There has been lots of discussion of a mission to Europa in the http://www.unmannedspaceflight.com/index.php?showtopic=1039. I thought that since a Europa mission seems to be once again becoming a possibility, it deserved its own thread for news, updates and discussion. I thought I'd kick things off with a summary of past efforts on a Europa mission, and on where things stand now. If I make a mistake, please correct me!
In the course of its prime and extended missions, Galileo found http://www.spacedaily.com/news/life-00p1.html under the icy surface of the planet. Planning began on a Europa Orbiter mission, with a projected arrival date of 2008, to confirm the presence of the ocean, characterize the thickness of the icy crust and identify places for a future landing. One thing to note about these earlier plans: they included a direct trajectory to Jupiter, presumably to minimize mission duration and qualms about RTGs re-entering Earth atmosphere after some (highly unlikely) targeting mishap. But NASA lacked a nice category of missions to place the Europa Orbiter in. Eventually it got lumped together with Pluto Express and Solar Probe in a Outer Solar System program labelled "Fire and Ice", a term which also got applied to the Galileo Europa Mission extension. Without a solid program to support it, (like Mars Exploration, Great Observatories, or Discovery) the mission looked like an orphan.
As Bruce Moomaw has well documented, attempts to kill off the Pluto mission led to a tug of war between NASA, the planetary scientists and the public, resulting in Congressional directives to NASA. Pluto Express became the Pluto/Kuiper Belt Explorer and then New Horizons and New Frontiers 1. (New Frontiers 2 is of course Juno.) But the cost for the Europa mission continued to rise, and the launch date recede, as the difficulty of radiation shielding and the large delta-v requirements hit home, and the mission's public profile fell. The launch date moved to 2010 and the costs moved over a $1b. Then along came Sean O'Keefe and JIMO, a justification for the Prometheus program through developing nuclear electric propulsion, not with RTGs, but with an in-space fission reactor. Launch got moved to http://www.astrobio.net/news/modules.php?op=modload&name=News&file=article&sid=713, http://www.spacedaily.com/news/outerplanets-03k.html, while the cost went even further http://www.space.com/businesstechnology/050406_prometheus_techwed.html.
With the arrival of Mike Griffin, JIMO was cancelled. As Griffin said to Congress, "It was not a mission, in my judgment, that was well-formed." But interest in a Europa mission remained and remains strong. In 2003 the National Academy of Science's http://books.nap.edu/catalog/10432.html flatly stated that a Europa Orbiter was the top priority for the next Large scale (aka Flagship) mission. (See page 196 of the report.) NASA's current http://www.hq.nasa.gov/office/apio/pdf/solar/solar_roadmap.pdf reaffirmed a Europa orbiter as the next flagship mission. The question as always is money. As Administrator Griffin said, "The Science Mission directorate wants to do a Europa mission, the National Academy of Sciences wants to do a Europa mission, I want to do a Europa mission. When we can afford it in the budget, we'll do it."
Evidence of that support beyond rhetoric and reports trickled out with a letter from Andy Danzler, NASA's Solar System chief, to the Outer Planets Assessment Group (OPAG). He reported that he had "funded a team to take a quick look at the boundary conditions of a mission to Europa, that is, how much power, mass, travel time, etc. for various realistic scenarios. For planning purposes, this group is looking at launch dates in the 2012-2015 range, although the later dates are more likely in terms of funding." For funding details however, we have to wait for the FY 2007 budget.
OK, now the good stuff.
The http://www.space.com/scienceastronomy/050614_outer_planets.html included http://www.lpi.usra.edu/opag/jun_05_meeting/presentations/EGE_Mission_Study.pdf for the mission. A kind of first draft which establishes a baseline which can be tweaked and modified to extract the best science return.
There are many things to like about this draft design:
* The mission is now permitted to use Earth flybys, and uses a proven trajectory, the same as used by Galileo (Venus-Earth-Earth Gravity Assist). This allows a BIG increase in the available mass.
* The orbiter uses RTGs, but not super advanced ones that require further years of development.
* The orbiter is similar to Cassini in appearance, with 2 engines, a cylindrical tank structure, RTGs at the base, the magetometer boom at the top, and space for a lander bolted to side. The similarities may make it easier to convince Congress that this is something NASA knows how to do. The most obvious configuration change is with science payload and HGA having switched places, and the addition of a radar array. And there looks like a camera the size of MRO's HiRISE!
* The mission is definitely Flagship in scope with a launch mass of over 7000 kg on a heavy lift launch vehicle. For comparison Cassini was 5712 kg at launch on a Titan IV, and Galileo was 2223 kg when launched using the Shuttle and an Inertial Upper Stage.
* There is a good opportunity for ESA participation with the lander and science instruments. NASA/ESA co-operation is on the agenda for the next OPAG meeting.
* The mission does not assume big upgrades to the Deep Space Network. If the http://dsnarray.jpl.nasa.gov/ does come along, that's just gravy.
* Despite the Europa focus, the mission appears to give at least part of a Galilleo II style tour with multiple flybys of the outer Galileans over 18 months. Only Io will have to wait.
The OPAG Europa working group is also expected to present further work at the next meeting in October. More details will emerge then. I think there is room for cautious optimism on this mission. While we won't be seeing a mission launch for at least another 7 years, the combined weight of the planetary science community does tend to get it's way in the long run. I think the momentum is finally starting to build.
Very nice work. (My saying this, by the way, has no connection whatsoever with your praising my work on the Great Pluto Probe War...) Absolutely the only error I can detect -- and I've long been obsessed with Europa exploration -- is that the original design for Europa Orbiter DID have a big radar array that in fact looked very much like this new one; it was just located at a different place on the craft.
And, yep, they seem determined now to add a very big HiRISE-type camera, in addition to the much smaller one they planned from the start. Not only are high-res shots of Europa important for understanding its surface processes; they're crucial for figuring out how to safely land spacecraft on what looks like a VERY rugged surface. While I'd love to see a small lander (if properly designed) added to this mission, however -- as would Jack Farmer -- it is very much up in the air whether they'll have the money to do so. (I'm currently planning a future article arguing that the best possible design by far for a small lander on this mission would be a penetrator rather than a surface lander.)
45% to 50% of the cost of the Europa orbiter mission is the cost of mission design and test.I would build 4 more space craft of identical design except for the mass set aside for the lander/probe.this mass would be used by a payload best suited for the target planet. targets? saturn(a cassini follow on) uranus and neptune. the 4th spacecraft would be insurence or a mission of oppertunity.
Europa/Io complete mapping is a must.
What a disappointment with mapping from Galileo. Even with the extended mission Europa is still poorly mapped.
I think you have to balance the size and capability of the spacecraft against the permissible frequency of visits. Because of Europa's distance, and the large delta-v required to go into orbit, a sequential program like that for Mars is not going to be feasible. So there is more demand for the number of question-answer cycles to be kept to a minimum, even if that means more capable, and hence more expensive missions.
When it comes to any form of lander, I think anything complex will send mission risk and cost too high. But penetrometers may be vulnerable to being axed once the squeeze begins for spacecraft resources and funding, even if we are looking at 7 tonnes for the mission. The Decadal Survey *did* identify a Europa orbiter and lander as separate missions, after all. If the lander is an international contribution, that would make it more secure.
The HiRISE style camera is interesting. Certainly the 30 day prime mission is way too short a time to return the amount of data involved in mapping at that kind of resolution. Since the mission will have a wide angle camera for the global mapping, the question would be where to aim the big mirror. One aspect of the mission that would help is the many flybys and steady final approach to Europa before orbit insertion, which would give lots of opportunities for preliminary surveys. Also, if the mission carried a lot of onboard memory, then once in orbit thumnails could be sent, and then selected detail returned. But at that point the mission team would have to make up its mind *fast* (i.e. on a daily basis) on what was to come back in high resolution.
With a HiRISE style camera, you can do an enormous amount of high quality "raster" style mapping of moons from a distance. Either with a framing camera or a pushbroom sensor (I'd go with framing cause of low light levels), you couild build up low-distortion gigapixel mapping mosaics before the spacecraft moves a lot or the moon rotates a lot.
Somebody do the math and tell me for Galileo-type orbits, what resolution you get 6, 12, 24 and 48 hours from a flyby of the 3 ice moons, and what resolution <km/pixel> you get on Io.
http://www2.jpl.nasa.gov/galileo/europa/hst.html
"Europa's oxygen atmosphere is so tenuous that its surface pressure is barely one hundred billionth that of the Earth,"
I guess my dream of having a stereo camera with 360 PAN capability on Europa shatters here. A soft lander seems impossible for now......
Even a simple very small lander (a kilogram of instruments) would be useful for learning some things that we'll need to know for a more complex lander/rover. The Hi resolution camera won't be able to resolve things better than a few meters, and will be unable to actually test the surface composition.
I was thinking more in the lines of a Melt its way threw type probe.
Or how about this!
I'm 30 now, I hope that before I kick the bucket that I'll know for sure if there is a Subsurface ocean or not.
Life or No life.
Just the fact that a ocean other than our own is out is very cool.
