Geysers on Saturn's little moon Enceladus are throwing off Saturn's internal clock, making it hard to measure the length of the Saturn day. Image credit: NASA/JPLMarch 22, 2007
Pasadena, Calif. -- In a David and Goliath story of Saturnian proportions,
the little moon Enceladus is weighing down giant Saturn's magnetic field
so much that the field is rotating slower than the planet. This phenomenon
makes it nearly impossible to measure the length of the Saturn day using
techniques that work at the other giant planets.
"No one could have predicted that the little moon Enceladus would have such
an influence on the radio technique that has been used for years to determine
the length of the Saturn day," said Dr. Don Gurnett of the University of Iowa,
Iowa City. Gurnett is the principal investigator on the radio and plasma wave
science experiment onboard NASA's Cassini spacecraft. The radio technique
measures the rotation of the planet by taking its radio pulse rate -- the rhythm
of natural radio signals from the planet.
A new study of Cassini data reported this week in the online version of
the journal Science determined that Saturn's magnetic field lines, invisible lines
originating from the interior of a magnetized planet, are being forced to slip
relative to the rotation of the planet by the weight of electrically charged
particles originating from geysers spewing water vapor and ice from Enceladus.
These results are based on joint observations by two Cassini instruments-the radio
and plasma wave instrument and the magnetometer.
The neutral gas particles ejected from the geysers on Enceladus form a donut-like
torus around Saturn. As these particles become electrically charged, they are
captured by Saturn's magnetic field, forming a disk of ionized gas, or plasma,
which surrounds the planet near the equator. The particles weigh down the magnetic
field so much that the rate of rotation of the plasma disk slows down slightly.
This slippage causes the radio period, controlled by the plasma disk rotation,
to be longer than the planet's actual rotation period.
Scientists conclude the period Cassini has been measuring from radio emission is
not the length of the Saturn day, but rather the rotation period of the plasma disk.
At present, because of Saturn's cloud motion, no technique is known that can
accurately measure the planet's actual internal rotation.
Finding out the length of Saturn's day has been a challenge because the gaseous
planet has no surface or fixed point to clock its rotation rate. Initially, the
approach was to use periodic regular radio signals, as has been done for Jupiter,
Uranus and Neptune.
However, Saturn's radio period has turned out to be troubling in two ways. It seems
to be a pulsed signal rather than a rotating, lighthouse-like beam. Secondly, the
period seems to be slowly changing over months to years. The day measured by Cassini
is some six minutes longer than the day recorded by NASA's Voyager spacecraft in
the early 1980s, a change of nearly 1 percent.
"We have linked the pulsing radio signal to a rotating magnetic signal. Once each
rotation of Saturn's magnetic field, an asymmetry in the field triggers a burst of
radio waves," said Dr. David Southwood, co-author, Imperial College London, and
director of science at the European Space Agency. "We have then linked both signals
to material that has come from Enceladus."
Based on the new observations, scientists now think there are two possible reasons for
the change in radio period. The first theory is that the geysers on Enceladus could
be more active now than in Voyagers' time. The second is that there may be seasonal
variations as Saturn orbits the sun once every 29 years.
"One would predict that when the geysers are very active, the particles load down
the magnetic field and increase the slippage of the plasma disk, thereby increasing
the radio emission period even more. If the geysers are less active, there would be
less of a load on the magnetic field, and therefore less slippage of the plasma disk,
and a shorter period," said Gurnett.
"The direct link between radio, magnetic field and deep planetary rotation has been
taken for granted up to now. Saturn is showing we need to think further," said Michele
Dougherty, principal investigator on Cassini's magnetometer instrument, Imperial College London.
The Saturn radio emissions detected by Cassini have been converted into an audio
file available at: http://www.nasa.gov/cassini and http://saturn.jpl.nasa.gov .
The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency
and the Italian Space Agency. The Jet Propulsion Laboratory, a division of the California
Institute of Technology in Pasadena, manages the Cassini-Huygens mission for NASA's
Science Mission Directorate, Washington. The Cassini orbiter was designed, developed
and assembled at JPL. The radio and plasma wave science experiment team is based at
the University of Iowa, Iowa City. The magnetometer team is based at Imperial College London.
Media contact: Carolina Martinez 818-354-9382
Jet Propulsion Laboratory, Pasadena, Calif.
2007-032