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Wednesday, 28 December 2016
NASA Preps for Space Station Power Upgrade Spacewalks; Live NASA TV Coverage
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Saturday, 24 December 2016
NASA Administrator Remembers NASA Scientist, Astronaut Piers Sellers
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Friday, 23 December 2016
Once Upon a Time: The amazing adventures of Rosetta and Philae
Watch the amazing cartoon adventures of Rosetta and Philae, now back-to-back in one special feature-length production.
Find out how Rosetta and Philae first got inspired to visit a comet, and follow them on their incredible ten-year journey through the Solar System to their destination, flying around planets and past asteroids along the way. Watch as Philae tries to land on the comet and deals with some unexpected challenges! Learn about the fascinating observations that Rosetta made as she watched the comet change before her eyes as they got closer to the Sun and then further away again. Finally, wish Rosetta farewell, as she, too, finishes her amazing adventure on the surface of the comet. Keep watching for one last surprise!
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German version coming soon!
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Rosetta’s complete journey – animation
Now in one complete animation: Rosetta’s trajectory around Comet 67P/Churyumov–Gerasimenko, from arrival to mission end.
The animation begins on 31 July 2014, during Rosetta’s final approach to the comet after its ten-year journey through space. The spacecraft arrived at a distance of 100 km on 6 August, from where it gradually approached the comet and entered initial mapping orbits that were needed to select a landing site for Philae. These observations also enabled the first comet science of the mission.
The manoeuvres in the lead up to, during and after Philae’s release on 12 November are seen, before Rosetta settled into longer-term science orbits.
In February and March 2015 the spacecraft made several flybys. One of the closest triggered a ‘safe mode’ that forced it to retreat temporarily until it was safe to draw gradually closer again.
The comet’s increased activity in the lead up to and after perihelion in August 2015 meant that Rosetta remained well beyond 100 km for several months.
In June 2015, contact was restored with Philae again – albeit temporary, with no permanent link able to be maintained, despite a series of dedicated trajectories flown by Rosetta for several weeks.
Following the closest approach to the Sun, Rosetta made a dayside far excursion some 1500 km from the comet, before re-approaching to closer orbits again, enabled by the reduction in the comet’s activity.
In March–April 2016 Rosetta went on another far excursion, this time on the night side, followed by a close flyby and orbits dedicated to a range of science observations.
In early August the spacecraft started flying elliptical orbits that brought it progressively closer to the comet. On 24 September Rosetta left its close, flyover orbits and switched into the start of a 16 x 23 km orbit that was used to prepare and line up for the final descent.
On the evening of 29 September Rosetta manoeuvred onto a collision course with the comet, beginning the final, slow descent from an altitude of 19 km. It collected scientific data throughout the descent and gently struck the surface at 10:39 GMT on 30 September in the Ma’at region on the comet’s ‘head’, concluding the mission.
The trajectory shown in this animation is created from real data, but the comet rotation is not. Distances are given with respect to the comet centre (except for the zero at the end to indicate completion), but may not necessarily follow the exact comet distance because of natural deviations from the comet’s gravity and outgassing. An arrow indicates the direction to the Sun as the camera viewpoint changes during the animation.
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Impressions of Rosetta’s legacy
In September–October 2016, over 200 people contributed to the Rosetta Legacy campaign, sharing stories, images, videos, creations and experiences to convey what the mission had meant to them.
We decided to collect all contributions in an e-book, to keep a long-lasting record of the mission’s impact on a variety of public audiences. This publication presents a collection of these outstanding contributions and provides a taste of Rosetta’s legacy for fellow science communicators, scientists and engineers, educators, space enthusiasts – anyone who was fascinated by the mission.
The e-book (pdf, 33MB) is available here.
Thanks again to everyone who shared with us what the mission meant to them, and to all followers of Rosetta and Philae worldwide.
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Thursday, 22 December 2016
OSIRIS Data Release: March–May 2015
A new batch of thousands of images from Rosetta's OSIRIS imaging system have been released into ESA's Archive Image Browser and the Planetary Science Archive.
This latest OSIRIS data release comprises 2423 narrow-angle camera images and 4378 wide-angle camera images from the period 11 March – 24 May 2015. You can browse through the new images in the MTP 014, 015 and 016 albums here.
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Wednesday, 21 December 2016
Space Laser Reveals Boom-and-Bust Cycle of Polar Ocean Plants
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Tuesday, 20 December 2016
Voyager Mission Celebrates 30 Years Since Uranus
Humanity has visited Uranus only once, and that was 30 years ago. NASA's Voyager 2 spacecraft got its closest look at the mysterious, distant, gaseous planet on Jan. 24, 1986.
Voyager 2 sent back stunning images of the planet and its moons during the flyby, which allowed for about 5.5 hours of close study. The spacecraft got within 50,600 miles (81,500 kilometers) of Uranus during that time.
"We knew Uranus would be different because it's tipped on its side, and we expected surprises," said Ed Stone, project scientist for the Voyager mission, based at the California Institute of Technology, Pasadena. Stone has served as project scientist since 1972, continuing in that role today.
Uranus revealed itself to be the coldest planet known in our solar system, even though it's not the farthest from the sun. This is because it has no internal heat source.
Scientists determined that the atmosphere of Uranus is 85 percent hydrogen and 15 percent helium. There was also evidence of a boiling ocean about 500 miles (800 kilometers) below the cloud tops.
Scientists found that Uranus has a magnetic field different from any they had ever encountered previously. At Mercury, Earth, Jupiter and Saturn, the magnetic field is aligned approximately with the rotational axis.
"Then we got to Uranus and saw that the poles were closer to the equator," Stone said. "Neptune turned out to be similar. The magnetic field was not quite centered with the center of the planet."
