NASA’s Planning on Visiting the Water Worlds of the Solar System and Beyond

Next stop the ocean worlds of Enceladus and Europa

This illustration shows Cassini diving through the Enceladus plume in 2015. New ocean world discoveries from Cassini and Hubble will help inform future exploration and the broader search for life beyond Earth.
Credits: NASA/JPL-Caltech

Space news (planetary science: water worlds of the solar system; Enceladus and Europa) – planets and moons around the solar system and exoplanets across the universe covered with water

This graphic illustrates how scientists on NASA’s Cassini mission think water interacts with rock at the bottom of the ocean of Saturn’s icy moon Enceladus, producing hydrogen gas (H2).
The Cassini spacecraft detected the hydrogen in the plume of gas and icy material spraying from Enceladus during its deepest and last dive through the plume on Oct. 28, 2015. Cassini also sampled the plume’s composition during previous flybys, earlier in the mission. From these observations, scientists have determined that nearly 98 percent of the gas in the plume is water vapor, about 1 percent is hydrogen, and the rest is a mixture of other molecules including carbon dioxide, methane, and ammonia.
The graphic shows water from the ocean circulating through the seafloor, where it is heated and interacts chemically with the rock. This warm water, laden with minerals and dissolved gasses (including hydrogen and possibly methane) then pours into the ocean creating chimney-like vents.
The hydrogen measurements were made using Cassini’s Ion and Neutral Mass Spectrometer, or INMS, instrument, which sniffs gasses to determine their composition.
The finding is an independent line of evidence that hydrothermal activity is taking place in the Enceladus ocean. Previous results from Cassini’s Cosmic Dust Analyzer instrument, published in March 2015, suggested hot water is interacting with rock beneath the ocean; the new findings support that conclusion and indicate that the rock is reduced in its geochemistry. With the discovery of hydrogen gas, scientists can now conclude that there is a source of chemical free energy in Enceladus’ ocean.
The Cassini mission is a cooperative project of NASA, ESA (the European Space Agency) and the Italian Space Agency. The Jet Propulsion Laboratory, a division of Caltech in Pasadena, manages the mission for NASA’s Science Mission Directorate, Washington. The Cassini orbiter and its two onboard cameras were designed, developed and assembled at JPL. The Ion and Neutral Mass Spectrometer was designed and built by NASA Goddard Space Flight Center, Greenbelt, Maryland; the team is based at Southwest Research Institute (SwRI) in San Antonio.
For more information about the Cassini mission, visit http://www.nasa.gov/cassini and http://saturn.jpl.nasa.gov.
Image Credit: NASA.

The solar system’s awash in water! NASA missions have provided verifiable facts showing ocean worlds and moons exist in our solar system and beyond, other than Earth. Planetary bodies where water is locked in a frozen embrace and even flowing beneath miles of ice. Liquid water exobiologists are keen to explore for life forms they would love to meet and get to know a little better during the next phase of the human journey to the beginning of space and time. Watch this YouTube video on NASA’s search for life on the ocean worlds of the solar system.

Best Evidence Yet for Reoccurring Water Vapor Plumes Erupting from Jupiter’s Moon
When Galileo discovered Jupiter’s moon Europa in 1610, along with three other satellites whirling around the giant planet, he could have barely imagined it was such a world of wonder.
This revelation didn’t happen until 1979 when NASA’s Voyager 1 and 2 flew by Jupiter and found evidence that Europa’s interior, encapsulated under a crust of ice, has been kept warm over billions of years. The warmer temperature is due to gravitational tidal forces that flex the moon’s interior — like squeezing a rubber ball — keeping it warm. At the time, one mission scientist even speculated that the Voyagers might catch a snapshot of geysers on Europa.
Such activity turned out to be so elusive that astronomers had to wait over three decades for the peering eye of Hubble to monitor the moon for signs of venting activity. A newly discovered plume seen towering 62 miles above the surface in 2016 is at precisely the same location as a similar plume seen on the moon two years earlier by Hubble. These observations bolster evidence that the plumes are a real phenomenon, flaring up intermittently in the same region on the satellite.
The location of the plumes corresponds to the position of an unusually warm spot on the moon’s icy crust, as measured in the late 1990s by NASA’s Galileo spacecraft. Researchers speculate that this might be circumstantial evidence for material venting from the moon’s subsurface. The material could be associated with the global ocean that is believed to be present beneath the frozen crust. The plumes offer an opportunity to sample what might be in the ocean, in the search for life on that distant moon. Credits: NASA/JPL

Papers published by the journal Science and written by Cassini mission scientists and researchers working with the Hubble Space Telescope indicate hydrogen gas believed pouring from the subsurface ocean of Enceladus could potentially provide chemical energy life could use to survive and evolve. Watch this YouTube video called “NASA: Ingredients for Life at Saturn’s moon Enceladus“, it shows the proof scientists used to come to these conclusions. Their work provides new insights concerning possible oceans of water on moons of Jupiter and Saturn and other ocean moons in the solar system and beyond. 

Best Evidence Yet for Reoccurring Water Vapor Plumes Erupting from Jupiter’s Moon
When Galileo discovered Jupiter’s moon Europa in 1610, along with three other satellites whirling around the giant planet, he could have barely imagined it was such a world of wonder.
This revelation didn’t happen until 1979 when NASA’s Voyager 1 and 2 flew by Jupiter and found evidence that Europa’s interior, encapsulated under a crust of ice, has been kept warm over billions of years. The warmer temperature is due to gravitational tidal forces that flex the moon’s interior — like squeezing a rubber ball — keeping it warm. At the time, one mission scientist even speculated that the Voyagers might catch a snapshot of geysers on Europa.
Such activity turned out to be so elusive that astronomers had to wait over three decades for the peering eye of Hubble to monitor the moon for signs of venting activity. A newly discovered plume seen towering 62 miles above the surface in 2016 is at precisely the same location as a similar plume seen on the moon two years earlier by Hubble. These observations bolster evidence that the plumes are a real phenomenon, flaring up intermittently in the same region on the satellite.
The location of the plumes corresponds to the position of an unusually warm spot on the moon’s icy crust, as measured in the late 1990s by NASA’s Galileo spacecraft. Researchers speculate that this might be circumstantial evidence for material venting from the moon’s subsurface. The material could be associated with the global ocean that is believed to be present beneath the frozen crust. The plumes offer an opportunity to sample what might be in the ocean, in the search for life on that distant moon. Credits: NASA/JPL

“This is the closest we’ve come, so far, to identifying a place with some of the ingredients needed for a habitable environment,” said Thomas Zurbuchen, associate administrator for NASA’s Science Mission Directorate at Headquarters in Washington. ”These results demonstrate the interconnected nature of NASA’s science missions that are getting us closer to answering whether we are indeed alone or not.”

Portrait of Thomas Zurbuchen taken on Monday, October 17, 2016, at NASA Headquarters in Washington. Photo Credit: (NASA/Aubrey Gemignani)

Researchers believe they have found evidence indicating hydrogen gas could be pouring out of hydrothermal vents on the floor of Saturn’s moon Enceladus and into these oceans of water. Any microbes existing in these distant waters could use this gas as a form of chemical energy to operate biological processes. By combining hydrogen with carbon dioxide dissolved in this ocean of water in a chemical reaction called methanogenesis, geochemists think methane could be produced which could act as the basis of a tree of life similar to the one observed on Earth. 

