Full text: Resource and environmental monitoring

  
  
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Fig. 1: Extended normalisation funktion 
As already mentioned above the correction due to the 
observation angle will not be pursued any longer in our 
current work. We recommend further investigations. The 
examples later show that the influence of the observation 
angle seems to be negligibly small. 
Before we continue with the determination of the para- 
meters of the normalisation function it is advisible to prove 
that in reality this function may serve as suitable model. For 
that reason we chose our test area in the Austrian Alps 
where high mountains and steep slopes guarantee all sorts 
of illumination effects, from brightly sun lit regions with 
incidence angles around 0°, to dark shadows where the 
(virtual) incidence angle is greater than 90°, all sorts of 
shades in between, and eventually even cast shadows. 
Figure 2 shows an overview of the some 35 km x 25 km 
large area in the so-called "Salzkammergut" with its lakes. 
We use in our investigation the six optical bands of a 
Landsat TM image (1 to 5 and 7). 
The DTM provided by the Austrian Federal Office for 
Metrology and Surveying has a grid width of 25 m x 25 m. 
The geometrically rectified satellite image has the same 
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rea located in the Austrian Salzkammergut (Landsat TM, Band 4) 
      
    
resolution. We want to emphasize that the geometric 
rectification must be performed with the help of a parametric 
model, so that displacements due to terrain heights are also 
rectified. In our case we used the bundle block adjustment 
program ORIENT [Kager, 1989] in conjunction with the 
digital orthophoto modul of SCOP DOP [Molnar et al. 1998]. 
High geometric accuracy is a prerequisite for a good quality 
of topographic normalisation in particular along terrain 
discontinuities, such as steep ridges or narrow valleys. 
  
  
Fig.3: cos i of the DTM (black = i greater 90°) 
10 Intemational Archives of Photogrammetry and Remote Sensing. Vol. XXXII, Part 7, Budapest, 1998 
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