This surface magnetic field of Uranus was also stronger than that of Saturn. Data from Voyager 2 helped scientists determine that the magnetic tail of Uranus twists into a helix stretching 6 million miles (10 million kilometers) in the direction pointed away from the sun. Understanding how planetary magnetic fields interact with the sun is a key part of NASA's goal to understand the very nature of space. Not only does studying the sun-planet connection provide information useful for space travel, but it helps shed light on the origins of planets and their potential for harboring life.
Voyager 2 also discovered 10 new moons (there are 27 total) and two new rings at the planet, which also proved fascinating. An icy moon called Miranda revealed a peculiar, varied landscape and evidence of active geologic activity in the past. While only about 300 miles (500 kilometers) in diameter, this small object boasts giant canyons that could be up to 12 times as deep as the Grand Canyon in Arizona. Miranda also has three unique features called "coronae," which are lightly cratered collections of ridges and valleys. Scientists think this moon could have been shattered and then reassembled.
Mission planners designed Voyager 2's Uranus encounter so that the spacecraft would receive a gravity assist to help it reach Neptune. In 1989, Voyager 2 added Neptune to its resume of first-ever looks.
"The Uranus encounter was very exciting for me," said Suzanne Dodd, project manager for Voyager, based at NASA's Jet Propulsion Laboratory, Pasadena, California, who began her career with the mission while Voyager 2 was en route to Uranus." It was my first planetary encounter and it was of a planet humanity had never seen up close before. Every new image showed more details of Uranus, and it had lots of surprises for the scientists. I hope another spacecraft will be sent to explore Uranus, to explore the planet in more detail, in my lifetime."
Voyager 2 was launched on Aug. 20, 1977, 16 days before its twin, Voyager 1. In August 2012, Voyager 1 made history as the first spacecraft to enter interstellar space, crossing the boundary encompassing our solar system's planets, sun and solar wind. Voyager 2 is also expected to reach interstellar space within the next several years.
The Voyagers were built by JPL, which continues to operate both spacecraft. JPL is a division of Caltech. For more information about the Voyager spacecraft, visit:
Media Contact
Elizabeth Landau
NASA's Jet Propulsion Laboratory, Pasadena, Calif.
818-354-6425
elizabeth.landau@jpl.nasa.gov
2016-019
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Saturday, 17 December 2016
NASA Television to Air Programs Celebrating Space Pioneer John Glenn
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Friday, 16 December 2016
New NASA Hurricane Tracking Mission on Track
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NASA Reveals the Unknown in 2016
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Thursday, 15 December 2016
Rosetta’s last words: science descending to a comet
On 30 September 2016, at 11:19:37 UT in ESA’s mission control, Rosetta’s signal flat-lined, confirming that the spacecraft had completed its incredible mission on the surface of Comet 67P/Churyumov-Gerasimenko some 40 minutes earlier and 720 million km from Earth. Rosetta was working up to the very end, collecting reams of science data as it descended towards a region of pits in the Ma’at region on the comet’s ‘head’.
Before we ‘retire’ the blog, we wanted to catch up with the instrument teams following this grand finale to find out how their instruments performed and if there were any surprises in Rosetta’s last ‘words’ from the comet.
First a reminder of the impact site: Rosetta was targeting a point within a 700 x 500 m ellipse, between two pits in the Ma’at region. Reconstruction of the final descent trajectory showed that the spacecraft touched down at 10:39:34 UT at the comet, only 33 metres away from the target point and just inside a shallow, ancient pit. This accuracy once again highlights the excellent work done by the flight dynamics specialists who supported the entire mission.
The touchdown site was subsequently named Sais after a town in Egypt where the Rosetta Stone, for which the mission was named, is thought to have been originally located.
Right before impact, one of Rosetta’s star trackers generated an event reporting a ‘Large Object’ in the field of view: this was the local comet ‘horizon’. Upon touchdown, the signal coming from Rosetta was lost, and mission operators believe that this was most likely caused by the high gain antenna immediately off-pointing from Earth at impact. No further telemetry was received subsequently, indicating that the planned safe mode and subsequent shut down of the spacecraft likely occurred successfully.
Rosetta’s last image was taken with the OSIRIS wide-angle camera about 20 m above the surface. Prior to that, much of the imaging campaign during the descent focused on the 130 metre-wide pit named Deir el-Medina, as shown by the blue ‘footprints’ in the plot below. As seen on 30 September, the camera succeeded in capturing detailed images of the inside of the pit and its walls. These images will be used to help understand the comet’s subsurface and thus its geological history. The trail of orange and red squares then reflects the change in pointing of the spacecraft’s camera towards the impact site at Sais.
Pressure rising
Several other Rosetta science instruments were in operation during the descent, including ROSINA’s Double Focusing Mass Spectrometer (DFMS) and Comet Pressure Sensor (COPS). Both recorded data “down to the ground”, as ROSINA Principal Investigator Kathrin Altwegg puts it. As reported on the day itself, and shown now in the plot below, ROSINA measured an increase in the surrounding gas pressure by more than a factor of 100 as the spacecraft neared the surface.
“We saw the gas velocity and ram pressure drop to zero before we reached the ground, suggesting there is an interesting acceleration of gas slightly away from the nucleus,” says Kathrin. “We also collected good data with the DFMS, and will be looking at which kind of atoms and molecules were present in the gas.”
Temperature measurements below the surface
Mark Hofstadter, Principal Investigator for the MIRO instrument, reported that good data were collected throughout the descent, with the last measurement made at 10:39:07 UT at the comet on 30 September 2016. The MIRO team think the spacecraft was about 20 m above the surface at this point.
“For the last two minutes of data, our sub-millimetre beam footprint on the surface was less than 20 cm in diameter,” says Mark.
During the descent, MIRO collected continuum emission data from the nucleus, providing temperature measurements ~1 and 5 cm below the surface.