Dramatic plumes, both large and small, spray water ice and vapor from many locations along the famed “tiger stripes” near the south pole of Saturn’s moon Enceladus. The tiger stripes are four prominent, approximately 84-mile- (135-kilometer-) long fractures that cross the moon’s south polar terrain.
This two-image mosaic is one of the highest resolution views acquired by Cassini during its imaging survey of the geyser basin capping the southern hemisphere of Saturn’s moon Enceladus. It clearly shows the curvilinear arrangement of geysers, erupting from the fractures. .From left to right, the fractures are Alexandria, Cairo, Baghdad, and Damascus.
As a result of this survey, 101 geysers were discovered: 100 have been located on one of the tiger stripes (PIA17188), and the three-dimensional configurations of 98 of these geysers have also been determined (PIA17186). The source location of the remaining geyser could not be definitively established. These results, together with those of other Cassini instruments, now strongly suggest that the geysers have their origins in the sea known to exist beneath the ice underlying the south polar terrain.
These findings from the imaging survey, of which the two images composing this mosaic are a part, were presented in a paper by Porco, DiNino, and Nimmo and published in the online version of the Astronomical Journal in July 2014: http://dx.doi.org/10.1088/0004-6256/148/3/45.
A companion paper, by Nimmo et al., is available at http://dx.doi.org/10.1088/0004-6256/148/3/46.
The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency, and the Italian Space Agency. NASA’s Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the mission for NASA’s Science Mission Directorate, Washington. The Cassini orbiter and its two onboard cameras were designed, developed and assembled at JPL. The imaging operations center is based at the Space Science Institute in Boulder, Colo.
For more information about the Cassini-Huygens mission visit http://saturn.jpl.nasa.gov and http://www.nasa.gov/cassini. The Cassini imaging team homepage is at http://ciclops.org.
Photojournal notes: This image has been rotated 180 degrees from its original orientation published on February 2, 2010.
Image Credit:
NASA/JPL/Space Science Institute

On Earth, this process is thought to be at the root of the tree of life, and could even be essential, critical to the origin of life on our little blue dot. Life existing on our planet requires three main ingredients, liquid water, a source of energy for metabolic processes, and specific chemical ingredients to develop and continue to thrive. This study shows Enceladus could have the right ingredients for life to exist, but planetary scientists and exobiologists are looking for evidence of the presence of sulfur and phosphorus. 

This set of images from NASA’s Cassini mission shows how the gravitational pull of Saturn affects the amount of spray coming from jets at the active moon Enceladus. Enceladus has the most spray when it is farthest away from Saturn in its orbit (inset image on the left) and the least spray when it is closest to Saturn (inset image on the right).
Water ice and organic particles gush out of fissures known as “tiger stripes” at Enceladus’ south pole. Scientists think the fissures are squeezed shut when the moon is feeling the greatest force of Saturn’s gravity. They theorize the reduction of that gravity allows the fissures to open and release the spray. Enceladus’ orbit is slightly closer to Saturn on one side than the other. A simplified version of that orbit is shown as a white oval.
Scientists correlate the brightness of the Enceladus plume to the amount of solid material being ejected because the fine grains of water ice in the plume are very bright when lit from behind. Between the dimmest and brightest images, they detected a change of about three to four times in brightness, approximately the same as moving from a dim hallway to a brightly lit office.
This analysis is the first clear finding that shows the jets at Enceladus vary in a predictable manner. The background image is a mosaic made from data obtained by Cassini’s imaging science subsystem in 2006. The inset image on the left was obtained on Oct. 1, 2011. The inset image on the right was obtained on Jan. 30, 2011.
A related image, PIA17039, shows just the Enceladus images. The Saturn system mosaic was created from data obtained by Cassini’s imaging cameras in 2006.
The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency, and the Italian Space Agency. NASA’s Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the mission for NASA’s Science Mission Directorate, Washington, DC. The Cassini orbiter was designed, developed and assembled at JPL. The visual and infrared mapping spectrometer was built by JPL, with a major contribution by the Italian Space Agency. The visual and infrared mapping spectrometer science team is based at the University of Arizona, Tucson.
For more information about the Cassini-Huygens mission, visit http://www.nasa.gov/cassini and http://saturn.jpl.nasa.gov/.
Image Credit:
NASA/JPL-Caltech/University of Arizona/Cornell/SSI

Previous data shows the rocky core of this moon is similar to meteorites containing these two elements, so they’re thought to be chemically similar in nature, and scientists are looking for the same chemical ingredients of life found on Earth, primarily carbon, nitrogen, oxygen, and of course hydrogen, phosphorus, and sulphur.

Linda Spilker
Cassini Project Scientist. Credits: NASA

“Confirmation that the chemical energy for life exists within the ocean of a small moon of Saturn is an important milestone in our search for habitable worlds beyond Earth,” said Linda Spilker, Cassini project scientist at NASA’s Jet Propulsion Laboratory (JPL) in Pasadena, California.

This illustration shows NASA’s Cassini spacecraft about to make one of its dives between Saturn and its innermost rings as part of the mission’s grand finale.
Cassini will make 22 orbits that swoop between the rings and the planet before ending its mission on Sept. 15, 2017, with a final plunge into Saturn. The mission team hopes to gain powerful insights into the planet’s internal structure and the origins of the rings, obtain the first-ever sampling of Saturn’s atmosphere and particles coming from the main rings, and capture the closest-ever views of Saturn’s clouds and inner rings.
During its time at Saturn, Cassini has made numerous dramatic discoveries, including a global ocean that showed indications of hydrothermal activity within the icy moon Enceladus, and liquid methane seas on its moon Titan.
The Cassini mission is a cooperative project of NASA, ESA (the European Space Agency) and the Italian Space Agency. The Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the mission for NASA’s Science Mission Directorate, Washington.
For more information about the Cassini-Huygens mission, visit http://www.nasa.gov/cassini and http://saturn.jpl.nasa.gov.
Image Credit: NASA/JPL-Caltech

Cassini detected hydrogen in plumes of gas and frozen matter spewing from Enceladus during the spacecraft’s deepest pass over its surface on October 28, 2015. This combined with previous data obtained by Cassini’s Ion and Neutral Mass Spectrometer (INMS) during earlier flybys around 2005, helped scientists determine that nearly 98 percent of the material spraying from the surface of the moon is water. The remaining two percent is thought to be around 1 percent hydrogen with some carbon dioxide, methane, ammonia and assorted unknown molecules in the mix. 

Cassini has shown us two independent detections of possible water spewing from the surface of Enceladus. NASA and its partners are currently looking over proposals to send spacecraft to determine if there is an ocean of water beneath its surface by taking a sample. The Europa Life Finder (ELF) is the proposal NASA’s seriously looking at undertaking at this point, but reports indicate a few other proposals are also being discussed. We’ll provide additional information on other proposals as they’re released to media outlets.

“Although we can’t detect life, we’ve found that there’s a food source there for it. It would be like a candy store for microbes,” said Hunter Waite, lead author of the Cassini study.

Two different observations of possible plumes of water spraying from the icy surface of Saturn’s moon Enceladus provides proof hydrothermal activity is occurring beneath. Geophysicists believe hot water is combining chemically with rock and other matter at the bottom of an ocean of water underneath its icy surface to produce hydrogen gas. Hydrogen gas exobiologists think could be used as energy, food of a sort, to sustain life forms exobiologists want to meet and learn more about. A meeting that would change our place in the cosmos, the way we think about the universe, and reality.

