by Paul Gilster | Apr 10, 2012 | Outer Solar System |
Getting to the stars may involve a sudden breakthrough — we can’t rule out disruptive technologies, nor can we predict them — but my guess is that interstellar flight is going to be a longer, more gradual process. I can see a sort of tidal expansion into the outer system, forays to Mars, for example, followed by reassessment, retrenchment, then one day deeper study of Jupiter’s moons with advanced robotics that can get under Europa’s ice. The search for life may become so provocative that we have to explore Titan and Enceladus with human crews, and the imperative for planetary protection may help us further tune up our deep space technologies.
The thing is, one wave of exploration inevitably begets another. Let’s put no timeframe on that kind of expansion because, like the tides, it may surge at times and then fall back, hostage to budgetary problems and waves of public interest that can as easily ebb. But I could see an eventual civilization that extends throughout the Solar System and, in shaping its essential infrastructure, pushes its propulsion and life support systems to begin exploring out into the Kuiper Belt and beyond. This assumes that we keep doing what we can right now, with resources that are stretched thin but may still give us something like the AVIATR airplane on Titan, or perhaps an instrument package that can splash down in one of Titan’s seas.
We build the Solar System infrastructure one step at a time, and our robotic missions have given us a glimpse of what is waiting for us. Imagine the scientific return when we can begin sending human crews to some of the places so far glimpsed only by our probes! But the probes come first and the Titan Mare Explorer (TiME), which Johns Hopkins Applied Physics Laboratory (JHU/APL) champions, is a cost-capped $425 million mission concept that would parachute a robotic boat right into Ligeia Mare, the second largest of Titan’s northern seas. Active mission time on Titan would be 96 days, with a launch between 2016 and 2018 if TiME is chosen over two competing proposals as a NASA Discovery-class mission. We’ll know the answer to that later this year.
Image: Ligeia Mare, in Titan’s northern polar region, could reveal its secrets to the TiME probe following a 2023 splashdown. Credit: NASA/JPL.
Every time we get a closer look at a distant world (think Cassini), we find compelling reasons to revisit the destination with ever more sophisticated technologies. Voyager and Galileo ramped up interest in Europa’s hidden ocean, and it’s likely that a Neptune orbiter would tell us things about Triton that might compel a future mission there. A major player in all this, of course, is the search for life, which makes Enceladus well nigh irresistible along with more likely targets.
As for Titan, it is already the site of the farthest landfall in human history, and it could now become the first place in which a probe lands in an alien sea. The interaction between liquid methane and ethane with Titan’s climate and weather patterns would be a prime area for study, but TiME would also look at the kind of complex organic chemistry that may be similar to what led to life’s formation on Earth billions of years ago. Says TiME project scientist Ralph Lorenz:
“These are disciplines that, to this point, have been strictly Earth science. How are heat and moisture exchanged between the ocean surface and atmosphere? How are waves generated? We have an opportunity to explore these processes in a completely different, alien environment.”
A 2009 presentation to the Decadal Survey by principal investigator Ellen Stofan (Proxemy Research) notes that the lakes and seas of Titan are probably at least tens of meters deep and may extend down beyond 100 meters, and they clearly play a major role in the overall methane cycle on the moon. Ethane has been detected in Ontario Lacus near the south pole, and the same lake shows changes to its shoreline over time that suggest seasonal effects. A key goal of TiME will be to examine the methane cycle and show its similarities and differences from the hydrologic cycle on Earth from the probe’s unique vantage point awash in Ligeia Mare.
Like AVIATR, the TiME mission would also offer a useful technology shakeout of the Advanced Stirling Radioisotope Generators (ASRGs) that would provide power for the probe, both in the deep space environment and in a non-terrestrial atmosphere. This first nautical exploration of an extraterrestrial sea could be providing science from Titan by 2023, including imagery from Ligeia Mare’s surface showing us clouds and rain moving across the moon’s orange skies. As I speculated last week, the choice of TiME would probably make the AVIATR airplane mission less likely to fly, given the inexorable logic of budgeting. We may be looking, then, at a choice between two compelling concepts to deepen our exploration of Saturn’s most intriguing moon.
