Full text: Papers accepted on the basis of peer-review full manuscripts (Part A)

ISPRS Commission III, Vol.34, Part 3A ,,Photogrammetric Computer Vision“, Graz, 2002 
  
  
  
  
  
  
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Figure 7. Project Svinesund, six strips. Left: strips. Right: 
elevation 
In this case the crossing strip helped to discover a deformation 
of the strip. It is not clear what has caused the deformation but 
the guess is a scale factor error in the mirror roll angle. The 
same kind of deformation was found by (Crombaghs et al. 
2000). This deformation was not modelled or compensated for. 
The final corrections for the project Svinesund are presented in 
table 5. 
  
  
  
  
  
  
  
  
  
  
  
  
  
  
Flightlin | Points | Z shift | Hshift | Rshift | P shift 
e [m] [rad] [rad] [rad 
1 778 -0.010 | -0.0005 | -0.0001 | +0.0001 
5 626 +0.027 | -0.0004 | -0.0001 | -0.0000 
2 1188 | -0.028 | -0.0008 | -0.0003 | +0.0001 
4 1070 | -0.001 | -0.0000 | -0.0001 | 40.0000 
3 1180 | -0.023 | -0.0003 | -0.0001 | 40.0002 
6 777 +0.009 | -0.0001 | -0.0000 | +0.0003 
  
Table 5. List of final corrections in the Svinesund project. 
3.5 Project Gävle 
Fotonor flew this mission for the National Land Survey of 
Sweden. The main purpose was to investigate the possibilities 
of using laser scanning to update the National Height Data 
Base in Sweden. Therefore, the flying altitude was rather high 
(about 1700 m). They wanted cover different land use 
categories, which lead to a rather elongated flight with five 
different strips (figure 8). The area was rather flat (figure 9) 
and most of it was covered by forest. 
  
  
  
  
  
Figure 8. Strips in the Gävle project 
  
  
  
  
  
Figure 9. Elevation in the Gävle project 
The final corrections are listed in table 6. 
  
  
  
  
  
  
  
  
Flightline | Points | Z shift | R shift 
[m] [deg] 
5 816 | -0.120 | -0.0192 
4 1784 | -0.029 | -0.0004 
3 2212 | +0.015 | +0.0099 
2 2033 | -0.178 | -0.0026 
1 3278 | +0.137 | +0.0017 
  
  
  
  
Table 6. List of final corrections in the Gävle project. 
In this case there was an elevation offset between the two 
strips in the north. This can be illustrated by thinning the 
ground points where there is a small change in gradient, i.e. 
  
 
	        
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