Looking for an interplanetary vacation destination? Consider a visit to Europa, one of the Solar System’s most tantalizing moons. Ice-covered Europa follows an elliptical path in its 85-hour orbit around our ruling gas giant Jupiter. Heat generated from strong tidal flexing by Jupiter’s gravity keeps Europa’s salty subsurface ocean liquid all year round. That also means even in the absence of sunlight Europa has energy that could support simple life forms. Unfortunately, it is currently not possible to make reservations at restaurants on Europa, where you might enjoy a dish of the local extreme shrimp. But you can always choose another destination from Visions of the Future.

Astronomers and researchers working with the Hubble Space Telescope in 2016 reported on an observation of a possible plume erupting from the icy surface of Europa in the same general location Hubble observed a possible plume in 2014. This location also corresponds to the unusually warm region with cracks in the icy surface observed by NASA’s Galileo spacecraft back in the 1990s. This provides evidence this phenomenon could be periodic, intermittent in this region of the moon. Mission planners are looking at this region as a possible location to obtain a sample of water erupting from a possible ocean of water beneath its icy surface. Watch this video on Europa.

Estimates of the size of this most recently observed plume indicate it rose about 62 miles (~100 kilometers) from the surface of Europa, while the plume in 2014 only reached a height of around 30 miles (50 kilometers). 

William Sparks
Space Telescope Science Institute. Credits: Space Science Institute/NASA/JPL

“The plumes on Enceladus are associated with hotter regions, so after Hubble imaged this new plume-like feature on Europa, we looked at that location on the Galileo thermal map. We discovered that Europa’s plume candidate is sitting right on the thermal anomaly,” said William Sparks of the Space Telescope Science Institute in Baltimore, Maryland. Sparks led the Hubble plume studies in both 2014 and 2016.

One interesting thought’s the plumes and the hot spot is somehow linked. If this is the case, it could mean the vented water’s falling onto the surface of the moon, which would change the structure and chemistry of the surface grains and allow them to retain heat longer than the surrounding region. This location would be a great place to search for the ingredients of life and a possible entry point into an ocean of water beneath.

NASA’s Europa Clipper mission is being designed to fly by the icy Jovian moon multiple times and investigate whether it possesses the ingredients necessary for life.
Credits: NASA/JPL-Caltech/SETI Institute

These observations by the Hubble Space Telescope and future looks enable future space missions to Europa and other ocean worlds in the solar system. Specifically, laying the groundwork for NASA’s Europa Clipper mission, which is set for a launch sometime in the 2020s. 

James Green: Director of Planetary Science, NASA Headquarters. Credits: NASA

“If there are plumes on Europa, as we now strongly suspect, with the Europa Clipper we will be ready for them,” said Jim Green, Director of Planetary Science, at NASA Headquarters.

NASA has indicated they’re looking to identify a possible site with persistent, intermittent plume activity as a target location for a mission to Europa to explore using its powerful suite of science instruments. Another team’s currently at work on a powerful ultraviolet camera to add to the Europa Clipper that would offer data similar to that provided by the Hubble Space Telescope, while some members of the Cassini team are working on a very sensitive, next generation INMS instrument to put on the spacecraft. 

Water’s the story of life on Earth! Science has shown it played and plays the main part in the birth, evolution, and sustenance of life on Earth. 

NASA’s planning on taking the human journey to the beginning of space and time to the ocean worlds of the solar system during the decades ahead. To search for the ingredients of life and even possibly simple one-celled life forms, of an unknown type. We plan on going along for the ride to have a look for ourselves and we hope to see your name on the ship manifest. We’ll save a seat for you.

Join the human journey to the beginning of space and time by taking part in NASA’s Backyard Worlds: Planet 9. Participants take part in the search for hidden worlds between Neptune and Proxima Centauri.

NASA’s and FEMA are currently tracking the progress of a 300 to 800 ft asteroid they think has around a 2 percent chance of hitting the Earth around September 20, 2020.

Planetary scientists searching the Red Planet for signs of past and present water believe they have found evidence indicating Mars once was a lot wetter and a possible location for the evolution of life.

NASA Engineers Test Prototype Robotic Asteroid Capture System 

In order to better understand intricate operations and detailed planning needed to capture multi-ton boulder from asteroid surface

A prototype of the Asteroid Redirect Mission (ARM) robotic capture module system is tested with a mock asteroid boulder in its clutches at NASA’s Goddard Space Flight Center in Greenbelt, Maryland. The robotic portion of ARM is targeted for launch in 2021. Located in the center’s Robotic Operations Center, the mockup helps engineers understand the intricate operations required to collect a multi-ton boulder from an asteroid’s surface. The hardware involved here includes three space frame legs with foot pads, two seven degrees of freedom arms that have with microspine gripper “hands” to grasp onto the boulder. NASA and students from West Virginia University built the asteroid mockup from rock, styrofoam, plywood and an aluminum endoskeleton. The mock boulder arrived in four pieces and was assembled inside the ROC to help visualize the engagement between the prototype system and a potential capture target. Inside the ROC, engineers can use industrial robots, a motion-based platform, and customized algorithms to create simulations of space operations for robotic spacecraft. The ROC also allows engineers to simulate robotic satellite servicing operations, fine tuning systems and controllers and optimizing performance factors for future missions when a robotic spacecraft might be deployed to repair or refuel a satellite in orbit. Image Credit: NASA
A prototype of the Asteroid Redirect Mission (ARM) robotic capture module system is tested with a mock asteroid boulder in its clutches at NASA’s Goddard Space Flight Center in Greenbelt, Maryland. The robotic portion of ARM is targeted for launch in 2021.
Located in the center’s Robotic Operations Center, the mockup helps engineers understand the intricate operations required to collect a multi-ton boulder from an asteroid’s surface. The hardware involved here includes three space frame legs with footpads, two seven degrees of freedom arms that have with microspine gripper “hands” to grasp onto the boulder.
NASA and students from West Virginia University built the asteroid mockup from rock, styrofoam, plywood and an aluminum endoskeleton. The mock boulder arrived in four pieces and was assembled inside the ROC to help visualize the engagement between the prototype system and a potential capture target.
Inside the ROC, engineers can use industrial robots, a motion-based platform, and customized algorithms to create simulations of space operations for robotic spacecraft. The ROC also allows engineers to simulate robotic satellite-servicing operations, fine-tuning systems and controllers and optimizing performance factors for future missions when a robotic spacecraft might be deployed to repair or refuel a satellite in orbit.
Image Credit: NASA

Space news (Asteroid Redirect Mission: testing of prototype of robotic capture module system) – The Robotic Operations Center of NASA’s Goddard Space Flight Center

NASA's Asteroid Redirect Missions. Credits: NASA/Goddard
A new report provides expert findings from a special action team on how elements of the Asteroid Redirect Mission (ARM) can address decadal science objectives and help close Strategic Knowledge Gaps (SKGs) for future human missions in deep space. Credits: NASA/Goddard

Inside the Robotic Operations Center (ROC) of NASA’s Goddard Space Flight Center engineers are at work preparing the robotic section of the Asteroid Redirect Mission (ARM). The most recent work involved testing a prototype of the asteroid capture system with a mock boulder built by NASA and students from West Virginia University. This work will help engineers learn more about the intricate operations needed to capture a multi-ton boulder from the surface of an asteroid. The robotic section of ARM is targeted for a 2021 launch window.

The capability built into the ROC allows engineers to create a simulation of the capture of a boulder from the surface of an asteroid. Here they can also simulate servicing of the satellite, fine tuning of systems and controllers, and even optimize all performance factors for future repairs and refueling. An important capability when building spacecraft worth hundreds of millions of dollars and even more. One that saves money and time.

