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PD0RDD > NASA     25.10.98 00:25l 124 Lines 6009 Bytes #-10028 (0) @ WW
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Onderwerp:  Jupiter's Moon Callisto May Hide Salty Ocean
Douglas Isbell 
Headquarters, Washington, DC              October 21, 1998 
(Phone:  202/358-1753)

Jane Platt
Jet Propulsion Laboratory, Pasadena, CA
(Phone:  818/354-5011)

RELEASE:  98-192

JUPITER'S MOON CALLISTO MAY HIDE SALTY OCEAN 

     Jupiter's second largest moon, Callisto, may have a liquid 
ocean tucked under its icy, cratered crust, according to 
scientists studying data gathered by NASA's Galileo spacecraft. 

          The Galileo findings, to be published in the Oct. 22 
issue of the journal Nature, reveal similarities between Callisto 
and another of Jupiter's moons, Europa, which has already 
displayed strong evidence of a subsurface ocean. 

     "Until now, we thought Callisto was a dead and boring moon, 
just a hunk of rock and ice," said Dr. Margaret Kivelson, space 
physics professor at the University of California at Los Angeles 
(UCLA) and principal investigator for Galileo's magnetometer 
instrument, which measures magnetic fields around Jupiter and its 
moons.  "The new data certainly suggest that something is hidden 
below Callisto's surface, and that something may very well be a 
salty ocean." 

     This premise was inspired by Galileo data indicating that 
electrical currents flowing near Europa's surface cause changes in 
Europa's magnetic field.  "This seemed to fit nicely with other 
data supporting the idea that beneath Europa's icy crust, a liquid 
ocean might be serving as a conductor of electricity," said 
Kivelson. 

     Armed with that information, Kivelson and UCLA colleagues 
Drs. Krishan K. Khurana, Raymond J. Walker, and Christopher T. 
Russell set out to test a similar theory about Callisto, "although 
it seemed far-fetched at the time," Kivelson said.  The team went 
back and studied data obtained during Galileo's flybys of Callisto 
in November 1996, and June and September of 1997. 

     Kivelson and her colleagues found signs that Callisto's 
magnetic field, like Europa's, is variable, which can be explained 
by the presence of varying electrical currents associated with 
Jupiter that flow near Callisto's surface.  Their next challenge 
was to discover the source of the currents. 

     "Because Callisto's atmosphere is extremely tenuous and 
lacking in charged particles, it would not be sufficient to 
generate Callisto's magnetic field; nor would Callisto's icy crust 
be a good conductor, but there very well could be a layer of 
melted ice underneath," Kivelson said.  "If this liquid were salty 
like Earth's oceans, it could carry sufficient electrical currents 
to produce the magnetic field." 

     Lending further credence to the premise of a subsurface ocean 
on Callisto, Galileo data showed that electrical currents were 
flowing in opposite directions at different times.  "This is a key 
signature consistent with the idea of a salty ocean," Khurana 
added, "because it shows that Callisto's response, like Europa's, 
is synchronized with the effects of Jupiter's rotation." 

     Although scientists consider the possible presence of an 
ocean on Europa as one factor hinting that life could have 
developed there at some point, it is doubtful that Callisto could 
harbor life, according to Galileo Project Scientist Dr. Torrence 
Johnson of NASA's Jet Propulsion Laboratory (JPL), Pasadena, CA. 

     "The basic ingredients for life -- what we call 'pre-biotic 
chemistry' -- are abundant in many solar system objects, such as 
comets, asteroids and icy moons," Johnson explained.  "Biologists 
believe liquid water and energy are then needed to actually 
support life, so it's exciting to find another place where we 
might have liquid water.  But, energy is another matter, and 
currently, Callisto's ocean is only being heated by radioactive 
elements, whereas Europa has tidal energy as well," from its 
greater proximity to Jupiter. 

     Galileo flies by Callisto four more times between May and 
September of 1999, which may yield more clues about the 
possibility of a Callisto ocean.  However, Kivelson said that 
scientists will rely heavily on theoretical models to test their 
interpretations about Callisto. 

     Kivelson and her team also are reexamining magnetometer data 
from Jupiter's largest moon, Ganymede, to address the tantalizing 
concept that Callisto and Europa may not be the only moons of 
Jupiter with subsurface oceans. 

     The latest Galileo exterior images of Callisto, released on 
Oct. 13, and a new artist's concept of a cutaway view of the 
moon's interior are available on the Internet at the Galileo 
website:  http://www.jpl.nasa.gov/galileo 

     Galileo has been in orbit around Jupiter, studying the huge 
planet, its moons and its magnetic environment, for over 2 1/2 
years.  It is currently in the midst of a two-year extension known 
as the Galileo Europa Mission.  Galileo is managed by JPL for 
NASA's Office of Space Science, Washington, DC.  JPL is a division 
of Caltech, Pasadena, CA. 

                               -end-

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