mercredi 11 octobre 2017

Giant Exoplanet Hunters: Look for Debris Disks












JPL - Jet Propulsion Laboratory logo.

Oct. 11, 2017


Image above: This artist's rendering shows a large exoplanet causing small bodies to collide in a disk of dust. Image Credits: NASA/JPL-Caltech.

There's no map showing all the billions of exoplanets hiding in our galaxy -- they're so distant and faint compared to their stars, it's hard to find them. Now, astronomers hunting for new worlds have established a possible signpost for giant exoplanets.

A new study finds that giant exoplanets that orbit far from their stars are more likely to be found around young stars that have a disk of dust and debris than those without disks. The study, published in The Astronomical Journal, focused on planets more than five times the mass of Jupiter. This study is the largest to date of stars with dusty debris disks, and has found the best evidence yet that giant planets are responsible for keeping that material in check.

"Our research is important for how future missions will plan which stars to observe," said Tiffany Meshkat, lead author and assistant research scientist at IPAC/Caltech in Pasadena, California. Meshkat worked on this study as a postdoctoral researcher at NASA's Jet Propulsion Laboratory in Pasadena. "Many planets that have been found through direct imaging have been in systems that had debris disks, and now we know the dust could be indicators of undiscovered worlds."

Astronomers found the likelihood of finding long-period giant planets is nine times greater for stars with debris disks than stars without disks. Caltech graduate student Marta Bryan performed the statistical analysis that determined this result.

Researchers combined data from 130 single-star systems with debris disks detected by NASA's Spitzer Space Telescope, and compared them with 277 stars that do not appear to host disks. The two star groups were between a few million and 1 billion years old. Of the 130 stars, 100 were previously scanned for exoplanets. As part of this study, researchers followed up on the other 30 using the W. M. Keck Observatory in Hawaii and the European Southern Observatory's Very Large Telescope in Chile. They did not detect any new planets in those 30 systems, but the additional data helped characterize the abundance of planets in systems with disks.

The research does not directly resolve why the giant exoplanets would cause debris disks to form. Study authors suggest the massive gravity of giant planets causes small bodies called planetesimals to collide violently, rather than form proper planets, and remain in orbit as part of a disk.

"It's possible we don't find small planets in these systems because, early on, these massive bodies destroyed the building blocks of rocky planets, sending them smashing into each other at high speeds instead of gently combining," said co-author Dimitri Mawet, a Caltech associate professor of astronomy and a JPL senior research scientist.

On the other hand, giant exoplanets are easier to detect than rocky planets, and it is possible that there are some in these systems that have not yet been found.

Our own solar system is home to gas giants responsible for making "debris belts" -- the asteroid belt between Mars and Jupiter, shaped by Jupiter, and the Kuiper Belt, shaped by Neptune. Many of the systems Meshkat and Mawet studied also have two belts, but they are also much younger than ours -- up to 1 billion years old, compared to our system's present age of 4.5 billion years. The youth of these systems partly explains why they contain much more dust -- resulting from the collisions of small bodies -- than ours does.

One system discussed in the study is Beta Pictoris, which has been directly imaged from ground-based telescopes. This system has a debris disk, comets and one confirmed exoplanet. In fact, scientists predicted this planet's existence well before it was confirmed, based on the presence and structure of the prominent disk.

In a different scenario, the presence of two dust belts in a single debris disk suggests there are likely more planets in the system whose gravity maintains these belts, as is the case in the HR8799 system of four giant planets. The gravitational forces of giant planets nudge passing comets inward toward the star, which could mimic the period of our solar system's history about 4 billion years ago known as the Late Heavy Bombardment. Scientists think that during that period, the migration of Jupiter, Saturn, Uranus and Neptune deflected dust and small bodies into the Kuiper and asteroid belts we see today. When the Sun was young, there would have been a lot more dust in our solar system as well.