The Asteroid Redirect Mission is expected to offer benefits that should teach us more about operating in space and enable future space missions. You can read a report here on some of the expected benefits.

The report reflects the findings of a two-month study conducted by members of the Small Bodies Assessment Group (SBAG). It explains many of ARM’s potential contributions to the future of the human journey to the beginning of space and time.

“This report is an important step in identifying ways that ARM will be more scientifically relevant as we continue mission formulation for the robotic and the crew segments,” said Gates. “We’re currently in the process of selecting hosted instruments and payloads for the robotic segment, and hope to receive an updated analysis from the SBAG after we announce those selections in spring 2017.”

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Discover and learn more about the ferocious winds near the biggest magnets discovered during the human journey to the beginning of space and time, magnetars.

Read about NASA’s latest additions to its plans to send manned missions to Mars.

Discover and learn about the feedback mechanisms of supermassive black holes.

Learn more about NASA’s contributions to the human journey to the beginning of space and time here.

Read about NASA’s Asteroid Redirect Mission.

Discover NASA’s Goddard Space Flight Center.

ESA’s ExoMars 2016 Trace Gas Orbiter Prepares to Descend to the Red Planet

Schiaparelli module separates from Trace Gas Orbiter in preparation for orbit-raising maneuver 

This artist's concept from the European Space Agency (ESA) depicts the Trace Gas Orbiter and its entry, descent and landing demonstrator module, Schiaparelli, approaching Mars. The separation occurred on Oct. 16, 2016. The orbiter and the lander are components of the ExoMars 2016 mission of ESA and Roscosmos. Image Credit: ESA/ATG medialab
This artist’s concept from the European Space Agency (ESA) depicts the Trace Gas Orbiter and its entry, descent and landing demonstrator module, Schiaparelli, approaching Mars. The separation occurred on Oct. 16, 2016. The orbiter and the lander are components of the ExoMars 2016 mission of ESA and Roscosmos.
Image Credit: ESA/ATG medialab

Space news (space exploration: ExoMars 2016; orbit insertion and Schiaparelli module descent to surface) – Over 34 million miles (56 million kilometers) from Earth, preparing to descend to the surface of the Red Planet – 

This image show a fan-shaped deposit where a channel enters a crater. This suggests that water once flowed through the channel into a crater lake, depositing material in a similar manner to river deltas on Earth. Credits: NASA/ESA/medialab
This image shows a fan-shaped deposit where a channel enters a crater, which suggests to planetary scientists and geologists that water once flowed through the channel into a crater lake, depositing material in a similar manner to river deltas on Earth. Credits: NASA/ESA/medialab

NASA’s Curiosity rover and other Mars explorers are about to get a little help from their European and Russian brothers and sisters in the form of the ExoMars Trace Gas Orbiter (TGO). One of two joint space missions between Europe and Russia designed to explore Mars for signs that life once existed, the ExoMars TGO will investigate the environment, and blaze a path for a future 2020s mission to return a sample of Martian terrain for planetary scientists to examine in detail for signs of life. 

This stereo scene recorded by the Pancam on NASA's Mars Exploration Rover Opportunity on Aug. 15, 2014, looks back toward part of the west rim of Endeavour Crater marked with the rover's wheel tracks. It appears three-dimensional when seen through blue-red glasses with the red lens on the left. Credits: NASA/ESA
This stereo scene recorded by the Pancam on NASA’s Mars Exploration Rover Opportunity on Aug. 15, 2014, looks back toward part of the west rim of Endeavour Crater marked with the rover’s wheel tracks. It appears three-dimensional when seen through blue-red glasses with the red lens on the left. Credits: NASA/ESA

The ExoMars TGO completed its final trajectory maneuver at 08.:45 GMT on October 14 and at 14:42 GMT/16:42 CEST today the Schiaparelli module separated from the orbiter. Tomorrow around 02:42 GMT/04:42 CEST the robotic spacecraft will conduct an orbit-raising maneuver in preparation for orbit insertion and the descent of Schiaparelli to the surface of Mars at around 14:48 GMT/16:48 CEST. The module is scheduled to land in a region of Mars near the equator called Meridiani Planum, where it will search for signs of life once having existed on the Red Planet. 

On Nov. 1, 2016, the High Resolution Imaging Science Experiment (HiRISE) camera on NASA's Mars Reconnaissance Orbiter observed the impact site of Europe's Schiaparelli test lander, gaining the first color view of the site since the lander's Oct. 19, 2016, arrival. These cutouts from the observation cover three locations where parts of the spacecraft reached the ground: the lander module itself in the upper portion, the parachute and back shell at lower left, and the heat shield at lower right. The heat shield location was outside of the area covered in color. The scale bar of 10 meters (32.8 feet) applies to all three cutouts. Where the lander module struck the ground, dark radial patterns that extend from a dark spot are interpreted as "ejecta," or material thrown outward from the impact, which may have excavated a shallow crater. From the earlier image, it was not clear whether the relatively bright pixels and clusters of pixels scattered around the lander module's impact site are fragments of the module or image noise. Now it is clear that at least the four brightest spots near the impact are not noise. These bright spots are in the same location in the two images and have a white color, unusual for this region of Mars. The module may have broken up at impact, and some fragments might have been thrown outward like impact ejecta. At lower right are several bright features surrounded by dark radial impact patterns, located where the heat shield was expected to impact. The bright spots appear identical in the Nov. 1 and Oct. 25 images, which were taken from different angles, so these spots are now interpreted as bright material, such as insulation layers, not glinting reflections. Credits: NASA/ESA/JPL/Caltech
On Nov. 1, 2016, the High-Resolution Imaging Science Experiment (HiRISE) camera on NASA’s Mars Reconnaissance Orbiter observed the impact site of Europe’s Schiaparelli test lander, gaining the first color view of the site since the lander’s Oct. 19, 2016, arrival.
These cutouts from the observation cover three locations where parts of the spacecraft reached the ground: the lander module itself in the upper portion, the parachute and back shell at lower left, and the heat shield at lower right. The heat shield location was outside of the area covered in color. The scale bar of 10 meters (32.8 feet) applies to all three cutouts. Where the lander module struck the ground, dark radial patterns that extend from a dark spot are interpreted as “ejecta,” or material is thrown outward from the impact, which may have excavated a shallow crater. From the earlier image, it was not clear whether the relatively bright pixels and clusters of pixels scattered around the lander module’s impact site are fragments of the module or image noise. Now it is clear that at least the four brightest spots near the impact are not noise. These bright spots are in the same location in the two images and have a white color, unusual for this region of Mars. The module may have broken up at impact, and some fragments might have been thrown outward like impact ejecta. At lower right are several bright features surrounded by dark radial impact patterns, located where the heat shield was expected to impact. The bright spots appear identical in the Nov. 1 and Oct. 25 images, which were taken from different angles, so these spots are now interpreted as bright material, such as insulation layers, not glinting reflections. Credits: NASA/ESA/JPL/Caltech

Unfortunately, after the separation from the ExoMars TGO, the Schiaparelli module didn’t return telemetry (onboard status information) and only sent its carrier signal, which indicates it’s operational and waiting for commands. Mission control’s currently looking into this anomaly and a resolution to the problem’s expected within a few hours. You can check for updates to this on the ESA website here