Related: Planetary Lake Lander is an attempt to study these technologies right here on Earth, with implications for what could fly aboard the TiME mission. From Five Steps Toward Future Exploration, in Astrobiology Magazine:
The Planetary Lake Lander project is led by Principal Investigator Nathalie Cabrol of NASA Ames Research Center and the SETI Institute, and involves a three-year field campaign at Laguna Negra (Black Lagoon) in the Central Andes of Chile. Here the team will test mission scenarios and technologies for deploying a floating, robotic platform that can perform scientific studies remotely while swimming the waters of Laguna Negra. Ultimately, this work will pave the way for a lake lander mission to Saturn’s moon Titan. NASA has never attempted a lake landing before, so this field campaign is an essential first step in identifying the challenges that mission developers must contend with when they turn their sights toward the methane lakes of Titan.
You can follow the ongoing work of the Planetary Lake Lander project here. From the most recent blog entry (December 15, 2011), as the team prepared to return to the US, leaving the robotic device behind to monitor Laguna Negra:
Our plane takes off at 9:15 pm the following evening, and we are back in the US and home by 11:00 am on December 17. The morning air is clean and brisk, not unlike that of the lake, where for now, PLL is a reminder that we were there. It is logging data every hour and calling “home” (at NASA Ames) every evening, sharing more knowledge about melting glaciers and climate change. In a few months, it will be proactively monitoring the environment at Echaurren, as a precursor to what, maybe some day, another Lake Lander will do on Titan.
by Paul Gilster | Apr 9, 2012 | Outer Solar System |
I closed last week with two posts about the AVIATR mission, an unmanned airplane that could be sent to Titan to roam its skies for a year of aerial research. It’s a measure of Titan’s desirability as a destination that it has elicited so many mission proposals, and I want to get into the Titan Mare Explorer (TiME) as well, but let’s pause a moment to consider the nature of what we’re doing. Out of necessity, all our missions to the outer system have been unmanned, but as we learn more about long-duration life-support and better propulsion systems, that may change. The question raised this past weekend in an essay in The Atlantic is whether it should.
Ian Crawford, a professor of planetary sciences at Birkbeck College (London) is the focus of the piece, which examines Crawford’s recent paper in Astronomy and Geophysics. It’s been easy to justify robotic exploration when we had no other choice, but Crawford believes not only that there is a place for humans in space, but that their presence is indispensable. All this at a time when even a return to the Moon seems beyond our budgets, and advanced robotics are thought by many in the space community to be the inevitable framework of all future exploration.
But not everyone agrees, even those close to our current robotic missions. Jared Keller, who wrote The Atlantic essay, dishes up a quote from Steve Squyres, who knows a bit about robotic exploration by virtue of his role as Principal Investigator for the Spirit and Opportunity rovers on Mars. Squyres points out that what a rover could do even on a perfect day on Mars would be the work of less than a minute for a trained astronaut. Crawford accepts the truth of this and goes on to question what robotic programming can accomplish:
“We may be able to make robots smarter, but they’ll never get to the point where they can make on the spot decisions in the field, where they can recognize things for being important even if you don’t expect them or anticipate them,” argues Crawford. “You can’t necessarily program a robot to recognize things out of the blue.”
Landing astronauts is something we’ve only done on the Moon, but the value of the experience is clear — we’ve had human decision-making at work on the surface, exploring six different sites (some of them with the lunar rover) and returning 382 kilograms of lunar material. The fact that we haven’t yet obtained samples from Mars doesn’t mean it’s impossible to do robotically, but a program of manned exploration clearly points to far more comprehensive surface study. Crawford points out that the diversity of returned samples is even more important on Mars, which is more geologically interesting than the Moon and offers a more complicated history.
Image: Apollo 15 carried out 18.5 hours of lunar extra-vehicular activity, the first of the “J missions,” where a greater emphasis was placed on scientific studies. The rover tracks and footprints around the area give an idea of the astronauts’ intense activity at the site. Credit: NASA.
Sending astronauts by necessity means returning a payload to Earth along with intelligently collected samples. From Crawford’s paper:
Robotic explorers, on the other hand, generally do not return (this is one reason why they are cheaper!) so nothing can come back with them. Even if robotic sample return missions are implemented, neither the quantity nor the diversity of these samples will be as high as would be achievable in the context of a human mission — again compare the 382 kg of samples (collected from over 2000 discrete locations) returned by Apollo, with the 0.32 kg (collected from three locations) brought back by the Luna sample return missions.
