. “We think there is a Wolf-Rayet star buried inside the nebula, and we think the nebula is being created by this mass-transfer process. So this type of sloppy stellar cannibalism actually makes Nasty 1 a rather fitting nickname.”

The star’s catalogue name, NaSt1, is derived from the first two letters of each of the two astronomers who discovered it in 1963, Jason Nassau and Charles Stephenson.

Viewing the Nasty 1 system hasn’t been easy. The system is so heavily cloaked in gas and dust, it blocks even Hubble’s view of the stars. Mauerhan’s team cannot measure the mass of each star, the distance between them, or the amount of material spilling onto the companion star.

Previous observations of Nasty 1 have provided some information on the gas in the disk. The material, for example, is travelling about 22,000 miles per hour in the outer nebula, slower than similar stars. The comparatively slow speed indicates that the star expelled its material through a less violent event than Eta Carinae’s explosive outbursts, where the gas is travelling hundreds of thousands of miles per hour.

Hubble Space Telescope in orbit. Image Credit: NASA

Nasty 1 may also be shedding the material sporadically. Past studies in infrared light have shown evidence for a compact pocket of hot dust very close to the central stars. Recent observations by Mauerhan and colleagues at the University of Arizona, using the Magellan telescope at Las Campanas Observatory in Chile, have resolved a larger pocket of cooler dust that may be indirectly scattering the light from the central stars. The presence of warm dust implies that it formed very recently, perhaps in spurts, as chemically enriched material from the two stellar winds collides at different points, mixes, flows away, and cools. Sporadic changes in the wind strength or the rate the companion star strips the main star’s hydrogen envelope might also explain the clumpy structure and gaps seen farther out in the disk.

To measure the hypersonic winds from each star, the astronomers turned to NASA’s Chandra X-ray Observatory. The observations revealed scorching hot plasma, indicating that the winds from both stars are indeed colliding, creating high-energy shocks that glow in X-rays. These results are consistent with what astronomers have observed from other Wolf-Rayet systems.

The chaotic mass-transfer activity will end when the Wolf-Rayet star runs out of material. Eventually, the gas in the disk will dissipate, providing a clear view of the binary system.

“What evolutionary path the star will take is uncertain, but it will definitely not be boring,” said Mauerhan. “Nasty 1 could evolve into another Eta Carinae-type system. To make that transformation, the mass-gaining companion star could experience a giant eruption because of some instability related to the acquiring of matter from the newly formed Wolf-Rayet. Or, the Wolf-Rayet could explode as a supernova. A stellar merger is another potential outcome, depending on the orbital evolution of the system. The future could be full of all kinds of exotic possibilities depending on whether it blows up or how long the mass transfer occurs, and how long it lives after the mass transfer ceases.”

The team’s results will appear May 21 in the online edition of the Monthly Notices of the Royal Astronomical Society.

The Hubble Space Telescope is a project of international cooperation between NASA and the European Space Agency. NASA's Goddard Space Flight Center in Greenbelt, Maryland, manages the telescope. The Space Telescope Science Institute (STScI) in Baltimore, Maryland, conducts Hubble science operations. STScI is operated for NASA by the Association of Universities for Research in Astronomy, Inc., in Washington.

For images and more information about Nasty 1 and the Hubble Space Telescope, visit:

  http://www.nasa.gov/hubble
  http://hubblesite.org/news/2015/21
     http://www.spacetelescope.org/

Images (mentioned), Video, Text, Credits: NASA/ESA/Space Telescope Science Institute/Ray Villard/Holly Zell.

Greetings, Orbiter.ch

Impact crater or supervolcano caldera?












ESA - Mars Express Mission patch.

21 May 2015

Siloe Patera

At first glance, the region covered by this latest Mars Express image release appears to be pockmarked with impact craters. But the largest structure among them may hold a rather explosive secret: it could be remains of an ancient supervolcano.

The images presented here were taken by the high-resolution stereo camera on ESA’s Mars Express on 26 November 2014, and focus on the Siloe Patera feature in the Arabia Terra region of Mars.

Siloe Patera comprises two large nested craters, close to the centre of the main colour image. The outer rim measures about 40 x 30 km and, at its deepest point, the crater dips as low as 1750 m below the surrounding plains.

Siloe Patera in context

Some scientists believe that Siloe Patera and a number of similar features inArabia Terra are calderas, the collapsed centres of volcanoes. But not just any volcanoes: these are thought to be martian supervolcanoes.

On Earth, a supervolcano is defined as a volcano that can produce at least 1000 cubic kilometres of volcanic materials in an eruption – thousands of times larger than ‘normal’ volcanic eruptions and powerful enough to alter global climate. An example is the Yellowstone caldera in the United States.

Supervolcanoes occur when magma is trapped below the surface, leading to a huge built up in pressure. They erupt suddenly in violent explosions and thus do not ‘grow’ sloping mountains like Olympus Mons. That makes them hard to identify, especially millions or billions of years later.

But a number of irregularly shaped craters have been detected in the Arabia Terra region that could represent a family of ancient supervolcano calderas.