"By showing astronomers where future missions such as NASA's James Webb Space Telescope have their best chance to find giant exoplanets, this research paves the way to future discoveries," said Karl Stapelfeldt of JPL, chief scientist of NASA's Exoplanet Exploration Program Office and study co-author.

For more information about exoplanets, visit: https://exoplanets.nasa.gov

Image (mentioned), Text, Credits: NASA/Tony Greicius/JPL/Elizabeth Landau.

Greetings, Orbiter.ch

Secrets of hidden ice canyons revealed







ESA - Cryosat Mission logo.

11 October 2017

We are all aware that Antarctica’s ice shelves are thinning, but recently scientists have also discovered huge canyons cutting through the underbelly of these shelves, potentially making them even more fragile. Thanks to the CryoSat and Sentinel-1 missions, new light is being shed on this hidden world.

Antarctica is surrounded by ice shelves, which are thick bands of ice that extend from the ice sheet and float on the coastal waters. They play an important role in buttressing the ice sheet on land, effectively slowing the sheet’s flow as it creeps seaward.

Hidden ice canyons in the making

The ice sheet that covers Antarctica is, by its very nature, dynamic and constantly on the move. Recently, however, there has been a worrying number of reports about its floating shelves thinning and even collapsing, allowing the grounded ice inland to flow faster to the ocean and add to sea-level rise.

While scientists continue to study the changing face of Antarctica, monitor cracks in the surface of the ice that might signal the demise of a shelf and learn how these changes are affecting the biology of coastal waters, they are also aware of dramatic changes taking place below the surface, hidden from view.

There are huge inverted canyons in the underside of ice shelves, but little is known about how they form and how they affect the stability of the ice sheet.

One type is thought to be caused by subglacial water that drains from beneath the ice sheet and runs into the ocean. In this region, the ocean water is stratified, with the warmer water at the bottom. However, as the colder meltwater pours down into the ocean it then rises because it is less dense than the seawater – but as it rises it drags up the warm bottom water which causes the underbelly of the floating ice shelf to melt.

Ice shelf appears flat

Another type is thought to be caused by the way ocean water circulates under the shelf.

Scientists have been using ESA’s CryoSat to study changes in the surface of the ice shelf and the Copernicus Sentinel-1 mission to study how shelves flow to learn more about what’s going on hidden from view.

Their focus has been on the Dotson ice shelf in West Antarctica.

Noel Gourmelen from the University of Edinburgh said “We have found subtle changes in both surface elevation data from CryoSat and ice velocity from Sentinel-1 which shows that melting is not uniform, but has centred on a 5 km-wide channel that runs 60 km along the underside of the shelf.

“Unlike most recent observations, we think that the channel under Dotson is eroded by warm water, about 1°C, as it circulates under the shelf, stirred clockwise and upward by Earth’s rotation.

“Revisiting older satellite data, we think that this melt pattern has been taking place for at least the entire 25 years that Earth observation satellites have been recording changes in Antarctica.

Dotson ice shelf from Sentinel-1

“Over time, the melt has calved in a broad channel-like feature up to 200 m deep and 15 km across that runs the entire length of the underside of Dotson ice shelf.

“We can see that this canyon is deepening by about 7 m a year and that the ice above is heavily crevassed.

“Melt from Dotson ice shelf results in 40 billion tonnes of freshwater being poured into the Southern Ocean every year, and this canyon alone is responsible for the release of four billion tonnes – a significant proportion.

ESA's Ice Mission CryoSat

”The strength of an ice shelf depends on how thick it is. Since shelves are already suffering from thinning, these deepening canyons mean that fractures are likely to develop and the grounded ice upstream will flow faster than would be the case otherwise.

“It is the first time that we’ve been able to see this process in the making and we will now expand our area of interest to the shelves all around Antarctica to see how they are responding. We couldn’t do this without CryoSat and the European Commission’s Copernicus Sentinel missions,” added Dr Gourmelen.

