Full text: Technical Commission IV (B4)

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to reduce the computational complexity a pyramidal approach is 
used. In the second step the integer disparity values are refined 
to sub-pixel accuracy using a gradient based approach with an 
affine adaptive window (Nefian et al. 2009). In the third step 
the disparity values are transformed back to the original image 
geometry and a forward intersection is calculated which results 
in a 3D point cloud. In the last step this point cloud is 
interpolated and map projected using a pixel size of 2 m to 
derive the DTM. A shaded relief representation of the DTM is 
shown in Fig. 4. As expected no matching results are available 
in the shadowed areas leaving larger areas and small holes 
without height values which have to be filled by other stereo 
pairs and LOLA data. 
  
s hes A % 
Figure 3. Section of the left pre-rectified input image 
(M139716114RE) at SRI site 
Figure 4. Shaded relief of the DTM at SRI site derived from the 
first stereo pair 
After processing all four stereo pairs the good-quality areas are 
manually selected and cropped for mosaicking. The resulting 
2m mosaic is blended into an upsampled 5m LOLA DTM 
(LDEM 875S 5M) in order to fill areas without matching 
results and to fill holes. As can be seen in Fig. 5 the LOLA 
dataset contains many outliers but this will likely change in the 
future. 
  
Figure 5. Mosaicked DTM blended into LOLA data in a 
colorized shaded relief representation 
4. CONCLUSIONS AND OUTLOOK 
LandSAfe assists the user in selecting safe landing sites on the 
lunar surface by automatically generating DTMs, detecting 
craters and boulders and derived products like risk maps. In this 
paper it has been shown that an automatic generation of high 
resolution DTMs at the south pole of the Moon in face of 
unfavorable illumination conditions is feasible. For the future 
accuracy assessment processes will be included in order to 
derive a confidence level for the safety of the landing site. 
Additionally, the measurement of GCPs will be included in 
order to obtain a better co-registration of the high resolution 
DTM and the LOLA dataset. 
S. REFERENCES 
Acton, C. H., 1996. Ancillary data services of NASA's 
Navigation and Ancillary Information Facility. Planetary and 
Space Science, 44(1), pp. 65-70. 
Anderson, J. A., Sides, S. C., Soltesz, D. L., Sucharski, T. L, 
Becker, K. J., 2004. Modernization of the integrated software 
for imagers and spectrometers. 35th Lunar and Planetary 
Science Conference, March 15-19, League City, Texas, abstract 
#2039. 
Archinal, B. A., Rosiek, M. R., Kirk, R. L., Redding, B. L., 
2006. The Unified Lunar Control Network 2005. U.S. 
Geological Survey, Open-File Report 2006-1367 - Version 1.0. 
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