Titan is the oddity among the
moons and this is an effort to sort it all out.
It is a reservoir of volatiles that may be of actual economic interest
in the distant future.
In the meantime we are still at
least a generation away from actually landing on it and looking around.
This work at least shows us that
the upper crustal layer is floating on something that is liquid.
A Water Ocean on Titan
by Charles Q. Choi
This artist's illustration shows the likely interior structure of
Saturn's moon Titan.
The cool and sluggish interior failed to separate into completely
differentiated layers of ice and rock. In addition to the hazy surface of Titan
(yellow), the layers in the cutaway show an ice layer starting near the surface
(light gray), an internal ocean (blue), another layer of ice (light gray) and
the mix of rock and ice in the interior (dark gray). In the background are theCassini spacecraft and
Saturn, not to scale. Image credit: NASA/JPL
Oddities in the rotation of Saturn's largest moon Titan might add to growing evidence that it harbors an underground ocean, researchers suggest. Titan, which is larger than Mercury, is the only world besides Earth known to have liquid on its surface. Its seas, made of liquid methane instead of water, have often led to speculation as to whether or not they could host life.
In addition to its seas on its surface, scientists recently also
discovered hints that Titan possesses an internal ocean, one of water and
ammonia. Using radar to peer through Titan's dense atmosphere, NASA's Cassini spacecraft
found that over time, a number of prominent surface features had
shifted from their expected positions by up to 19 miles (30 kilometers),
showing that the crust was moving and suggesting that it rested on liquid.
Now Cassini's gravity and radar observations of Titan have discovered
more clues that it might have an underground sea.
Titan apparently has an orbit very similar to our moon's - for
instance, it always presents the same face toward its planet.
However, they noted that Titan's axis of rotation was tilted by about
0.3 degrees. This tilt, or obliquity, seems high, given the estimate of Titan's
moment of inertia, or its resistance to changes to its rotation.
One implausible reason for these findings is that Titan is a solid body
that is denser near the surface than at its center. "This is in
contradiction with all we know about others planets and satellites and
planetary formation processes," said researcher Rose-Marie Baland, a
planetary scientist at the Royal Observatory of Belgium
in Brussels .
Another more likely explanation is that Titan is not solid all the way
through, but has an icy shell overlying a liquid water ocean, an icy mantle and
an icy, rocky core. The research team's models can give a wide range of
thicknesses for the liquid ocean, anywhere from three to 265 miles (five to 425
km), as well as for the icy shell, anywhere from 90 to 125 miles (150 to 200
km).
"We found it very exciting to use some measurements that seem in
contradiction and to try to reconcile them," Baland said. "It was like
putting together pieces of a puzzle."
Still, the case for Titan having an underground ocean is not closed
yet. Its orbit and rotation might also be explained by a recent disturbance,
such as a collision with a comet or asteroid.
"Our analysis strengthens the possibility that Titan has a
subsurface ocean, but it does not prove it undoubtedly," Baland told
Astrobiology Magazine. "So there is still work to do."
Since life as we know it needs liquid water, if Titan does have a
subsurface water ocean that may increase the chances the moon could harbor
alien life.
In the future, Baland noted that she and her colleagues would like to
use this method to analyze Jupiter's four largest satellites, the Galilean
moons - Io, Europa, Ganymede and Callisto.
"The measurement of the obliquity of Europe
or Ganymede could bring additional evidence for subsurface liquid layers,"
Baland said.
Baland and her colleagues will detail their findings in a forthcoming
issue of the journal Astronomy and Astrophysics.
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