Related links:

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

Access CryoSat data: https://earth.esa.int/web/guest/missions/esa-operational-eo-missions/cryosat

AGU Geophysical Research Letters Channelized melting drives thinning under Antarctic ice shelves: http://onlinelibrary.wiley.com/doi/10.1002/2017GL074929/abstract

University of Edinburgh–School of Geosciences: http://www.ed.ac.uk/geosciences

Support to Science Element: http://due.esrin.esa.int/stse/

Images, Video, Text, Credits: ESA/N. Gourmelen/contains modified Copernicus Sentinel data (2017), processed by A. Hogg/CPOM.

Greetings, Orbiter.ch

mardi 10 octobre 2017

This is a Test: Asteroid Tracking Network Observes Oct. 12 Close Approach










Asteroid Watch logo.

Oct. 10, 2017

On Oct. 12, a small asteroid designated 2012 TC4 will safely pass by Earth at a distance of approximately 26,000 miles (42,000 kilometers). This is a little over one-tenth the distance to the Moon and just above the orbital altitude of communications satellites. This encounter with TC4 is being used by asteroid trackers around the world to test their ability to operate as a coordinated international asteroid warning network.


Animation above: On Oct. 12, 2017, a small (15-30 meter) asteroid known as 2012 TC4 will safely fly past Earth. Based on continuing observations, scientists have determined that it will pass the Earth at a distance of about 26,000 miles (42,000 kilometers). Animation Credits: NASA/JPL-Caltech.

2012 TC4 is estimated to be 45 to 100 feet (15 to 30 meters) in size. Orbit prediction experts say the asteroid poses no risk of impact with Earth. Nonetheless, its close approach to Earth is an opportunity to test the ability of a growing global observing network to communicate and coordinate their optical and radar observations in a real scenario.

This asteroid was discovered by the Panoramic Survey Telescope and Rapid Response System (Pan-STARRS) on Hawaii back in 2012. Pan-STARRS conducts a near-Earth object (NEO) survey funded by NASA’s NEO Observations Program, a key element of NASA’s Planetary Defense Coordination Office. However, 2012 TC4 traveled out of the range of asteroid-tracking telescopes shortly after it was discovered.

Based on the observations they were able to make in 2012, asteroid trackers predicted that it should come back into view in the fall of 2017. Observers with the European Space Agency and the European Southern Observatory were the first to recapture 2012 TC4, in late July 2017, using one of their large 8-meter aperture telescopes.  Since then, observers around the world have been tracking the object as it approaches Earth and reporting their observations to the Minor Planet Center.

This “test” of what has become a global asteroid-impact early-warning system is a volunteer project, conceived and organized by NASA-funded asteroid observers and supported by the NASA Planetary Defense Coordination Office (PDCO).

As explained by Michael Kelley, program scientist and NASA PDCO lead for the TC4 observation campaign, “Asteroid trackers are using this flyby to test the worldwide asteroid detection and tracking network, assessing our capability to work together in response to finding a potential real asteroid-impact threat."

No asteroid currently known is predicted to impact Earth for the next 100 years.

Asteroids passing Earth. Image Credit: ESA

Asteroid TC4’s closest approach to Earth will be over Antarctica at 1:40 AM EDT. Tens of professionally run telescopes across the globe will be taking ground-based observations from visible to near-infrared to radar. Amateur astronomers may contribute more observations, but the asteroid will be very difficult for backyard astronomers to see, as current estimates are that it will reach a visual magnitude of only about 17 at its brightest, and it will be moving very fast across the sky.

Many of the observers who are participating in this exercise are funded by NASA’s NEO Observations Program but observers supported by other countries’ space agencies and space institutions around the world are now involved in the campaign.

Vishnu Reddy, an assistant professor at the University of Arizona's Lunar and Planetary Laboratory in Tucson, is leading the 2012 TC4 campaign. Reddy is principal investigator for a NASA-funded near-Earth asteroid characterization project. "This campaign is a team effort that involves more than a dozen observatories, universities and labs around the globe so we can collectively learn the strengths and limitations of our near-Earth object observation capabilities," he said. "This effort will exercise the entire system, to include the initial and follow-up observations, precise orbit determination, and international communications."

