Year: 2018

Spiders on Mars!

9:34 am

spiders on Mars

Cool image time! Today’s release of new captioned images from the high resolution camera on Mars Reconnaissance Orbiter (MRO) included a wonderful image of the melting carbon dioxide cap of Mars’s south pole. On the right is a cropped portion of the full image, showing what the MRO scientists nickname spiders, features that appear as the CO2 begins to turn into gas.

But these aren’t actual spiders. We call it “araneiform terrain,” to describe the spider-like radiating channels that form when carbon dioxide ice below the surface heats up and releases. This is an active seasonal process we don’t see on Earth. Like dry ice on Earth, the carbon dioxide ice on Mars sublimates as it warms (changes from solid to gas) and the gas becomes trapped below the surface.

Over time the trapped carbon dioxide gas builds in pressure and is eventually strong enough to break through the ice as a jet that erupts dust. The gas is released into the atmosphere and darker dust may be deposited around the vent or transported by winds to produce streaks. The loss of the sublimated carbon dioxide leaves behind these spider-like features etched into the surface.

The image above shows older spiders, formed during past seasonal events. If you click on the image you can see the full image, which shows darker spiders produced by this season’s cycle.

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The dying Russian space program, from a Russian’s perspective

9:21 am

Link here. I have written previously about how Russia’s space effort seems to be steadily shrinking, month-to-month. This article gives the perspective from the point of view of a Russian who writes about space, and provides some concrete further examples of the program’s bureaucratic problems:

For example, the Russian space agency has been developing a “new” science and research module for the space station, “Nauka,” since 1995. More than two decades later, the module still awaits a decision on whether it should actually be completed.

Borisov asserts that this is because there are concerns about post-launch problems. “No official from Russia’s space industry wants to take responsibility for the laboratory module and its safety for use as part of the ISS, about which many questions have arisen,” he writes. (A translation of the 3,000-word article was provided to Ars by Robinson Mitchell).

The story is similar for Russia’s next-generation spacecraft, Federation. Instead of investing in this new vehicle designed for deep-space crew activities, which has been under development for a decade, Russia will likely opt to continue revising the Soyuz spacecraft, which first launched 52 years ago. This was before NASA’s Apollo capsule had flown.

The Putin government made a decision in the past decade to consolidate their entire space industry into one giant government-run corporation. In the process they eliminated all competition, and put every new project under the control of government bureaucrats whose first concern is not innovation and risk, but covering their behinds. As such, Russia has found it impossible to produce new space technology fast enough to compete.

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Global topographic maps of Pluto and Charon

9:14 am

Using data and images from New Horizons scientists have now produced the first global topographic maps of Pluto and Charon.

Obviously, the resolution for the maps of both planets is very uneven, since the spacecraft only saw part of each planet at high resolution during its fly-by. Nonetheless, they note some of the more interesting details revealed:

These maps reveal a rich variety of landforms on both Pluto and Charon. The topographic maps confirm that the highest known mountains on Pluto are the Tenzing Montes range, which formed along the southwestern margins of the frozen nitrogen ice sheet of Sputnik Planitia. These steep-sided icy peaks have slopes of 40° or more and rise several kilometers above the floor of Sputnik Planitia. The highest peak rises approximately 6 kilometers (3.7 miles) above the base of the range, comparable to base-to-crest heights of Denali in Alaska, and Kilimanjaro in Kenya. Pluto’s mountains must be composed of stiff water ice in order to maintain their heights, as the more volatile ices observed on Pluto, including methane and nitrogen ice, would be too weak and the mountains would collapse.

The topographic maps also reveal large-scale features that are not obvious in the global mosaic map. The ice sheet within the 1000-kilometer (625-mile) wide Sputnik Planitia is on average 2.5 kilometers (1.5 miles) deep while the outer edges of the ice sheet lie an even deeper 3.5 km (or 2.2. miles) below Pluto’s mean elevation, or ‘sea level’ surface. While most of the ice sheet is relatively flat, these outer edges of Sputnik Planitia are the lowest known areas on Pluto, all features that are evident only in the stereo images and elevation maps. The topographic maps also reveal the existence of a global-scale deeply eroded ridge-and-trough system more than 3000 kilometers (or 1864 miles) long, trending from north-to-south near the western edge of Sputnik Planitia. This feature is the longest known on Pluto and indicates that extensive fracturing occurred in the distant past. Why such fracturing occurred only along this linear band is not well understood.

On Charon the topographic maps also reveal deep depressions near the north pole that are ~14 kilometers (8.7 miles) deep, deeper than the Marianas Trench on Earth. The equatorial troughs that form the boundary between the northern and southern plains on Charon also feature high relief of ~8 kilometers. The mapping of fractured northern terrains and tilted crustal blocks along this boundary could be due to cryovolcanic resurfacing, perhaps triggered by the foundering of large crustal blocks into the deep interior of Charon. The rugged relief also indicates that Charon retains much of its original topography caused by its history of fracturing and surface disruption.

These maps are obviously only our first stab at mapping both planets. We will need orbiters around both to truly detail their surface features.

