NASA Spacecraft Detects Changes in Martian Sand Dunes
Calif. -- NASA's Mars Reconnaissance Orbiter has revealed that
movement in sand dune fields on the Red Planet occurs on a surprisingly
large scale, about the same as in dune fields on Earth.
This is unexpected because Mars has a much thinner atmosphere than
Earth, is only about one percent as dense, and its high-speed winds are
less frequent and weaker than Earth's.
For years, researchers debated whether sand dunes observed on Mars were
mostly fossil features related to past climate, rather than currently
active. In the past two years, researchers using images from Mars
Reconnaissance Orbiter's High Resolution Imaging Science Experiment
(HiRISE) camera have detected and reported sand movement.
Now, scientists using HiRISE images have determined that entire dunes as
thick as 200 feet (61 meters) are moving as coherent units across the
Martian landscape. The study was published online today by the journal
Nature.
"This exciting discovery will inform scientists trying to better
understand the changing surface conditions of Mars on a more global
scale," said Doug McCuistion, director, NASA's Mars Exploration Program,
Washington. "This improved understanding of surface dynamics will
provide vital information in planning future robotic and human Mars
exploration missions."
Researchers analyzed before-and-after images using a new software tool
developed at the California Institute of Technology (Caltech) in
Pasadena, Calif. The tool measured changes in the position of sand
ripples, revealing the ripples move faster the higher up they are on a
dune.
The study examined images taken in 2007 and 2010 of the Nili Patera sand
dune field located near the Martian equator. By correlating the
ripples' movement to their position on the dune, the analysis determined
the entire dunes are moving. This allows researchers to estimate the
volume, or flux, of moving sand.
"We chose Nili Patera because we knew there was sand motion going on
there, and we could quantify it," said Nathan Bridges, a planetary
scientist at Johns Hopkins University Applied Physics Laboratory in
Laurel, Md., and lead author of the Nature paper. "The Nili dunes also
are similar to dunes in places like Antarctica and to other locations on
Mars."
The study adds important information about the pace at which blowing
sand could be actively eroding rocks on Mars. Using the new information
about the volume of sand that is moving, scientists estimate rocks in
Nili Patera would be worn away at about the same pace as rocks near sand
dunes in Antarctica, where similar sand fluxes occur.
"Our new data shows wind activity is indeed a major agent of evolution
of the landscape on Mars," said Jean-Philippe Avouac, Caltech team
leader. "This is important because it tells us something about the
current state of Mars and how the planet is working today,
geologically."
Scientists calculate that if someone stood in the Nili Patera dunes and
measured out a one-yard (one-meter) width, they would see more than two
cubic yards (1,500 liters) of sand pass by in an Earth year, about as
much as in a child's sand box.
"No one had estimates of this flux before," said Bridges. "We had seen
with HiRISE that there was dune motion, but it was an open question how
much sand could be moving. Now, we can answer that."
Scientists will use the information to understand broader mysteries on
Mars, like why so much of the surface appears heavily eroded, how that
occurred, and whether it is a current process or it was done in the
past. Scientists can now point to sand flux as a mechanism capable of
creating significant erosion today on the Red Planet.
The HiRISE camera provides unprecedented resolution in studying the
Martian landscape. NASA's Jet Propulsion Laboratory, Pasadena, Calif., a
division of Caltech, manages the Mars Reconnaissance Orbiter for NASA's
Science Mission Directorate in Washington. Lockheed Martin Space
Systems, Denver, built the spacecraft. HiRISE is operated by the
University of Arizona and was built by Ball Aerospace & Technologies
Corp., Boulder, Colo.