mardi 6 janvier 2015

Kepler Marks 1,000th Exoplanet Discovery, Uncovers More Small Worlds in Habitable Zones












NASA - Kepler Mission patch.

January 6, 2015


Image above: NASA Kepler's Hall of Fame: Of the more than 1,000 verified planets found by NASA's Kepler Space Telescope, eight are less than twice Earth-size and in their stars' habitable zone. All eight orbit stars cooler and smaller than our sun. The search continues for Earth-size habitable zone worlds around sun-like stars.

How many stars like our sun host planets like our Earth? NASA’s Kepler Space Telescope continuously monitored more than 150,000 stars beyond our solar system, and to date has offered scientists an assortment of more than 4,000 candidate planets for further study -- the 1,000th of which was recently verified.

Using Kepler data, scientists reached this millenary milestone after validating that eight more candidates spotted by the planet-hunting telescope are, in fact, planets. The Kepler team also has added another 554 candidates to the roll of potential planets, six of which are near-Earth-size and orbit in the habitable zone of stars similar to our sun.

Three of the newly-validated planets are located in their distant suns’ habitable zone, the range of distances from the host star where liquid water might exist on the surface of an orbiting planet. Of the three, two are likely made of rock, like Earth.

"Each result from the planet-hunting Kepler mission's treasure trove of data takes us another step closer to answering the question of whether we are alone in the Universe," said John Grunsfeld, associate administrator of NASA’s Science Mission Directorate at the agency’s headquarters in Washington. “The Kepler team and its science community continue to produce impressive results with the data from this venerable explorer."

To determine whether a planet is made of rock, water or gas, scientists must know its size and mass. When its mass can’t be directly determined, scientists can infer what the planet is made of based on its size.

Two of the newly validated planets, Kepler-438b and Kepler-442b, are less than 1.5 times the diameter of Earth. Kepler-438b, 475 light-years away, is 12 percent bigger than Earth and orbits its star once every 35.2 days. Kepler-442b, 1,100 light-years away, is 33 percent bigger than Earth and orbits its star once every 112 days.

Both Kepler-438b and Kepler-442b orbit stars smaller and cooler than our sun, making the habitable zone closer to their parent star, in the direction of the constellation Lyra. The research paper reporting this finding has been accepted for publication in The Astrophysical Journal.

NASA’s Kepler Space Telescope

"With each new discovery of these small, possibly rocky worlds, our confidence strengthens in the determination of the true frequency of planets like Earth," said co-author Doug Caldwell, SETI Institute Kepler scientist at NASA's Ames Research Center at Moffett Field, California. "The day is on the horizon when we’ll know how common temperate, rocky planets like Earth are.”

With the detection of 554 more planet candidates from Kepler observations conducted May 2009 to April 2013, the Kepler team has raised the candidate count to 4,175. Eight of these new candidates are between one to two times the size of Earth, and orbit in their sun's habitable zone. Of these eight, six orbit stars that are similar to our sun in size and temperature. All candidates require follow-up observations and analysis to verify they are actual planets.

“Kepler collected data for four years -- long enough that we can now tease out the Earth-size candidates in one Earth-year orbits”, said Fergal Mullally, SETI Institute Kepler scientist at Ames who led the analysis of a new candidate catalog. “We’re closer than we’ve ever been to finding Earth twins around other sun-like stars. These are the planets we’re looking for”.

These findings also have been submitted for publication in The Astrophysical Journal Supplement.

Work is underway to translate these recent discoveries into estimates of how often rocky planets appear in the habitable zones of stars like our sun, a key step toward NASA's goal of understanding our place in the universe.

Scientists also are working on the next catalog release of Kepler’s four-year data set. The analysis will include the final month of data collected by the mission and also will be conducted using sophisticated software that is more sensitive to the tiny telltale signatures of small Earth-size planets than software used in the past.

