Dry ice evaporation creates the fresh gullies on Mars

New data from Mars Reconnaissance Orbiter shows that the fresh gullies that have been seen on the Red Planet are caused by dry ice evaporation, not liquid water as had been hoped.

Dundas and collaborators used the High Resolution Imaging Science Experiment (HiRISE) camera on MRO to examine gullies at 356 sites on Mars, beginning in 2006. Thirty-eight of the sites showed active gully formation, such as new channel segments and increased deposits at the downhill end of some gullies.

Using dated before-and-after images, researchers determined the timing of this activity coincided with seasonal carbon-dioxide frost and temperatures that would not have allowed for liquid water.

Frozen carbon dioxide, commonly called dry ice, does not exist naturally on Earth, but is plentiful on Mars. It has been linked to active processes on Mars such as carbon dioxide gas geysers and lines on sand dunes plowed by blocks of dry ice. One mechanism by which carbon-dioxide frost might drive gully flows is by gas that is sublimating from the frost providing lubrication for dry material to flow. Another may be slides due to the accumulating weight of seasonal frost buildup on steep slopes.

The findings in this latest report suggest all of the fresh-appearing gullies seen on Mars can be attributed to processes currently underway, whereas earlier hypotheses suggested they formed thousands to millions of years ago when climate conditions were possibly conducive to liquid water on Mars.

Update on the LDSD partly successful test flight

Another eleven news stories were published today on the LDSD test flight (go here to find them all), but only two gave an honest and informative appraisal of the parachute failure and the program’s future. This CBS report clarified the results well with these two quotes:

The Low-Density Supersonic Decelerator then fell toward impact in the Pacific Ocean northwest of Hawaii. The carrier balloon apparently came apart after the LDSD’s release and it was not immediately clear what recovery crews standing by in the landing zone might be able to retrieve.

and this:

Two more LDSD vehicles are being built for “flights of record” next summer.

Another report from Space Insider also provided this key information, something I would have expected every journalist in the world to have considered essential to their report.

Sadly, not one of the other news stories saw fit to mention that the test vehicle might have been destroyed because of the failure of the chute, nor did any of them bother to report that two more such test vehicles are under construction, allowing program to continue anyway.

That so many news stories were published on this test flight indicates the interest that exists in it. Too bad most reporters writing these stories were only interested in providing us propaganda and pro-NASA cheer-leading.

A flawed first flight for NASA’s saucer for testing Mars landing techniques.

NASA’s Low-Density Supersonic Decelerator (LDSD), the saucer shaped system for testing new landing techniques on Mars, did its first flight today with mixed results.

A saucer-shaped NASA vehicle testing new technology for Mars landings rocketed high over the Pacific on Saturday and deployed a novel inflatable braking system, but its massive parachute failed to fully unfurl as it descended to a splashdown. Control room cheers that greeted successful steps in the complex test rapidly died as the parachute appeared to emerge tangled. “Please inform the recovery director we have bad chute,” a mission official ordered.

I have found two other stories on this test flight, one from nasaspaceflight and the second from reuters. Both the Huffington Post story above and these two fail entirely to tell us whether the test vehicle was damaged when its parachute failed to open and it hit the water. Worse, all three articles seem to ignore this significant detail in describing enthusiastically NASA’s future plans for the LDSD.

As a reader, I instead think: NASA’s future plans are not the story now. The story is whether this program can even continue.

My Space Show appearance June 14, 2014.

For those who wish to listen to the podcast of my two hour appearance on the Space Show yesterday, you can get the podcast here. You can also comment on my discussion with David Livingston and his callers at the Space Show blog, or here.

The two major topics we discussed were first, Russia’s future in space in the context of that government’s effort to retake control of its entire aerospace industry, and second, the evidence that there is fraud and data manipulation going on in the climate research units of both NOAA and NASA. I also discussed some recent space science stories, such as Yutu on the Moon, Curiosity on Mars, and Cassini’s recent imagery of the lakes of Titan.

Glaciers on Mars!

A geological study of orbital images of Gale Crater has led scientists to conclude that the crater was once covered in glaciers.

To carry out the study, the team has used images captured with the HiRISE and CTX cameras from NASA’s Mars Reconnaissance Orbiter, together with the HRSC onboard the Mars Express probe managed by the European Space Agency (ESA).