“Over the last few hours, we see temperatures varying between about 80 and 160 K as our beam moved across the nucleus. We think these differences are due to topography and shadowing – but we still need to correlate the details with topographic models and OSIRIS images to confirm that.”
“We also noticed that the temperature of our telescope rose over the last couple hours of the mission. We haven’t figured out yet if that is due to the angle of the Sun changing, or if we were being heated by the nucleus as it filled more and more of the sky.”
Mark also told us that MIRO’s last spectroscopic measurement of water in the coma was made in a limb-observing mode on 27 September at 13:26 UT. This resulted in a very rough estimate of the global average water production rate at that time of about 10^24 molecules per second or the equivalent of two tablespoons (this preliminary estimate may be refined following further analysis). During its most active period in August 2015, estimates were in the region of two bathtubs’ worth of water every second.
Comet chameleon
The Alice instrument also made observations at ultraviolet wavelengths all the way to the surface. The final spectrum transmitted was an exposure that started at 10:20:16 and ended at 10:30:21 UT at the comet, about nine minutes before impact. The Alice team estimates that the final data were collected over a range of about 1000 to 500 metres altitude above the surface, with each row on the Alice instrument covering an average spatial scale of about four metres.
At the time of impact, Alice was 8.5 minutes into a 10-minute exposure. The last communication from Alice was a housekeeping packet received at 10:39:00 UT, about half a minute before impact. The housekeeping data included the count rate of the total ultraviolet flux over the Alice bandpass, which was being reported every 30 seconds, and which showed a steady increase in the UV flux during the descent.
Looking at the last hour of data from Alice as an overall averaged spectrum, the trend of the slope and lack of broad absorption features is very similar to previously published results. That is, Alice did not see significant differences in the surface composition at these high spatial resolutions when compared to observations over larger areas. There was also no obvious indication of small icy patches.
“Of course, these are very quick-look results that may change as we look more carefully at the data,” notes Joel Parker, Alice’s deputy Principal Investigator.
Data gathered from both Alice housekeeping and science telemetry indicated that the strength of a feature in the spectra nicknamed the ‘chameleon’ (the curved lines on the left side of the spectral image above) also increased throughout the descent.
“This feature has appeared throughout the mission with lots of variability, and we believe it is a result of dust and sometimes ions entering the instrument,” says Alan Stern, Alice’s Principal Investigator. “The morphology of the chameleon during this time period matches the morphologies seen during dusty time periods, indicating that there may have been an increase in nano-grain dust density as the altitude decreased.”
The last off-nucleus observation that Alice obtained of the comet’s coma was on 29 September, and was typical of limb spectra observed since the beginning of May 2016, when the comet was about 3 AU from the Sun. It showed that carbon dioxide outgassing was still on-going at the end of the mission, at greater distances from the Sun than seen when the comet was still approaching the Sun earlier in the mission.
“Overall, Alice worked exactly as planned throughout the end of mission and the descent, and provided an excellent dataset that will need much more detailed analysis,” adds Joel.
Steady solar wind and cometary plasma peak
The Rosetta Plasma Consortium sensors also enjoyed a good ride to the comet surface, with steady solar wind measurements.
“These data are actually very useful, providing us with a ‘quiet’ time reference profile covering a large altitude interval for a steady solar wind, which will help us calibrate the datasets that were took throughout the whole comet phase,” comments Hans Nilsson, Principal Investigator for the RPC-ICA sensor.
RPC-LAP and RPC-MIP both reported very low plasma densities through the descent, though slowly and evenly increasing, similar to that seen by ROSINA-COPS for neutral gas. However, the plasma reached a broad peak of up to about 100–150 cm^-3 (preliminary measurement) at about 2 km from surface, before dropping off again. This is as expected for a plasma originating from the neutral gas released by the comet: its density must be low at the surface since the molecules found there have just left the nucleus and have not had any time to become ionised.
“There is some plasma structure to be seen, but not much: this counts among the weakest ionospheres we have seen at the comet, but as may be expected in the northern hemisphere, which was winter at the time,” adds Anders Eriksson, Principal Investigator of the RPC-LAP sensor. “If there was any local outgassing from the Ma’at pits, it is at least not immediately striking in our data.”
RPC-IES demonstrated that the ions in the coma showed a modest increase in energy while the total flux of electrons decreased very near the comet, as expected and in line with the reduced coma density observations. The increase in observed coma ion energy could have been caused by an increase in negative spacecraft potential as the density decreased – something that is being looked into.
Finally, RPC-MAG made measurements down to a distance of about 11 m above the surface, showing no increase in the magnetic field with proximity. This confirms the finding, made during Philae’s landing in November 2014, that the comet is non-magnetic.
A dust free descent?
Of Rosetta’s three dust instruments, only GIADA was on during the descent, with MIDAS and COSIMA completing their missions in the days before. As it turns out, GIADA did not detect any dust, but this non-detection is itself an interesting observation.
“During the final descent, the environment was like a clean room!” remarked GIADA Principal Investigator, Alessandra Rotundi.
ROSINA, MIRO, and Alice team members confirmed the GIADA view. For example, the water production rate observed by MIRO over the region where Rosetta impacted was likely far too low to lift dust particles detectable by GIADA off the surface. Any dust grains present must have been very small indeed to evade detection, below GIADA’s limit of 50 micrometres diameter.
One last dust particle…
Even though COSIMA was off during the final descent, the instrument’s Principal Investigator, Martin Hilchenbach, told us that one last dust particle was collected during their final day of operations, on 27 September. At that time, Rosetta was about 20 km from the comet centre.
The particle has the name ‘Yaman Evijarvi’. Earlier in the mission, COSIMA particles were named for COSIMA team members, but with thousands of particles collected, this list was soon exhausted. Instead, ‘Yaman’ was the next name on a random list of international names (this one from Turkey), and ‘Evijarvi’, the name of a Finnish lake, comes from the theme used by the team to identify times period of dust collection.