Siloe Patera topography

Siloe Patera is one such example. It is characterised by two depressions with steep-sided walls, collapse features and low topographic relief. The two depressions could even represent two different eruptive episodes due to collapse as the underlying magma pressure was released, or as the magma chamber migrated below the surface.

By comparison, impact craters include features such as a central peak, uplifted crater rims and ejecta blankets surrounding them. Indeed, impact craters are widespread in this scene: textbook examples can be found in the two side-by-side craters just above Siloe Patera, and in the large crater at the far right of the scene. These craters each exhibit a central peak, terraced crater walls and a surrounding ejecta blanket.

An impact crater with depth to diameter ratio comparable to Siloe Patera would be expected to show these features – unless perhaps the crater had undergone extensive erosion or modification – but it does not.  

Perspective view of Siloe Patera

Looking in more detail at Siloe Patera, as shown in the perspective view, numerous small channels and gullies are seen, cut into the walls and partly flowing into the depression. A prominent valley-like feature is present in the foreground, which cuts into the depression on one side.

The valley, along with numerous other small channels in the immediate vicinity, appears to cut through material to the lower left of the craters that could be either ejecta from an impact or volcanic flow.

If it is impact ejecta, then its asymmetric distribution could be explained either by an oblique meteoroid impact or by selective erosion of the blanket. Alternatively, it could be the product of lava flow from this part of the caldera.

Siloe Patera in 3D

Arabia Terra is already known to comprise plains of fine-grained, layered sulphate- and clay-bearing materials. The source of the material has been much debated, but lava and dust from eruptions could be the explanation.

Without any doubt, more data and high-resolution coverage – and even in situ sampling – would be necessary to resolve this mystery. And since the gases released in supervolcano eruptions could have had significant effects on the martian climate, this is a topic of great interest.

More about...

Mars Express overview: http://www.esa.int/Our_Activities/Space_Science/Mars_Express_overview

Mars Express 10 year brochure: http://esamultimedia.esa.int/multimedia/publications/BR-312/

Related links:

Looking at Mars: http://www.esa.int/Our_Activities/Space_Science/Mars_Express

High Resolution Stereo Camera: http://berlinadmin.dlr.de/Missions/express/indexeng.shtml

Behind the lens...: http://www.esa.int/Our_Activities/Space_Science/Mars_Express/Behind_the_lens

Frequently asked questions: http://www.esa.int/Our_Activities/Space_Science/Mars_Express/Frequently_asked_questions

ESA Planetary Science archive (PSA): http://www.rssd.esa.int/PSA

NASA Planetary Data System: http://pds-geosciences.wustl.edu/missions/mars_express/hrsc.htm

HRSC data viewer: http://hrscview.fu-berlin.de/

In depth:

Mars Express in depth: http://sci.esa.int/science-e/www/area/index.cfm?fareaid=9

Mars Express top 10 discoveries: http://sci.esa.int/jump.cfm?oid=51820

Images, Text, Credits: ESA/DLR/FU Berlin, CC BY-SA 3.0 IGO/NASA MGS MOLA Science Team.

Best regards, Orbiter.ch

mercredi 20 mai 2015

SpaceX Dragon Set For Thursday Departure












ISS - Expedition 43 Mission patch.

May 20, 2015

The Expedition 43 crew completed preparations on Wednesday to send SpaceX’s Dragon cargo vehicle back to Earth.

NASA astronauts Scott Kelly and Terry Virts transferred samples from two of the station’s Minus Eighty Degree Celsius Laboratory Freezer for ISS, or MELFI, freezers for return on Dragon. These included samples from the Cell Shape and Expression, CASIS PCG-3, Nematode Muscles experiments along with human research samples.


Image above: SpaceX’s Dragon cargo capsule is seen here docked to the Earth facing port of the Harmony module. SpaceX’s sixth commercial resupply flight to the International Space Station launched on April 14th and arrived three days later. It will depart with over 3,100 pounds of research samples and equipment and splashdown in the Pacific Ocean on May 21.

After final cargo loading was completed, the crew closed the hatch to Dragon and began preparing it for release tomorrow. Dragon has been grappled by the station’s robotic arm and is set to be released on Thursday, May 21 at 7:04 a.m. EDT.

Full Coverage Times: http://www.nasa.gov/press-release/nasa-tv-to-air-us-cargo-ship-departure-from-international-space-station

Related links:

Minus Eighty Degree Celsius Laboratory Freezer for ISS, or MELFI: http://www.nasa.gov/mission_pages/station/research/experiments/MELFI.html

Cell Shape and Expression: http://www.nasa.gov/mission_pages/station/research/news/spacex_six

CASIS PCG-3 experiments: http://www.nasa.gov/mission_pages/station/research/experiments/1289.html

Nematode Muscles experiments: http://www.nasa.gov/mission_pages/station/research/experiments/1012.html

For more information about the International Space Station (ISS), visit: http://www.nasa.gov/mission_pages/station/main/index.html

Image, Text, Credits: NASA/NASA TV.

Cheers, Orbiter.ch