A little early to start a topic maybe
I'm just so excited about this flyby.
I do have questions about this flyby.
1. What hemisphere will be imaged on this flyby?
2. Will Radar be used this time?
3. Any Non targeted Observations? (Besides Enceladus)
2 weeks to go!
I'm already excited!
*Trys to Kick start thred*
Will the Huygens landing site be studied further on this flyby? I think VIMS reveals the surface of Titan better than ISS. Will VIMS be used to on this flyby too?
VP will the Images be more to the east compared to the last flybys?
In his recent very informative NAI lecture, Don Lunine agreed that the best resolution for VIMS at Titan is indeed about equal to the best possible resolution for ISS, IF -- and it's a big if -- the latter is handled the right way. The reason, sez he, is that VIMS' CCDs aren't as sensitive as those on the ISS cameras.
There are a couple of new images of Titan available from jpl:
http://saturn.jpl.nasa.gov/multimedia/images/raw/raw-images-details.cfm?feiImageID=31851
http://saturn.jpl.nasa.gov/multimedia/images/raw/raw-images-details.cfm?feiImageID=31850
^ Very Nice!
Looking forward to the radar map.
I wonder whats taking so long for a Titan global map updates with the previous flybys.
Looks like some interesting features. Here is my enhancement. Two circular features look interesting.
Those features are also seen in an image that Sunspot posted to the Titan Surface Features topic on 12/17/04:
I thought at first that the bright semicircle had to be a cloud, but it is seen on the image from two months ago and has not changed. The more northerly structure definitely strikes me as a large impact crater that has been modified by fluids, something like http://antwrp.gsfc.nasa.gov/apod/ap001213.html in Quebec. The other feature seems odder. A mountain range left over from an impact? Or raised by some other process, like vulcanism?
I created a mask based on smoothed versions of images that only showed the atmosphere. I then partially subtracted an enhanced contast version of this from the original image. That brought out surfaced details without making the image look too terribly awkward. I would have done more, but the jpeg effects in the original image made this not useful. I think the Lake Lake Manicouagan analogy and the volcano idea are possible. Hopefully radar will cross one of these regions soon. Remember, after Mariner 7 they thought Nix Olympica was a crater. Nix Olympica ("Snows of Olympus," so-called because it is often surrounded by clouds and thus looked bright in groundbased telescopes without the resolution to reveal its true nature) turned out to be Olympus Mons. I doubt there is anything of that scale in terms of topography on Titan, but I bring this up to say you never know what a feature might be from imagery of this quality.
Ted
I havn't been able to find a picture showing the T3 SAR path so I made my own estimate
http://img142.exs.cx/my.php?loc=img142&image=t3sar2ds.jpg
Wow, very nice.
The first set of raw images are now posted.
Wow, look at the layers in the upper atmosphere.
http://saturn.jpl.nasa.gov/multimedia/images/raw/raw-images-details.cfm?feiImageID=31954
Nice map of the T3 swath, Jason, but there is another one at http://www.lpi.usra.edu/meetings/lpsc2005/pdf/1714.pdf (which also shows the T-a swath).
Looks like that radar swath gets close to that suspected crater to the side of the Sideways looking "H: figure.
Do we get close to it or part of it?
Oh. Sorry. I got you and Alan mixed up somehow.
Jason, your map seems to go up only about to 35° N but I thought that parts of the Titanian northern hemisphere were visible up to about 45° N for this season? Is there a northward extension of the map -- and how long will it be before we can get illumination of the entire northern hemisphere?
New RAW images have been posted, this is a great view of the haze layers in the upper atmosphere:
http://saturn.jpl.nasa.gov/multimedia/images/raw/casJPGFullS08/W00004800.jpg
Quite a few RAW images availbale here too:
http://ciclops.lpl.arizona.edu/view_event.php?id=10
Here's my attempt at processing one of the Titan RAW images
The circular feature should have been observed with the radar during the flyby .
RADAR!!
Giant Crater!
http://www.jpl.nasa.gov/news/news.cfm?release=2005-029
Wow! I wasn't expecting that until next week.
Giant cat scratches?
http://saturn1.jpl.nasa.gov/multimedia/images/image-details.cfm?imageID=1371
Very interesting...
Bill
Giant Crater? Are they referring to the large "bulls eye" feature visible in the image attached?
This is where I believe the radar patches are
http://s04.imagehost.org/view.php?image=/1919/radar_patches.jpg
I'm assuming the dark patches in the radar correspond to dark patches in the photos, I may be wrong.
Maybe Cassini should do more radar imaging and reduce on the images.
Clearly we are seeing the surface much better than imaging it.
Trust me, I thought I would never say that.
I think they are doing the maximum possible. The two patches that have been released are about 1/4 of the radar pass for this orbit. I suspect they were focusing on the atmosphere during Tb to prepare for Huygens so they had no radar pass then.
The radar views of Crater "Manicouagan"
show what I take to be two river systems flowing into the crater -- lower left corner.
So Titan DOES have some craters. Speak of the Devil (and assure everyone that he doesn't exist) and he shall appear. Obviously Titan has dramatically refaced itself, but not as dramatically as Io.