A subsurface/orbiter probe should be Top Priority. *Ducks at Tomato's*
I've been thinking for some time about a modified version of Ice Clipper, in which the spacecraft would be based not on Stardust (with a small impactor) but on Deep Impact (with a much bigger Impactor kicking up a much larger amount of debris, and kicking up almost all of it from depths far below the radiation-modified upper layer). The Impactor's camera could also get extremely high-res final photos which could provide additional valuable information on small-scale surface ruggedness for the purposes of lander design.
I've even wondered if it might be advisable to launch such a mission BEFORE the Orbiter; a high-res camera and near-IR camera on the main craft, coupled to a very high-capacity and high-speed data recorder, could get high-resolution terrain and compositional data on quite a respectable part of Europa's surface just from a flyby (like the "Firebird" Io flyby once proposed as a Discovery mission). One possible motivation for such a mission flying first has disappeared, though: Janus Eluszkiewicz's argument that Europa's upper layers might be riddled with large cavities that would seriously interfere with the depth penetration of a radar sounder -- making it advisable to test the effectiveness of Europan radar sounding from a flyby first -- has come under very serious fire on the grounds that he simply assumed that such cavities could exist when the physical evidence is against it: http://www.lpi.usra.edu/meetings/lpsc2005/pdf/2346.pdf .
And the big problem with a smash-and-grab mission remains: given the very small amount of surface material that it would collect, could even supersensitive Earth-based labs properly inspect the sample for biological evidence? (Especially since it's quite possible that the heating the samples would inevitably undergo as they plowed through the aerogel collector layer would break down organic compounds.) if so, it might be preferable to initially analyze Europa's ice using in-situ instruments, even given their greatly reduced sensitivity and flexibility, simply because they could analyze much bigger amounts of material. JPL's own design study for an initial lightweight Europa soft lander ( http://www.lpi.usra.edu/opag/jun_05_meeting/presentations/EGE_Mission_Study.pdf ; http://www.lpi.usra.edu/opag/jun_05_meeting/presentations/EGE_Science_Instruments_Trace_OPAG.pdf ) calls for such an organic-isotopic analysis -- using a combined liquid chromatograph and mass spectrometer -- as one of the two top priority instruments for a Europa lander, the other being a seismometer for data on ice-layer total thickness. I myself would regard organic analysis as even more important.
The problem is collecting a big enough sample for such analysis on a small lander -- and collecting it from a fair depth, below the radiation-scrambled surface layer, using a lightweight sample-collection system. The JPL study (which focuses on a surface lander, just because that's the one design it was contracted to examine) expresses concern about this, but doesn't mention specific solutions. A penetrator would seem to be the logical solution. The "Polar Night" Discovery mission proposed to analyze lunar polar ices -- which could well end up as the second in the new series of US lunar exploration probes -- called for three penetrators, each weighing only 30 kg, surviving a crash into the surface at 75 meters/sec and burying themselves 1-2 meters deep ( http://www.nrl.navy.mil/techtransfer/exhibits/pdfs/Info%20Sheet%20pdfs/Space%20Info%20Sheets/PolarNight.pdf ; http://www.mae.usu.edu/faculty/tmosher/GeneratedItems/media/Mosher.pdf ). They would each carry a neutron spectrometer (not necessary for Europa) and a mass spectrometer, and impact tests in which these instruments were fired into a 2-meter layer of plywood and exposed to 1200 Gs (four times their planned load) showed them surviving just fine.
Again, though, if interesting compounds are seriously diluted in the Europan ice, the problem is acquiring enough of them to analyze -- which might require a heated probe to melt its way down through several dozen meters of ice and filter diluted compounds out of the resulting large amount of meltwater ( http://lasp.colorado.edu/icymoons/europaclass/Chyba_Phillips_EurAbode.pdf ). But such a probe would almost certainly be too big to carry as a piggyback on Europa Orbiter.
If a small penetrator COULD have a chance of analyzing enough material to be worthwhile, however, it would seem vastly preferable to a surface lander as a piggyback on Europa Orbiter in almost every way. It would easily dig below the radiation-modified surface layer (unlikely to be more than a meter or so deep); it would be much lighter than a surface lander; it could land on virtually any terrain, no matter how rugged; it would bury itself and thus provide its own shielding from Jupiter's radiation (which is otherwise a major problem for a moderately long-lived lander); and it would couple its seismometer to Europa far more rigidly than a surface lander. It would probably be unable to obtain post-landing terrain photos, but it could record descent photos during the last few seconds before impact and play them back later for almost equally good imaging data.
Stop press! While poking around on the Web for the above note, I've just found that Paul G. Lucey -- the Principal Investigator for "Polar Night" -- is also working on "Thunderbolt: In-Situ Detection of Biotic Compounds on Europa" ( http://www.higp.hawaii.edu/cgi-bin/higp/directory.cgi?func=disp&searchname=PaulG.Lucey ). This is surely a Europa penetrator, and I intend to talk to him about it immediately.
Not being familliar with Luna-9, I checked it out and.....did the engineers include something of an easter egg in http://en.wikipedia.org/wiki/Image:Luna_9_landing_capsule.jpgimage?
Someone mentioned an impactor - how about using a small stream of impactors to blast successive craters, and at the end of the stream would be the instrument-laden lander itself? It might still need to drill, but not nearly as much.
Uh-uh -- you'd need a huge weight in impactors to blast a hole of any significant depth, whereas you could achieve much greater penetration for tremendously less weight just by making the probe a melt probe (or giving the surface lander a longer drill). To say nothing of the gargantuan targeting difficulties...
Back in 1998 I initiated a discussion list for landing a probe on Europa to explore its subsurface global ocean. Named Icepick, the discussion lasted until just a few months ago.
http://www.klx.com/europa/
You can read the discussions here. I think we hit on many if not most of the scenarios for making this mission plan a reality.
http://www.mail-archive.com/europa%40klx.com/
If someone wants to revive the Icepick list and get discussions going again, I would be most grateful. Jeff Foust ran the intial list and Web site.
Yep, that's the site where I got my start as a space commentator -- and where Simon first ran into me. Sad to see that it's finally disappeared. Maybe I should have hung around there, but I've been juggling several plates at one time for the last few years and just never got around to dropping back in. It starts to look as though the discussion site for Europa exploration may migrate over here.
Apologies if this has already been discussed, but on the OPAG site, there's http://dosxx.colorado.edu/%7Ebagenal/OPAG/ESSP_Report_Final2.pdf on Europa Surface Science options. It runs to 86 pages and covers radiation issues as well as landing methods. It was based on the JIMO as the mothership, but much of the discussion is still relevant, I think. I haven't had the chance to go through it in detail, but one point caught my eye: for 375 kg, you can soft land 167 kg on the surface using powered descent. For comparison, the Huygens probe had a mass of 320 kg.
Jeff: I saw that OPAG report -- and the two more recent papers att the OPAG site that I mentioned previously elaborate on it somewhat.
Hendric: The idea of a fiber-optic line for communications -- originally the favored idea -- got the boot several years ago, both because of weight problems and becuase the slow but steady ductile sliding of Europa's ice layers would almost certainly snap it. The current plan is to have the probe carry a stack of tiny disk-shaped radio repeater packages powered by tiny RTGs, and release one every kilometer or so that it descends -- so that they're close enough to pick up each other's radio signals through the ice and thus chain-link the signal from the melt probe all the way to its surface carrier.
I should add that the heat from the extremely tiny RTG that each such package would require would not be nearly enough to melt the surounding ice and make it sink deeper.
Wouldn't it? Let's say you want a 10W transmitter. You will need at least, I don't know, ~15W total for electronics and losses and such..? The abysmal efficiency of RTGs meas you will need at least a ~100W heat source to power the thing......ice is a very good insulator.....
I would very much like to see a plot of EM wave attenuation vs frequency for ice so that any "windows" could be identified and the necessary transmitter power could be constrained with higher confidence.
Hmm http://www.phys.hawaii.edu/~anita/web/project/meetings/fall03/Ice%20Measurements%20-%20Barwick.pptlooks interesting...
There are two relevant JPL Technical Reports on this design. Unfortunately, JPL's technical-report server seems to be offline for now, so I've attached both reports.
Actually, each transceiver would use a mere 0.12 W power source, hooked up to a capacitor to allow periodic bursts of 1.3 W transmission power. So that's why there's no RTG ice-melting problem.
And here's the other JPL report.
hmmm! very interesting thank you!
Was anyone at the recent (October) OPAG meeting where the new Europa Orbiter was due to be discussed?
The October report and documents aren't up yet, but surely it can't be too long now. Wonder how the talks with ESA went? Hope there was some more support for the 2013 opportunity, given the extra dry mass that could be delivered (probably enough for the soft lander studied by Balint, Nov. 2004).
Roly
I wasn't able to make it to OPAG, and have been monitoring their site for news on the presentations and final report from the October meeting. They haven't turned up yet, but I expect them soon.
http://www.lpi.usra.edu/opag/meetings.html
http://www.lpi.usra.edu/opag/reports.html
The presentations from the third OPAG meeting have just arrived: http://www.lpi.usra.edu/opag/oct_05_meeting/agenda.html . (The final report from the meeting isn't available yet, though.)