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Mars 2020 gets fourth candidate landing site

9:04 am

The science team for the next American Mars rover, Mars 2020, has decided to consider a fourth candidate landing site, located between two other candidate sites.

The site has been dubbed “Midway,” because it’s roughly halfway between two other candidate landing locations — Jezero delta and Northeast Syrtis. The third previously identified candidate is the Columbia Hills region of Gusev Crater, which NASA’s now-defunct Spirit rover explored after touching down in January 2004.

Jezero, Northeast Syrtis and Columbia Hills were selected as finalists at the third 2020 rover landing site workshop, which was held in February 2017.

Midway has the same morphologic units as Northeast Syrtis and is relatively close to Jezero, explained John Mustard, a professor in the Department of Earth Environmental and Planetary Sciences at Brown University in Providence, Rhode Island. “It has emerged from Mars 2020 science team members I believe brainstorming on possibly getting two birds with one rover,” Mustard told Inside Outer Space.

Based on this story, it sounds to me as this new site has emerged as the favorite. It would put the rover down in the transition zone between Mars’s northern low plains and its southern highlands, an area where evidence of the receding shoreline of any past intermittent ocean might exist. It would also allow it to study geology similar to two previous candidate sites.

One problem they may have is that this candidate site has not yet been photographed in detail by Mars Reconnaissance Orbiter’s (MRO) high resolution camera, as have the other sites. They will need to get time on MRO to do this in order to make sure this site is acceptable.

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Israel’s former Google Lunar X-Prize contestant to launch in 2018

8:54 am

Capitalism in space: Despite a failure of all contestants to to win the Google Lunar X-Prize, Israel’s competitor announced today that they still plan to launch, and will do so in December of this year.

The SpaceIL spacecraft will be launched from the United States on a Falcon 9 orbital launch vehicle, built by Elon Musk’s Space Exploration Technologies Corporation, or SpaceX. At a press conference on Tuesday, SpaceIL representatives announced that the unmanned lunar landing craft will be transferred to the US in November, with a launch date in December.

According to SpaceIL, the unmanned space vessel will reach the moon and complete the lunar landing on February 13th next year.

They say the lander will plant an Israeli flag on the Moon, but the images at the link, as well as the announcement, suggests that the lander will no longer have the ability to rove, as required for the X-Prize. It appears to me that they have simplified the mission in order to fly it quickly and gain the public relations such a flight will give them.

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First manned Dragon capsule completes thermal vacuum tests

8:46 am

Capitalism in space: SpaceX’s first manned Dragon capsule has completed its thermal vacuum tests ahead of its test orbital flight, presently scheduled for September of this year.

There have been hints that this schedule could be further delayed. That neither SpaceX nor NASA were willing to comment about the results of the thermal tests could be a cause for concern, or it could simply be that they have not yet digested the material and wish to do so first before commenting.

I suspect a more firm schedule will be announced before the end of this month.

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China launches GPS satellite, matches record for annual launches

8:40 am

China today completed its 20th launch in 2018, putting a GPS satellite into orbit with its Long March 3C rocket.

Twenty launches matches China’s 2016 record for annual launches, but they have done so in just over half a year. They continue on track to meet their prediction of about 40 launches in2018.

The updated 2018 leader launch standings:

20 China
12 SpaceX
8 Russia
5 ULA
4 Japan

China now leads the U.S. 20 to 18 in the national rankings.

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All thirteen trapped cavers rescued alive!

8:13 am

Miracles happen: Cave divers today successfully rescued the last four boys and their soccer coach from a flooded cave in Thailand.

All 12 members of a Thai youth football team and their coach have been brought safely out of the cave in northern Thailand. The final five members rescued join eight team members taken to hospital on Sunday and Monday and said to be doing well. Each person was pulled through the cave by expert divers. The last Navy Seals – three divers and a doctor – are out of the cave, the rescue chief says.

As I said, this is a miracle. The press is likely going to focus on the kids and their coach, but the real heroes are the cave divers who risked their lives, with one man dying, to save these children.

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Sunspot update for June 2018: Activity increases again

5:56 pm

NOAA today posted its monthly update of the solar cycle, covering sunspot activity for June 2018. Below is this month’s annotated graph.

For the third straight month the Sun showed a small increase in sunspot activity. The pattern also continued to follow the two-week-on/two-week-off pattern of activity caused by the Sun’s 27-day rotation, as I described in my update last month.

June 2018 sunspot activity

The graph above has been modified to show the predictions of the solar science community. The green curves show the community’s two original predictions from April 2007, with half the scientists predicting a very strong maximum and half predicting a weak one. The red curve is their revised May 2009 prediction. The yellow line compares the present activity with the activity during solar minimum in 2008 and 2009.

This pattern is continuing. As of today, there have been no sunspots since June 28, almost two weeks. I would not be surprised if some sunspots appeared within the next week, especially because today’s image of the Sun from Solar Dynamic Observatory shows bright faculae rotating into view. Faculae are, like sunspots, a sign of solar magnetic activity. The two usually go together.

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