Martin commented that the last days of Rosetta were as busy as ever for their team, as the COSIMA primary ion source parameters had to be adjusted in the very last minutes to acquire the last secondary ion spectra. “I was really impressed that after 26 months of operations, the motivation was just as high as on the first day,” he said. “In the end, our primary ion beam source outlived the total predicted hours of operation by a factor of two.”
Martin adds “And as planned, we returned all of the dust particles we collected back to the surface of the comet on 30 September – cosmic recycling, over 700 million km from Earth!”
“It’s great to have these first insights from Rosetta’s last set of data,” says Matt Taylor, ESA’s Rosetta project scientist. “Operations have been completed for over two months now, and the instrument teams are very much focused on analysing their huge datasets collected during Rosetta’s two-plus years at the comet.
“Data from this period will eventually be made available in our archives in the same way as all Rosetta data.”
And finally… from the blog editors to the Rosetta teams all around the world: thank you for sharing your stories and discoveries with us, to make this blog such a rich source of information for everyone to enjoy. We’re looking forward to the discoveries to come and continuing our science coverage on esa.int and sci.esa.int.
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NASA, 4-H Launch Expeditionary Skills For Life
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NASA, 4-H Launch Expeditionary Skils For Life
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Wednesday, 14 December 2016
Nantucket Students to Speak to Space Station Commander
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Tuesday, 13 December 2016
NASA Targets Wednesday for Launch of Small Satellite Constellation
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Monday, 12 December 2016
Reflections
Some ten weeks have passed since Rosetta ended its mission on the surface of Comet 67P/Churyumov–Gerasimenko, and it is time for a little reflection here on the Rosetta blog...
Over the past three years, we have written over 670 posts covering mission operations, science highlights, special events, images of the comet, and so much more. The blog has become a reference for a wide audience, ranging from science journalists to space enthusiasts, from casual readers to educators and even Rosetta mission scientists and operators.
Beyond that, it has become a place for people to share their ideas and concerns. When we re-launched the blog in 2013, we did not expect the huge number of comments that came in – almost 18,600 to date – and certainly we didn’t envision the considerable amount of time needed to moderate them! But we learned a lot from the comments, some of which became lengthy discussions, and which on occasion triggered new blog posts or direct engagement between readers and mission experts.
However, with the flight phase of the mission now over there are obviously no longer any news updates to share about current operations, and so we have decided to close the blog. We will soon publish our last post and close the comments section for good, although naturally, all of the material will remain online for the foreseeable future.
And of course, we will keep writing about new scientific results based on data from the mission as they’re published, and news such as updates on the availability of data in the public archives. These will be reported via our websites (Space Science Portal and Science & Technology) and on social media, especially via our @esascience Twitter account.
It's been an amazing and intense three years for us, and we hope that you also enjoyed the ride. It has been our pleasure to have you join in. As a final farewell, we would like to invite all blog readers to tell us a little about yourselves – after all, many of the contributors to the comment section are long since familiar to us by their names and nicknames, but in many cases, we don’t know a lot more.
So, make a comment to this post and feel free to tell us when, how, and why you became interested in Rosetta/comets/space science in general, how you found out about the blog, whether you followed it regularly, and what you enjoyed (or disliked!) most about it.
As ever, there are rules, however:: only one comment allowed per contributor and, as usual, off-topic posts will not be published
In your comment to this post, feel free to tell us when, how and why you became interested in Rosetta/comets/space science in general, how you found out about the blog, whether you followed it regularly and what you enjoyed most about it.
The comment function of the blog will be deactivated before the holiday break, so please post your comments before then.
We are looking forward to reading your contributions!
Best wishes,
– The Rosetta blog team
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NASA Invites Media to Hidden Figures Book Discussion in Washington
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Friday, 9 December 2016
NASA Remembers American Legend John Glenn
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NASA Highlights Ceres, Earth’s Flowing Ice, Mars at American Geophysical Union
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Thursday, 8 December 2016
NASA Shares the Universe on Pinterest and GIPHY
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NASA Awards Launch Services Program Support Contract
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Wednesday, 7 December 2016
NASA Announces First Geostationary Vegetation, Atmospheric Carbon Mission
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Tuesday, 6 December 2016
NASA Awards Contract for Refueling Mission Spacecraft
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NASA TV Coverage Set for Japanese Cargo Ship Destined for Space Station
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Spinoff 2017 Shows How NASA Technology Makes a Difference on Earth
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Saturday, 3 December 2016
NASA Administrator Statement on ESA’s Commitment to Space Station
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NASA Sets Coverage for Briefings, Launch of Small Satellite Constellation
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Friday, 2 December 2016
NASA Announces Early Stage Innovation Space Technology Research Grants
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Russian Resupply Ship Experiences Anomaly; International Space Station Crew is Fine
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NASA Invites Media to Talk with Cast of Hidden Figures at Kennedy Space Center
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Tuesday, 29 November 2016
NASA’s ISS-RapidScat Earth Science Mission Ends
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NASA Opens Media Accreditation for Hurricane Microsatellites Launch
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Monday, 28 November 2016
NASA Television to Air International Space Station Cargo Ship Launch, Docking
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Wednesday, 23 November 2016
Real People Behind Hidden Figures, Stars Join NASA to Mark Anniversary, Celebration of Diversity
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NASA Selects Launch Services for Global Surface Water Survey Mission
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Tuesday, 22 November 2016
NASA TV News Conference, Media Availability with Next Space Station Crew
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Sunday, 20 November 2016
NASA Successfully Launches NOAA Advanced Geostationary Weather Satellite
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Saturday, 19 November 2016
NASA Awards Space Studies Board Contract
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Friday, 18 November 2016
New Crew Launches to Space Station to Continue Scientific Research
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Icy surprises at Rosetta’s comet
This article is mirrored from the main ESA Web Portal.