Though this may sound terribly obvious, any Europa landers/ocean explorers had better be designed to last a long time if their main goal is going to be the search for life on that Jovian moon.
Unless the ice crust is encrusted with dead microbes or such similar creatures and their alien jellyfish counterparts are saturating Europa's ocean, I do not want to end up with the same situation as the Viking landers, who were stuck on two tiny spots on Mars and had scientists and the media declaring the Red Planet a dead world (again) when a few scoopfuls of dirt revealed no native microbes. Europa will require a long exploration.
To add: The global ocean on Europa is estimated to be *60 miles* deep. Thankfully in one sense the moon's much smaller mass makes the bottom water pressure on Europa no "worse" than that found in the deepest parts of the Pacific Ocean (7 miles down), but if there are black smokers and alien versions of red tubes worms and giant crabs living around them, can we design a probe that could make it all the way to the bottom of the Europan Ocean and return the data to Earth?
Another question: Life may be able to survive on Europa in its present state, but based on what we know, could it ever have gotten off to a start in the first place?
The reply to the second question is simply: we don't know. We don't know whether life could have evolved out of prebiotic molecules on Earth had the water been as acid and/or saline as Europa's appears to be; there has been at least one abstract I've read expressing doubt, but given our stupefying continuing level of ignorance about how the chemical process occurred on Earth itself, we just don't know.
As for the first question: even if we don't get all the way down to isolated "smokers" on the floor of Europa's ocean, we should be able to detect microbes (or their remnants) from such locations spread uniformly through the ocean water -- after all, that's how life on Earth gets transferred from one isolated smoker to another and so survives after the first smoker finally goes out. And if the alternative theory is true that Europan microbes may derive their nourishment instead from chemicals manufactured by radiation in Europa's upper ice layer and then gradually transferred down to the ocen by geological processes in that ice layer, the principle is even more true -- in fact, in that case the life would probably be concentrated at the TOP of the liquid-water layer.
This also leaves the question of whether we can find evidence of microbes in Europa's liquid ocean without even having to bore down through the ice layer to the ocean, by instead analyzing the surface ice itself to look for such remains transported up to the surface by those same slow geological processes in the ice layer. The consensus seems to be that this is a real possibility -- but, since there's a thin layer of brittle supercold "nonconvective" ice 1-3 km thick on top of the warmer main ice layer which slowly convects (and which even perhaps carries pockets of still-liquid brine upwards), we are going to have to be careful to choose landing sites that look likely to have had buried material erupted all the way up to the surface. (There are several types of Europan surface features that show promise of this, which is another reason why we do need a Europa orbiter first to pick out good landing sites.)
The beauty of an RTG is that it creates a LOT of "waste" heat that can be put to use here for "free".
Also the electricity generation efficiency can be increased if there is an effective cold sink.
So an RTG probe is Perfect - as long as you don't hit a buried rock/meteorite.
Nick
If they do add a small lander to the first Europa orbiter -- and that is a very big "if" -- I've been a fan for some time of making it a penetrator rather than a surface lander, for a whole swarm of reasons:
(1) Such a penetrator can punch down a meter or two into the ice just by impact, giving it a good chance of getting below the radation-modified upper layer. (As far as I'm concerned, no lander that doesn't drill down that far is worth sending.)
(2) It could couple a seismometer -- the second most important instrument for a Europa lander, according to the science working group -- to the crust far more firmly than a surace lander.
(3) It would bury itself in the ice deeply enough to be shielded from Jupiter's radiation -- a very serious problem for an exposed surface lander.
(4) It could land on virtually any kind of terrain, no matter how rugged.
As far as I can tell, its ONLY disadvantage is that it would have more trouble getting post-landing surface photos -- but it could carry a descent camera and memory buffer to record and later play back the last few images before impact to get imaging data almost as good.
Sure enough, Paul G. Lucey -- the Univ. of Hawaii scientist who has proposed the "Polar Night" Discovery-class penetrators to look for lunar ice (they would weigh only 65 kg, penetrate 1-2 meters into the surface, and carry mass spectrometers which have already survived impact tests at four times the planned landing speed) -- is now proposing "Thunderbolt", a mission to look for Europan surface organics. He hasn't yet described it -- and I'm still waiting to hear any details from him -- but it is surely another penetrator mission.
However, there's another problem, as Chris Chyba pointed out in "Europa As An Abode of Life": the probe may have to process one hell of a lot of meltwater to filter out enough organics for study -- quite possibly 100 times more than any pentrator or small surface lander could possibly collect. We may have instead to fall back on a larger and later surface lander with an attached heated melt probe capable of melting down at least 100-200 meters, and filtering all the large amount of meltwater which it produces in the process. And while the waste heat from an RTG would do just fine to generate the melting heat -- that's been the plan from the start -- if Europa's ice is as highly saline as many think, a salt crust would build up ahead of any simple melt probe. It may need both a melting head AND a rotating drill head to chew through the accumulated salt. In any case, I don't see any way to put either of these on a penetrator.
Here's a use for an Europa Ocean Probe - as a neutrino detector!
Paper: astro-ph/0511243
Date: Wed, 9 Nov 2005 17:14:51 GMT (304kb)
Title: Development of Acoustic Sensors for the ANTARES Experiment
Authors: Christopher Lindsay Naumann, Gisela Anton, Kay Graf, Juergen Hoessl,
Alexander Kappes, Timo Karg, Uli Katz, Robert Lahmann and Karsten Salomon
Comments: 5 pages, 3 figures. Proceedings of the ARENA 2005 Workshop
\\
In order to study the possibility of acoustic detection of ultra-high energy
neutrinos in water, our group is planning to deploy and operate an array of
acoustic sensors using the ANTARES Neutrino telescope in the Mediterranean Sea.
Therefore, acoustic sensor hardware has to be developed which is both capable
of operation under the hostile conditions of the deep sea and at the same time
provides the high sensitivity necessary to detect the weak pressure signals
resulting from the neutrino's interaction in water. In this paper, two
different approaches to building such sensors, as well as performance studies
in the laboratory and in situ, are presented.
\\ ( http://arXiv.org/abs/astro-ph/0511243 , 304kb)
Anyone know if clay minerals exist on Europa, or could exist?
http://www.spaceref.com/news/viewpr.html?pid=18272
I know this has come up before but is it possible to do a Europa fly-by within a Discovery cost-cap?
Given that the Europa Orbiter is going to be 2012 at the earliest, surely there is scope for someone to propose something for Europa at the next Discovery AO.
I don't know that much about the design of orbiters, and this may
demonstrate (and probably does) some fundamental misconceptions, but I was
curious about a return to fly-by missions instead of orbiters like Galileo,
Cassini, EO etc. From what I have gathered, for many missions, the largest
problem is the energy required to brake into science orbit, particularly
where there is no potential for aerobraking, meaning a huge percentage of
the mass budget must be spent on a powerful engine and the requisite
propellant. I was under the impression that these problems were vastly
reduced in fly-by trajectories (?) With VEEGA trajectory perhaps this would be possible on a very economical LV (though it seems everything going forward is flying on Delta IV and Atlas now, not Delta II?) Okay so not a Taurus but there must be something in between Taurus and Delta/Atlas EELVs.
So instead of spending mass on an large engine with enough fuel to get into
a science orbit, couldn't the spacecraft instead focus on acquiring a huge
amount of data over a very short period of time in a low-altitude fly-by?
It would then sample a small area of the target at high-resolution.
It could carry (and I'm only guessing, the exposure/integration
times/pointing accuracy might make it truly impossible) stereo cameras and a
high
resolution imaging spectrometer on a motion compensation
scan-platform. All would operate
simultaneously, with power from advanced Solar arrays (Rosetta heritage?) lithium-ion batteries,
which would be charged during the cruise phase by the array to make up for any
power deficit during the very short and high-demand encounter phase. They could even be augmented with lithium primary batteries if required. The
spacecraft would be equipped with extremely wide and fast data busses,
caching the acquired data to memory and writing it out to solid-state disks
for later playback. No-RPS, easier admin. burden, compatibility with Discovery AO.
It would record this to high-capacity solid-state data recorders (multi-100s
GB), and then replay it once it had left its target, potentially over a
period of months or even years, depending on how much power was available,
local limits on the downlink and so on. This eases DSN management perhaps? Offline compression would be helpful, especially given that there might be issues with heavy compression in the Jovian environment (I'm suprised ICT did so amazingly well).
As an added bonus some of the
radiation hardening requirements would be reduced, as the spacecraft would
not be remaining in the most dangerous areas for a prolonged period,
repartitioning mass away from shielding and to the science payload. Lithium polymer batteries might be decent for providing some incidental shielding in any case.
I suspect I am heavily overestimating the ability of the scan platform to
provide adequate motion compensation, and the amount of time needed for the
instruments to acquire data - but I was curious about the idea because it
leverages some of the things that have become much better and cheaper over
time, like bus bandwidth, memory, disk write performance, processing power,
detector resolution/sensitivity - to replace things that have not, like
putting large amounts of propellant and engine mass into orbit.