Ames is responsible for Kepler's mission operations, ground system development and science data analysis. NASA's Jet Propulsion Laboratory in Pasadena, California, managed Kepler mission development. Ball Aerospace & Technologies Corp. in Boulder, Colorado, developed the Kepler flight system and supports mission operations with the Laboratory for Atmospheric and Space Physics at the University of Colorado in Boulder. The Space Telescope Science Institute in Baltimore archives, hosts and distributes Kepler science data. Kepler is NASA's 10th Discovery Mission and was funded by the agency's Science Mission Directorate in Washington.

For more information about the Kepler mission, visit: http://www.nasa.gov/kepler

Images, Text, Credits: NASA/Felicia Chou/Ames Research Center/Michele Johnson.

Greetings, Orbiter.ch

New Years at Mars












ESA - Mars Express Mission patch.

January 6, 2015


This image was taken on 2 January just after midday GMT, and is one of the first of the Red Planet this year from the low-resolution Visual Monitoring Camera – the ‘Mars Webcam’ – on ESA’s Mars Express orbiter.

It was recorded from an altitude of about 10 000 km and shows the south pole of Mars, including the ice cap of mostly solid carbon dioxide.

The camera is not a scientific instrument but originally captured the separation of the Beagle lander. It now provides images of Mars, including crescent views of the planet, not obtainable from Earth.

The images are acquired and downlinked to Earth on a substantially automated cycle, and original images are posted automatically into a dedicated Flickr channel: http://www.flickr.com/esa_marswebcam/

More via the blog: http://blogs.esa.int/vmc

Related links:

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

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

Image, Text, Credits: ESA - European Space Agency, CC BY-SA 3.0 IGO.

Cheers, Orbiter.ch

Hubble captures the Pillars of Creation twenty years on












ESA - Hubble Space Telescope logo.

6 January 2015

Revisiting an icon

New view of the Pillars of Creation — visible

The NASA/ESA Hubble Space Telescope has captured many breathtaking images of the Universe, but one snapshot stands out from the rest: the Eagle Nebula’s Pillars of Creation. In 1995 Hubble’s iconic image revealed never-before-seen details in the giant columns and now the telescope is kickstarting its 25th year in orbit with an even clearer, and more stunning, image of these beautiful structures.

New view of the Pillars of Creation — infrared

The three impressive towers of gas and dust captured in this image are part of the Eagle Nebula, otherwise known as Messier 16. Although such features are not uncommon in star-forming regions, the Messier 16 structures are by far the most photogenic and evocative ever captured. The Hubble image of the pillars taken in 1995 is so popular that it has appeared in film and television, on tee-shirts and pillows, and even on postage stamps.

The Pillars of Creation — visible and infrared comparison

Now Hubble has revisited the famous pillars, capturing the multi-coloured glow of gas clouds, wispy tendrils of dark cosmic dust, and the rust-coloured elephants’ trunks with the newer Wide Field Camera 3, installed in 2009. The visible-light image builds on one of the most iconic astronomy images ever taken and provides astronomers with an even sharper and wider view.

The Pillars of Creation — 1995 and 2015 comparison

In addition to this new visible-light image, Hubble has also produced a bonus image. This image is taken in infrared light, which penetrates much of the obscuring dust and gas and unveils a more unfamiliar view of the pillars, transforming them into wispy silhouettes set against a background peppered with stars. Here newborn stars, hidden in the visible-light view, can be seen forming within the pillars themselves [1].

Digitized Sky Survey Image of the Eagle Nebula

Although the original image was dubbed the "Pillars of Creation", this new image hints that they are also pillars of destruction. The dust and gas in these pillars is seared by intense radiation from the young stars forming within them, and eroded by strong winds from massive nearby stars. The ghostly bluish haze around the dense edges of the pillars in the visible-light view is material that is being heated by bright young stars and evaporating away.

Pillars of Creation

With these new images come better contrast and clearer views of the region. Astronomers can use these new images to study how the physical structure of the pillars is changing over time. The infrared image shows that the reason the pillars exist is because the very ends of them are dense, and they shadow the gas below them, creating the long, pillar-like structures. The gas in between the pillars has long since been blown away by the winds from a nearby star cluster.

Pan over Pillars of Creation — visible

At the top edge of the left-hand pillar, a gaseous fragment has been heated up and is flying away from the structure, highlighting the violent nature of star-forming regions.