This Oct. 25, 2016, image shows the area where the European Space Agency's Schiaparelli test lander reached the surface of Mars, with magnified insets of three sites where components of the spacecraft hit the ground. It is the first view of the site from the High Resolution Imaging Science Experiment (HiRISE) camera on NASA's Mars Reconnaissance Orbiter taken after the Oct. 19, 2016, landing event. This Oct. 25 observation shows three locations where hardware reached the ground, all within about 0.9 mile (1.5 kilometer) of each other, as expected. The annotated version includes insets with six-fold enlargement of each of those three areas. Brightness is adjusted separately for each inset to best show the details of that part of the scene. North is about 7 degrees counterclockwise from straight up. The scale bars are in meters. At lower left is the parachute, adjacent to the back shell, which was its attachment point on the spacecraft. The parachute is much brighter than the Martian surface in this region. The smaller circular feature just south of the bright parachute is about the same size and shape as the back shell, (diameter of 7.9 feet or 2.4 meters). At upper right are several bright features surrounded by dark radial impact patterns, located about where the heat shield was expected to impact. The bright spots may be part of the heat shield, such as insulation material, or gleaming reflections of the afternoon sunlight. Image Credit: NASA/JPL-Caltech/Univ. of Arizona
This Oct. 25, 2016, image shows the area where the European Space Agency’s Schiaparelli test lander reached the surface of Mars, with magnified insets of three sites where components of the spacecraft hit the ground. It is the first view of the site from the High-Resolution Imaging Science Experiment (HiRISE) camera on NASA’s Mars Reconnaissance Orbiter taken after the Oct. 19, 2016, landing event. This Oct. 25 observation shows three locations where hardware reached the ground, all within about 0.9 miles (1.5 kilometers) of each other, as expected. The annotated version includes insets with six-fold enlargement of each of those three areas. Brightness is adjusted separately for each inset to best show the details of that part of the scene. North is about 7 degrees counterclockwise from straight up. The scale bars are in meters.
At lower left is the parachute, adjacent to the back shell, which was its attachment point on the spacecraft. The parachute is much brighter than the Martian surface in this region. The smaller circular feature just south of the bright parachute is about the same size and shape as the back shell, (diameter of 7.9 feet or 2.4 meters).
At upper right are several bright features surrounded by dark radial impact patterns, located about where the heat shield was expected to impact. The bright spots may be part of the heat shield, such as insulation material, or gleaming reflections of the afternoon sunlight. Image Credit: NASA/JPL-Caltech/Univ. of Arizona

What’s next for ExoMars?

If everything goes as planned, mission control should get an update from the ExoMars TGO on October 20, along with images of the surface of the planet as Schiaparelli descended to Mars. Continuous updates from the orbiter and module are expected through the duration of the ExoMars TGO mission. The events of the mission will also be live streamed on the ESA website here, along with reports on Twitter using the hashtag #ExoMars

Watch this YouTube video on ten magnificent years of exploration for the Mars Reconnaissance Orbiter.

Read about NASA’s recent selection of five US-based aerospace firms to work on Mars Orbiter concepts.

Read and learn more about NASA’s selection of eight US university teams to work on the newest, latest space habitats.

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Learn more about the ExoMars 2016 TGO and the Schiaparelli module here

Learn more about the things planetary scientists have discovered about Mars

Rosetta Spacecraft Says Its Final Goodbye

An image of the surface of comet 67P/Churyumov-Gerasimenko worth a thousand words

The OSIRIS narrow-angle camera aboard the Space Agency's Rosetta spacecraft captured this image of comet 67P/Churyumov-Gerasimenko on September 30, 2016, from an altitude of about 10 miles (16 kilometers) above the surface during the spacecraft’s controlled descent. The image scale is about 12 inches (30 centimeters) per pixel and the image itself measures about 2,000 feet (614 meters) across. Credits: ESA/Rosetta/MPS/UPD/LAM/IAA/SSO/INTA/UPM/DASP/IDA
The OSIRIS narrow-angle camera aboard the Space Agency’s Rosetta spacecraft captured this image of comet 67P/Churyumov-Gerasimenko on September 30, 2016, from an altitude of about 10 miles (16 kilometers) above the surface during the spacecraft’s controlled descent. The image scale is about 12 inches (30 centimeters) per pixel and the image itself measures about 2,000 feet (614 meters) across.
Credits: ESA/Rosetta/MPS/UPD/LAM/IAA/SSO/INTA/UPM/DASP/IDA

Space news (solar system science: planetary science; cometary science) – 66 feet above the surface of comet 67P/Churyumov-Gerasimenko; in a controlled descent –

Rosetta's last image of Comet 67P/Churyumov-Gerasimenko, taken shortly before impact, at an estimated altitude of 66 feet (20 meters) above the surface. The image was taken with the OSIRIS wide-angle camera on 30 September. The image scale is about 5 mm/pixel and the image measures about 2.4 m across. Credits: ESA/Rosetta/MPS for OSIRIS Team MPS/UPD/LAM/IAA/SSO/INTA/UPM/DASP/IDA
Rosetta’s last image of Comet 67P/Churyumov-Gerasimenko, taken shortly before impact, at an estimated altitude of 66 feet (20 meters) above the surface. The image was taken with the OSIRIS wide-angle camera on 30 September. The image scale is about 5 mm/pixel and the image measures about 2.4 m across.
Credits: ESA/Rosetta/MPS for OSIRIS Team MPS/UPD/LAM/IAA/SSO/INTA/UPM/DASP/IDA

The image above is the last thing the OSIRIS narrow-angle camera aboard the European Space Agency”s (ESA)Rosetta spacecraft captured before it hit the surface of comet 67P/Churyumov-Gerasimenko at 4:19 a.m. PDT (7:19 a.m. EDT/1:19 p.m. CEST) on September 30, 2016. During this controlled crash landing of the first spacecraft in history to rendezvous and escort a comet as it orbits the Sun. Astronomers were able to conduct an additional study of the gas, dust and plasma environment close to the surface of the comet and take these high-resolution images.

Comet from 5.7 km – narrow-angle camera Credit: ESA/Rosetta/MPS for OSIRIS Team MPS/UPD/LAM/IAA/SSO/INTA/UPM/DASP/IDA
Comet from 5.7 km – narrow-angle camera
Credit: ESA/Rosetta/MPS for OSIRIS Team MPS/UPD/LAM/IAA/SSO/INTA/UPM/DASP/IDA

The OSIRIS narrow-angle camera also captured the image shown at the top of the page from a height of around 10 miles (16 kilometers) from the surface of comet 67P/Churyumov-Gerasimenko. This image spans a distance of around 2,000 feet (614 meters) across the comet’s icy and volatile surface. Attempting to walk across such a surface as Bruce Willis and his drilling crew did in the movie Armageddon is going to be tricky at best.

OSIRIS narrow-angle camera image with Philae, 2 September Credit: ESA/Rosetta/MPS for OSIRIS Team MPS/UPD/LAM/IAA/SSO/INTA/UPM/DASP/IDA
OSIRIS narrow-angle camera image with Philae, 2 September
Credit: ESA/Rosetta/MPS for OSIRIS Team MPS/UPD/LAM/IAA/SSO/INTA/UPM/DASP/IDA

It might seem like a waste to purposely crash the Rosetta spacecraft on comet 67P/Churyumov-Gerasimenko, but in the end, it’s probably the best solution. This comets headed out beyond the orbit of Jupiter, which is further from the Sun than the spacecraft has traveled before, and there wouldn’t be enough solar power to operate its systems. Communicating with the spacecraft’s also about to become difficult for a month, with the Sun being close to the line-of-sight between Earth and Rosetta during this time period.