I read a bit about Firebird recently, which seemed to utilize a similar approach. Perhaps there is geometry which would make possible a "Fire and Ice bird" (like the old JPL 'Fire and Ice' theme) ?
I've wondered out loud about this on other forums but no-one ever seems to have any ideas (other than Orbiters are better, which of course they are...)
Roly
It's not just that orbiters are better (though that rather goes without saying, in many ways).
First, there is the issue of time-and-change-dependent observations. If one of your goals at Europa is finding places where the ice crust is thin enough to provide some form of access to the ocean below, you need to observe Europa over a matter of weeks and months and track the movements of the crust.
Second, there is the issue of coverage. No matter how you design your approach trajectory, you're going to be able to observe only a tiny fraction of the surface during a fast fly-by. And there will only be one side sunlit during that snapshot. So no matter how capable a fly-by probe might be, its choice of what it can view is severely limited.
Lastly, there is the politics of funding. We are *barely* to a point where we can think about getting Congress to fund a Europa Orbiter mission -- a mission that we really need, in order to answer fundamental questions and set up a possible landing mission (and, more ambitiously, a mission to explore the subsurface ocean). Because of the points I raised above, a fly-by mission is far less likely to provide those answers, no matter how much data it returns about a very small portion of Europa. And now, *in addition* to funding an orbiter for a billion or more dollars, we're going to ask them to fund an interim fly-by mission for another half a billion dollars? If we were to do that, we'd end up with either the less-useful fly-by and NO orbiter, or (more likely) just getting laughed off the Hill for trying to get them to fund *two* different missions to the same chunk of ice millions and millions of miles away -- a chunk of ice most of them think is worthless in the first place.
Is that a little better answer than a simple "orbiters are better" statement?
-the other Doug
That is exactly the plan that has ALWAYS been written for Europa Orbiter -- it will make, first, about 6 flybys of Ganymede and about 3 of Callisto, and then (in the so-called "Tour Endgame") as many as a dozen close flybys of Europa itself to almost match orbits with that moon before orbital insertion. (For a drawing of a typical such tour, see page 10 of http://www.lpi.usra.edu/opag/jun_05_meeting/presentations/EGE_Mission_Study.pdf .) The whole process will take roughly 18 months, during which EO will soak up about 900 kilorads of radiation -- equal to the dose it will get during its 1 month in orbit around Europa itself.
As for aerocapture for EO, it's been considered, but -- besides the fact that aerocapture technology won't even nearly be ready for an EO launch by 2014 -- I was told at the COMPLEX meeting that studies indicate that aerocapture doesn't provide much of an advantage for this particular mission. (The plan, by the way, is also to use a flyby of Ganymede to help brake the craft into orbit around Jupiter initially, as Galileo used a flyby of Io for that purpose.) But -- even with all this gravity-assist -- half of EO's weight must be propellant. This is simply a difficult mission.
Another description of the "Tour and Endgame" can be found on pg. 23-26 of the most detailed description of the original Europa Orbiter concept at http://outerplanets.larc.nasa.gov/outerplanets/Europa_MPD.pdf . (One nice recent development: calculations now indicate that the total radiation dose that EO will get during this mission is less than half of the originally estimated 4 megarads. This by itself lops 200 kg off the needed shielding weight, and thus about 400 kg off the total spacecraft weight.)
Also, you'll notice that the Endgame involves only about half a dozen Europa flybys, rather than a dozen as I stated above.
Perhaps this will require a separate topic, but what will it take to put a lander on Io? Just imagine what surface images will look like from there!
That will be a while coming -- the radiation level at Io is 30 times that at Europa!
Thanks for the replies about the orbiters - the constitute the most compelling explanation yet of why you don't bother with fly-by missions unless the target is exceptionally hard. I can see the political point is also important when there is a [F]lagship class mission looking for money (that's a capital 'F' for the large clas flagship that EO will doubtless end up being).
Counting the days until EO arrives. I wish Juno could do some science on the Galilean moons, but I guess that's totally not the point, given the orbit. New Horizons Jupiter encounter should be great.
Roly
Yeah, it's been made clear to me by Scott Bolton that they don't WANT to fly Juno close to any of the Galilean moons, even if they get the chance. (Although I would presume that its camera could make some observations of Io's continuing activity.)
In fact, he's now made one interesting point that I had never thought of: Juno is definitely NOT going to have a long prolonged mission. It will have taken a considerable radiation dose by the end of its one-year primary mission, and they want to make sure it doesn't break down before they have a chance to deliberately crash it into Jupiter to make sure it doesn't eventually hit Europa. He's talking about an extended mission of -- at most -- one month, and they will in fact be monitoring its behavior carefully on the chance that they may have to end its mission a little ahead of schedule. (A landslide majority of its useful science will have been done by the first 6 months.)
This one is scientifically aimed at Jupiter -- period -- and (like Mars Climate Orbiter had it succeeded) it's going to do very little that will be of interest to the general public.
By the way, its launch has definitely been bumped now into July 2010 or August 2011.
Is the Europa Orbiter Still on? on was it replaced by Juno?
Just saw a program on Science Channel that mentioned it
You know this is very confusing lately. I was gonna suggest a area on this board with a listings of approved missions and future mission as well as canceled/on ice missions.
No, Juno AND the Europa orbiter (under its new name, "Europa Geophysical Explorer") are both planned, although EGE won't get its official program start until 2007.
However, one thing that is on hold for now is the previous plan for a Deep Jupiter Multiprobe mission, for which they won't give any go-ahead until they examine the Juno results -- that is, not for quite a while (since Juno won't arrive till 2016). There has recently been a very dramatic, but apparently firm, change in the science community's attitude toward the giant-planet entry probe program, which is yet another item in my "Astronomy" article that I must leave dangling for now.
My article will be appearing in either the February or March issue. Unfortunately, I ended up with enough material to write a 9.5 page article (AFTER extensive trimming), and so the editors will be hacking it down to 4 pages -- and I'm not sure what complete sections they're going to cut out to do so. I will, at any rate, try to get "SpaceDaily" to publish whatever info "Astronomy" doesn't; and anything relevant that gets cut out there will get put into this blog at some point, rest assured.
Nope, no blog -- I've never quite had the time and/or the nerve. (One recent "New Yorker" cartoon shows one dog telling another: "I considered starting a blog, but I finally just decided to go in for pointless barking instead.")
As for the article, they told me from the start that 4 pages was the length. The trouble is that whenever I attend one of these damn conferences, I get enough interesting material for SEVERAL articles, and then go through the torments of hell trying desperately to hack a 12 to 15-page article down to a few pages while the article bleeds and screams piteously. As with my 2004 article on the MER-A landing for "Astronomy", I finally just had to throw myself on the mercy of the editors by submitting an oversized article and letting them do the dirty work. (A far cry from those bright college days when I was straining desperately to inflate puny term papers.)
And I've always wondered why the articles are so fricken short.
Editors are evil. They should be outlawed.
Bruce:
I dunno what the copyright issues are (hopefully, you'd be paid *twice*), but perhaps the editors of Astronomy could be persuaded to do a web-only version of your articles, perhaps a month or two after the print version, and which would be somewhat longer? It'd be the sort of thing which might drive us guys to their website, thus giving them a double-whammy on the advertising...
There are publishing imperatives in print media which don't always suit in-depth articles, but there's no reason these days not to claim back the high ground on the WWW!
Bob Shaw
Heh. I dare say almost everything is a pact-with-the-editor story.. and I dare also say that almost everything is dulled down and bland-ized so that it won't 'confuse anyone'. Yeah, why make people think when they can just read pap that reinforces their already long-held beliefs.. WHERE'S MY PAYCHECK SO I CAN WATCH MORE 'FRIENDS'
But I digress...
Here
http://www.unmannedspaceflight.com/index.php?showtopic=1647
was dicussed the idea of using unconventionnal electronics to sustain the high temperatures (460°C) at the surface of Venus.
There was mainly three methods proposed:
-unconventionnal semiconductors
-micro-sized vacuum tubes implemented witht he techniques of integrated circuits
-micro-sized electrostatic relays
I note that the two latest proposals are also suited to resist to high radioactivity levels, so that they will be a good solution for a Europa orbiter (and even a Io orbiter) by increasing reliability and removing the weigh of shielding.
Developing such techniques will need only a series of small scale test, and then after a relatively short period of large scale development, in a total duration which is not uncompatible with the launching of the mission.
Uh-uh. Back when I was posting to the Europa Icepick website, I once did the actual calculations on the energy flux from Jupiter's radiation belts -- which turned out to be pathetically small: about five orders of magnitude less than you need to power a spacecraft! The belts are splendid at poisoning solid-state electronics (or biochemistry), but as a power source they stink.
However, running a long conductive tether from a spacecraft and letting it plow through Jupiter's intense magnetic field is a very different matter -- for an orbiter of Jupiter or one of the moons, that will work beautifully, if you're willing to put up with the tether.
