High-­resolution free-air gravity overlaid on terrain based on Lunar Orbiter Laser Altimeter (LOLA) and Camera (LROC) data. Gravity is painted onto the areas that are in the shadow, where red corresponds to mass excesses and blue corresponds to mass deficits. Credit: NASA/SVS

Two satellites orbiting the Moon as a part of NASA’s Gravity Recovery and Interior Laboratory (GRAIL) mission have been mapping its inner structure by measuring subtle shifts in the pull of gravity on the satellites from points on the ground below. The stronger the shift is, the greater the mass of structures below the surface is.

Although the Moon-wide models produced by this mission are highly precise and have improved, Goossens et al. note that having to rely on many parameters could make the estimation of the models unstable. The authors instead created a local model of the Moon’s south pole that can serve as a basis for ­higher-­precision global models.

To do this, the authors took raw data from the GRAIL mission and tweaked the mathematical formulas so that they could extract more information than typically found from formulas used in global models. They created a highly precise model that represents structures under the Moon’s south pole more accurately than the global models. The authors note that their model has the potential to improve observations of small-scale features on and in the Moon. (doi:10.1002/2014GL060178)

—JoAnna Wendel

© 2014. American Geophysical Union. All rights reserved.

© 2014. American Geophysical Union. All rights reserved.