Close-up of the Philae lander, imaged by Rosetta’s OSIRIS narrow-angle camera on 2 September 2016 from a distance of 2.7 km. The image scale is about 5 cm/pixel. Philae’s 1 m-wide body and two of its three legs can be seen extended from the body. The images also provide proof of Philae’s orientation. The image is a zoom from a wider-scene, and has been interpolated. More information: Philae found! Credit: ESA/Rosetta/MPS for OSIRIS Team MPS/UPD/LAM/IAA/SSO/INTA/UPM/DASP/IDA
Close-up of the Philae lander, imaged by Rosetta’s OSIRIS narrow-angle camera on 2 September 2016 from a distance of 2.7 km. The image scale is about 5 cm/pixel. Philae’s 1 m-wide body and two of its three legs can be seen extended from the body. The images also provide proof of Philae’s orientation.
The image is a zoom from a wider-scene, and has been interpolated.
More information: Philae found!
Credit: ESA/Rosetta/MPS for OSIRIS Team MPS/UPD/LAM/IAA/SSO/INTA/UPM/DASP/IDA

Rosetta mission complete

Feel happy for Rosetta and team, they both did the job, and then some in the end. It took a decade of careful planning and travel to rendezvous with comet 67P/Churyumov-Gerasimenko and write history. Just one month and two days later, a smaller lander named Philae touched down on the surface of the comet. It bounced on the surface a few times, before finally setting down. During the next few days, it took the first images ever of a comet’s surface up close and sent back important data planetary scientists will use to look for clues to the role comets played in the formation of the planets 4.5 billion years ago. Clues they hope to use to learn more about the origin and evolution of our solar system and possibly the formation of solar systems in general.

JPL/NASA Rosetta Team From left to right: Dongsuk (Don) Han- Outer Planet Navigation Bruce Tsurutani - Rpc-mag Essam Heggy - Consert Sam Gulkis - Miro Danny Tran - Aspen Josh Doubleday - Aspen Gregg Rabideau - Aspen Tim Koch - Miro Martina Troesch - Software Barbara Hesselgesser - Acquisitions Paul Von Allmen - Miro Belinda Arroyo - DSN Sophia Lee - Scheduling Paul Friz-Rosetta Shadow Project Liz Barrios - Illustrator Paul Springer - Miro Steve Chien - Aspen Cynthia Kahn-Former SE David Delgado - Public Engagement Claudia Alexander - Project Scientist Grant Faris - MA Shyam Bhaskaran - NAV Mark Hofstadter - Miro Seungwon Lee - Miro Lei Pan - Miro Jacky Bagumyan - Assistant Adans Ko - MA Sarah Marcotte - Mars consultant Charlene Barone - Rosetta Web Project Lead Dan Goods - Creative Director Virgil Adumitroale - Miro Richard Flores - Acquisitions Artur Chmielewski - Rosetta Project Manager Veronica McGregor - Social Media Credits: NASA/JPL
JPL/NASA Rosetta Team
From left to right:
Dongsuk (Don) Han- Outer Planet Navigation
Bruce Tsurutani – Rpc-mag
Essam Heggy – Consert
Sam Gulkis – Miro
Danny Tran – Aspen
Josh Doubleday – Aspen
Gregg Rabideau – Aspen
Tim Koch – Miro
Martina Troesch – Software
Barbara Hesselgesser – Acquisitions
Paul Von Allmen – Miro
Belinda Arroyo – DSN
Sophia Lee – Scheduling
Paul Friz-Rosetta Shadow Project
Liz Barrios – Illustrator
Paul Springer – Miro
Steve Chien – Aspen
Cynthia Kahn-Former SE
David Delgado – Public Engagement
Claudia Alexander – Project Scientist
Grant Faris – MA
Shyam Bhaskaran – NAV
Mark Hofstadter – Miro
Seungwon Lee – Miro
Lei Pan – Miro
Jacky Bagumyan – Assistant
Adans Ko – MA
Sarah Marcotte – Mars consultant
Charlene Barone – Rosetta Web Project Lead
Dan Goods – Creative Director
Virgil Adumitroale – Miro
Richard Flores – Acquisitions
Artur Chmielewski – Rosetta Project Manager
Veronica McGregor – Social Media
Credits: NASA/JPL

Watch this YouTube video of the last few hours of ESA’s Rosetta mission.

Read and learn more about planetary scientists anticipation of studying a sample of material from the surface of comet 67P/Churyumov-Gerasimenko, material left over from the early moments of the birth of the solar system.

Read about comet 67P/Churyumov-Gerasimenko.

Prepare to journey to comet 103P/Hartley.

Join the space journey of NASA.

Learn more about comet 67P/Churyumov-Gerasimenko here.

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Learn more about the work of the ESA.

Read and learn more about comets here.

 

Feedback Mechanisms of Actively Feeding Supermassive Black Holes

Can blow star-forming gas 1000 light-years out of core region of host galaxies 

This artist's rendering shows a galaxy being cleared of interstellar gas, the building blocks of new stars. New X-ray observations by Suzaku have identified a wind emanating from the black hole's accretion disk (inset) that ultimately drives such outflows. Credits: ESA/ATG Medialab
This artist’s rendering shows a galaxy being cleared of interstellar gas, the building blocks of new stars. New X-ray observations by Suzaku have identified a wind emanating from the black hole’s accretion disk (inset) that ultimately drives such outflows.
Credits: ESA/ATG Medialab

Space news (astrophysics: evolution of galaxies; feedback mechanisms) – about 2.3 billion years ago in a galaxy far, far away and standing in a fierce, 2 million mile per hour (3 million kilometers per hour) outflow of star-forming gas – 

Astrophysicists studying the evolution of galaxies using the Suzaku X-ray satellite and the European Space Agency’s Herschel Infrared Space Observatory have found evidence suggesting supermassive black holes significantly influence the evolution of their host galaxies. They found data pointing to winds near a monster black hole blowing star-forming gas over 1,000 light-years from the galaxy center. Enough material to form around 800 stars with the mass of our own Sol. 

“This is the first study directly connecting a galaxy’s actively ‘feeding’ black hole to features found at much larger physical scales,” said lead researcher Francesco Tombesi, an astrophysicist at NASA’s Goddard Space Flight Center in Greenbelt, Maryland, and the University of Maryland, College Park (UMCP). “We detect the wind arising from the luminous disk of gas very close to the black hole, and we show that it’s responsible for blowing star-forming gas out of the galaxy’s central regions.” 

The artist’s view of galaxy IRAS F11119+3257 (F11119) above shows 3 million miles per hour winds produced near the supermassive black hole at its center heating and dispersing cold, dense molecular clouds that could form new stars. Astronomers believe these winds are part of a feedback mechanism that blows star-forming gas from galaxy centers, forever altering the structure and evolution of their host galaxy.  

A red-filter image of IRAS F11119+3257 (inset) from the University of Hawaii's 2.2-meter telescope shows faint features that may be tidal debris, a sign of a galaxy merger. Background: A wider view of the region from the Sloan Digital Sky Survey. Credits: NASA's Goddard Space Flight Center/SDSS/S. Veilleux
A red-filter image of IRAS F11119+3257 (inset) from the University of Hawaii’s 2.2-meter telescope shows faint features that may be tidal debris, a sign of a galaxy merger. Background: A wider view of the region from the Sloan Digital Sky Survey.
Credits: NASA’s Goddard Space Flight Center/SDSS/S. Veilleux

Astronomers have been studying the Monster of the Milky Way, the supermassive black hole with an estimated mass six million times that of Sol thought to reside at the center of our galaxy, for years. The monster black hole at the core of F11119 is thought to contain around 16 million times the mass of Sol. The accretion disk surrounding this supermassive black hole is measured at hundreds of times the diameter of our solar system. The 170 million miles per hour (270 million kilometers per hour) winds emanating from its accretion disk push the star-forming dust out of the central regions of the galaxy. Producing a steady flow of cold gas over a thousand light-years across traveling at around 2 million mph (3 million kph) and moving a volume of mass equal to around 800 Suns. 

