The spacecraft, which entered Mars’ orbit September 21, now is lowering its orbit and testing its instruments. MAVEN was launched to Mars in November 2013 to help solve the mystery of how the Red Planet lost most of its atmosphere.
“All the instruments are showing data quality that is better than anticipated at this early stage of the mission,” said Bruce Jakosky, MAVEN principal investigator at the University of Colorado, Boulder. “All instruments have now been turned on — although not yet fully checked out — and are functioning nominally. It’s turning out to be an easy and straightforward spacecraft to fly, at least so far. It really looks as if we’re headed for an exciting science mission.”
Solar energetic particles (SEPs) are streams of high-speed particles blasted from the Sun during explosive solar activity like flares or coronal mass ejections (CMEs). Around Earth, SEP storms can damage the sensitive electronics on satellites. At Mars, they are thought to be one possible mechanism for driving atmospheric loss.
A solar flare on September 26 produced a CME that was observed by NASA satellites on both sides of the Sun. Computer models of the CME propagation predicted the disturbance and the accompanying SEPs would reach Mars on September 29. MAVEN’s Solar Energetic Particle instrument was able to observe the onset of the event that day.
“After traveling through interplanetary space, these energetic particles of mostly protons deposit their energy in the upper atmosphere of Mars,” said SEP instrument lead Davin Larson of the Space Sciences Laboratory at the University of California, Berkeley. “A SEP event like this typically occurs every couple weeks. Once all the instruments are turned on, we expect to also be able to track the response of the upper atmosphere to them.”
The hydrogen and oxygen coronas of Mars are the tenuous outer fringe of the planet’s upper atmosphere, where the edge of the atmosphere meets space. In this region, atoms that were once a part of carbon dioxide or water molecules near the surface can escape to space. These molecules control the climate, so following them allows astronomers to understand the history of Mars over the last 4 billion years and to track the change from a warm and wet climate to the cold, dry climate we see today. MAVEN observed the edges of the martian atmosphere using the Imaging Ultraviolet Spectrograph (IUVS), which is sensitive to the sunlight reflected by these atoms.
“With these observations, MAVEN’s IUVS has obtained the most complete picture of the extended martian upper atmosphere ever made,” said MAVEN Remote Sensing Team member Mike Chaffin of the University of Colorado, Boulder. “By measuring the extended upper atmosphere of the planet, MAVEN directly probes how these atoms escape to space. The observations support our current understanding that the upper atmosphere of Mars, when compared to Venus and Earth, is only tenuously bound by the Red Planet’s weak gravity.”
IUVS also created a map of the atmospheric ozone on Mars by detecting the absorption of ultraviolet sunlight by the molecule.
“With these maps, we have the kind of complete and simultaneous coverage of Mars that is usually only possible for Earth,” said MAVEN Remote Sensing Team member Justin Deighan of the University of Colorado, Boulder. “On Earth, ozone destruction by refrigerator CFCs is the cause of the polar ozone hole. On Mars, ozone is just as easily destroyed by the byproducts of water vapor breakdown by ultraviolet sunlight. Tracking the ozone lets us track the photochemical processes taking place in the martian atmosphere. We’ll be exploring this in more complete detail during MAVEN’s primary science mission.”
There will be about two weeks of additional instrument calibration and testing before MAVEN starts its primary science mission. This includes an end-to-end test to transmit data between NASA’s Curiosity rover on the surface of Mars and Earth using the MAVEN mission’s Electra telecommunications relay. The mission aims to start full science gathering in early to mid-November.