"except that the mechanical forces acting on the cable were stronger than expected, breaking the cable"
Actually, they had undetected flaws in the insulation on the conductive tether, possibly some grit in the insulation or between it and the wire (not sure working from memory). It electrally shorted through to one of the pulleys or guides on the deployment mechanism, and the considerably higher ELECTRIC CURRENT than expected burned through and severed the tether. That part of the experiment worked too well... oops!
Yep. In fact, when I finally read about that incident in detail, I was startled to learn that it was due to a completely unexpected phenomenon that they still can't explain: they had an electrical arc run from the cable to the end of the deployment boom that -- amazingly -- continued to flow for several seconds after it had melted through the cable, while the end of the cable was drifting away from the boom. Apparently some kind of gas leaked out of the Shuttle to allow the arc, but they have never solved the mystery. This makes me a bit more inclined to forgive the Italians for having us fly that Shuttle mission twice and have it fail both times.
Some bad news about the prospects for a Europa Orbiter have just been posted by Lou Friedman of The Planetary Society
see this link:
http://www.planetary.org/programs/projects/explore_europa/update_12142005.html
first 3 paragraphs:
By Louis Friedman
December 14, 2005
In the recently passed NASA Appropriations bill, the US Congress directed NASA to begin work on a Europa orbiter and to make a request for a new start for a Europa mission project in fiscal year 2007. This was welcome news to NASA, who lost their focus on Europa when the nuclear propelled Jupiter Icy Moon Orbiter mission was cancelled last spring.
But now word has it that there will be no Europa proposal in the 2007 budget proposal that will be made to Congress early next year. The Washington Aerospace Briefing, a respected newsletter publication of Space News, is reporting that the Administration’s Office of Management and Budget is denying the Europa request on budget grounds.
The Planetary Society will fight for a Europa mission. Whether or not is in the budget request, we will lobby in Congress for its inclusion in the NASA program. Our Explore Europa Campaign is already in full swing. Having Congress insert funds in the ’06 budget was a good start, but we need to ensure support in 2007 and beyond.
NASA's science budget is a mess -- too many missions, several with large overruns. It would be irresponsible to add a $1B+ mission into the pie until everything else gets straightened out. What might be useful, though, is some early development money next year to get things moving again.
The plan was to just insert about $10 million this year for initial design studies -- including making absolutely sure that they DO want to fly Europa Orbiter before any of the other possible Flagship-class missions. Once again, we have a case of the idiotic manned program eating the rest of NASA alive.
The very fact that Congressmen fund NASA as pork to their home districts indicates that if the manned-program budget was cut, SOME of the money thus saved would get transferred to the unmanned program.
Actually, the Europa Orbiter is a good deal more complex as a mission than a replay of Galileo would be, given the technology and experience we now have. Indeed, a Jupiter orbiter that makes dozens of Io flybys is one of the second-rank candidates for a New Frontiers mission -- which means, given NASA's likely change to the NF proposal rules, that they'll accept ideas for it in the next round of NF selections in 2008. Such a craft would make Ganymede and Callisto flybys anyway to keep modifying its orbit to fly over different parts of Io's surface and at different phase angles, so it could easily be turned into a mission to study all three of the remaining Galilean moons. Indeed, it could be a virtual duplicate of the Europa Orbiter but with much less onboard fuel -- the radiation shielding for EO would allow such a craft to make at least 25 close Io flybys (maybe 50; I've got to recheck my records).
In fact, since EO itself will have to make a total of about a dozen Ganymede and Callisto flybys to get into position for Europa orbit insertion, it is virtually certain to make major observations of those moons -- and Jupiter itself -- during the 18 months or so before it goes into orbit around Europa itself.
There has always been a firm restriction applied to Europa Orbiter designs: no supplementation or change at all in the spacecraft for pre-Europa science. That being said, the new design for the mission -- which uses Earth gravity-assist flybys, and thus allows them to carry fully half a ton of additional payload into orbit around Europa -- would seem to provide some flexibility for this possibility.
I wince at asking this given the tight budget constraints, but has any thought been given to maybe adding a simple surface science experiment to EO? Something like the Deep Space 2 penetrometers with conductivity, salinity and maybe seismic sensors or a sonar transducer/receiver for crust mechanical property measurements could provide a LOT of vital information that is otherwise quite difficult or impossible to interpolate from remote sensing. A low-power low-rate UHF FSK data link would be quite sufficient for the probe support equipment suite, I would think...
Understand that the necessary sterilization procedures might prove too onerous and expensive for this to even be considered, aside from the existing budget problems...but the beauty of this concept is that most of the instrumentation I described has already been engineered to rugged deep-sea oceanographic standards as COTS equipment. NOAA uses this stuff all the time (and, no, I wouldn't expect them to punch through to any hypothetical ocean...but wouldn't that be cool!!!! )
The debate over whether to use that huge new payload margin to put a small piggyback lander on EO was one of the primary subjects at the November COMPLEX meeting, since there has already been quite a lot of design work on possible landers with varying degrees of complexity. (In particular, there was an unbelievably long drawn-out wrangle over whether a seismometer and magnetometer might be worthwhile on a small short-lived lander, which eventually began to resemble that 10-year debate among the savants on Jonathan Swift's Laputa over how long to boil a 3-minute egg.)
The group was nowhere near a recommendation when the meeting ended, but the impression I got was that there wasn't much enthusiasm because it is probably impossible for such a small lander to drill down deep enough into the surface to find any organic compounds that haven't been hopelessly scrambled by Jupiter's radiation -- and without that, the science return from a lander is just not that high. The leader of the team of graduate students who did the hypothetical "Endurance" lander design study described in a poster at the December AGU meeting told me that his group had reached the same conclusion: it would probably be more scientifically productive to put that extra mass into more Orbiter science instruments, a higher bit-rate communications system, and (especially) more shielding to prolong the orbiter's working lifetime in Europa orbit. (It takes 100 kg of shielding to extend the Orbiter's lifeime there by 1 month.)
Oh, well; at least it was considered. Thanks, Bruce!
I am surprised that surface (or just below!) conductivity/permittivity studies wouldn't be considered high priority; we could learn a lot about the amalgam of salts present in the crust--and therefore those present in the possible ocean--that way.
No "fiscal windfall", true. But it strikes me as an exaggeration to say that NASA would "not continue" without a major manned flight component. After all, the things keeping NASA going are (1) its actual valid justifications, and (2) its pork value -- and the latter includes spending on unmanned as well as manned projects. No doubt NASA's total budget would shrink, but it's very implausible that it would "not continue" -- instead, a lot of the Congressional and Presidential hunt for politically useful space pork would be transferred to the unmanned space program, leading to some degree of increase in spending the latter, and quite possibly a large one.
But that takes us to the obvious next question: what if NASA SHOULD vanish, and what if the unmanned space science program should also be radically shrunk after the manned program is eliminated, on the grounds that most space science projects are appallingly low in scientific cost-effectiveness compared to spending on other types of scientific research? We ourselves would certainly regret that, but you would have a hard time coming up with a morally convincing argument against it.
It's hardly surprising, however, that Plescia is pushing the manned program for all he's worth -- he has always done so, although virtually the only argument he's ever been able to come up with for the science value of humans rather than robots on the Moon is that the latter would have more trouble doing deep drilling operations.
Planetary Society Charges Administration with Blurring its Vision for Space Exploration
The Planetary Society Cites Cancelled Plans for a Europa and Other Science Missions
Pasadena, CA, — The NASA Budget released today shortchanges space science in order to fund 17 projected space shuttle flights. Despite recent spectacular results from NASA's science programs, this budget puts the brakes on their growth within the agency. It seriously damages the hugely productive and successful robotic exploration of our solar system and beyond.
According to this budget, flight projects that were already underway, such as the Space Interferometry Mission, will be delayed. Others, such as the Terrestrial Planet Finder and a mission to Jupiter's moon Europa, will be deferred indefinitely. Furthermore, the new budget slashes funding for the fundamental space science that makes such missions possible and turns raw data into discoveries.
http://www.planetary.org/about/press/releases/2006/0206_Planetary_Society_Charges.html
Outrage
Maybe, there will more robot exploration between Earth and Moon. These will be the first robots as a model to conquer to other planets. I bet after that, there will be a leap technology to explore others bodies of our solar system. It is a just a change of aim but the robot technology will continue improving and the there will be no lost time.
Rodolfo
I suppose I do have something to thank LBJ on in this respect -- even if he was the one who almost single-handedly persuaded JFK to launch the Moon Race (while telling his own friends that he had done so mostly to provide economic pork for the South). The Manned Spacecraft Center was originally supposed to be built in Vallejo, California before he rediverted it to Houston. Had he not done so, it would have been my own state's Senators who were constantly making dishonest jackasses of themselves on the subject of manned space exploration.
Spaceflight:
* Europa Mission: Lost In NASA Budget
http://www.space.com/news/060207_europa_budget.html
NASA's newly issued budget has lowered a flagship mission of exploration to
half-mast. Backed by scientists and study groups, a mission to Jupiter's moon
Europa is missing in action within the pages of NASA's Fiscal Year 2007 budget
unveiled yesterday.