Pan over Pillars of Creation — Infrared

These massive stars may be slowly destroying the pillars but they are also the reason Hubble sees the structures at all. They radiate enough ultraviolet light to illuminate the area and make the clouds of oxygen, hydrogen and sulphur glow.

The Pillars of Creation — fade from visible to infrared

Although structures like these exist throughout the Universe, the Pillars of Creation — at a distance of 6500 light-years away — provide the best, and most dramatic, example. Now, these images have allowed us to see them more clearly than ever, proving that at 25 years of age, Hubble is still going strong.

Zoom into Pillars of Creation

This image and the associated results were presented today at the 225th meeting of the American Astronomical Society in Seattle, Washington, USA.

3D exploration of Pillars of Creation

Tour of Eagle Nebula

Notes:

[1] There is evidence to suggest that the Sun formed in a similar turbulent star-forming region to the one we see in this image.
Notes for editors

The Hubble Space Telescope is a project of international cooperation between ESA and NASA.

Links:

Images of Hubble: http://www.spacetelescope.org/images/archive/category/spacecraft/

Link to NASA release: http://hubblesite.org/newscenter/archive/releases/2015/01/

Hubblecast 82: New view of the Pillars of Creation: http://www.spacetelescope.org/videos/heic1501a/

Images, Text, Credits: ESA/NASA/Hubble and the Hubble Heritage Team/ESO/Digitized Sky Survey 2. Acknowledgment: Davide De Martin/Jeff Hester and Paul Scowen (Arizona State University)/Videos:  NASA, the Hubble Heritage Team, ESO, M. McCaughrean & M. Andersen (AIP)/Music: movetwo.

Best regards, Orbiter.ch

lundi 5 janvier 2015

NASA’s Chandra Detects Record-Breaking Outburst from Milky Way’s Black Hole












NASA - Chandra X-ray Observatory patch.

January 5, 2015

Astronomers have observed the largest X-ray flare ever detected from the supermassive black hole at the center of the Milky Way galaxy. This event, detected by NASA’s Chandra X-ray Observatory, raises questions about the behavior of this giant black hole and its surrounding environment.

The supermassive black hole at the center of our galaxy, called Sagittarius A*, or Sgr A*, is estimated to contain about 4.5 million times the mass of our sun.

Astronomers made the unexpected discovery while using Chandra to observe how Sgr A* would react to a nearby cloud of gas known as G2.

“Unfortunately, the G2 gas cloud didn’t produce the fireworks we were hoping for when it got close to Sgr A*,” said lead researcher Daryl Haggard of Amherst College in Massachusetts. “However, nature often surprises us and we saw something else that was really exciting.”

On Sept. 14, 2013, Haggard and her team detected an X-ray flare from Sgr A* 400 times brighter than its usual, quiet state. This “megaflare” was nearly three times brighter than the previous brightest X-ray flare from Sgr A* in early 2012. After Sgr A* settled down, Chandra observed another enormous X-ray flare 200 times brighter than usual on Oct. 20, 2014.


Image above: Astronomers have detected the largest X-ray flare ever from the supermassive black hole at the center of the Milky Way using NASA’s Chandra X-ray Observatory. This event was 400 times brighter than the usual X-ray output from the black hole. Credit: NASA/CXC/Northwestern Univ/D.Haggard et al. X-ray Image Credit: NASA/CXC/Stanford/I. Zhuravleva et al.

Astronomers estimate that G2 was closest to the black hole in the spring of 2014, 15 billion miles away. The Chandra flare observed in September 2013 was about a hundred times closer to the black hole, making the event unlikely related to G2.

The researchers have two main theories about what caused Sgr A* to erupt in this extreme way. The first is that an asteroid came too close to the supermassive black hole and was torn apart by gravity. The debris from such a tidal disruption became very hot and produced X-rays before disappearing forever across the black hole's point of no return, or event horizon.