Analyses of the photographs have revealed the presence of concave basins, lobated structures, remains of moraines and fan-shaped deposits which point to the existence of ancient glaciers on Gale. In fact they seem to be very similar to some glacial systems observed on present-day Earth. “For example, there is a glacier on Iceland –known as Breiðamerkurjökull– which shows evident resemblances to what we see on Gale crater, and we suppose that is very similar to those which covered Gale’s central mound in the past,” says Fairén.

This is not the first place on Mars where scientists believe glaciers once flowed. The northwestern slopes of Arsia Mons, one of Mars’s giant volcanoes in the Tharsis Bulge, is also believed to have once harbored glaciers.

The Curiosity science team celebrates the completion of a full Martian year since the rover’s landing.

The Curiosity science team celebrates the completion of a full Martian year since the rover’s landing.

This is mostly a press event aimed at convincing the world that the project is accomplishing its goals. Though they are justified in touting the many significant things about Mars and the past environment in Gale Crater that Curiosity has uncovered, we mustn’t forgot that the main goal was always to climb the slopes of Mt Sharp in order to study its geological layers and thus the long term geological history of Mars. The rover has not yet done this, and because of the greater-than-expected wheel damage the rover is experiencing, is at risk of not being able to get where it has to go.

The test of a new parachute system for Mars landing has been delayed until the end of June due to high winds.

The test of a new parachute system for Mars landing has been delayed until the end of June due to high winds.

The space agency was forced to scrub six launch attempts over the past two weeks — the latest and last planned for this Saturday (June 14) — as a result of unusually poor wind conditions at the U.S. Navy’s Pacific Missile Range facility in Kauai, Hawaii. The balloon-launched Low-Density Supersonic Decelerator (LDSD) craft is intended to help NASA develop the means to land heavier spacecraft, and eventually humans, on Mars.

“All of the vehicle systems [and] our team were ready and prepared for all of the launch days; we were ready to go,” said Mark Adler, LDSD project manager at NASA’s Jet Propulsion Laboratory (JPL) in Pasadena, California. “The only thing that held us up was that none of the launch dates had or will have acceptable weather conditions.”

They have literally run out of their available time at the range, and must let others play through first while they renegotiate for a new slot of time later.

A place on Mars that was possibly habitable only 200 million years ago.

A place on Mars that was possibly habitable only 200 million years ago.

This article discusses the possibility of liquid water from the melting of the glaciers that scientists think once covered the western slopes of the giant volcano Arsia Mons. I have also written about this area in an article I wrote for Sky & Telescope last year on exploring caves in space. It is thought that there might be caves here in which some of that water from those glaciers might still be found.

As one scientist is quoted as saying in this article, “Arsia Mons would be the next place I would want to go.” Like the south pole of the Moon, it likely has all the ingredients for establishing a habitable colony.

The first preliminary list of candidate landing sites for NASA’s next Mars rover have been proposed.

The first preliminary list of candidate landing sites for NASA’s next Mars rover have been proposed.

At the conclusion of the workshop, attendees voted informally on the nearly 30 candidate sites that researchers had presented—ranking the sites as being of high, medium, or low scientific interest. Floating to the top was a site called Northeast Syrtis Major, a terrain at the edge of the Isidis Basin, the remnant of one of Mars’s biggest and most ancient asteroid impacts. Jack Mustard, a planetary scientist at Brown University and an advocate for the site, says material from the impact could offer a precise date for that event. Scientists also want a piece of nearby lava flows, thought to have oozed out and cooled several hundred million years later.

Nothing is even close to being decided yet, however.

In related news, a new study suggests that dozens of microbes might have stowed away on Curiosity when it left for Mars.

Emphasis must be placed on the word “suggests” however.

Engineers commanded Curiosity to drill its third drill hole on Tuesday on what looks like an outcrop of sandstone in Gale Crater.

Engineers commanded Curiosity to drill its third drill hole on Tuesday on what looks like an outcrop of sandstone in Gale Crater.

This hole is shallow and is merely a test to see if a deeper full bore would be worthwhile geological.