Interesting quotes:
One additional payload on Europa Explorer: a simple lander.
Pappalardo said a lander is still being bandied about, but carrying what kind of technology and at what cost are questions awaiting answers.
“We’re not going to search for life with this mission. But just like the Mars rovers in their search for habitable environments…we’re going to characterize the habitability of Europa,” Pappalardo said.
An orbiter to the moon of Jupiter would allow a now sketchy view to become sharp as to how this world works, Pappalardo concluded. This mission, he said, has compelling science and broad community support and “we’re ready to go.”
and:
Also, the European Space Agency (ESA) is currently studying the Jovian Minisat Explorer (JME). The JME focuses on exploration of the Jovian system and particularly the exploration of its moon Europa. The ESA study is also looking into deploying a compact microprobe onto Europa to perform on-the-spot measurement of the moon’s ice crust.
* NASA Seeks 30-Percent Increase for Exploration Program
http://www.space.com/news/060206_nasa_budget.html
Efforts to replace the space shuttle fleet with new Moon-bound spacecraft would
receive big spending increases under NASA's 2007 budget request, while nearly
every other part of the U.S. space agency's budget would be held flat or
decline.
* SPACE NEWS: Policy or Politics? NASA Accused of Intimidating Climatologist
http://www.space.com/spacenews/businessmonday_060206.html
NASA is battling accusations that it tried to stifle its top climatologist, a
man well known for speaking his mind about the causes and consequences of global warming.
Remember this budget is just a request. Congress has the final decision on how much gets allocated to NASA. For several cycles, the Administration allocated no money to New Horizons, but Congress funded it anyway, and now it is on its way to Pluto. And it was Congress that told NASA to prepare to start a Europa mission last year. I would not be surprised if some small part of the 30% boost to ESMD is shaved off and tranferred for a Europa mission. The same goes for SIM. The important thing is that the scientists, advocacy groups and media push for it. That looks to be happening.
National Geographic:
NASA Budget Diverts Funds From Science to Spaceships
http://news.nationalgeographic.com/news/2006/02/0208_060208_nasa.html
See my post in
Policy and Strategy > The Creature That Ate Nasa Takes Another Big Bite
as to what you might be able to do to help remind Congress about Europa.
Let me suggest a conspiracy theory behind the EO cancelation. While money is sure to be tight, and an axe is going to be aimed somewhere, the choice of EO and TPF may have been performed by someone who wanted to see as little as possible in the way of cuts and reckoned slyly that those two missions are most likely to get a reprieve (by Congressional fiat). If so, putting them in harm's way, which they will, as my theory goes, escape, leads to the least eventual cuts, because putting some other projects in harm's way might have been harder to reverse.
In other words, the sort of campaign that saved NH is not to be considered an extraordinary follow-on to "the system", but part of the de facto system. And in some sense, these missions aren't in jeopardy until a similar movement fails to save them. Warm oceans nearby and earthlike worlds far off should perk some interest, what say...
I hope you are right.
I agree with Emily. These proposals are simply too big to be subject to this kind of subterfuge to preserve them. Moreover, Congress has already made it clear (with justification) that they are not going to spend any more on NASA as a whole - and the Administration has made it clear that it considers manned spaceflight much more important than unmanned spaceflight and space science.
As for WHY the Administration considers it so much more important -- well, we just got another clue yesterday, when the House GOP (as a consolation prize to Tom DeLay for getting the boot as House leader) gave him seats both on the Appropriations Committee, and on the subcommittee which oversees the Justice Department (which of course is currently investigating DeLay himself) and which also (as a result of DeLay's recent redesign of the House committee system) controls NASA. (The Manned Spacecraft Center is of course now in DeLay's district, and that earlier Washington Post article hinted that he was already the main figure keeping Shuttle/ISS from being trimmed back):
http://news.yahoo.com/s/ap/20060208/ap_on_go_co/delay_appropriations;_ylt=Ati99m85pYT69MCWIMPeIiFp24cA;_ylu=X3oDMTA5aHJvMDdwBHNlwN5bmNhdA
Both the White House and the GOP are still terrified of DeLay -- he is, after all, the one who knows where all the bodies are buried in the gigantic nationwide Tweed Ring that the GOP has now set up in this country -- and it's a safe bet that they will continue to give him everything he wants, if they think they can get away with it, until the moment when he is either indicted or defeated for reelection. After he's gone, we may see some fairly major readjustments in the NASA budget as a side effect.
Don't forget that the new budget also axes all preliminary research for Mars Sample Return as well -- and the message communicated to the November COMPLEX meeting by Andy Dantzler and Doug McKutcheon had been that Europa Orbiter is definitely higher-priority than MSR for now, and indeed should fly over a decade earlier.
What happened is simply that the continuing attempt to keep Shuttle/ISS going has bled off huge amounts of money from EVERYTHING else -- not just from space science, but from Bush's own manned lunar program (and his tentative moves toward a manned Mars program, which have now been totally eliminated). He wouldn't have done that unless he had been forced to do it.
I was, however, wrong in saying that that Nov. 21 Washington Post article ( http://www.washingtonpost.com/wp-dyn/content/article/2005/11/23/AR2005112301970_pf.html ) said that unnamed Congressional leaders were forcing him to do it. The actual passage is:
"Several sources confirmed that the budget office in the early negotiations proposed stopping shuttle flights altogether. 'It sucks money out of the budget, and it's a dead-end program,' one source said.
"But 'that argument's over,' another source said. 'The political side of the White House said, "We're keeping it." If you kill the shuttle right now, it will be heavy lifting for your foreign policy because of the international obligations' around the space station."
However, that argument -- as Jeffrey Bell points out -- is utter twaddle; we could end the Shuttle/ISS program much more cheaply and cost-effectively by simply repaying our "partners" for their wasted money, especially since they themselves are getting increasing local pressure about flushing money down the ISS rathole. Something else happened -- and the single most likely cause is indeed pressure from Congressional leaders. Specifically, Texan Congressional leaders, since Texas relies specifically on the manned part of the NASA programs, while Florida and the other states could adjust much more easily to NASA spending that was reoriented toward unmanned programs. Feel free to fill in the gaps.
"
Also, historically, note that Captain Crazy's proposals for Mars Sample Return were even loonier than his proposals for OP/SP -- MSR missions starting in 2003, at $500 million per flight -- and COMPLEX, I shudder to report, found that program entirely plausible in a review in November 1998:
http://www7.nationalacademies.org/ssb/marsarchmenu.html
Well, they were only 21 years and $1.5 billion off.
A bit more on Bugsy DeLay's possible hand in all of this at:
http://www.hillnews.com/thehill/export/TheHill/News/Frontpage/020806/news2.html
As I say, he knows where all the bodies are buried.
A few reality checks here:
There's a nice summary of them (and the remaining problems) on the second page of an LPSC abstract co-authored by none other than Bob Pappalardo:
http://www.lpi.usra.edu/meetings/lpsc2006/pdf/1459.pdf
Where Flagship missions are concerned, NASA's original plan was to fly one per decade to a non-Martian target in addition to its separate Mars program.
Even within its hoped-for yearly funding for the Mars Program alone, however, NASA had been having trouble fitting MSR into the Mars schedule -- which is why they ended up bumping it all the way to 2024. About a billion dollars worth of its total estimated cost (now roughly $4 billion) must be poured into preliminary R&D starting a decade or more before launch.
http://www.washingtonpost.com/wp-dyn/content/article/2006/04/01/AR2006040100022_pf.html
Is NASA in Outer Space?
Not After a Surprise Round of Budget Cuts
By Michael Benson
Washington Post
Sunday, April 2, 2006
page B02
© 2006 The Washington Post Company
In her NOVA interview, Carolyn Porco made it clear she would prefer to forgo Europa and take another stab at Enceladus.
As fascinating as Saturn is, I would prefer a fully-loaded Jovian mission first. There is much to learn.
You know, that's a good point -- Enceladus has geysers and Europa does not, at least not at present.
And yet, Europa's cratering record shows that its surface has been reworked pretty extensively over time -- there just isn't anything like the crater count that you find on, say, Callisto or portions of Ganymede.
On Enceladus, it's pretty obvious that the resurfacing is happening via the geyser activity. Older, more rugged terrain is being buried in massive "snowfalls" on Enceladus.
But on Europa, the relatively young surface isn't simply a visually homogenous covering layer of snow. It is a very complexly cracked surface that appears to have, at least at some pont, been a pretty thin covering over a large liquid ocean. As I understand it, it's hard to explain the cycloidal (I think that's the term) cracks if the ice layer has always been kilometers-thick.
But the Europan resurfacing *appears* to have had everything to do with repeated release of liquid water onto the surface and nothing to do with plume-deposited ice crystals. All slosh, no whoosh.
So, does this mean that Europa hasn't really seen geyser activity in the geologically recent past (i.e., since its last major resurfacing)?
And if so, what does the lack of such eruptions tell us about Europa?
-the other Doug
Rule 3.5 - un-needed quote removed - Doug
I could have sworn there was an article in a circa 1980 issue of Sky & Telescope
magazine that showed what might have been a plume on Europa. Does anyone
have the details/image?