“If an asteroid was torn apart, it would go around the black hole for a couple of hours – like water circling an open drain – before falling in,” said co-author Fred Baganoff of the Massachusetts Institute of Technology in Cambridge, Massachusetts. “That’s just how long we saw the brightest X-ray flare last, so that is an intriguing clue for us to consider.”

If this theory holds up, it means astronomers may have found evidence for the largest asteroid to produce an observed X-ray flare after being torn apart by Sgr A*.

A second theory is that the magnetic field lines within the gas flowing towards Sgr A* could be tightly packed and become tangled. These field lines may occasionally reconfigure themselves and produce a bright outburst of X-rays. These types of magnetic flares are seen on the sun, and the Sgr A* flares have similar patterns of intensity.

“The bottom line is the jury is still out on what’s causing these giant flares from Sgr A*,” said co-author Gabriele Ponti of the Max Planck Institute for Astrophysics in Garching, Germany. “Such rare and extreme events give us a unique chance to use a mere trickle of infalling matter to understand the physics of one of the most bizarre objects in our galaxy.”

In addition to the giant flares, the G2 observing campaign with Chandra also collected more data on a magnetar: a neutron star with a strong magnetic field, located close to Sgr A*. This magnetar is undergoing a long X-ray outburst, and the Chandra data are allowing astronomers to better understand this unusual object.

NASA’s Chandra X-ray Observatory.Image Credit: NASA/CXC

These results were presented at the 225th meeting of the American Astronomical Society being held in Seattle.  NASA's Marshall Space Flight Center in Huntsville, Alabama, manages the Chandra program for NASA's Science Mission Directorate in Washington. The Smithsonian Astrophysical Observatory in Cambridge, Massachusetts, controls Chandra's science and flight operations.

NASA is exploring our solar system and beyond to understand the universe and our place in it. The agency seeks to unravel the secrets of our universe, its origins and evolution, and search for life among the stars.

An interactive image, a podcast, and a video about the findings are available at: http://chandra.si.edu

For more Chandra images, multimedia and related materials, visit: http://www.nasa.gov/chandra

Images (mentioned), Text, Credits: NASA/Felicia Chou/Marshall Space Flight Center/Janet Anderson/Chandra X-ray Center/Megan Watzke.

Greetings, Orbiter.ch

Astronaut feels the force












ESA - Space Robotics logo.

5 January 2015

In a milestone for space robotics, the International Space Station has hosted the first full run of ESA’s experiment with a force-reflecting joystick.

Think of the kind of tasks you can do with your hands without looking down, such as typing or tying laces. These are helped by ‘force feedback’ – the touch you feel in your hands and fingertips.

Force-feedback experiment on Space Station

Harnessing that sensation for robotics would extend the human sense of touch to space or other remote areas, making robotic control much more natural and easy.

Ultimately, robots could work thousands or tens of thousands of kilometres away, yet perform tasks of equal complexity to those a human operator could manage with objects immediately at hand.

NASA crewmember Barry Wilmore operated the force-feedback joystick to gather information on physiological factors such as sensitivity of feeling and perception limits. He finished a first run on New Year’s Eve.

The deceptively simple-looking lever is connected to a servomotor that can withstand any force an astronaut operator might unleash on it, while generating forces that the astronaut will feel in turn – just like a standard video gaming joystick as a player encounters an in-game obstacle. The joystick measures such forces at a very high resolution.

Body-mounted astronaut joystick

To stop the weightless users being pushed around by the force, the ‘Haptics-1’ experiment can be mounted either to a body harness or be fixed to the Station wall.

“With Haptics-1 we are paving the way towards an entirely new type of combined human–robot mission,” explains André Schiele, the experimenter and founder of ESA’s Telerobotics and Haptics Laboratory.

“We are investigating in fine detail the limits of human perception and ability to apply fine forces and manipulation with their limbs and hands in a weightless environment.

“This allows us to understand the technology boundaries for advanced robotic equipment to support human astronauts in space when performing remote robotic control tasks.

“In addition to measuring physiological factors, Haptics-1 is providing important insights into how force-reflection from a remote robotic system changes human perception in space.

“With these measurements, advanced robotic control equipment can be better designed to reflect the realities of human manipulation through a robotic interface in a weightless environment.”

