NASA Probe Data Show Evidence Of Liquid Water On Icy Europa

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Nov. 16, 2011

Dwayne Brown 
Headquarters, Washington      
202-358-1726 
dwayne.c.brown@xxxxxxxx 

Marc Airhart 
University of Texas at Austin 
512-471-2241 
mairhart@xxxxxxxxxxxxxx 

RELEASE: 11-386

NASA PROBE DATA SHOW EVIDENCE OF LIQUID WATER ON ICY EUROPA



WASHINGTON -- Data from a NASA planetary mission have provided 
scientists evidence of what appears to be a body of liquid water, 
equal in volume to the North American Great Lakes, beneath the icy 
surface of Jupiter's moon, Europa. 

The data suggest there is significant exchange between Europa's icy 
shell and the ocean beneath. This information could bolster arguments 
that Europa's global subsurface ocean represents a potential habitat 
for life elsewhere in our solar system. The findings are published in 
the scientific journal Nature. 

"The data opens up some compelling possibilities," said Mary Voytek, 
director of NASA's Astrobiology Program at agency headquarters in 
Washington. "However, scientists worldwide will want to take a close 
look at this analysis and review the data before we can fully 
appreciate the implication of these results." 

NASA's Galileo spacecraft, launched by the space shuttle Atlantis in 
1989 to Jupiter, produced numerous discoveries and provided 
scientists decades of data to analyze. Galileo studied Jupiter, which 
is the most massive planet in the solar system, and some of its many 
moons. 

One of the most significant discoveries was the inference of a global 
salt water ocean below the surface of Europa. This ocean is deep 
enough to cover the whole surface of Europa and contains more liquid 
water than all of Earth's oceans combined. However, being far from 
the sun, the ocean surface is completely frozen. Most scientists 
think this ice crust is tens of miles thick. 

"One opinion in the scientific community has been if the ice shell is 
thick, that's bad for biology. That might mean the surface isn't 
communicating with the underlying ocean," said Britney Schmidt, lead 
author of the paper and postdoctoral fellow at the Institute for 
Geophysics, University of Texas at Austin. "Now, we see evidence that 
it's a thick ice shell that can mix vigorously and new evidence for 
giant shallow lakes. That could make Europa and its ocean more 
habitable." 

Schmidt and her team focused on Galileo images of two roughly 
circular, bumpy features on Europa's surface called chaos terrains. 
Based on similar processes seen on Earth -- on ice shelves and under 
glaciers overlaying volcanoes -- they developed a four-step model to 
explain how the features form. The model resolves several conflicting 
observations. Some seemed to suggest the ice shell is thick. Others 
suggest it is thin. 

This recent analysis shows the chaos features on Europa's surface may 
be formed by mechanisms that involve significant exchange between the 
icy shell and the underlying lake. This provides a mechanism or model 
for transferring nutrients and energy between the surface and the 
vast global ocean already inferred to exist below the thick ice 
shell. This is thought to increase the potential for life there. 

The study authors have good reason to believe their model is correct, 
based on observations of Europa from Galileo and of Earth. Still, 
because the inferred lakes are several miles below the surface, the 
only true confirmation of their presence would come from a future 
spacecraft mission designed to probe the ice shell. Such a mission 
was rated as the second highest priority flagship mission by the 
National Research Council's recent Planetary Science Decadal Survey 
and is being studied by NASA. 

"This new understanding of processes on Europa would not have been 
possible without the foundation of the last 20 years of observations 
over Earth's ice sheets and floating ice shelves," said Don 
Blankenship, a co-author and senior research scientist at the 
Institute for Geophysics, where he leads airborne radar studies of 
the planet's ice sheets. 

Galileo was the first spacecraft to directly measure Jupiter's 
atmosphere with a probe and conduct long-term observations of the 
Jovian system. The probe was the first to fly by an asteroid and 
discover the moon of an asteroid. NASA extended the mission three 
times to take advantage of Galileo's unique science capabilities, and 
it was put on a collision course into Jupiter's atmosphere in 
September 2003 to eliminate any chance of impacting Europa. 

The Galileo mission was managed by NASA's Jet Propulsion Laboratory in 
Pasadena, Calif., for the agency's Science Mission Directorate. 

For images and a video animation of the findings, visit: 

http://tinyurl.com/csukksm 

For more information about the Galileo mission, visit: 

http://solarsystem.nasa.gov/galileo 

	
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