There was some speculation by one researcher that that photo MIGHT show a plume -- but later study did not bear him out. Cynthia Phillips, in particular, has been going over every damn spacecraft photo of Europa ever taken looking either for plumes, or any signs at all of visible changes in surface features -- and, so far, she hasn't found a thing.
The evidence continues to grow that Europa undergoes cycles of varying levels of tidal heating, over periods of 50-100 million years, as it and the other Galilean moons slowly shift their precise orbital relationships -- and that at the moment it is in one of its cool periods, with a thicker crust and thus no cracks or vents punching through the ice (but with solid diapirs of warm ice, perhaps accompanied by local pockets of briny meltwater, slowly creeping up through the current thick ice layer to produce the "lenticulae" and chaotic terrain, which seem to exist on the fresher areas of Europa's crust).
I suggest that, since most of the water spewed off Enceladus' plumes immediately falls back onto the moon, the logical course is to touch down a modest distance from the plumes, just collect the falling snow, and then periodically melt, filter and analyze it for organic remains.
After all, even if (as Bob Pappalardo suggests) the plumes may just be due to ice sublimating off the surface of Enceladus, when that surface is heated from underneath by warm liquid water, you're going to get a conveyor-belt recycling over geological time -- the snow will reaccumulate on top of the ice near the plumes, and its weight will cause more of the ice on the bottom layer to sink down to depths where it in turn will be melted before later being refrozen into the bottom of the ice layer. And since Saturn, unlike Jupiter, does not have an intense radiation environment, there's a good chance that any biological or prebiological remains in the warm liquid water will survive for a long time on the surface after having been frozen into the bottom ice, slowly carried upwards by the solid-state convection in the ice, and then expelled onto the surface. (This, after all, is precisely why we're hoping for frozen biological remains in Europa's near-surface ice, once you dig down the relatively short distance below its radiation-damaged upper layer. In the case of Enceladus, the sampling is easier. And if Titan's cryovolcanism is as strong as it currently appears likely to be, a similar search for frozen biological remains in the surface ice from its probable subsurface ocean also makes sense -- and, in fact, the instrumentation for the suggested Titan Organics Explorer WOULD look for chirality in any surface organics that it finds.)
Clearly the first step is to try to (1) get more detailed information on the trace components in Enceladus' plumes; and (2) try to get a measurement of the precise surface temperature at the central source of the plumes. Which, of course, is prcisely what Cassini will be trying to do in its super-low 2008 flyby, which is why its controllers have decided to run that risk. (Notice how Enceladus, so far, has been the ONLY thing found in the Saturn system that has made Cassini's controllers change their original mission plan?) Only then -- and only after Cassini has also told us a lot more about Titan's global surface layout -- will we be able to make any reasonable judgement as to what to do about these three worlds, and the order in which we should do it.
If Enceladus does indeed have a conveyor-belt snow recycling system, then it might also be that we'd find analogous sites to the Antarctic locations where meteorites fetch up. By sampling along such a 'shoreline' where fresh snow gets trapped and sublimates away, we might have access to the greatest repository of objects from other worlds anywhere we've yet found!
Bob Shaw
You misunderstand me. Once the snow lands a certain distance away from the warm regions where the ejection of water vapor occurs (either by direct geysers or by sublimation of ice from the top surface of the warm regions), it stays in place permanently. And the only debris carried up with the water, even if geysering occurs, is possible rocky material from Enceladus' interior -- and then it won't be kicked a long way from the geysers unless it's quite fine material. (If the plumes consist of water vapor just sublimating off a warm ice surface, no other material at all will be spread farther by the plumes, except of course for the trace gases mixed with the water vapor -- but the glacially slow convective "conveyor belt" of warm ice creeping upward in the central warm region, and descending again in the cooler peripheral regions where the snow is accumulating, might carry some rocky debris from the interior up to the surface in the plume regions.)
In any case, those trace gases that get expelled along with the water vapor explain the frozen CO2 and other "light organics" which the VIMS HAS seen spread on the surface for some distance from the vents, along the Tiger Stripes -- and getting a better look at the composition of those other substances with the VIMS must be yet another urgent goal of the coming super-close 2008 Enceladus flyby. (Bob Pappalardo, by the way, obligingly sent me copies of the "Science" articles on the VIMS and mass spectrometer findings, which I'm reviewing right now and will report on later.) If it turns out that the plumes ARE just due to vapor boiling gently off the surface of a quite wide area of relatively warm ice, then it would almost certainly be safe for a lander to touch down right in the middle of the plume region -- and analyze the ice right there to see what else was oozing up from Enceladus' interior along with the warm ice.
I just have to ask this question: When it comes to Scientific information, would a mission to Enceladus provide more information than a mission to Europa assuming no life, or complex organics, are found?
I know the liquid water = life argument is trotted out with regularity, but that is still pretty uncertain. At least a Europa Orbiter, or some analagous mission, would provide us with lots of extra information on the Galilean Moons, but this proposed Enceladus mission seems totally focused on life,life,life. If the life does not show up, then it would seem that the mission would be mostly a waste. It seems a bit risky to me.
I would hope that the people at NASA can conceive that -there may be liquid water there-, and -we may get clues to the formation of the solar system- are not the only good reasons to send out space probes. Io, for example, is a fascinating place. There is also a certain satisfaction is getting the first good images of an object that was previously just a dot or a smudge, at least to me. That's pure exploration.
So what I am saying is that I find throwing away a mission that will return valuable, non-search-for-life science , in return for a mission with a remote chance of hitting the jackpot, rather reckless.
I must respectfully disagree with you, James. Although finding life on Enceladus via a lander mission would of course be the scientific coup of Western civilization, in situ observation of the plume processes and associated chemistry would still be valuable in its own right, and certainly enlightening in a wide variety of ways.
Consider: We don't really understand why Enceladus is even active at all at this time. Pure tidal influences seem inadequate; is there something unique about the moon's geochemistry? This is a valid research question with profound implications for the formation of the Saturnian system that alone would justify a lander.
By comparison, Europa does not seem to demonstrate any recent cryovulcanism (although I acknowledge that the Galileo dataset may not have been sufficient to rule it out completely) despite the fact that it's much more massive than Enceladus and also exposed to significantly greater tidal stress.
Therefore, if forced to choose (as we must given the newly austere budget environment), it seems rational to study the more geologically active target in detail first. Finding life would be nice, but it cannot be the entire rationale for such high-risk missions.
[size=2]
Back to the subject of the Europa Orbiter, I think that we need to call
Griffin on his remarks last week at the NSS (National Space Symposium).
He suggested that we wait 10 years until the heavy-lift CLV and CaLV
are available. Then, NASA could fly a Jumbo mission to Europa.
This is the same old trick that Goldin, and company, tried in 2000 when
NASA wanted to cancel a mission to Pluto. At that time, it was suggested
that we wait until an advanced nuclear ion propulsion system becomes available.
Then we could launch a Pluto probe on a really fast trip to that planet.
Fortunately, Congress saw through the "smoke-and-mirrors" and added
funds to NASA's budget for the New Horizons probe. As the UMSF community
can see in another post on this site, the advanced propulsion effort, Project
Prometheus, has been cancelled.
I hope that Congress is not tempted to believe that there is merit in Griffin's
suggestions at the NSS. We need to reject Griffin's siren call to wait, and
instead get on with a mission to Europa using technology already in hand.
Another Phil
As if flying a scientific mission on a man-rated mammoth booster would ever be an option. How many unmanned probes did we launch on the Saturn boosters? Even when they they were ordered and payed for, they were send to a museum rather than to Jupiter or Saturn. Mr. Griffin's suggestions are starting to sound pretty desperate, if you ask me. I still hope ESA can play a leading role in a Europa orbiter, it seems such a logical next step.
Pluto was a special case - the atmosphere is a ticking bomb waiting to go bye bye - we needed to get there by X to have a good chance of investigating it before it froze out.
I agree that Enc and Eur can 'wait' as it were. But only for financial reasons (i.e. we can't afford them at the moment) however - there is no need or requirement for the new heavy LV for those missions. If what you're building busts an Atlas V Heavy, Delta IV Heavy or any other LV mass budget, then you need to be more creative with your mission - slingshots, ion prop - whatever it takes.
Doug
Doug
The Skylab booster was the Apollo 20 Saturn 5. The abandoned flight vehicles were the boosters for 18 and 19. However, there are 3 Saturn 5's on display!
All of them incorporate parts from something that LOOKS like a Saturn 5 but was never a flight vehicle: the "Facilities checkout vehicle"... used to test VAB/Crawler/Launch-Umbical Tower/Pad equipment, including fueling exercises. But it didn't have real engines or lots of other stuff.
Things are a bit more complicated than that IRL, but you'd need to read the exhaustively detailed new book on Saturn 5 to find out.
So, if it's not NASA (too much vision), not Russia (never been interested) and not ESA (ExoMars will keep them busy)... who is going to take us back to Europa/Titan/Enceladus?
