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Analysis of Local Slopes at the InSight Landing Site on Mars
- Source :
- Space Science Reviews. 211:109-133
- Publication Year :
- 2016
- Publisher :
- Springer Science and Business Media LLC, 2016.
-
Abstract
- To evaluate the topography of the surface within the InSight candidate landing ellipses, we generated Digital Terrain Models (DTMs) at lander scales and those appropriate for entry, descent, and landing simulations, along with orthoimages of both images in each stereopair, and adirectional slope images. These products were used to assess the distribution of slopes for each candidate ellipse and terrain type in the landing site region, paying particular attention to how these slopes impact InSight landing and engineering safety, and results are reported here. Overall, this region has extremely low slopes at 1-meter baseline scales and meets the safety constraints of the InSight lander. The majority of the landing ellipse has a mean slope at 1-meter baselines of 3.2°. In addition, a mosaic of HRSC, CTX, and HiRISE DTMs within the final landing ellipse (ellipse 9) was generated to support entry, descent, and landing simulations and evaluations. Several methods were tested to generate this mosaic and the NASA Ames Stereo Pipeline program dem_mosaic produced the best results. For the HRSC-CTX-HiRISE DTM mosaic, more than 99 % of the mosaic has slopes less than 15°, and the introduction of artificially high slopes along image seams was minimized.
- Subjects :
- 010504 meteorology & atmospheric sciences
Space and Planetary Science
0103 physical sciences
Astronomy and Astrophysics
Terrain
Mars Exploration Program
Safety constraints
Ellipse
010303 astronomy & astrophysics
01 natural sciences
Geology
0105 earth and related environmental sciences
Remote sensing
Subjects
Details
- ISSN :
- 15729672 and 00386308
- Volume :
- 211
- Database :
- OpenAIRE
- Journal :
- Space Science Reviews
- Accession number :
- edsair.doi...........58e54d602cfb90880af33af4618badd3
- Full Text :
- https://doi.org/10.1007/s11214-016-0292-x