Illumination conditions of the lunar polar regions using LOLA topography

被引:227
|
作者
Mazarico, E. [1 ,2 ]
Neumann, G. A. [1 ]
Smith, D. E. [1 ,2 ]
Zuber, M. T. [2 ]
Torrence, M. H. [1 ,3 ]
机构
[1] NASA, Goddard Space Flight Ctr, Planetary Geodynam Lab, Greenbelt, MD 20771 USA
[2] MIT, Dept Earth Atmospher & Planetary Sci, Cambridge, MA 02139 USA
[3] Stinger Ghaffarian Technol Inc, Greenbelt, MD 20770 USA
关键词
Moon; PLANETARY SCIENCE; NEUTRON DETECTOR; MOON; POLES; SHAPE; ICE;
D O I
10.1016/j.icarus.2010.10.030
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
We use high-resolution altimetry data obtained by the Lunar Orbiter Laser Altimeter instrument onboard the Lunar Reconnaissance Orbiter to characterize present illumination conditions in the polar regions of the Moon. Compared to previous studies, both the spatial and temporal extent of the simulations are increased significantly, as well as the coverage (fill ratio) of the topographic maps used, thanks to the 28 Hz firing rate of the five-beam instrument. We determine the horizon elevation in a number of directions based on 240 m-resolution polar digital elevation models reaching down to similar to 75 degrees latitude. The illumination of both polar regions extending to similar to 80 degrees can be calculated for any geometry from those horizon longitudinal profiles. We validated our modeling with recent Lunar Reconnaissance Orbiter Wide-Angle Camera images. We assessed the extent of permanently shadowed regions (PSRs, defined as areas that never receive direct solar illumination), and obtained total areas generally larger than previous studies (12,866 and 16,055 km(2), in the north and south respectively). We extended our direct illumination model to account for singly-scattered light, and found that every PSR does receive some amount of scattered light during the year. We conducted simulations over long periods (several 18.6-years lunar precession cycles) with a high temporal resolution (6 h), and identified the most illuminated locations in the vicinity of both poles. Because of the importance of those sites for exploration and engineering considerations, we characterized their illumination more precisely over the near future. Every year, a location near the Shackleton crater rim in the south polar region is sunlit continuously for 240 days, and its longest continuous period in total darkness is about 1.5 days. For some locations small height gains (similar to 10 m) can dramatically improve their average illumination and reduce the night duration, rendering some of those particularly attractive energy-wise as possible sites for near-continuous sources of solar power. (C) 2010 Elsevier Inc. All rights reserved.
引用
收藏
页码:1066 / 1081
页数:16
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