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The Planetary Society BlogBy Emily Lakdawalla
Jul. 3, 2009 | 16:51 EDT | 20:51 UTC LRO Sends First Imagesby Amir Alexander On June 30, one week after entering lunar orbit, the Lunar Reconnaissance Orbiter turned on its LROC camera and began taking images of the Moon. The first ones were taken along the termination line, showing a hilly region a few kilometers east of Hell E crater in the southern hemisphere, south of Mare Nubium. LROC, which stands for the Lunar Reconnaissance Orbiter Camera, is in fact composed of of two instruments: a low-resolution wide-angle camera and a high-resolution narrow-angle camera. Both came online on June 30, and LRO's other six instruments are also in the process of being activated. Once the instruments are calibrated, the spacecraft will move from its current commissioning orbit to its near-circular primary orbit, 50 kilometers above the lunar surface.
Jul. 3, 2009 | 13:36 EDT | 17:36 UTC Down Under with Jim Bellby Susan Lendroth Planetary Society President Jim Bell will give a talk in Melbourne, Australia on July 10. Jointly sponsored with the Mars Society, the event will take place in the Fritz Loewe Theatre at the School of Earth Sciences, University of Melbourne. Jim is the Payload Element Lead for the Mars Exploration Rover "Pancam" multispectral, stereoscopic imaging systems on the Spirit and Opportunity rovers. So, expect great images in his presentation about the exciting discoveries made on Mars in the last five years, including evidence of water in the planet's history. The talk is free and begins at 4:00 pm on Friday, July 10. For more information contact event organizer, Kevin Walsh, at kevin.walsh@unimelb.edu.au. Jul. 2, 2009 | 00:42 EDT | 04:42 UTC The Enigma of Enceladusby Kelly Beatty
This week we celebrate a milestone in the annals of planetary exploration:Five years ago, on July 1, 2004, the Cassini orbiter slipped between the tenuous F and G rings of Saturn and settled into orbit around that famously ringed planet. Little did we know at the time all the wondrous views this enduring craft would return. At last count, NASA has released nearly 1,800 images of the Saturnian system &mdash and that's just from the craft's Imaging Science Subsystem, its visible-light camera. Someday there'll be entire books dedicated to everything that Cassini (and its sidekick Huygens, the European-built Titan probe) has discovered over the years. But even now, with the mission not nearly over, few planetary scientists would dispute that any Top Ten discovery list would surely include the image below.
The center of attention here isn't Saturn's faint E ring, first spotted telescopically from Earth in 1967, but rather the modest moon Enceladus that's in the center of the frame. Astronomers had long known that the E ring overlaps the moon's orbit, and they suspected a connection. Not long after Cassini arrived, its camera revealed that powerful eruptions near the south pole of Enceladus are spewing a constant stream of water vapor and ice particles into space. Spread that out, and you've got the E ring. Amazing stuff! William Herschel discovered this moon in 1789. He named it Enceladus, after one of the Gigantes in Greek mythology. These enormous children of Gaia had, among other things, long serpentlike lower limbs. Hmm... how did Herschel know that the name Enceladus would prove so fitting?
Mind you, Enceladus was considered odd even before Cassini arrived. Some 30 years ago, Voyagers 1 and 2 found that its surface is virtually 100% reflective and nearly pure water ice. This moon averages only 313 miles (505 km) across — it's only 4% the diameter of Earth and has just 0.00002 as much mass. So how could an ice ball no larger than the British Isles be so active? What's going on inside it? Three years ago, Cassini investigators led by ISS honcho Carolyn Porco (Space Science Institute) published a long article in Science to provide some answers. But first, here's some useful background: An orbital resonance with nearby Dione forces Enceladus into a very slightly elliptical orbit. This, in turn, means Enceladus can't keep exactly the same hemisphere pointing toward Saturn; from the planet's perspective, the moon nods slightly side to side. The upshot is that Enceladus's icy crust flexes rhythmically during each orbit, causing frictional heat to build up inside. All that bumping and grinding is generating about 1015 ergs per second — equivalent to more than 100,000 hair dryers set on "high"! On paper, that's enough heat to create a subsurface ocean of global extent, the "lubricant" that decouples the flexing crust from the moon's deeper interior. So what's this ocean like, and what's it got to do with all that south-polar spewing? Porco and her team proposed the jets must be powered by a not-very-deep reservoir of liquid water that boils spontaneously and violently once it finds a way to reach the the vacuum of space. These escape hatches are provided by four 80-mile-long cracks (dubbed "tiger stripes" but officially designated sulci) near the south pole.