Astrophysicists have been searching for clues to a possible correlation between the masses of a galaxy’s central supermassive black hole and its galactic bulge. They have observed galaxies with more massive black holes generally, have bulges with proportionately larger stellar mass. The steady flow of material out of the central regions of galaxy F11119 and into the galactic bulge could help explain this correlation. 

“These connections suggested the black hole was providing some form of feedback that modulated star formation in the wider galaxy, but it was difficult to see how,” said team member Sylvain Veilleux, an astronomy professor at UMCP. “With the discovery of powerful molecular outflows of cold gas in galaxies with active black holes, we began to uncover the connection.” 

“The black hole is ingesting gas as fast as it can and is tremendously heating the accretion disk, allowing it to produce about 80 percent of the energy this galaxy emits,” said co-author Marcio Meléndez, a research associate at UMCP. “But the disk is so luminous some of the gas accelerates away from it, creating the X-ray wind we observe.” 

tidal_disruption_art_as
In this artist’s rendering, a thick accretion disk has formed around a supermassive black hole following the tidal disruption of a star that wandered too close. Stellar debris has fallen toward the black hole and collected into a thick chaotic disk of hot gas. Flashes of X-ray light near the center of the disk result in light echoes that allow astronomers to map the structure of the funnel-like flow, revealing for the first time strong gravity effects around a normally quiescent black hole. Credits: NASA/Swift/Aurore Simonnet, Sonoma State University

The accretion disk wind and associated molecular outflow of cold gas could be the final pieces astronomers have been looking for in the puzzle explaining supermassive black hole feedback. Watch this video animation of the workings of supermassive black hole feedback in quasars

Black-hole-powered galaxies called blazars are the most common sources detected by NASA's Fermi Gamma-ray Space Telescope. As matter falls toward the supermassive black hole at the galaxy's center, some of it is accelerated outward at nearly the speed of light along jets pointed in opposite directions. When one of the jets happens to be aimed in the direction of Earth, as illustrated here, the galaxy appears especially bright and is classified as a blazar. Credits: M. Weiss/CfA
Black-hole-powered galaxies called blazars are the most common sources detected by NASA’s Fermi Gamma-ray Space Telescope. As matter falls toward the supermassive black hole at the galaxy’s center, some of it is accelerated outward at nearly the speed of light along jets pointed in opposite directions. When one of the jets happens to be aimed in the direction of Earth, as illustrated here, the galaxy appears especially bright and is classified as a blazar.
Credits: M. Weiss/CfA

When the supermassive black hole’s most active, it clears cold gas and dust from the center of the galaxy and shuts down star formation in this region. It also allows shorter-wavelength light to escape from the accretion disk of the black hole astronomers can study to learn more. We’ll keep you updated on any additional discoveries. 

What’s the conclusion?

Astrophysicists conclude F11119 could be an early evolutionary phase of a quasar, a type of active galactic nuclei (AGN) with extreme emissions across a broad spectrum. Computer simulations show the supermassive black hole should eventually consume the gas and dust in its accretion disk and then its activity should lessen. Leaving a less active galaxy with little gas and a comparatively low level of star formation. 

Blazar 3C 279's historic gamma-ray flare can be seen in these images from the Large Area Telescope (LAT) on NASA's Fermi satellite. Both images show gamma rays with energies from 100 million to 100 billion electron volts (eV). For comparison, visible light has energies between 2 and 3 eV. Left: A week-long exposure ending June 10, before the eruption. Right: An exposure for the following week, including the flare. 3C 279 is brighter than the Vela pulsar, normally the brightest object in the gamma-ray sky. The scale bar at left shows an angular distance of 10 degrees, which is about the width of a clenched fist at arm's length. Credits: NASA/DOE/Fermi LAT Collaboration
Blazar 3C 279’s historic gamma-ray flare can be seen in these images from the Large Area Telescope (LAT) on NASA’s Fermi satellite. Both images show gamma rays with energies from 100 million to 100 billion electron volts (eV). For comparison, visible light has energies between 2 and 3 eV. Left: A week-long exposure ending June 10, before the eruption. Right: An exposure for the following week, including the flare. 3C 279 is brighter than the Vela pulsar, normally the brightest object in the gamma-ray sky. The scale bar at left shows an angular distance of 10 degrees, which is about the width of a clenched fist at arm’s length.
Credits: NASA/DOE/Fermi LAT Collaboration

Astrophysicists and scientists look forward to detecting and studying feedback mechanisms connected with the growth and evolution of supermassive black holes using the enhanced ability of ASTRO-H. A joint space partnership between Japan’s Aerospace Exploration Agency (ISAS/JAXA) and NASA’s Goddard Space Flight Center, Suzaku’s successors expected to lift the veil surrounding this mystery even more and lay the foundation for one day understanding a little more about the universe and its mysteries.

Watch an animation made by NASA’s Goddard Space Flight Center showing how black hole feedback works in quasars here.

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Learn what astronomers have discovered about the Monster of the Milky Way.  

 

Binary Star System V404 Cygni Flares to Life

Forming rings of X-ray light that expand with time, creating a shooting target effect 

rings_full
Rings of X-ray light centered on V404 Cygni, a binary system containing an erupting black hole (dot at center), were imaged by the X-ray Telescope aboard NASA’s Swift satellite from June 30 to July 4. A narrow gap splits the middle ring in two. Color indicates the energy of the X-rays, with red representing the lowest (800 to 1,500 electron volts, eV), green for medium (1,500 to 2,500 eV), and the most energetic (2,500 to 5,000 eV) shown in blue. For comparison, visible light has energies ranging from about 2 to 3 eV. The dark lines running diagonally through the image are artifacts of the imaging system. Credits: Andrew Beardmore (Univ. of Leicester) and NASA/Swift

Space news (astrophysics: binary star systems; black hole/sun-like star systems) – 8,000 light-years away toward the constellation Cygnus, next to flaring 10 solar mass black hole – 

It all started just before 2:32 p.m. on June 15, 2015, when NASA’s Swift X-ray Burst Alert Satellite detected a rising wave of high-speed, extremely-energetic X-rays emanating from the direction of the constellation Cygnus. Additional detections of the same flare ten minutes later by a Japanese experiment on the International Space Station called the Monitor of All-sky X-ray Image (MAXI) and other detectors. Allowed astronomers to determine the outburst detected originated 8,000 light-years away in low-mass X-ray binary V404 Cygni, where previous data indicated a stellar-mass black hole and sun-like star orbited each other. A black hole and sun-like star binary system that up to this point had been sleeping since its last outburst in 1989. 

moon_v404cyg_comp
The Swift X-ray image of V404 Cygni covers a patch of the sky equal to about half the apparent diameter of the full moon. This image shows the rings as they appeared on June 30. Credits: NASA’s Scientific Visualization Studio (left), Andrew Beardmore (Univ. of Leicester); NASA/Swift (right)

Fifteen days later on June 30, a team of scientists from around the world led by Andrew Beardmore of the University of Leicester in the United Kingdom investigated V404 Cygni a little closer using NASA’s Swift X-ray Burst Alert Satellite. Images taken (above) revealed a series of concentric rings of X-ray light centered on a 10 solar mass black hole (dot at the center of image). 

