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New data from Cassini reveals Saturn's moon Titan has canyons filled with liquid methane

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http://www.extremetech.com/extreme/...i-reveals-titan-canyons-filled-liquid-methane

6106_PIA18432_feature-640x352.jpg


As recently as 2004, we knew Saturn‘s largest moon Titan basically as a fuzzy orange blob, a cold, Mercury-sized satellite of a distant gas giant. Scientists knew it had a dense, nitrogen-rich atmosphere — the only one that we knew of, other than our own — but they weren’t sure about how the atmosphere was organized, nor how the planet’s surface dynamics went. Now Cassini has changed all that. In a recently released study worthy of NASA’s Titan Hall of Fame, Cassini peers through the nitrogen fog at the surface, and specular highlights and radar measurements confirm our predictions. Titan is covered in surface features that are just like what we have on Earth… but a whole lot different, too.

It’s hard to describe Titan without getting a little breathless — the place is a little like Earth’s “upside down.” Earth is a wet, temperate planet, with continents bounded by surface water, clouds, and a water cycle. Titan is so cold that it has liquid methane, and yet it also has clouds and surface weather that imply a hydrocarbon cycle. There are lakes of methane near Titan’s north pole, and closer to its equator lie vast deserts of hydrocarbon dunes, made of granules of water ice coated in dark hydrocarbons that fall from the sky like rain. Perhaps upside-down-iest is the fact that there’s a hidden interior ocean of water and ammonia that covers the entire moon — submerged beneath the thick rime of frozen organic chemistry. It’s all topsy-turvy.


As hydrocarbon rain turns into rivers and carve through the surface, canyons proportionate to our Grand Canyon run with flowing methane. New photos from Cassini show us rivers of methane and ethane that stretch for hundreds of miles before they empty into Titan’s northerly sea, Ligeia Mare. And Cassini has been watching the transition from fall to winter at Titan’s south pole: Seasons on Titan last for seven years or so, and winter is coming. In fact, this is the first time anyone has ever seen the onset of a Titan winter. “We’re monitoring the weather on Titan, watching for predicted methane rainstorms at the north pole,” said Linda Spilker, Cassini project scientist at NASA’s Jet Propulsion Laboratory.

“I am intrigued by how many features on Titan’s surface are remarkably Earth-like,” said Spilker, “including hydrocarbon rivers, lakes and seas, and equatorial dunes, with liquid methane playing the role on Titan that water plays on Earth.”

Observations like the ones we get from Cassini and Huygens are important because they bear out our expectations about what we can safely infer from spectrographic readings of remote worlds. Before Cassini, we knew very little about Titan, except that we had seen nitrogen in its atmosphere with a spectrograph. Cassini’s instrumentation not only confirmed our predictions of nitrogen, but gave us the power to peer through the obfuscating atmosphere to the surface below — and beamed back a gallery of visual imagery to bring it all together. With a robust theory of Titan’s composition and chemical dynamics, we’ll be able to keep digging deep into our solar system’s history — and also rest more securely on the idea that we can point a prism at a planet light-years away, and still gather useful data that reflects reality.

Titan’s planetary chemistry also poses some fascinating questions about the origin of life, and what extraterrestrial life might look like on the fine scale. Think about this. The entire chemistry of life on earth depends on how life probably arose in seawater, a polar solvent. What sort of fantastical information-transfer biopolymer might life on a nonpolar planet employ? Imagine a DNA analog from a hydrocarbon planet, where the information is encoded in benzene rings and stereochemistry. If we can use Titan to advance our own understanding, we could put forth answers to some big questions about life, the universe, and everything.
 
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http://www.extremetech.com/extreme/...i-reveals-titan-canyons-filled-liquid-methane

6106_PIA18432_feature-640x352.jpg


As recently as 2004, we knew Saturn‘s largest moon Titan basically as a fuzzy orange blob, a cold, Mercury-sized satellite of a distant gas giant. Scientists knew it had a dense, nitrogen-rich atmosphere — the only one that we knew of, other than our own — but they weren’t sure about how the atmosphere was organized, nor how the planet’s surface dynamics went. Now Cassini has changed all that. In a recently released study worthy of NASA’s Titan Hall of Fame, Cassini peers through the nitrogen fog at the surface, and specular highlights and radar measurements confirm our predictions. Titan is covered in surface features that are just like what we have on Earth… but a whole lot different, too.

It’s hard to describe Titan without getting a little breathless — the place is a little like Earth’s “upside down.” Earth is a wet, temperate planet, with continents bounded by surface water, clouds, and a water cycle. Titan is so cold that it has liquid methane, and yet it also has clouds and surface weather that imply a hydrocarbon cycle. There are lakes of methane near Titan’s north pole, and closer to its equator lie vast deserts of hydrocarbon dunes, made of granules of water ice coated in dark hydrocarbons that fall from the sky like rain. Perhaps upside-down-iest is the fact that there’s a hidden interior ocean of water and ammonia that covers the entire moon — submerged beneath the thick rime of frozen organic chemistry. It’s all topsy-turvy.


As hydrocarbon rain turns into rivers and carve through the surface, canyons proportionate to our Grand Canyon run with flowing methane. New photos from Cassini show us rivers of methane and ethane that stretch for hundreds of miles before they empty into Titan’s northerly sea, Ligeia Mare. And Cassini has been watching the transition from fall to winter at Titan’s south pole: Seasons on Titan last for seven years or so, and winter is coming. In fact, this is the first time anyone has ever seen the onset of a Titan winter. “We’re monitoring the weather on Titan, watching for predicted methane rainstorms at the north pole,” said Linda Spilker, Cassini project scientist at NASA’s Jet Propulsion Laboratory.

