NASA
PROBE DATA SHOW EVIDENCE OF LIQUID WATER ON ICY EUROPA
From
NASA
Nov.
16, 2011
"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.
[Liquid
water………? Well, we all know what that means!]
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