BTW, I thought I heard something like using a Saturn (I or V, don't remember) for launching a Viking style mission to Mars or even a Voyager type mission to the outer planets. Is there any truth in that?
Cugel,
There were plans in the 1960s for a mission to land on Mars called... beleive it or not ... Voyager.
Those missions, I think planned to start in 1973, would have used Saturn launch vehicles. One plan I can recall even had a dual launch on top of a Saturn V !!!!!
Well, Voyager got canned due to the amazing costs (I think). Born out of the ashes was a slimmed down mission called Viking. Slimmed down, that is, at a then staggering final cost of one billion dollars (roughly 4 bilion today, I think).
A few years later, the TOPS mission - Thermoelectric Outer Planets Spacecraft - was also canceled due to the high costs. It was replaced by a slimmed down mission called Mariner Jupiter-Saturn. There are many stories of the ressurection of the mission.... one version has it that the OMB was actually surprised that TOPS was killed since they had bought into the idea of the economy of multiple spacecraft of identical design visiting so many new planets all in one mission. Thus, they were very receptive to a lower cost mission that addressed many of the same goals. Another point often made was that the very name Mariner implied design inheritance and continuation of a very sucessful program. Recall that Mariners were the first to Venus, Mars, and Mercury.
Several years into the program, I think people decided that since Viking was a snazzier name than something like Mariner Mars 75 would have been... why not do the same with mariner Jupiter-Saturn? Eventually, much to everyone's surprise, NASA came up with Voyager, in spite of the fact that the name was linked with a politically dead project.
I'm not sure what this portends for the future. I can't think how you could name a future mission JIMO for example... unless the acronym was changed to "JIMO - Justification for Incredible Monetary Overruns".
Thanks! Apparently, I got it mixed up.
Very interesting links!
Here is an interesting new twist to the Europa Orbiter and SIM sagas. As posted on
NASA Watch, a letter from Rep. Wolf appears to be directing NASA to alter their
FY06 Operating Plan so that NASA obeys Congress' specific instructions to start
funding the Europa Orbiter project, and to maintain proper funding for SIM.
Doesn't this mean that Mike Griffin has now been warned that he is in danger
of breaking the law unless he immediately takes steps to comply with Congress'
directions?
You can check out the letter at this site.
http://images.spaceref.com/news/2006/Wolf.Op.Plan.04.07.06.pdf
Another Phil
Actually, it isn't that dramatic. Wolf simply demands that NASA add another $28 million to aeronautics research and $30 million to the Mars program (with no specifications on how it should be spent), and that it "continue funding for Terrestrial Planet Finder [not SIM], and...begin planning for a mission to Europa in fiscal year 2006...With the exception of these significant deviations from Congressional direction, the Commitee has no objection to the allocations of funding proposed in your letter."
Besides the vagueness on just what that $30 million more for Mars is supposed to be for, Wolf doesn't give any order how much NASA should spend this year on Europa Orbiter planning (50 cents, maybe?) And I've said before that I think Terrestrial Planet Finder spending, like Mars Sample Return planning, can be safely delayed for several years until we have a better idea just what general kind of mission we actually want to fly. (In the case of TPF, there are two completely different possible mission concepts; and which of them should be chosen depends very strictly on Kepler's census of how common Earthlike planets really are -- something we won't have until 2012 at the earliest.) Nor does Wolf tell us what projects he thinks that funding should be pulled out of.
Here's a bit from Emily's write-up of the OPAG meeting:
http://planetary.org/blog/article/00000567/
I'll put in here the full sales pitch comparison from Karla Clark:
EO = Europa Orbiter (cancelled 2001)
EE = Europa Explorer (current idea from JPL)
Instrument mass: EO: 27 kg; EE: 180 kg
Instrument power: EO: 27 W; EE: 100 W
Number of instruments: EO: 4; EE: 10
Lander: EO: not possible; EE: 340 kg mass available (which had some audience members shaking their heads, as a chunk of that will be taken up in margin)
Duration: EO: 30 days; EE: 90 days plus
Data return: EO: 100 Gb; EE 3000 Gb
Extended mission possible: EO: none; EE: 125 days.
--Emily
That's what was said at the Europa Focus Group, too. (I have no idea whether "Astronomy" will EVER get around to printing my small Web article on that meeting, although they did pay me for it -- and even if they do, I doubt it contains much by now that Emily hasn't since reported on her blogsite anyway. Grrrr.)
I don't know why they've eased up on sterilization requirements -- it may just be that they decided, after reexamination, that the initial ones were simply too costly and unjustified. I hope NASA isn't cutting corners on this; as the 2000 SSB report ( http://www7.nationalacademies.org/ssb/europamenu.html ) pointed out , if you get a single viable germ into Europa's ocean it could spread all the way around that world almost immediately -- which is not the case with Mars.
Two other notes about the redesigned Europa Orbiter (now rechristened "Europa Explorer", as Bob Pappalardo recently indignantly reminded me). First, (as Emily has also now pointed out), it now has a large gimballed, swivellable high-gain antenna, allowing it to take data and relay it back to Earth simultaneously and thus vastly increase its total data return. Second, besides the decision to utilize Earth and/or Venus gravity assists to send it to Jupiter -- which by itself utterly revolutionized the mission design by doubling or tripling the spacecraft's possible mass -- there's been another stroke of luck: the latest reanalyses of Galileo's radiation measurements indicate that the expected dose for a Europa orbiter is only half that previously estimated, allowing them to economize greatly on radiation shielding while still tripling the craft's previous 1-month design life in Europa orbit.
I just saw Emily's entry on the second day of the new OPAG meeting, which was devoted to discussions as to how to try to deal with NASA's space-science spending problems ( http://www.planetary.org/blog/article/00000573/ ). Cripes! In retrospect, it was an understatement for me to say earlier that space scientists have now hit the "Raft of the Medusa" stage -- they've now gone far beyond that, and are now eating not only each other but themselves. (They are, apparently, also now considering trying to save Europa Orbiter by cancelling not just the next Discovery and New Frontiers selections, but also the 2011 Mars Scout.)
As we wait for NASA to come to their senses and start work on the Europa
Orbiter, here is an image to whet our appetites. According to NASA, it is the
highest resolution image of Europa obtained by Galileo. This image is from
Galileo's 12th orbit around Jupiter and was recorded on December 16, 1997.
I've always liked this image as it reminds one of the view you would
get looking out of an airplane window (I know that Europa has no atmosphere.).
I consider it in the same class as the famous Lunar Orbiter 2 oblique photo
of the crater Copernicus obtained about 30 years before the Europa image.
It's been over 8 years since the Europa photo was taken. How many more years
before we get back - 8? 10? 15?
Here is the Europa photo
http://photojournal.jpl.nasa.gov/jpeg/PIA01180.jpg
Here is the Copernicus photo
http://upload.wikimedia.org/wikipedia/en/2/2d/Lo2_h162_3.gif
At the rate we are going I hope to see any probe to Europa. I'm 30 now.
I was hoping for a Subsurface Probe buy the time I was retired.
Wow, the added context puts the view into perspective. I recall seeing the left half image separately before, but did not associate it with the right half image. I gather you "mind the gap" comment is referring to the data dropout, but I also find "gap" going from side to side striking, particularly in revealing the cross sections on the right side.
Thanks for posting the image!
Has anybody ever done a photometric analysis of this image to try to determine how much of the dark areas is due to genuine sun-angle shadowing, and how much is due to dark-albedo material in the lower-altitude places?
Noticed that the slab at the bottom left fit neatly into the mid-left section. Like putting a jigsaw puzzle together
I wonder if the slabs on the top and bottom drifted apart and the blocky terrain welded up from below. That blocky piece of terrain has a different texture all together, sort of chaotic, where the two slabs are much more grooved.
Remember the Voyager days, when Europa was touted as being "the smoothest object in the solar
system"? Now, everybody talks about how rough the surface is for a landing !
For those Europaphiles who might have missed this, from the Planetary Society. Additional info is on Emily's TPS blog. The House Subcommittee, at least, wants to see a Europa new start.
http://www.planetary.org/about/press/releases/2006/0614_House_Subcommittee_Helps_Save_Our.html
June 14, 2006
House Subcommittee Helps Save Our Science
Pasadena, CA, — The fiscal year 2007 budget proposed by the Administration for NASA threatens to end a dazzling era of planetary exploration. Today, the House Appropriations Subcommittee on Science, the Departments of State, Justice, and Commerce, and Related Agencies marked-up the NASA budget, prior to sending the budget to full Committee.
The subcommittee today approved a budget of $16.7 billion, $100 million less than that requested by the Administration. But, it restored $75 million (out of $330 million) of the funding that the Administration had cut from space science plans. ...
Especially noteworthy was $15 million directed for a mission to explore Europa, the icy moon of Jupiter, with a subsurface ocean that is considered by many scientists as a possible habitat for life. This had been cut out of the plan by the Administration, and The Planetary Society vigorously campaigned for its reinstatement. Rep. John Culberson (R-TX) has been a strong supporter of this mission. Funding for the Terrestrial Planet Finder mission was also provided, another mission that the Society strongly supported.
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