It’s hard to top a yield like that with any forseeable robotic effort. Adds Crawford:
The Apollo sample haul might also be compared with the ? 0.5 kg generally considered in the context of future robotic Mars sample return missions… Note that this comparison is not intended in any way to downplay the scientific importance of robotic Mars sample return, which will in any case be essential before human missions can responsibly be sent to Mars, but merely to point out the step change in sample availability (both in quantity and diversity) that may be expected when and if human missions are sent to the planet.
Large sample returns have generated, at least in the case of the Apollo missions, huge amounts of refereed scientific papers, especially when compared to the publications growing out of robotic landings. Crawford argues that it is the quantity and diversity of sample returns that have fueled the publications, and points out that all of this has occurred because of a mere 12.5 days total contact time on the lunar surface (and the actual EVA time was only 3.4 days at that). Compare this to the 436 active days on the surface for the Lunokhods and 5162 days for the Mars Exploration Rovers. Moreover, the Apollo publication rate is still rising. Quoting the paper again:
The lesson seems clear: if at some future date a series of Apollo-like human missions return to the Moon and/or are sent on to Mars, and if these are funded (as they will be) for a complex range of socio-political reasons, scientists will get more for our money piggy-backing science on them than we will get by relying on dedicated autonomous robotic vehicles which will, in any case, become increasingly unaffordable.
Will the Global Exploration Strategy laid out by the world’s space agencies in 2007 point us to a future in which international cooperation takes us back to the Moon and on to Mars? If so, science should be a major beneficiary as we learn things about the origin of the Solar System and its evolution that we would not learn remotely as well by using robotic spacecraft. So goes Crawford’s argument, and it’s a bracing tonic for those of us who grew up assuming that space exploration meant sending humans to targets throughout our Solar System and beyond. That robotic probes should precede them seems inevitable, but we have not yet reached the level of artificial intelligence that will let robots supercede humans in space.
The paper is Crawford, “Dispelling the myth of robotic efficiency: why human space exploration will tell us more about the Solar System than will robotic exploration alone,” Astronomy and Geophysics Vol. 53 (2012), pp. 2.22-2.26 (abstract). Thanks to Joseph Kittle for calling this paper to my attention.
by Paul Gilster | Apr 6, 2012 | Outer Solar System |
Yesterday’s discussion of the AVIATR mission to Titan inevitably brought up another prominent Titan mission concept: Titan Mare Explorer (TiME). I’ll have more to say about this one next week, as today I want to continue talking about AVIATR, but you can once again see how Titan enthralls us with its ‘Earth-like’ aspects. Need a thick atmosphere around a moon? Titan is your only play, and if, as with TiME, you want to put an instrument package into an off-planet surface lake, you’ll be hard pressed to do it anywhere else, at least in this Solar System.
These two mission concepts fire the imagination — they’re the kind of thing kids like me used to dream about when we plunked down our money at the newsstand for copies of Galaxy or Fantasy & Science Fiction. It’s unlikely, though, that both missions will fly. If TiME, which is a Discovery-class mission finalist and thus cost-capped at $425 million, is chosen, then the odds on AVIATR probably drop. AVIATR, a New Frontiers-class mission, ups the cost to $715 million, and because it didn’t make it into the National Research Council’s ‘Decadal Survey,’ the mission will be pushed back into the next decade at the earliest even if TiME loses out to a competing proposal.
Soaring in Titan’s Skies
Nonetheless, this is one intriguing idea. One of the benefits of using an actual aircraft — as opposed to the balloon concept envisioned in the Titan Saturn System Mission (TSSM) concept — is that AVIATR would not be carried at random by the local winds, but would have the ability to fly directly to a location and to remain at that site for as long as needed to study it. It would be capable of descending for close-in, high-resolution views (3.5 kilometers) and then returning to a cruising altitude somewhere in the neighborhood of 14 kilometers. There would be, in other words, no latitude restrictions for AVIATR, which unlike a balloon would be able to visit high-latitude lakes and polar regions as easily as the equatorial zone.