Not everyone agrees with this "Cold Faithful" model. Others (most notably University of Illinois geologist Susan Kieffer) speculate that an ocean might not be needed at all. Instead, frozen compounds called clathrates, which lock up volatile molecules like methane, carbon dioxide, or nitrogen in water-ice crystals, could be decomposing to create the jets of gas and ice. A few weeks ago I attended a meeting of geophysicists in Toronto, which included a session titled the "Great Enceladus Debates". It was an apt choice; to be perfectly honest, there is much disagreement about the moon's inner workings. At the meeting, James Roberts (Applied Physics Laboratory) explained there almost has to be a layer of liquid water down there somewhere — it's the only physically plausible way to channel so much heat out of the interior. But right now the orbit of Enceladus isn't nearly elliptical enough (by at least a factor of three) to sustain all that tidal friction indefinitely. However the subsurface ocean came to exist, Roberts says, it's likely to freeze quickly on a geological timescale. Fortunately, Cassini has been getting quite close to Enceladus recently. The craft brushed past the moon four times last year, and two more close flybys are planned for November 2nd and 21st. (Another dozen could occur if NASA approves a proposed 7-year extension to the mission.) Two new results, discussed in Toronto and published last week in Nature, put important constraints on the putative ocean. According to Frank Postberg (Max Planck Institute for Nuclear Physics) and others, about 6% of the tiny E-ring particles swept up by Cassini's Cosmic Dust Analyzer are quite salty. They contain up to 1.5% sodium chloride (NaCl), about half the salt content of terrestrial seawater. So, the thinking goes, any liquid water inside Enceladus must have been in contact with deep-seated rocks for a long time — millions of years — to allow sodium and other elements to leach into the water. But something else, published in the same issue of Nature, is at odds with the CDA results. Nicholas Schneider (University of Colorado) led a group of observers who used telescopes on Earth to search for sodium in the escaping plumes spectroscopically. They turned up nothing, not even a trace, even though atomic sodium has very strong emissions in yellow light. Schneider says that the lack of sodium in the plumes' vapor rules out the violent geyser model proposed by Porco's team, because if briny water were boiling explosively, both the gas and particles should contain salt.
Meanwhile, all this talk of warm saltwater has really gotten the attention of astrobiologists. Enceladus appears to have a sustained source of heat, a suitable chemical mix, and liquid water. Throw in a subterranean environment protected from space radiation, and you've got what might be just the kind of place that's conducive to life. Jun. 30, 2009 | 14:00 EDT | 18:00 UTC Webcast of Ulysses last day of operationsAfter 18.6 years in space and defying several earlier expectations of its demise, the joint ESA/NASA solar orbiter Ulysses will achieve "end of mission" on June 30, 2009. The final communication pass with a ground station will start at 17:35 CEST and run until 22:20 CEST (15:35-20:20 UTC) or until the final command is issued to switch the satellite's radio communications into "monitor only" mode. No further contact with Ulysses is planned. The ESA/NASA Ulysses team at the Jet Propulsion Laboratory will livestream the Ulysses final ground pass and shut down tomorrow, June 30, starting at about 17:00 CEST (15:00 UTC). For more details and to watch live, visit http://www.esa.int/ops or http://www.livestream.com/eurospaceagency For the latest updates and more information on Ulysses operations, check out the Ulysses mission operations page. We
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A veteran space reporter and Senior Contributing Editor of Sky & Telescope, Kelly Beatty enjoys writing for a wide spectrum of audiences, from children to professional astronomers. He's also on the astronomy faculty at the Clay Center Observatory in suburban Boston. Although the skies above his home are aglow with light pollution, Kelly observes when he can through one of his six telescopes.
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