Cryogeomorphic characterization of shaded regions in the Artemis exploration area
V. T. Bickel, B. Moseley, E. Hauber, M. Shirley, J.-P. Williams, and D. A. Kring are the authors of this study. The study is based on research involving Valentin Bickel, then a postdoctoral researcher at the Max Planck Institute for Solar System Research (MPS) in Goettingen, Germany. The researchers had developed an AI algorithm called "Hyper-effective nOise Removal Unet Software" (HORUS) to clean up noisy images of the background of unlit craters collected by other spacecraft, such as the Lunar Reconnaissance Orbiter (LRO) and correct for other factors, including the motion of the LRO itself. Currently, most science and mission planning efforts for a crewed mission and a number of robotic missions, are focused on a ridge adjacent to Shackleton Crater, a huge 12 mile (19kms) depression. This area is of great interest to NASA, first, a permanent shadow is cast in the crater's troughs, the low temperatures make it a promising place for ice formation and second, two topographically high points on the ridge have been identified that could provide optimal illumination and direct communications to Earth. Due to the lack of primary illumination, permanently shaded regions (PSRs) are difficult to image with high-resolution optical sensors. Yet, a detailed knowledge of their cryo-geomorphic characteristics would allow :- Identification of science targets, including small double-shaded regions, i.e., regions protected from primary and secondary lighting, especially cold regions, and potential hazards in target SSRs;
- The planning of efficient and safe crossings through the target PSRs, including the PSR terminator, i.e., the sun-shade transition zone;
- The overall reduction of the associated risk of operating in permanent shadow;
- The contextualization of science measurements made by future ground and orbital missions.
- V. T. Bickel, ETH Zurich, Switzerland;
- B. Moseley, University of Oxford, UK;
- E. Hauber, German Aerospace Center, Berlin, Germany;
- M. Shirley, NASA Ames Research Center, Mountain View, CA, USA;
- J.-P. Williams, University of California Los Angeles, USA;
- D. A. Kring, Lunar and Planetary Institute, USRA, Houston, TX, USA.
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