In terms of maximizing science, then, AVIATR is holding plenty of cards, and I haven’t even mentioned the fact that because the airplane would be flying at a significant fraction of Titan’s rotational velocity, flying west could keep our instruments on Titan’s daylight side for longer periods, maximizing the scientific return as well as the communications link with Earth. The airplane could also be conceived as fitting into a broader pattern of Titan exploration:
In addition to its own science, AVIATR could be a pathfinder for future landed missions at Titan – one of our objectives is to “Identify potential landing sites of scientific interest and constrain their safety”. Using our full instrument complement would allow us to discover places on Titan at which future missions may elect to land. These places may be of interest for geological, geophysical, chemical, meteorological, or astrobiological reasons. The best spatial resolution of the AVIATR cameras will be of the same order as that of HiRISE at Mars (25 cm/pixel), and this data will be able to constrain the engineering safety of surface environments for landers.
This could be a critical factor in future missions:
Such landing-site candidate analysis may include characterization of rock hazards, slope determinations, the persistence of liquid, and rover trafficability. Our global wind field measurements can reduce the size of the landing ellipse for those future missions as they descend through the atmosphere to their destinations.
Image: An artist’s conception of the parachuted descent portion of the AVIATR EDD sequence. Credit: Mike Malaska.
And while a large imaging instrument like HiRISE on the Mars Reconnaissance Orbiter can map the Martian surface in detail, we lack the same kind of imaging capability for Titan because of the opacity of the atmosphere and because orbiters need to keep to altitudes higher than 1000 kilometers here, so the kind of close-in look AVIATR can provide is otherwise unavailable.
A ‘Gravity Battery’
Taking advantage of AVIATR’s ability to climb and descend as needed, the team has worked out an ingenious method of power management that uses excess power — available when the vehicle is not transmitting data back to Earth — to climb to high altitude, storing these energies as gravitational potential energy in a process the team refers to as a ‘gravity battery.’ During periods of data transmission, the power to the propeller is drastically reduced and the extra power made available is then used to boost transmitted power for the uplink to Earth.
The plan the team discusses in their paper is to have one 8-hour downlink session to the Earth each day:
At the start of a downlink we cut power to the propeller, using that power instead to improve the total radiated power from the telecommunications dish. The airplane then glides for the entire duration of the roughly 8-h downlink (Fig. 34). Once we arrive at our lowest safe altitude of 3.5 km we return to straight and level flight and reduce the transmitter power if the downlink session is still ongoing. Otherwise at the cessation of the downlink we would again pour the extra energy into the propeller, beginning a new climb. We call this mode of operation “climb/glide”.
The team figures AVIATR can manage a one-year mission, but the paper also notes that there are no expendables here that limit the aircraft’s total lifetime beyond the gradual decay of the plutonium-238 that powers the Advanced Stirling Radioisotope Generators (ASRGs). We’ve gotten used to missions that extend well past their intended lifetime, and the AVIATR vehicle’s electrically powered pusher propeller could keep it airborne until the onset of some kind of mechanical failure. If that happens, or if it runs out of funding, AVIATR would descent to an area of soft dunes on Titan, possibly producing still more science for at least a brief period.
While we wait to see whether AVIATR makes it as a New Frontiers mission into the next planetary science decadal survey, a variety of matters still need attention, especially the question of the power output of the ASRGs in the atmosphere of Titan. Also needed: A tune-up of the instrumentation to Titan-specific conditions. All told, though, the AVIATR team sees no showstoppers here and strongly urges Titan airplanes as a part of future missions to the moon. See yesterday’s entry for the full citation of the paper on this work.
by Paul Gilster | Apr 5, 2012 | Outer Solar System |
Each of our highest priority targets in the outer Solar System offers something unique, from Europa’s internal ocean to the geysers of Enceladus. But Titan exerts the kind of fascination that comes from the familiar. The imagery of lakes and river channels reminds us inescapably of our home world, even if the temperature on the Saturnian moon averages a brisk 94 K, which works out to -291 degrees on the Fahrenheit scale. But because of its thick atmosphere we have options for exploring Titan that are unavailable on the other icy moons, and we’re working with a landscape that is a compelling frozen doppelgänger of Earth, a landscape we’d like to explore up close.
As we saw yesterday, part of the outer system puzzle is getting supplies of plutonium-238 up to speed, and there is at least some movement on that front. If we want to get aggressive about exploring Titan, one excellent way to deploy that plutonium is aboard AVIATR (Aerial Vehicle for In-situ and Airborne Titan Reconnaissance), a 120 kg airplane that could study the moon’s atmosphere from within and give us views of its geography on demand. Under study by a team led by Jason Barnes (University of Idaho), the airplane could do some things a balloon could not, including not being at the mercy of equatorial winds and being more flexible in studying some of the interesting terrain around high-latitude lakes and in the turbulent weather near the poles.