To my way of thinking, though, the most interesting thing in that image ( http://saturn.jpl.nasa.gov/multimedia/images/image-details.cfm?imageID=1372 ) is the economy-size drainage channel running INTO the crater on the lower left -- right across its rim, which it clearly cuts into. We badly need altimetry on this crater; it would appear that it really is a flattened-out, softened palimpsest with very little actual vertical relief (as suggested by the optical analysis of the previous fuzzy ISS images of it). And, by God, we are looking at really major-scale liquid flow across the surface of Titan -- something I never thought had a serious chance.
The second newly released SAR image ( http://saturn.jpl.nasa.gov/multimedia/images/image-details.cfm?imageID=1371 ) is at least as interesting. Those parallel grooves scattered across its field look to me exactly like analogies of those three weirdly super-straight and near-parallel drainage channels -- they're unlike any rivers on Earth; they look instead like irrigation ditches -- visible in Huygens' mosaic of the area that drains into its dark playa ( http://www.futura-sciences.com/communiquer/g/showphoto.php/photo/510/sort/1/size/medium/cat/525/page/1 ). I think that we are looking here at Ganymede-style tectonic parallel grooves and ridges, not at wind-carved phenomena -- with the liquid methane draining along the centers of such parallel valleys in the Huygens image.
By the way, Jonathan Lunine recently told either Aviation Week or Science -- I can't remember which -- that Cassini's later flybys do indeed need to be modified to provide more radar than had been thought.
I'm sure that a top priority for an extended Cassini mission will be full radar mapping of Titan. The wonders will never cease for years to come!
There are more channels visible in the lower right of the "cat scratch" radar image. These are, in fact, the upper reaches of the valleys which we see flowing into the crater in the lower left "Manicouagan" image -- I'm afraid someone with more skill than I have will have to patch the two together, but they do fit very nicely. This suggests to me that the "cat scratches" are actually a highland terrain, as the rivers appear to be flowing down from them.
To my eye it also seems that there are several channels flowing west to east from the western wall of the crater to a north-south "shoreline" within the crater. On the eastern wall there seem to be more channels that flow down the wall to the crater floor and then stop -- if the shoreline represents a single altitude, then perhaps the western floor of the crater is raised higher than the eastern floor.
It is very interesting to compare the ISS and RADAR images of this new terrain. EVERY dark patch in the ISS image is a grooved 'hole' in the RADAR image! The Ta-VIMS image also showed grooved terrain in the dark areas.
Maybe the entire surface of Titan is grooved, only covered with a thick 'snow'-layer in the bright areas such as Xanadu.
It is difficult to see depth in the RADAR-mosaic, but it looks like the ridged holes are lower than the bright stuff, as if the snow melted there to the bottom. In the lowerleft corner you can even see a small channel flowing into the ridged terrain.
I find it interesting that all the "scratches" are more-or-less parallel to the axis of the RADAR strip. If a ridge were to be perpendicular to this direction, would it be picked up in the image?
Bill
David, I think you're right about the bright ridges being the same material as the bright plains, and that dark line does look more like a crack to me now. However, the Huygens panorama also showed a lowlying dark basin with bright ridges in it...
I still think all of the reasonably large dark areas are ridged. Take a look again at the VIMS-Ta image. Compare it to part of the catscratch RADAR image ( same scale ). Both images are 150 km high.
New radar images!!!
http://saturn.jpl.nasa.gov/news/events/titan3/index.cfm
Second crater in two days... Who said Titan had no craters?
That is a very nice crater -- or two, if that's its little brother to the right and below.
But I still have not yet had my surfeit of channels:
http://saturn.jpl.nasa.gov/multimedia/images/image-details.cfm?imageID=1379
This is a beautiful image of at least three very large rivers flowing into a basin -- which, interestingly, appears bright in this image, like the rivers themselves -- and their lakes.
This patch is said to be just to the east of "Manicouagan" (which jpl insists on calling "Circus Maximus"
) but doesn't exactly fit; there seems to be a small gap between the two. Our ISS images of the area are also rather sketchy.
The big thing I'm taking away from this is that what appears dark in ISS images can be several different kinds of terrain! The "cat scratches" for one, but also this smooth radar-bright region.
ObsessedwithWorlds will happily note the presence of more grooves -- or, perhaps, ripples -- in the upper right of this image; perhaps comparable to those in the Ta VIMS image.
These *craters* look more like calderas to me. Notice that they seem to be positioned higher in the bright terrain. Very, very eroded rims but still bubble like non eroded features internally. The calderas even seem to have flows and crevasses on thier flanks (like glaciers). Perhaps this is what made the cat scratches that we see in the latest radar images. I am curious what some of you think.
Approximate positions of SAR patches
http://s05.imagehost.org/view.php?image=/0722/Radarpatches2.jpg
A movie showing the locations is here
http://www.nasa.gov/mission_pages/cassini/multimedia/pia07369.html
JPL retains its annoying habit of not publicly releasing the entire "noodle" (long, thin strip) mapped by Cassini's SAR on each flyby. I didn't get a good look at the whole strip from the T-A pass until it was finally released at http://www.lpi.usra.edu/meetings/lpsc2005/pdf/2294.pdf -- and there's a lot of interesting-looking stuff in parts of it other than those which WERE publicly released early on.