On the left, an optical image from the Digitized Sky Survey shows Cygnus X-1, outlined in a red box. Cygnus X-1 is located near large active regions of star formation in the Milky Way, as seen in this image that spans some 700 light years across. An artist's illustration on the right depicts what astronomers think is happening within the Cygnus X-1 system. Cygnus X-1 is a so-called stellar-mass black hole, a class of black holes that comes from the collapse of a massive star. The black hole pulls material from a massive, blue companion star toward it. This material forms a disk (shown in red and orange) that rotates around the black hole before falling into it or being redirected away from the black hole in the form of powerful jets.
On the left, an optical image from the Digitized Sky Survey shows Cygnus X-1, outlined in a red box. Cygnus X-1 is located near large active regions of star formation in the Milky Way, as seen in this image that spans some 700 light years across. An artist’s illustration on the right depicts what astronomers think is happening within the Cygnus X-1 system. Cygnus X-1 is a so-called stellar-mass black hole, a class of black holes that comes from the collapse of a massive star. The black hole pulls material from a massive, blue companion star toward it. This material forms a disk (shown in red and orange) that rotates around the black hole before falling into it or being redirected away from the black hole in the form of powerful jets.

Astronomers believe the x-ray rings are the result of echoing x-ray light from a large flare on June 26, 2016, at 1:40 p.m. EDT. The flare emitted x-rays in all directions. Multiple dust layers at around 4,000 and 1,000 light-years from V404 Cygni reflected some of these x-rays towards Earth. This reflected light travels a greater distance and reaches us slightly later than light traveling a straighter path. The small time difference produced an x-ray echo, formed x-ray rings expanding in spacetime.  

“The flexible planning of Swift observations has given us the best dust-scattered X-ray ring images ever seen,” Beardmore said. “With these observations, we can make a detailed study of the normally invisible interstellar dust in the direction of this black hole.” 

What’s next?

The team is currently watching V404 Cygni, waiting for its next outburst, and preparing Swift to collect additional data to determine exactly what’s going on here. They hope to hit the bulls eye in human understanding of the collection on x-ray sources detected across the cosmos. Regular monitoring of this binary system using a suite of telescopes and instruments could give us clues to how a stellar-mass black hole and sun-like star end up orbiting each other. About the origin and formation of the unusual types of binary systems detected during the human journey to the beginning of space and time. 

Watch this YouTube video on the flaring of V404 Cygni.

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Discover V404 Cygni

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Travel across the Tarantula nebula on a runaway star.

Read about the Kepler Space Telescope’s recent observation of the shockwave from a nearby supernova for the first time in human history.

Take a look and learn more about NASA’s Europa spacecraft.

Advanced Satellite for Cosmology & Astrophysics (ASCA, formally Astro-D)

Study in space exploration collaboration between nations heading into the unknown 

pct_main_asuka
ASCA (ASTRO-D) scientific results included the first imaging of X-ray objects by the scintillation proportional counter on March 17, 1993, and observation of X-rays from the supernova SN1993J recently discovered in the M81 galaxy. Credits: Japanese Aerospace Exploration Agency (JAXA)

Space news (astrophysics & cosmology: x-ray astronomy; spectral resolution of supernovae, accreting binaries, active galactic nuclei, and galaxy clusters) – between 525 – 615 kilometers above the Earth, orbiting every 96 minutes while observing the x-ray universe –  

asuka_f_b
This diagram shows the configuration and overall shape of ASCA. Credits: JAXA

Japan’s 4th cosmic x-ray space mission and the second collaboration between NASA and ISAS to launch into orbit around the Earth, the Advanced Satellite for Cosmology & Astrophysics (ASCA) opened a new window on the x-ray universe. Designed and engineered to conduct x-ray spectroscopy ASCA (formally Astro-D) paved a path for NASA’s Chandra X-ray Observatory, XMM-Newton and Japan’s Suzaku (Astro-EII) to study x-ray emissions across the night sky. This smaller eye on the x-ray universe was the perfect complement to ROSAT’s all-sky survey of around 150,000 x-ray sources and RXTE’s study of the different types observed. Making this little satellite an essential, pivotal mile marker during the human journey to the beginning of space and time. Combined, these space missions have an advanced human understanding of the high-energy universe and revealed mysteries keeping astronomers up at night and peering into the unknown x-ray universe at the cosmos beyond human imagination. 

photo3_3_e
After the success of HAKUCHO, Japan launched an X-ray astronomy satellite every four or five years: HINOTORI (solar X-ray) in 1981, TENMA in 1983, GINGA in 1987, and ASCA in 1993. Credits: JAXA.

ASCA (Astro-D) launched from Japan’s Kagoshima Space Center at the southern tip of Japan on Kyushu island on February 20, 1993, aboard ISAS’s fourth generation Mu launch system M-3sII. Orbiting at a distance from Earth at perigee of 525 and 615 at apogee, it took only 96 minutes on average for Astro-D to complete one revolution of its nearly circular path around the planet. During a lifespan lasting nearly 8 years, Japan’s little x-ray satellite provided the first images of x-ray emitting objects and detected x-rays from supernova SN 1993J in galaxy M81. The data it supplied allowed astronomers to reveal clues to the origin and formation of accreting binaries, the accretion disks of active galactic nuclei, galaxy clusters, and supernovae. 

Using combined data from a trio of orbiting X-ray telescopes, including NASA’s Chandra X-ray Observatory and the Japan-led Suzaku satellite, astronomers have obtained a rare glimpse of the powerful phenomena that accompany a still-forming star. A new study based on these observations indicates that intense magnetic fields drive torrents of gas into the stellar surface, where they heat large areas to millions of degrees. X-rays emitted by these hot spots betray the newborn star’s rapid rotation. Credits: JAXA/NASA.
Using combined data from a trio of orbiting X-ray telescopes, including NASA’s Chandra X-ray Observatory and the Japan-led Suzaku satellite (ASCA), astronomers have obtained a rare glimpse of the powerful phenomena that accompany a still-forming star. A new study based on these observations indicates that intense magnetic fields drive torrents of gas into the stellar surface, where they heat large areas to millions of degrees. X-rays emitted by these hot spots betray the newborn star’s rapid rotation. Credits: JAXA/NASA.

A tough little satellite says goodbye

This tough little satellite operated until July of 2000 when fluctuations in solar activity caused Earth’s atmosphere to expand. ASCA experienced friction caused by the thinner atmosphere and fell into an uncontrolled spin. Minimal satellite operations continued until around 14:20 on March 2, 2001, when Astro-D fell deeper into the planet’s gravity well and disappeared. Bringing to a close a chapter in space history on a little satellite that opened a window to the x-ray universe and revealed clues to a weird, weird, weird cosmos beyond human imagination. 

Follow the space journey of NASA

Learn more about the space discoveries of ISAS here

Learn more about the things ASCA told us about the origins and formation of galaxy clusters

Read about the things Astro-D told us about the accretion disks of active galactic nuclei here

Discover what Astro-D discovered about accreting binaries

Read about what x-ray emissions ASCA detected from supernova SN 1006 told astronomers about its origins and formation

Learn how 3-D printer technology is changing the way humans live and work in space.

Read and learn about the star navigation skills of incredible Polynesian islanders.

Read about a supermassive black hole astronomers found in an out of the way part of the cosmos.