Rosetta’s comet approached its most active period last year, the spacecraft spotted carbon dioxide ice – never before seen on a comet – followed by the emergence of two unusually large patches of water ice.
The carbon dioxide ice layer covered an area comparable to the size of a football pitch, while the two water ice patches were each larger than an Olympic swimming pool and much larger than any signs of water ice previously spotted at the comet.
The three icy layers were all found in the same region, on the comet’s southern hemisphere.
A combination of the complex shape of the comet, its elongated path around the Sun and the substantial tilt of its spin, seasons are spread unequally between the two hemispheres of the double-lobed Comet 67P/Churyumov–Gerasimenko.
When Rosetta arrived in August 2014, the northern hemisphere was still undergoing its 5.5 year summer, while the southern hemisphere was in winter and much of it was shrouded in darkness.
However, shortly before the comet’s closest approach to the Sun in August 2015, the seasons changed and the southern hemisphere experienced a brief but intense summer, exposing this region to sunlight again.
In the first half of 2015, as the comet steadily became more active, Rosetta observed water vapour and other gases pouring out of the nucleus, lifting its dusty cover and revealing some of the comet’s icy secrets.
In particular, on two occasions in late March 2015, Rosetta’s visible, infrared and thermal imaging spectrometer, VIRTIS, found a very large patch of carbon dioxide ice in the Anhur region, in the comet’s southern hemisphere.
This is the first detection of solid carbon dioxide on any comet, although it is not uncommon in the Solar System – it is abundant in the polar caps of Mars, for example.
“We know comets contain carbon dioxide, which is one of the most abundant species in cometary atmospheres after water, but it’s extremely difficult to observe it in solid form on the surface,” explains Gianrico Filacchione from Italy’s INAF-IAPS Istituto di Astrofisica e Planetologia Spaziali, who led the study.
In the comet environment, carbon dioxide freezes at –193ºC, much below the temperature where water turns into ice. Above this temperature, it changes directly from a solid to a gas, hampering its detection in ice form on the surface.
By contrast, water ice has been found at various comets, and Rosetta detected plenty of small patches on several regions.
“We hoped to find signs of carbon dioxide ice and had been looking for it for quite a while, but it was definitely a surprise when we finally detected its unmistakable signature,” adds Gianrico.
The patch, consisting of a few percent of carbon dioxide ice combined with a darker blend of dust and organic material, was observed on two consecutive days in March. This was a lucky catch: when the team looked at that region again around three weeks later, it was gone.
Assuming that all of the ice had turned into gas, the scientists estimated that the 80 x 60 m patch contained about 57 kg of carbon dioxide, corresponding to a 9 cm-thick layer. Its presence on the surface is likely an isolated rare case, with the majority of carbon dioxide ice being confined to deeper layers of the nucleus.
Gianrico and his collaborators believe the icy patch dates back a few years, when the comet was still in the cold reaches of the outer Solar System and the southern hemisphere was experiencing its long winter. At that time, some of the carbon dioxide still outgassing from the interior of the nucleus condensed on the surface, where it remained frozen for a very long while, and vaporised only as the local temperature finally rose again in April 2015.
This reveals a seasonal cycle of carbon dioxide ice, which unfolds over the comet’s 6.5 year orbit, as opposed to the daily cycle of water ice, also spotted by VIRTIS shortly after Rosetta’s arrival.
Interestingly, shortly after the carbon dioxide ice had disappeared, Rosetta’s OSIRIS narrow-angle camera detected two unusually large patches of water ice in the same area, between the southern regions of Anhur and Bes.
“We had already seen many metre-sized patches of exposed water ice in various regions of the comet, but the new detections are much larger, spanning some 30 x 40 m each, and they persisted for about 10 days before they completely disappeared,” says Sonia Fornasier from LESIA–Observatoire de Paris and Université Paris Diderot, France, lead scientist of the study focusing on seasonal and daily surface colour variations.
These ice-rich areas appear as very bright portions of the comet surface reflecting light that is bluer in colour compared with the redder surroundings. Scientists have experimented with mixtures of dust and water ice to show that, as the concentration of ice in them increases, the reflected light becomes gradually bluer in colour, until reaching a point where equal amounts of light are reflected in all colours.
The two newly detected patches contain 20–30% of water ice mixed with darker material, forming a layer up to 30 cm thick of solid ice. One of them was likely lurking underneath the carbon dioxide ice sheet revealed by VIRTIS about a month before.
“On a global scale, we also found that the entire comet surface turned increasingly bluer in colour as it approached the Sun and the intense activity lifted off large amounts of dust, exposing more of the ice-rich terrain underneath,” explains Sonia.
As the comet moved away from the Sun, the scientists observed the overall colour of the comet surface gradually turning redder again.
They also revealed local variations of colour, indicative of the daily cycle of water ice. Quickly turning into water vapour when exposed to sunlight during the local daytime, it condensed back into thin layers of frost and ice as the temperature decreases after sunset, only to vaporise again on the following day.
The distribution of water ice beneath the dusty surface of the comet seems widely but not uniformly spread, with small patches punctuating the nucleus, appearing and disappearing as a result of the comet's activity.
Occasionally, larger and thicker portions of ice are also uncovered, dating back to a previous approach to the Sun.
“These two studies of the comet's icy content are revealing new details about the composition and history of the nucleus,” says Matt Taylor, ESA Rosetta project scientist.
“While the flight part of the mission is now over, the scientific exploitation of the enormous quantity of data collected by Rosetta continues.”
--
“Seasonal exposure of carbon dioxide ice on the nucleus of comet 67P/Churyumov–Gerasimenko” by G. Filacchione et al and “Rosetta’s comet 67P/Churyumov–Gerasimenko sheds its dusty mantle to reveal its icy nature” by S. Fornasier et al are published in the journal Science.