In September, asteroid observers were able to conduct a “pre-test” of a coordinated tracking for the close approach of a much larger asteroid known as 3122 Florence. Florence, one of the largest known NEOs, at 2.8 miles (4.5 kilometers) in size, passed by Earth on Sept. 1 at 18 times the distance to the Moon. Coordinated observations of this asteroid revealed, among other things, that Florence has two moons.

Related link:

Asteroids: https://www.nasa.gov/mission_pages/asteroids/main/index.html

NASA Planetary Defense Coordination Office (PDCO): https://www.nasa.gov/planetarydefense

Animation (mentioned), Image (mentioned), Text, Credits: NASA/Tricia Talbert.

Greetings, Orbiter.ch

Astronauts Back Inside Station After Second Spacewalk















ISS - Expedition 53 Mission patch / EVA - Extra Vehicular Activities patch.

October 10, 2017

Expedition 53 Commander Randy Bresnik and Flight Engineer Mark Vande Hei of NASA completed a 6 hour, 26 minute spacewalk at 2:22 p.m. EDT. The two astronauts lubricated components of the new latching end effector they installed in the previous spacewalk on the Canadarm2 robotic arm and replaced a faulty camera system.

They also completed a variety of additional tasks, including replacing a smudged lens cover and removing two handrails from outside the tranquility module in preparation for a future wireless antenna installation.


Image above: Astronaut Mark Vande Hei wraps up lubrication work on the latching end effector of the Canadarm2 robotic arm. Image Credit: NASA TV.

This was the second of three spacewalks planned for October. Bresnik will also lead the next spacewalk Oct. 18 joined by Flight Engineer Joe Acaba to continue the lubrication of the new end effector and to replace another camera system on the Destiny Lab.

Today’s spacewalk was the fourth for Bresnik’s career and the second for Vande Hei. The Oct. 18 spacewalk will mark the third of Acaba’s career.

Related links:

Expedition 53: https://www.nasa.gov/mission_pages/station/expeditions/expedition53/index.html

Space Station Research and Technology: https://www.nasa.gov/mission_pages/station/research/index.html

International Space Station (ISS): https://www.nasa.gov/mission_pages/station/main/index.html

Image (mentioned), Text, Credits: NASA/Mark Garcia.

Best regards, Orbiter.ch

Where Does the Sand Come From?












NASA - Mars Reconnaissance Orbiter (MRO) logo.

Oct. 10, 2017


This image from NASA's Mars Reconnaisance Orbiter (MRO) shows one possible place where sand grains are being produced on Mars today. Discovered in images from the Context Camera, this region exhibits dark material that is being eroded from dark layers in the bedrock of a semicircular depression near the boundary of the Southern highlands and the Northern lowlands. Downslope lineations support the notion that these dark sediments are derived locally, and did not accumulate here by coincidence because of the winds.

The grains of sand that make up sand dunes on Earth and Mars have a hazardous existence because of the way that they travel. Wind-blown sand is lifted above the surface of each planet before crashing onto the ground and bouncing in a sequence of repeated hops, a process called saltation.

Sand grains can also roll along the ground as they are blown by the wind, and they are also jostled by other sand gains that are similarly flying across the surface. All of these repeated impacts tend to wear down the sand grains, smoothing them into a more spherical shape and breaking off small fragments that supply the vast dust deposits of Mars. This process (known as comminution) ultimately destroys sand grains and limits the length of time that the particles exist. The fact that we see active sand dunes on Mars today requires that sand particles must be resupplied to replace the grains that are lost over time. Where are the modern day sources of sand on Mars?