I’ve been thinking about AVIATR and other Titan options this week because last weekend I had the chance to speak with Mike Malaska, an organic chemist who has been collaborating with members of the Cassini team in research that involves characterizing the Sikun Labyrinth canyon-land region and hydrocarbon channels located near Titan’s South Pole. I discovered that Mike is also a volunteer artist for the AVIATR mission proposal. Like I said, Titan fires the imagination, and the idea of a human aircraft in operations there sounds too fascinating not to attempt. Mike’s image of the unmanned AVIATR vehicle flying over the surface of Titan is below.
Image: A rendering of the AVIATR airplane flying over Titan. Credit: Mike Malaska.
But back to that thick atmosphere, which helps us on Titan in so many ways. In an environment where gravity is seven times less than on Earth, we’re dealing with an atmospheric pressure one and a half times greater than Earth’s. It was Robert Zubrin who suggested, back in the 1990s, that humans with wings strapped to their arms would be able to fly in this thick and soupy environment. We’ve already seen evidence of this atmosphere’s effect on the Huygens probe, which took fully two and a half hours to descend to the surface in early 2005.
A paper on the AVIATR concept notes Titan’s advantages:
With an Earth-like surface shaped by rainfall and atmospheric interaction, a rich and complex chemistry, and the astrobiological potential of complex organic molecules interacting with liquid water, Titan is one of the three most interesting targets in the solar system for planetary exploration. Like Mars, but unlike Europa, Titan can be explored inexpensively. Although cruise times to Titan are long (?7 years), arrival at Titan is easy. Titan’s dense atmosphere with a large scale height is perfect for decelerating landers and aerial elements cheaply and with low heating and acceleration loads. Orbiters at Titan can be mass-efficient, too, if they utilize aerocapture…
The plutonium-238 issue becomes still more interesting because the new type of radioisotope thermoelectric generators NASA is examining seem made to order for an airplane in Titan’s atmosphere, while they’re unlikely to function in alternative balloon proposals. Called Advanced Stirling Radioisotope Generators (ASRG), the new RTG’s are considerably more efficient than their predecessors, requiring less plutonium-238 and producing less waste heat. Barnes and team argue in their paper that a hot-air balloon would not work on Titan with an ASRG because of its lower heat production — balloon designs would need to function with the waste heat from an MMRTG [Multi-Mission Radioisotope Thermoelectric Generator]. In fact, Barnes’ calculations show that the 500 W of heat from an ASRG would support less than 10 kg in a balloon, which is actually less than the mass of the ASRG itself.
Contrast this with AVIATR, which can use the longevity of twin ASRGs for extended operations on Titan. Setting aside the power requirements for computers, actuators and instruments, Barnes and company find they have in the neighborhood of 80 W to power up the propeller for straight and level flight operations. From the paper:
The propeller’s thrust on an airplane with singly folded wings can keep aloft an airplane with a mass up to ?120 kg. Other nuclear power sources, such as the MMRTG, cannot satisfy the physical requirements for heavier-than-air flight at Titan subject to appropriate engineering and risk constraints. Thus the use of an ASRG makes the AVIATR mission concept possible…
In fact, once deployed in Titan’s atmosphere, AVIATR should be in a benign environment:
Heavier-than-air flight on Titan is easier than anywhere else in the solar system. With over 4 times more air and 7 times less gravity than Earth, flight on Titan is 28 times easier than it is here (in the sense that a vehicle with the same contours flying at the same velocity on both planets could lift 28 times more mass). It is over 1,000 times easier on Titan than on Mars.
Long-duration flight is the name of the game, and AVIATR is seen as capable of carrying out a 1-year mission. The stability of the design would return the aircraft to straight and level flight in case the autopilot failed, in which case stabilizing vanes would deploy automatically to keep the aircraft in a stable position while pointing its antenna at the Earth to receive safe-mode instructions. The paper notes that the materials for the airframe are conventional and based on designs for unmanned aerial vehicles (UAVs) that operate here on Earth. AVIATR would also be more robust than a balloon in handling atmospheric turbulence and wind shear.