“I am intrigued by how many features on Titan’s surface are remarkably Earth-like,” said Spilker, “including hydrocarbon rivers, lakes and seas, and equatorial dunes, with liquid methane playing the role on Titan that water plays on Earth.”

Observations like the ones we get from Cassini and Huygens are important because they bear out our expectations about what we can safely infer from spectrographic readings of remote worlds. Before Cassini, we knew very little about Titan, except that we had seen nitrogen in its atmosphere with a spectrograph. Cassini’s instrumentation not only confirmed our predictions of nitrogen, but gave us the power to peer through the obfuscating atmosphere to the surface below — and beamed back a gallery of visual imagery to bring it all together. With a robust theory of Titan’s composition and chemical dynamics, we’ll be able to keep digging deep into our solar system’s history — and also rest more securely on the idea that we can point a prism at a planet light-years away, and still gather useful data that reflects reality.

Titan’s planetary chemistry also poses some fascinating questions about the origin of life, and what extraterrestrial life might look like on the fine scale. Think about this. The entire chemistry of life on earth depends on how life probably arose in seawater, a polar solvent. What sort of fantastical information-transfer biopolymer might life on a nonpolar planet employ? Imagine a DNA analog from a hydrocarbon planet, where the information is encoded in benzene rings and stereochemistry. If we can use Titan to advance our own understanding, we could put forth answers to some big questions about life, the universe, and everything.
this is an old news, whats new in that:hitwall::hitwall::hitwall:
 
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this is an old news, whats new in that:hitwall::hitwall::hitwall:

hey I'm just relaying what NASA is reporting

http://www.jpl.nasa.gov/news/news.php?feature=6589

Cassini Finds Flooded Canyons on Titan
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NASA's Cassini spacecraft pinged the surface of Titan with microwaves, finding that some channels are deep, steep-sided canyons filled with liquid hydrocarbons. One such feature is Vid Flumina, the branching network of narrow lines in the upper-left quadrant of the imag

NASA's Cassini spacecraft has found deep, steep-sided canyons on Saturn's moon Titan that are flooded with liquid hydrocarbons. The finding represents the first direct evidence of the presence of liquid-filled channels on Titan, as well as the first observation of canyons hundreds of meters deep.

A new paper in the journal Geophysical Research Letters describes how scientists analyzed Cassini data from a close pass the spacecraft made over Titan in May 2013. During the flyby, Cassini's radar instrument focused on channels that branch out from the large, northern sea Ligeia Mare.

The Cassini observations reveal that the channels -- in particular, a network of them named Vid Flumina -- are narrow canyons, generally less than half a mile (a bit less than a kilometer) wide, with slopes steeper than 40 degrees. The canyons also are quite deep -- those measured are 790 to 1,870 feet (240 to 570 meters) from top to bottom.

The branching channels appear dark in radar images, much like Titan's methane-rich seas. This suggested to scientists that the channels might also be filled with liquid, but a direct detection had not been made until now. Previously it wasn't clear if the dark material was liquid or merely saturated sediment -- which at Titan's frigid temperatures would be made of ice, not rock.

Cassini's radar is often used as an imager, providing a window to peer through the dense haze that surrounds Titan to reveal the surface below. But during this pass, the radar was used as an altimeter, sending pings of radio waves to the moon's surface to measure the height of features there. The researchers combined the altimetry data with previous radar images of the region to make their discovery.

Key to understanding the nature of the channels was the way Cassini's radar signal reflected off the bottoms of the features. The radar instrument observed a glint, indicating an extremely smooth surface like that observed from Titan's hydrocarbon seas. The timing of the radar echoes, as they bounced off the canyons' edges and floors, provided a direct measure of their depths.

The presence of such deep cuts in the landscape indicates that whatever process created them was active for a long time or eroded down much faster than other areas on Titan's surface. The researchers' proposed scenarios include uplift of the terrain and changes in sea level, or perhaps both.

"It's likely that a combination of these forces contributed to the formation of the deep canyons, but at present it's not clear to what degree each was involved. What is clear is that any description of Titan's geological evolution needs to be able to explain how the canyons got there," said Valerio Poggiali of the University of Rome, a Cassini radar team associate and lead author of the study.

Earthly examples of both of these types of canyon-carving processes are found along the Colorado River in Arizona. An example of uplift powering erosion is the Grand Canyon, where the terrain's rising altitude caused the river to cut deeply downward into the landscape over the course of several million years. For canyon formation driven by variations in water level, look to Lake Powell. When the water level in the reservoir drops, it increases the river's rate of erosion.

"Earth is warm and rocky, with rivers of water, while Titan is cold and icy, with rivers of methane. And yet it's remarkable that we find such similar features on both worlds," said Alex Hayes, a Cassini radar team associate at Cornell University, Ithaca, New York, and a co-author of the study.

While the altimeter data also showed that the liquid in some of the canyons around Ligeia Mare is at sea level -- the same altitude as the liquid in the sea itself -- in others it sits tens to hundreds of feet (tens of meters) higher in elevation. The researchers interpret the latter to be tributaries that drain into the main channels below.

Future work will extend the methods used in this study to all other channels Cassini's radar altimeter has observed on Titan. The researchers expect their continued work to produce a more comprehensive understanding of forces that have shaped the Saturnian moon's landscape.

The Cassini-Huygens mission is a cooperative project of NASA, ESA (European Space Agency) and the Italian Space Agency. NASA's Jet Propulsion Laboratory, a division of Caltech in Pasadena, manages the mission for NASA's Science Mission Directorate, Washington. JPL designed, developed and assembled the Cassini orbiter. The radar instrument was built by JPL and the Italian Space Agency, working with team members fro
 
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