18 January 2005—European and American scientists
last Saturday morning unveiled the very first scientific
results sent back from the Huygens Titan probe following
its triumphant landing on Saturn's largest moon.
Though bleary-eyed from their all-night vigil, the
scientists gave a presentation that delighted a crowd of
journalists and staff assembled at the European
Space Agency's Space Operations Centre in Darmstadt,
Germany.
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In Living Color: An image from the Huygens landing site on
Titan. The rock-like objects may be ice blocks.
The two just below the middle of the image are
15 cm (left) and 4 cm (center) across and are 85
cm from the probe
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A joint project of NASA, the European Space
Agency (ESA), and the Italian Space Agency, the
Cassini-Huygens orbiter-lander mission was conceived
25 years ago to explore Saturn and its moons.
Piggybacked on the Cassini orbiter, the Huygens lander,
named for the 17th-century astronomer who discovered
Saturn's rings and Titan, was the European part of
the mission. On Friday, the 3-meter-wide
flying-saucer-shaped probe plunged through Titan's
thousand kilometer thick atmosphere, braving
extremes of heat and turbulence before coming to rest
intact on the moon's surface.
Images of Titan had previously been taken by
Cassini earlier in its mission and before it by the
Voyager probes in the early 1980s. But the pictures
frustrated scientists because of how hard it is to
discern the surface through Titan's thick, hazy
atmosphere. In contrast, the data sent back from
Huygens reveal with remarkable clarity features that
evoke things like riverbeds, rocks, and ground fog.
"We are the first visitors of Titan, and the
scientific data that we are collecting now shall unveil
the secrets of this new world," exulted ESA chief,
Jean-Jacques Dordain.
"It's almost impossible to resist the speculation
that this flat, dark material is some kind of drainage
channel," said Marty Tomasko, team leader for the
Huygens imaging component, about one image, "that
we're seeing some kind of shoreline, that we don't
know whether this still has liquid in it, or whether the
liquid has drained away or drained into the
surface." Indeed, experiments by the surface science
team indicate that the Huygens's landing site may have
the consistency of "wet sand or clay" topped by a
thin crust, leading one scientist to draw an analogy
to créme brûlée.
Scientists will spend years poring over the trove
of data returned during the few hours of transmission
from Huygens as it descended through the atmosphere and
landed on the surface, mirroring the years it took
to get Huygens to Titan.
After about a quarter-century of planning, the
lumbering Cassini finally headed into space in 1997 with
Huygens strapped to its back. It was heralded as the
last of the giant-sized, big-ticket unmanned space
missions.
But the seven-year Cassini voyage was not without
incident, and the Huygens mission was almost stillborn.
In 2000, ESA engineer Boris Smeds discovered a flaw in
the hardware onboard Cassini used to receive
Huygens's once-in-a-lifetime transmissions before
relaying them back to Earth (see "Titan Calling"
IEEE Spectrum, October 2004). The flaw meant that as
the smoggy atmosphere of Titan braked Huygens, the
deceleration would cause its transmission frequency
to shift due to the Doppler effect, and as built,
Cassini's receiver couldn't accommodate the shift.
Smeds's findings started a massive chain reaction
in NASA, ESA, and the mission's contractors to find
a fix. The solution involved altering Cassini's
trajectory, so that the orbiter would travel almost
parallel to Huygens's line of descent, reducing Doppler
shift to manageable levels.
So even though he was not an official member of
the Huygens landing team, it was no surprise to find
that Smeds was sitting in the Huygens control room
waiting to see if the fix worked and for the data to
flow onto their screens.