And, so far, the only view we've seen of the entire noodle from the T-3 pass is the very fuzzy view of it in this QuickTime movie. Notice the several bright, circular features on the left end. Are they additional impact craters? Who knows? JPL ain't giving us what we need to form an opinion yet.
I'm wondering when Cassini will get to turn its radar toward the Huygens landing site and compare the radar image with Huygens "ground truth". And it would be nice if Cassini could end up orbiting Titan to get a full look at its surface. Lots of interesting stuff....Titan is very reluctantly giving up its secrets.
Amen! I was waiting for someone to point that out.
I think they should focus more on Radar passes than imaging the surface.
Cleary
we are not seeing much with the imaging.

DOH!
There's been quite a lot of work on the likely height of waves on Titan -- and, yep, they would be several times higher (I'd have to do a little digging to get the exact estimates; Ralph Lorenz has done some work on it). The plan for determining whether a rough surface is waves or solid features is simply to re-observe it at different times and look for any changes in surface roughness that might be caused by changes in wind speed -- although, of course, this means that we can only check those small patches of Titan that will be SAR-mapped more than once, and it assumes that Titan's surface wind speeds change dramatically with time. (If I may bitch once again about the selection of instruments for Huygens: why didn't they put an anemometer on it as one of the Surface Science sensors?)
Yes, they can use Doppler to detect the speed at which Huygens was moving all the way down to the last moment before landing, and no doubt have done so.
As for the usefulness of an anemometer: they had no idea how long Hugyens would last on the surface. That three-minute figure was the period listed as defining officially complete mission success -- although they would hardly have been heartbroken if it hadn't survived landing at all; that part was always optional. If it DID survive landing, they thought it likely that it would continue to operate until the batteries wore out -- which meant at least 30 minutes. That period of time really would have made an anemometer (and a precipitation sensor) useful on the surface.
Once again, I don't understand why they instead put so many SSP sensors on Huygens that would be useful only if it landed in liquid -- and even then would only provide indirect compositional data that could be better provided by incorporating a heated core tube into the penetrometer shaft, with a feed to the GCMS.
I'm wondering why JPL didn't put there own probe on cassinni?
Yes indeedy. I've been following Cassini's history since 1978, when it was a mere twinkle in the eye of NASA itself -- and would have been an all-US project called "Cronus" (aka "Saturn Orbiter with Twin Probes") and including an entry probe of Saturn as well.
Indeed, I have a several-hundred page NASA document called "The Saturn System" which records the proceedings of a 1979 U. of Chicago conference to discuss its possible design -- and it's fascinating to see how much things have changed. After all, this was held even before Voyager revealed the utter weirdness of Jupiter's Galilean moons -- let alone the astonishing complexity of Saturn's rings (which at the time of the conference were still thought to be very simple in structure), or the strangeness of Enceladus. (The Committee agreed that the orbiter's official requirements should include flybys only of Iapetus and "one of the icy inner moons", since the latter were supposed to be very similar -- although it would be "desirable to add one small outer satellite to this list", presumably either Hyperion or Phoebe.)
In those days, they were talking about minimizing costs by basing both the main spacecraft and both entry probes on the Galileo designs as much as possible, just fiddling around with the experiment set a little. They were also thinking about launching it before the late 1990s Jupiter gravity-assist opportunity, which would have required fastening it to a solar-powered ion drive module that would have fired until partway through the Asteroid belt before being separated -- an idea they still very much have in mind for a lot of future outer Solar System missions.
Of course, the Shuttle was still in the process of sucking all the blood out of the US space science program at that point -- it hadn't quite completed the job yet. By 1982 that crisis had evolved further, and so the National Academy of Sciences study that recommended both Mariner Mark II and the Planetary Observer program (both of which soon died, to be reborn in new forms) suggested that the four most urgent Solar System missions after Galileo -- also including what later became Magellan, Mars Observer and the cancelled CRAF -- would be a simplified mission involving a Titan probe dropped off by a simplified spin-stabilized Saturn flyby craft (which would also make brief SAR and visible/near-IR observations of Titan). Had the ESA not decided to team up with NASA, the US might very well have flown this stripped-down Titan mission -- but Cassini allowed every part of the original ambitious SOTP scheme to be flown after all, except of course for the Saturn entry probe. (One study concluded that it would have been cost-effective to add that to Cassini -- but there just wasn't the money for it, especially since it would have required a larger version of the Titan 4's solid boosters.)
Interesting read. Thanks!
Complete radar swaths: http://volcanopele.blogspot.com/
T3 swath is full size. Wow.
And again: "cat scratches" in the dark areas! ![]()
These scratches have been described as windblown ripples, but I still think they look like cracks. The dunes on Mars look so different...
Linear dunes on Earth. Lake Eyre in Australia. Similar?
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