As NASA’s Cassini spacecraft zooms toward Saturn’s smoggy moon Titan for a
targeted flyby on June 18, mission scientists are excitedly hoping to repeat a
scientific tour de force that will provide valuable new insights into the nature
of the moon's surface and atmosphere.
For Cassini’s radio science team, the last flyby of Titan, on May 17, was one
of the most scientifically valuable encounters of the spacecraft’s current
extended mission. The focus of that flyby, designated “T-101,” was on using
radio signals to explore the physical nature of Titan’s vast northern seas and
probe the high northern regions of its substantial atmosphere.
The Cassini team hopes to replicate the technical success of that flyby
during the T-102 encounter, slated for June 18, during which the spacecraft will
attempt similar measurements of Titan. During closest approach, the spacecraft
will be just 2,274 miles (3,659 kilometers) above the surface of the moon while
travelling at 13,000 miles per hour (5.6 kilometers per second).
During the upcoming flyby, if all goes well as before, Cassini’s radio
science subsystem will bounce signals off the surface of Titan, toward Earth,
where they will be received by the ground stations of NASA’s Deep Space Network.
This sort of observation is known as a bistatic scattering experiment and its
results can yield clues to help answer a variety of questions about large areas
of Titan’s surface: Are they solid, slushy or liquid? Are they reflective? What
might they be made of?
During the May encounter, Cassini beamed radio signals over the two largest
bodies of liquid on Titan, seas named Ligeia Mare and Kraken Mare. During that
first attempt, scientists could not be certain the signals would successfully
bounce off the lakes to be received on Earth. They were thrilled when ground
stations received specular reflections -- essentially the glint -- of the radio
frequencies as they ricocheted off Titan.
“We held our breath as Cassini turned to beam its radio signals at the
lakes,” said Essam Marouf, a member of the Cassini radio science team of San
Jose State University in California. “We knew we were getting good quality data
when we saw clear echoes from Titan’s surface. It was thrilling.”
A second technical accomplishment -- an experiment to send precision-tuned
radio frequencies through Titan’s atmosphere -- also makes the May and June
flybys special. The experiment, known as a radio occultation, provides
information about how temperatures vary by altitude in Titan’s atmosphere.
Preparing for these experiments tested just how thoroughly the Cassini team has
come to understand the structure of Titan’s atmosphere during nearly a decade of
study by the mission.
During this type of radio occultation, a signal is beamed from Earth through
the atmosphere of Titan toward the Cassini spacecraft, which responds back to
Earth with an identical signal. Information about Titan is imprinted in the
signal as it passes through the moon’s atmosphere, encountering differences in
temperature and density. The trick is that the transmitted signal must be varied
during the experiment so that it remains nearly constant when received by the
spacecraft.
In order to give the occultation experiments any chance of success, the team
has to account for not only the relative motions of the spacecraft and the
transmitting antennas on the rotating planet Earth, but also the ways the signal
is bent by different layers in Titan’s atmosphere.
While this procedure has been used successfully for several Saturn
occultations in the past two years, it had not yet been tried at Titan. And
since the Titan occultations last just a few minutes, the team was concerned
about how quickly the frequency lockup between ground and spacecraft could be
established, if at all. For comparison, NASA’s Magellan mission tried the
technique at Venus in the 1990s, without success.
As they waited for signs of confirmation during the May encounter, the team
saw the signal lock occur in only a few seconds, indicating that their
predictions were spot-on. Data on Titan’s atmosphere flowed in, adding new
information to the mission’s campaign to monitor the changing of the seasons on
this alien moon.
“This was like trying to hit a hole-in-one in golf, except that the hole is
close to a billion miles away, and moving,” said Earl Maize, Cassini project
manager at NASA’s Jet Propulsion Laboratory in Pasadena, California. “This was
our first attempt to precisely predict and compensate for the effect of Titan’s
atmosphere on the uplinked radio signal from Earth, and it worked to
perfection.”
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