About VIRTIS
The Visible, InfraRed and Thermal Imaging Spectrometer VIRTIS was built by a consortium of Italy, France and Germany, under the scientific responsibility of IAPS, Istituto di Astrofisica e Planetologia Spaziali of INAF, Rome (IT), which lead also the scientific operations. The VIRTIS instrument development for ESA has been funded and managed by ASI, with contributions from Observatoire de Meudon financed by CNES and from DLR. The VIRTIS instrument industrial prime contractor was former Officine Galileo, now Leonardo (Finmeccanica Group) in Campi Bisenzio, Florence, IT.
About OSIRIS
The scientific imaging system OSIRIS was built by a consortium led by the Max Planck Institute for Solar System Research (Germany) in collaboration with CISAS, University of Padova (Italy), the Laboratoire d'Astrophysique de Marseille (France), the Instituto de AstrofÃsica de Andalucia, CSIC (Spain), the Scientific Support Office of the European Space Agency (The Netherlands), the Instituto Nacional de Técnica Aeroespacial (Spain), the Universidad Politéchnica de Madrid (Spain), the Department of Physics and Astronomy of Uppsala University (Sweden), and the Institute of Computer and Network Engineering of the TU Braunschweig (Germany). OSIRIS was financially supported by the national funding agencies of Germany (DLR), France (CNES), Italy (ASI), Spain (MEC), and Sweden (SNSB) and the ESA Technical Directorate.
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Thursday, 17 November 2016
NASA Receives Sixth Consecutive Clean Audit Opinion
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US Cargo Ship Set to Depart Space Station, Live NASA TV Coverage
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Wednesday, 16 November 2016
Colorado Students to Speak with NASA Astronaut on Space Station
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Tuesday, 15 November 2016
NASA Updates 2017 International Space Station Crew Assignments
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NASA Awards Contract for Atmospheric Science, Data Assimilation Support
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Monday, 14 November 2016
Space Science Image of the Week: NAVCAM close-ups
A trio of the closest NAVCAM images of Comet 67P-Churyumov Gerasimenko is featured as our ESA Space Science Image of the Week.
During the last few weeks of its mission at Comet 67P/C–G, the Rosetta spacecraft ventured closer than it had ever been to the surface of the nucleus. Eventually, it came to rest on the small lobe of the comet in a daring descent on 30 September 2016. No navigation images were taken during the descent; the last five NAVCAM images were taken several hours earlier, between about 20 and 17 km from the comet centre.
This montage features the three closest images of the comet's surface taken by Rosetta's navigation camera – acquired in the first half of September.
The left image in the composite (also shown below) was taken on 8 September, some 2.6 from the comet surface.
The image shows a portion of the large comet lobe, portraying the boundary between the Ash and Seth regions. A context view is provided in the image on the right.
This view reveals the dust-covered terrains of Ash in the lower right part of the frame, declining towards Seth in the upper left, where part of one of the many round features present in this region is visible.
The central frame in the composite (also shown below) was taken on 14 September, about 2.6 km from the comet surface.
This image provides a detailed view of small and large boulders scattered in the Anubis region, which is also located on the large comet lobe and separated by a scarp from Seth. A context view is provided in the image on the right.
On the right in the composite (and shown below), an image from 11 September shows another view of the Seth region.
Taken about 3.5 km from the comet surface, the view reveals a terrace casting dramatic shadows on the underlying terrain, covered in dust and boulders. A context view is provided in the image on the right.
Comet 67P/Churyumov–Gerasimenko is now moving along the part of its orbit that is farthest from the Sun, in the outer Solar System, between the orbits of Mars and Jupiter. Today, it is over 600 million km from the Sun and over 740 million km from Earth.
All images from Rosetta's navigation camera are available online via the Archive Image Browser.
The three original NAVCAM images are provided below.
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Friday, 11 November 2016
An encounter with Klim Churyumov
Two years ago this week, the entire world was getting ready for a historic endeavour in space: the first soft landing of a human-made probe on a comet.
On 12 November 2014, Rosetta's lander Philae landed on Comet 67P/Churyumov–Gerasimenko, and while the landing didn't go exactly as planned, Philae finally managed to secure itself to the nucleus and to conduct a series of scientific experiments in situ, while Rosetta kept observing the comet from a distance until the mission's end last September.
As communicators of ESA's science missions, we gathered at the European Space Operations Centre (ESOC) in Darmstadt, Germany, to follow Philae's landing and report it via ESA's web and social media. During the week, ESOC was packed with scientists and engineers from the Rosetta and Philae teams, members of the international press and a number of special guests. Among them was also Professor Klim Churyumov, who together with Svetlana Gerasimenko had discovered the comet back in 1969, and who sadly passed away last month.
The day before landing – two years ago today – I had the pleasure to briefly meet Professor Churyumov and even asked him a few questions, taking down notes with the help of his translators. Back then, I was planning to write down a transcript of that conversation for this blog, but in the end the chance did not materialise at the time. Then recently, while going through my old notebooks, I found the notes from that brief interview and finally had some time to share them with the readers of the blog.
At the time, in November 2014, Rosetta had been at the comet for only three months, during which it had taken many striking pictures of this incredible little world. I asked Klim what were his expectations of how “his” comet would look like, and the reaction to Rosetta's first close-up images. He said he was very amazed to discover that 67P/C-G consists of two lobes. Of course, he was not surprised that it had an irregular shape, as most comets do because of their small mass.
According to my notes and to the translation, Klim had compared Comet 19P/Borrelly to a potato, Comet 81P/Wild (also known as Wild 2) to an elongated grapefruit, and Comet 67P/C-G... well, to him it looked like a shoe! Indeed, he said the unexpected and beautiful shape of the comet nucleus reminded him of some traditional Ukranian shoes made of straw and used by local farmers. We all joked of how “his” comet was in fact a “cosmic slipper”.