Experiment setup

“Haptics-1 marks the first time a force-reflecting device has been used in space. Before today, ESA, NASA or any other spacefaring nation has gained such experience in this domain.”

In future, orbiting astronauts might be operating a rover in real time on a planet, allowing human dexterity and intuition to help explore an alien environment without the expense and danger of landing.

Such advanced robotic remote control also has many potential terrestrial applications working at sites that are inaccessible or dangerous to humans, such as deep under water or within contaminated zones.

Related links:

Telerobotics and Haptics Laboratory: http://esa-telerobotics.net/

Telerobotics flight experiments: http://esa-telerobotics.net/meteron/flight-experiments

ESA Bulletin article on Meteron: http://www.esa.int/About_Us/ESA_Publications/ESA_Publications_Bulletin/ESA_i_Bulletin_i_147_August_2011

@ESATelerobotics: https://twitter.com/esatelerobotics

Images, Text, Credit: ESA.

Best regards, Orbiter.ch

Is Europe an underestimated sink for carbon dioxide?











ESA - European Space Agency patch.

5 January 2015

A new study using satellite data suggests that Europe’s vegetation extracts more carbon from the atmosphere than previously thought.

Atmospheric carbon dioxide is the most important human-made greenhouse gas responsible for global warming. Large areas of vegetation, such as forests, are considered carbon ‘sinks’ because they assist in removing carbon dioxide from the atmosphere.

European carbon uptake

Without the natural carbon cycle, atmospheric carbon dioxide concentration would be much higher and, consequently, the effects of global warming would be much larger.

Current knowledge about the European terrestrial biospheric carbon sink mostly comes from ‘inverse modelling’ studies using in situ measurements, and from inventories of biomass and ecosystem studies.

To determine the amount of carbon dioxide absorbed by Europe’s vegetation, scientists from the University of Bremen analysed carbon dioxide concentration measurements from satellites.

The data were generated by the GHG-CCI  project under ESA's Climate Change Initiative, Japan’s National Institute for Environmental Studies and NASA’s Jet Propulsion Laboratory. It included eight years of data from the Sciamachy instrument on ESA’s Envisat mission, and one year of data from Japan’s greenhouse gas-observing satellite, GOSAT.

Each satellite dataset was generated using a different method, ensuring that the results did not depend on a potential calculation problem specific to a single method. All calculations showed that Europe’s terrestrial vegetation – between the Atlantic Ocean and Ural mountains – absorbs about twice the amount of carbon per year more than previous estimates.

Average satellite carbon dioxide concentrations over Europe

The use of in situ carbon dioxide measurements in inverse modelling yielded similar results as measurements derived from biomass inventories. But the in situ stations are sparsely distributed across western Europe. Satellite measurements, however, cover the entire European continent and acquire spatially denser data.

“Our estimate is at the high end of the uncertainty range estimated by previous studies, which did not use any satellite carbon dioxide observations,” said Maximilian Reuter, lead author of the study.

“Using satellite data for this application is challenging, as even small measurement errors can result in significant errors of the strength of the inferred carbon source or sink. This is because the amount of carbon dioxide in our atmosphere is already quite high, so that even a large source or sink of carbon dioxide only results in a quite small relative change of the atmospheric carbon dioxide amount which we are measuring.”

The study was published recently in Atmospheric Chemistry and Physics: http://www.atmos-chem-phys.net/14/13739/2014/acp-14-13739-2014.html

Frederic Chevallier, a climate modeller working at France’s Laboratoire des Sciences du Climat et de l’Environnement, and leader of the GHG-CCI’s Climate Research Group, notes, “The various satellite products tested in this study all suggest a large continental sink. However, differences in the inner-European carbon dioxide patterns should be subject to future research.

“Scientists agree that there are still open questions on carbon sinks, especially for the northern hemisphere, and that more research has to be performed on understanding the differences found by using satellite and in-situ carbon dioxide measurements and biomass inventory information.”