Mars Reconnaissance Orbiter (MRO)

The University of Arizona, Tucson, operates HiRISE, which was built by Ball Aerospace & Technologies Corp., Boulder, Colo. NASA's Jet Propulsion Laboratory, a division of Caltech in Pasadena, California, manages the Mars Reconnaissance Orbiter Project for NASA's Science Mission Directorate, Washington.

Mars Reconnaissance Orbiter (MRO): http://www.nasa.gov/mission_pages/MRO/main/index.html

Image, Text, Credits: NASA/Tony Greicius/JPL-Caltech/Univ. of Arizona.

Greetings, Orbiter.ch

Two Astronauts Begin Second Spacewalk of Mission














ISS - Expedition 53 Mission patch / EVA - Extra Vehicular Activities patch.

October 10, 2017

Two NASA astronauts switched their spacesuits to battery power this morning at 7:56 a.m., EDT aboard the International Space Station to begin a spacewalk planned to last about 6.5 hours. Live coverage is available on NASA Television and the agency’s website: http://www.nasa.gov/live


Image above: NASA astronaut Randy Bresnik (bottom center) is dwarfed by a set of basketball court-sized solar arrays and the Earth in the background during a spacewalk on Oct. 5, 2017. Image Credit: NASA.

Expedition 53 Commander Randy Bresnik and Flight Engineer Mark Vande Hei of NASA will lubricate components of the new latching end effector they installed on the Canadarm2 robotic arm in their first excursion Oct. 5. They will also replace a faulty camera system in the 204th spacewalk in support of assembly and maintenance in station history. This is the fourth spacewalk of Bresnik’s career and the second for Vande Hei.

A third spacewalk to continue the lubrication of the new end effector and to replace another camera system on the Destiny Lab is planned for Bresnik and Flight Engineer Joe Acaba of NASA Oct. 18.

Related links:

Expedition 53: https://www.nasa.gov/mission_pages/station/expeditions/expedition53/index.html

Space Station Research and Technology: https://www.nasa.gov/mission_pages/station/research/index.html

International Space Station (ISS): https://www.nasa.gov/mission_pages/station/main/index.html

Image (mentioned), Text, Credits: NASA/Mark Garcia.

Best regards, Orbiter.ch

lundi 9 octobre 2017

Successful Launch of H-IIA rocket carrying Michibiki 4












JAXA - Quasi-Zenith Satellite System (QZSS) patch.

October 9, 2017

Successful Launch, H-IIA Launch Vehicle No. 36 Encapsulating MICHIBIKI No. 4

H-IIA rocket carrying Michibiki 4 launch

Mitsubishi Heavy Industries, Ltd. and JAXA successfully launched H-IIA Launch Vehicle No. 36 (H-IIA・F36) which encapsulates MICHIBIKI No. 4, Quasi-Zenith Satellite System; at 7:01:37a.m., 2017 (JST) from the JAXA Tanegashima Space Center.

Quasi-Zenith Satellite MICHIBIKI 4/H-IIA Launch Vehicle No. 36 launch replay

The launch and flight of H-IIA Launch Vehicle No. 36 proceeded as planned. So did the separation of MICHIBIKI No. 4, which was confirmed at approximately 28 minutes and 20 seconds after liftoff.

Michibiki navigation satellite

Michibiki 4 navigation spacecraft, the fourth member of Japan’s Quasi-Zenith Satellite System. Japan plans to initially deploy four QZSS satellites to augment regional navigation services over Japan and neighboring countries provided by the U.S. Global Positioning System.

Related links:

MHI Launch Services: http://h2a.mhi.co.jp/en/index.html

H-IIA Launch Vehicle: http://global.jaxa.jp/projects/rockets/h2a/

Quashi-Zenith Satellite System (QZSS): http://qzss.go.jp/en/

Japan Aerospace Exploration Agency (JAXA): http://global.jaxa.jp/

Images, Video, Text, Credits: Japan Aerospace Exploration Agency (JAXA)/National Research and Development Agency/Mitsubishi Heavy Industries, Ltd.

Best regards, Orbiter.ch