NASA’s SOFIA Discovers Water on Sunlit Surface of Moon
NASA’s Stratospheric Observatory for Infrared Astronomy (SOFIA) has
confirmed, for the first time, water on the sunlit surface of the Moon.
This discovery indicates that water may be distributed across the lunar
surface, and not limited to cold, shadowed places.
SOFIA has detected water molecules (H2O) in Clavius Crater, one of
the largest craters visible from Earth, located in the Moon’s southern
hemisphere. Previous observations of the Moon’s surface detected some
form of hydrogen, but were unable to distinguish between water and its
close chemical relative, hydroxyl (OH). Data from this location
reveal water in concentrations of 100 to 412 parts per million – roughly
equivalent to a 12-ounce bottle of water – trapped in a cubic meter of
soil spread across the lunar surface. The results are published in the latest issue of Nature Astronomy.
“We had indications that H2O – the familiar water we know – might be
present on the sunlit side of the Moon,” said Paul Hertz, director of
the Astrophysics Division in the Science Mission Directorate at NASA
Headquarters in Washington. “Now we know it is there. This discovery
challenges our understanding of the lunar surface and raises intriguing
questions about resources relevant for deep space exploration.”
As a comparison, the Sahara desert has 100 times the amount of water
than what SOFIA detected in the lunar soil. Despite the small amounts,
the discovery raises new questions about how water is created and how it
persists on the harsh, airless lunar surface.