A future extended in-situ network in Europe, along with NASA’s recently launched Orbiting Carbon Observatory-2 and the possible CarbonSat mission – one of the two candidates for ESA’s eighth Earth Explorer – will potentially provide the data to continue such research to clarify these open questions on Europe’s and the global carbon budget.

Related links:

GHG-CCI  project: http://www.esa-ghg-cci.org/

Study: Satellite-inferred European carbon sink larger than expected: http://www.atmos-chem-phys.net/14/13739/2014/acp-14-13739-2014.html

University of Bremen, Institute of Environmental Physics: http://www.iup.unibremen.de/

ESA's Climate Change Initiative (CCI): http://www.esa-cci.org/

National Institute for Environmental Studies: http://www.nies.go.jp/gaiyo/index-e.html

NASA Jet Propulsion Laboratory: http://www.nasa.gov/centers/jpl/home/index.html

IPCC, AR5, ‘The Physical Science Basis’, Section 6: Carbon and Other Biogeochemical Cycles 2013: http://www.ipcc.ch/pdf/assessment-report/ar5/wg1/WG1AR5_Chapter06_FINAL.pdf

Related missions:

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

OCO-2: http://oco.jpl.nasa.gov/mission/

GOSAT: http://www.jaxa.jp/projects/sat/gosat/index_e.html

CarbonSat at University of Bremen: http://www.iup.uni-bremen.de/carbonsat/

Images, Text, Credits: ESA/University of Bremen.

Greetings, Orbiter.ch

Chasms and cliffs on Mars












ESA - Mars Express mission patch.

5 January 2015

(Click on the image for enlarge)

Although Mars is a very alien planet, some aspects of its geology are surprisingly familiar. This Mars Express image shows a snippet of a region of Mars filled with cliffs, trenches, faults, giant plateaus and volcanoes.

The flowing cracks and fault-like lines in this image form part of the Claritas Rupes escarpment, a 950 km-long network of steep cliffs and sloping outcrops. This escarpment lies within a larger geological system named Claritas Fossae, a weaving network of ‘grabens’ (a German term meaning ditch or trench) that stretches for some 2000 km.

The many chasms, fractures and cracks in this area are thought to have been caused by stress in the planet’s crust as it stretched and pulled apart, triggered by the formation of a nearby raised mound known as the Tharsis Bulge.

This bulge, located within the volcanic Tharsis region, extends to a height of about 10 km at its peak. Its violent formation caused parts of the crust to crack and shift, sliding into depressions and gaps, forming a distinctive pattern of geological features such as sunken grabens and raised blocks known as ‘horsts’. These two features can be very roughly imagined as an ‘M’ shape – grabens form the bottom of the central dip, while horsts form the two uppermost tips.

Similar patterns can be found on Earth around the Upper Rhine Valley between Basel in Switzerland, and Karlsruhe in Germany, or the Eger Graben in the Czech Republic, near the Ore Mountains.

Prominent examples of terrestrial grabens include California’s Death Valley, and the Dead Sea depression in the Jordan Rift Valley. Examples of horsts include France’s Vosges Mountains, and the Palestine Plateau.

Claritas Rupes forms the eastern boundary of the Tharsis region. This region contains some of the largest volcanoes in the Solar System, including the famous Olympus Mons, which stands some three times the height of Earth’s Mount Everest.

Mars Express spacecraft

This image was acquired by the High Resolution Stereo Camera of Mars Express on 30 November 2013 at a resolution of about 14 m per pixel. It was first published on 13 February 2014 on the DLR German Aerospace Center and Freie Universität Berlin websites.

Related links:

Chasms and cliffs on Mars - DLR German Aerospace Center: http://www.dlr.de/dlr/en/desktopdefault.aspx/tabid-10453/651_read-9514/year-all/#/gallery/13644

Chasms and cliffs on Mars -  Freie Universität Berlin: http://www.geo.fu-berlin.de/en/geol/fachrichtungen/planet/press/claritas1/index.html

For more information about Mars Express, visit: http://www.esa.int/Our_Activities/Space_Science/Mars_Express

Images, Text, Credits: ESA/DLR/FU Berlin.

Cheers, Orbiter.ch