He added that the landscapes of the comet reminded him of mountain ranges on Earth, with peaks and valleys, like in the Alps or in the Carpathians, but smaller.
He also pointed out that this comet has spent most of its life time much farther away from the Sun than it currently does, as it was an encounter with Jupiter in 1959 that reduced the comet's perihelion and led it to its present orbit, incidentally making it possible for Svetlana Gerasimenko and himself to discover it ten years later. As such, he thought of the comet as a time capsule, a “Greetings from the Past” message for scientists to investigate.
I also asked him about the next steps and what he'd be most looking forward to in terms of the scientific exploitation of the data from Rosetta. He was eagerly waiting for Philae's descent and the first measurements to be performed on the surface of a comet.
He also mentioned that comets might have brought to our planet water and other molecules crucial to the emergence of life as we know it on Earth, and recalled the findings of NASA's Stardust mission, which detected the amino acid glycine at Comet Wild 2. He was hoping Rosetta would find amino acids at “his” comet too... and many months later, it actually happened, as Rosetta detected glycine at Comet 67P/C-G.
As for water, Klim said he had no doubts that Earth's water comes from space, and was looking forward to Rosetta's measurements of the isotopic composition of water at the comet. In fact, that result was published only a month after our conversation, demonstrating that water at Comet 67P/C-G contains three times more deuterium than water on Earth, and fuelling once again the debate on the main carriers of water to our planet’s oceans – comets or asteroids?
Klim said he was also looking forward to the measurements of the electric and magnetic field by the Rosetta Plasma Consortium suite of sensors on the orbiter and the ROMAP instrument on Philae, as well as to the results of the Radio Science Experiment (RSI) and of the CONSERT radar experiment to probe the comet's interior. Several studies based on data from these instruments were published on scientific journals in the past couple of years, and I hope that he had a chance to read about these interesting results.
As a final remark, he mentioned having a dream: he would have loved to be an astronaut, travel to the comet to have a walk on the surface, take some pictures and safely come back to Earth. And he was sure something like this would become possible in the future.
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NASA Awards Contract for Flight Operations Support
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Thursday, 10 November 2016
Next Space Station Crew Set for Launch Nov. 17, Watch Live on NASA TV
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Rosetta Legacy winner announced
Between 6 September and 7 October 2016, we collected 235 contributions to the Rosetta Legacy tumblr. A huge and sincere thank you to all participants who shared experiences, stories and images of how the mission of Rosetta and Philae to Comet 67P/Churyumov-Gerasimenko has inspired their lives, including study and career choices, artistic practice and other creative endeavours!
The authenticity and ingenuity of the submitted entries was overwhelming, and it has been challenging to pick one top prize winner (apologies for the delay!).
One entry in particular caught the attention of the ESA judges for the combination of creative effort and motivation, so we selected Cristina Romero from Spain as the top prize winner. The prize consists in a special visit to ESTEC, ESA’s technical heart in Noordwijk (The Netherlands).
Below is Cristina's winning entry (translated into English):
“Missions like the one of Rosetta have allowed me to discover the wonderful world of space, and as a result I started to look for more information about these topics and I discovered my passion: space.
Since then, every day I need to learn something new, to read the news about advances in aerospace industry and follow the current missions.
I ended up with such a fascination with all this, that my big dream is to be able one day to study Aerospace Engineering, in order to take part to wonderful missions like this one. This is what's pushing me to keep working hard every day, to save up to accomplish my dream, and every time it takes a little less effort to achieve it.
On September 30, the day Rosetta landed on the comet, while I was watching the webcast, I created this pendant-shaped piece to remember everything that this mission has meant to me. It is entirely handmade with polymer clay, crafted while Rosetta was landing to finally rest on Comet 67P, together with Philae.
Many thanks to ESA and the entire team for sharing this mission with us.
Cristina”
We wish to thank again everyone who shared with us what the mission meant to them, and all followers of Rosetta and Philae worldwide. It is also thanks to you that the legacy of this extraordinary mission will live on forever.
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Rosetta’s deep-space ringtone
Editor's note: Today's post was sent in by Armelle Hubault, a Spacecraft Operations Engineer here at ESOC. Armelle worked on the Rosetta Flight Control Team until the mission ended on 30 September, and she is now part of the Cluster team. As background, note that at ESA, spacecraft are operated by a team comprising an experienced Spacecraft Operations Manager (SOM) and a Flight Control Team, who typically comprise from six to as many as fifteen experienced system engineers, analysts and other experts (depending on the complexity of the spacecraft and the mission – for more details, see Building a team).
One of the responsibilities of the engineers on any mission's Flight Control Team is to monitor the spacecraft and react immediately in case of trouble.
There are two levels of support for this:
- The Spacecraft Controllers ('Spacons'), who sit in the dedicated control room on shift and perform routine spacecraft control actions (monitor ground station passes, upload commands, etc.) as well as a undertake some contingency recovery activities
- The Spacecraft Operation Engineers (SOEs), who take turns being 'on-call' and who can be called by the Spacon in case an anomaly must be further investigated or if a critical problem is detected beyond the expertise of the Spacon
Typically, SOEs must remain within one hour travel time to ESOC when on call.
In order to make the Spacon's life easier (give them just a single number to call) and avoid that engineers must make calls via their personal mobile phones when having to call abroad in the middle of the night (in case of an on-board instrument failure requiring the intervention of the instrument teams, which can be anywhere in Europe or overseas), 'on-call phones' are available for all missions.
In 2004, we got a phone that was quite modern at the time – it had a colour display and rear-lit keyboard – and selected the only available ringtone that was not a beep or a ring, called 'Luminaa'.
