1. Objectives of a prospective Ukrainian orbiter mission to the moon
- Author
-
V.S. Kislyulk, Yu.G. Shkuratov, A.P. Vidmachenko, Leonid M. Lytvynenko, Ya. S. Yatskiv, and V.M. Shulga
- Subjects
Synthetic aperture radar ,Atmospheric Science ,Astrophysics::Instrumentation and Methods for Astrophysics ,Aerospace Engineering ,Astronomy and Astrophysics ,Lunar orbit ,Regolith ,Space-based radar ,Physics::Geophysics ,law.invention ,Orbiter ,Bistatic radar ,Geophysics ,Space and Planetary Science ,law ,Radar imaging ,Physics::Space Physics ,General Earth and Planetary Sciences ,Astrophysics::Earth and Planetary Astrophysics ,Radar ,Geology ,Remote sensing - Abstract
Ukraine has launch vehicles that are able to deliver about 300 kg to lunar orbit. A future Ukrainian lunar program may propose a polar orbiter. This orbiter should fill principal information gaps in our knowledge about the Moon after the Clementine and Lunar Prospector missions and future missions like Smart-1, Lunar-A, and Selene. We consider that this can be provided by radar studies of the Moon with supporting optical photopolarimetric observations from lunar polar orbit. These experiments allow one to better understand global structure of the lunar surface at a wide range of scales, from microns to kilometers. We propose three instruments for the prospective lunar orbiter. They are a synthetic aperture imaging radar, ground-penetrating radar, and imaging UV-spectropolarimeter. The main purpose of the synthetic aperture imaging radar experiment is to study with high-resolution (50 m) permanently shadowed sites in the lunar polar regions. These sites are cold traps for volatiles, and have a potential for resource utilization. Possible presence of water ice in the regolith in the sites makes them interesting for long-term manned bases on the Moon. Radar and optical imaging and mapping of other interesting regions could be also planned. Multi-frequency, multi-polarization sounding of the lunar surface with ground-penetrating radar can provide data about internal structure of the lunar surface from meters to several hundred meters deep. The ground-penetrating radar can be used for measuring megaregolith properties, detection of cryptomaria, and studies of internal structure of the largest craters. Modest spatial resolution (50 m) of the imaging UV-spectropolarimeter should provide total coverage (or coverage of a large portion) of the lunar surface in oblique viewing at large phase angles. Polarization degree at large (>90°) phase angles bears information about characteristic size of the regolith particles. Additional experiments could use the synthetic aperture imaging radar system, e.g., bistatic radar sounding with the on-board transmitter and Earth-based receiver, and interferometry with the on-board transmitter and two Earth-based receiving antennas that allows reconstruction of the surface topography with high resolution.
- Published
- 2003