How would AVIATR be deployed, and how would it conduct flight operations? More on this tomorrow, when I want to dig a little deeper into the science and the unusual telecommunications strategy afforded by an aircraft on Titan. The paper is Barnes et al., “AVIATR—Aerial Vehicle for In-situ and Airborne Titan Reconnaissance: A Titan airplane mission concept,” Experimental Astronomy, Volume 33, Issue 1 (2011), pp.55-127 (full text).
by Paul Gilster | Apr 4, 2012 | Missions |
Powering up a spacecraft is a lot easier to manage in the Sun-rich environment inside the orbit of Mars than it is out past the orbit of Jupiter. Solar panels provide plenty of power for a satellite in near-Earth orbit, for example, but moving into the outer system invokes the need for RTGs — radioisotope thermoelectric generators — powered by radioactive decay. If you read through the specs on the FOCAL mission design presented here last Friday, you saw that this attempt to reach the Sun’s gravitational lens would demand 20 RTGs, and thus requires resumed production of plutonium-238.
What’s happened is that US production of 238Pu was halted as far back as 1988, leaving us with stockpiles that should be sufficient for missions in the pipeline through the end of this decade. That’s the view of Leonard Dudzinski, NASA’s Radioisotope Thermoelectric Generator program executive, who was speaking at the opening session of the 43rd Lunar and Planetary Science and the Nuclear and Emerging Technologies for Space 2012 conferences. The two conferences were held in conjunction with each other in Texas from March 19 to 23.
There have been negotiations between the US and Russia to buy plutonium from Moscow, but according to Dudzinski. quoted in a release from Aviation Week Aerospace Daily & Defense Report, the talks have stalled and, in any case, Russia’s own supplies of plutonium are rapidly dwindling.
Thus it’s good to hear that NASA and the Department of Energy are poised to fund and restart the production of plutonium-238 within six to seven years — NASA won congressional approval to spend $10 million during 2012 on the restart and is seeking similar amounts in 2013-14. Meanwhile, the development of the Advanced Stirling Radioisotope Generator (ASRG) continues, the latter possibly to be used on Discovery-class missions like the Titan Mare Explorer (TiME) and Comet Hopper, both of which are being reviewed by NASA for a 2016 launch.
Image: Artist’s impression of the Titan Mare Explorer (TiME) capsule. TiME would perform the first direct inspection of an ocean environment beyond Earth by landing in, and floating on, a methane-ethane sea on Saturn’s largest moon. Credit: Johns Hopkins University Applied Physics Laboratory/Lockheed Martin.
From the report:
DOE is close to completing a restart assessment that attempts to make the best use of current production facilities to generate 1.5-2 kg (3.3-4.4 lb.) of plutonium-238 annually… In all, NASA counts 28 of the radioactively fueled missions over a half century, requiring a 3-kg average annual production. The Voyager 1 and 2 missions, launched in 1977, remain active as they exit the Solar System.
Of more modern vintage are the Mars Science Laboratory (MSL) and Curiosity rover, along with the New Horizons mission, which is scheduled for a flyby of Pluto/Charon in 2015. The Advanced Stirling Radioisotope Generator (ASRG) has never flown, but it would be useful indeed, increasing the heat-to-power-generation efficiency of plutonium to 30% from the 5-7% allowed by the solid-state RTGs in use on MSL and New Horizons. As the various agencies move to restart plutonium-238 production, a parallel step will be to learn whether ASRG is flight-worthy.
It’s worth considering the context in which all this occurs:
The provocative backdrop includes the proposed sharp drop in proposed spending on planetary science in NASA’s 2013 budget; an ambitious decadal road map from the National Research Council (NRC) that includes missions to assess the habitability of Jupiter’s moon Europa and Saturn’s moons Enceladus and Titan; and a three-year-old NRC report that warns U.S. space leadership is imperiled if it does not resume plutonium-238 production.
Missions to the outer system demand RTG power sources, without which the exploration of high-value targets like Titan and Enceladus cannot proceed. We should learn this year whether the TiME mission, which would attempt to land a probe in one of the lakes of Titan, or the Comet Hopper mission to explore a comet from its surface are selected. In any case, a wide range of potential missions remain in the queue, including the fascinating AVIATR, an ambitious concept to fly a heavily instrumented airplane through the thick atmosphere of Titan. I’ll be talking more about AVIATR tomorrow as we continue to ponder power generation in deep space.