This phone has followed us through the whole mission, its battery still holding almost the whole week (when not being called) even after 10 years. Its ringtone was literally engraved in our psyches, such that whenever it would ring, anywhere within earshot, the whole team would jump up and start looking around (until we remembered who was actually on call).
When on call, it also happened to several of us that we would hear the phone ring and we'd start frantically looking for it, before realising it was just a similar sound via the TV – with some of us then realising, 'Oh, I'm not the one having it this week anyway!'.
So when did the phone ring, for real?
Countless times! We all recall being rung up by the Spacon to tell us that a Safe Mode had happened (inevitably in the middle of the night), or that instrument temperatures were running through the roof (usually on Sundays), that ground stations were snowed in and had lost contact with the spacecraft while it was still busy downloading recorded science data (which – unavoidably – was then lost).
It also rang to tell to us that Philae had called home in June 2015, after we all thought we'd never hear from it again (see: How we heard from Philae).
We were also rung up for a multitude of smaller, less dramatic issues – things that needed an explanation or a just quick look. On a normal on-call shift, at least a few calls were to be expected.
I am quite certain that many years from now, we will still pause and look around, startled, if we happen to hear that 'Luminaa' ringtone or anything that sounds even close.
The ringtone @ESA_Rosetta engineers have been dreading for 10 years. Phone is now off too... http://pic.twitter.com/5OH923eShI
— Armelle Hubault (@Marmelleade) October 6, 2016
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Tuesday, 8 November 2016
NASA Small Satellites Set to Take a Fresh Look at Earth
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Friday, 4 November 2016
NASA Announces Media Briefing on New Hurricane Mission
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Thursday, 3 November 2016
NASA to Hold Media Call on New Small Satellite Missions to Study Earth
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Tuesday, 1 November 2016
NASA Sets GOES-R/Atlas V Launch Events Coverage
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Sunday, 30 October 2016
NASA Astronaut Kate Rubins, Crewmates Safely Return From the Space Station
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Friday, 28 October 2016
NASA TV to Broadcast Agency Innovation Mission Day Keynote
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Thursday, 27 October 2016
Washington Students to Speak with NASA Astronaut on Space Station
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Wednesday, 26 October 2016
NASA Invites Media to Meet New Science Directorate Chief
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NASA Awards Contract for Sustainable Land Imaging Spacecraft
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NASA Television to Air Return of Three Space Station Crew Members
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Friday, 21 October 2016
NASA, Citizen Scientists Discover Potential New Hunting Ground for Exoplanets
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NASA Astronaut Peggy Whitson Available for Interviews Before Space Station Launch
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Media Invited to Rare View of NASA's James Webb Space Telescope Mirrors
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Thursday, 20 October 2016
Last NAVCAM archive release
The last batch of NAVCAM images taken by Rosetta during the final month of its incredible mission at Comet 67P/Churyumov-Gerasimenko have been released to the Archive Image Browser.
The image set covers the period 2-30 September when the spacecraft was on elliptical orbits that sometimes brought it to within 2 km of the comet's surface (watch this video for a reminder of Rosetta's 'end of mission' orbits).
The archive release also includes the final five NAVCAM images that were published on 30 September, taken shortly after the spacecraft's collision manoeuvre was executed on 29 September.
The new image sets can be found in folders MTP034 and MTP035.
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NASA, Smithsonian’s National Air and Space Museum Host Discussion on Solar Hazards in Exploration
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Wednesday, 19 October 2016
NASA Astronaut Shane Kimbrough, Crewmates Launch to Space Station to Continue Research
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Tuesday, 18 October 2016
NASA Space Station Cargo Launches from Virginia on Orbital ATK Resupply Mission
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NASA’s Juno Team to Discuss Jupiter Mission Status, Latest Science Results
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Sunday, 16 October 2016
Klim Churyumov (1937-2016)
We were saddened to learn the news yesterday that Klim Churyumov, who discovered Rosetta's comet together with Svetlana Gerasimenko in 1969, has passed away.
Many of us had the pleasure to meet him at various Rosetta Mission events held at ESOC, and we are certainly very glad that he could see 'his' comet up close, and follow the mission right through until its conclusion just a couple of weeks ago.
Our condolences to his family and friends in this time.
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Thursday, 13 October 2016
Media Invited to First Test of Multiple Drones Flying Beyond Line-of-Sight
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Wednesday, 12 October 2016
Next Space Station Crew Set for Launch, Live on NASA TV
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Atlantic Storm System Delays NASA Resupply Launch to Space Station
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Friday, 7 October 2016
CometWatch from Kepler
During the last month of Rosetta's operations at Comet 67P/Churyumov-Gerasimenko, it was no longer possible to observe the comet with telescopes on Earth because it was too close to the Sun's position in the sky and therefore not visible in the night-time. Fortunately, NASA's Kepler space observatory stepped in, taking images of the comet every 30 minutes from 7 to 20 September, providing important context to Rosetta's in situ measurements.
A world-class exoplanet hunter, Kepler is now in its second mission, called K2, which started on 30 May 2014. While still looking for exoplanets, it is now performing observations along the ecliptic and so observing a wealth of Solar System objects, from large bodies like Neptune and Pluto to smaller ones, like comets. For example, it took images of Comet Siding Spring (C/2013 A1) in October 2014.
“Observing Comet 67P/C-G with Kepler was a unique opportunity to get a global perspective of the gas and dust in the comet's environment while Rosetta was getting closer and closer to the nucleus,” says Colin Snodgrass of the Open University, UK, who coordinates a consortium of professional astronomers that observed the comet remotely during the time of Rosetta's mission.
“Together with the many ground-based observations of the comet performed over the last couple of years, these images will be instrumental to understand the link between the activity observed locally by Rosetta and remotely from Earth (or near Earth), providing crucial information for the study of other comets that we cannot visit with spacecraft.”
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