On Sunday, Jan. 5, 2014, NASA's Lunar Atmosphere and Dust Environment Explorer (LADEE) passed a milestone: 1,000 lunar orbits. The spacecraft has traveled more than 10.4 million miles (17.4 million kilometers) in its journey from Earth to the moon. LADEE continues to perform splendidly. And on Wednesday, Jan. 15, orbital colleague Lunar Reconnaissance Orbiter (LRO) snapped LADEE’s picture. Then in the evening of Sunday, Jan. 19, LADEE executed a near-perfect periapsis-raising maneuver, one of a series of maneuvers designed to maintain LADEE’s science orbit within the desired altitude range. Without these maneuvers, LADEE’s orbit would decay in a matter of days, resulting in premature impact on the lunar surface. Such is life when you fly low over the lunar tropics! Fortunately, LADEE’s propulsion and guidance systems have performed exceptionally well.
The LADEE science team continued to analyze data acquired at the exciting time of the Chang'e 3 landing on Dec. 14, 2013, and the remarkable feat of quickly deploying and operating its Yutu rover. Along with many others, we wondered why there was no obvious signature of the descent and landing in either gas or ejected dust, which LADEE is equipped to measure. The instrument teams had carefully planned activities to provide a “before and after” set of measurements, so we could see if anything had changed, even temporarily. At first glance, nothing stood out. Now, it seems, something may be emerging from the data after all – but the story is complicated.
In studying their data from the time of the Chang’e 3 descent operations, the Lunar Dust Experiment (LDEX) team at Laboratory for Atmospheric and Space Physics, University of Colorado at Boulder noted an increase in the recorded dust impact rate around the time of the landing. However, the rise preceded the landing time by many hours, suggesting a different origin. Indeed, as often happens in space exploration multiple events collided: the Geminid meteor shower coincided with this landing event and produced elevated dust counts before, during and after the landing period! The LDEX dust impacts are thought to be due to the ejecta, or spray, of particles that result when the Geminid meteoroids slam into the lunar surface. If LDEX did encounter any lunar soil particles thrown up by the final descent of Chang’e 3, they would have been lost in the background of Geminid-produced events. LDEX would have to be very lucky to see these blasted regolith grains, because the descent engine interaction with the landing site soil lasted only a few tens of seconds at most. It’s quite likely that LADEE was simply not in the right place at the right time. But that’s just part of the story.
The Neutral Mass Spectrometer (NMS) team at NASA’s Goddard Space Flight Center, Greenbelt, Md., has been searching the data for exhaust species such as water (H2O), carbon monoxide and carbon dioxide (CO and CO2) as well as nitrogen (N2). They found there is a difference between what NMS observed before the Geminids shower and Chang’e 3 landing, and what was observed after. The results are very preliminary and require further study, but could be very exciting. Stay tuned!
The Ultraviolet and Visible light Spectrometer (UVS) carried out a series of before/after observations looking for effects of both the landing and meteor showers. Analysis by the UVS team at NASA's Ames Research Center in Moffett Field, Calif., revealed an increase in sodium in the exosphere in connection with the Geminids, as well as evidence of increased light scattering due to dust. The UVS also has been monitoring emission lines of atomic oxygen, and has seen emissions that may indicate the presence of both iron and titanium in the lunar exosphere. As constituents of the lunar regolith, we expected these elements to contribute in minor amounts to the lunar exosphere, but they have never before been observed.
All of this may say something important about both the persistence of a temporary lunar volatile exosphere and how species migrate across the lunar surface. One pathway for populating the lunar polar cold traps is via the moon’s tenuous exosphere: water molecules may hop across the lunar surface, and some may randomly find their way to the polar cold traps. But the effectiveness of the transport process depends on the extent to which a molecule “sticks” to surface grains. Such molecular stickiness depends on multiple factors – many of them are still unknown. The Geminid effect and the Chang’e 3 landing may afford us an opportunity to determine how “sticky” the lunar surface is for hopping water.
The LADEE science team continues to analyze the data from the Chang’e 3 landing, episodic meteoroid showers and repeating variations as the moon goes through its phases. More surprises likely await us!
Ames Research Center, Moffett Field, Calif.