That Curiosity has only drilled three holes, and is now only doing a test bore first is partly because engineers fear that using the drill too much will cause a short circuit that will disable the rover entirely. This fear is because of a design flaw in the construction of the rover and the drill.

Budget issues continue to threaten a number of successfully functioning science spacecraft, including Opportunity on Mars and Lunar Reconnaissance Orbiter circling the Moon.

Penny wise, pound foolish: Budget issues continue to threaten a number of successfully functioning science spacecraft, including Opportunity on Mars and Lunar Reconnaissance Orbiter circling the Moon.

Don’t be surprised if NASA announces soon that they are shutting down these spacecraft so they can save some money. Or as the article notes, “Money not spent on these extended missions will probably slide into [the Science Mission Directorate’s] Black Hole of Funding (the James Webb Space Telescope) or be dissipated on new paperwork, committee meetings and concept studies.”

New research suggests that, in general, Mars has always been too cold to harbor liquid water on its surface.

The uncertainty of science: New research suggests that, in general, Mars has always been too cold to harbor liquid water on its surface for long periods.

Mars’ atmosphere was probably never thick enough to keep temperatures on the planet’s surface above freezing for the long term, suggests research published today in Nature Geoscience1. Although the planet’s topography indicates that liquid water has flooded Mars in the distant past, evidence increasingly suggests that those episodes reflect occasional warm spells, not a consistently hospitable phase of the planet’s history.

The research does not say that liquid water never flowed on the Martian surface, only that such events were short-lived. They looked at craters and noted that the surface has impacts from meteorites that would not have survived to the surface had the atmosphere been thick enough for liquid water.

The research however did not address Mars’ relatively smooth northern hemisphere, where there are not a lot of craters and where some scientists think there might once have been a shallow ocean. If Mars never had liquid water for long periods, why does this area lack craters?

Scientists from the joint European/Russian ExoMars rover mission have narrowed their candidate landing sites to four.

Scientists from the joint European/Russian ExoMars rover mission have narrowed their candidate landing sites to four.

Last week, 60 scientists met at ESA’s European Space Astronomy Centre near Madrid to discuss eight potential sites. On 27 March, they cast an informal vote, and four sites emerged as favourites: Mawrth Vallis, Oxia Planum, Hypanis Vallis and Oxia Palus. An expert working group tasked with recommending a final landing site will now consider the proposals, before announcing a formal shortlist of three or four sites in June. Following detailed studies of the shortlisted sites, the panel will make a single recommendation to ESA and Roscosmos in late 2016.

This is maybe the most risky mission to Mars in decades, as the landing design is coming from the Russians, who have not had a successful interplanetary mission since the era of the Soviet Union, and even then had a 100% failure rate for their missions to Mars. (On a more optimistic note, the European Mars Express mission used a Russian rocket to take off, making it the first Mars mission with Russians participation that actually succeeded.)

One of the factors that has made this mission more risky is the fact that the U.S. was once a participant and backed out very late in the game. The Russians are our replacement, and have had to scramble to catch up.

Curiosity has reached another area of interesting terrain: rows of layered curvy rocks.

Curiosity has reached another area of interesting terrain: rows of layered curvy rocks.

The science team has been hunting for tasty rock outcrops suitable for the first drilling campaign since she departed the dried out lakebed at Yellowknife Bay in July 2013 and began her epic trek across the floor of Gale Crater towards the base of Mount Sharp. With each passing Sol, or Martian day, Mount Sharp looms larger and larger and the historical layers with deposits of hydrated minerals potentially indicative of an alien habitable zone come ever clearer into focus.

The panoramas are quite spectacular as the rover continues its journey toward Mt Sharp.

Before and after images from Mars Reconnaissance Orbiter have discovered the formation of a new gully on Mars sometime between November 2010 and May 2013.

Before and after images from Mars Reconnaissance Orbiter have discovered the formation of a new gully on Mars sometime between November 2010 and May 2013.

The winding gully seems to have poured out from an existing ribbon channel in a crater in Mars’ Terra Sirenum region. The leading hypothesis on how the gully formed is that debris flowed downslope from an alcove and eroded a new channel. Though it looks water-carved, the gully is much more likely to have been formed when carbon dioxide frost accumulated on the slope and grew heavy enough to avalanche down and drag material down with it.

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