Full text: Mapping surface structure and topography by airborne and spaceborne lasers

Table 1: Comparison between ALR and photogrammetry. 
  
  
  
  
photogrammetry laser ranging | 
data acquisition 
flying height H « 6000 m « 1000 m 
swath « 108^ < 40° 
coverage continuous irregular 
footprint size i5um x Hjf 1 mrad x H 
flying time ] hour 3 to 5 hrs 
weather cond. very restrictive flexible 
  
surface reconstruction 
  
  
  
  
redundancy 2 x photo — 3 0 
accuracy 
planimetry «1i5umxH/f 1dm«5"x H 
elevation = H/10,000 m = | dm 
surface charact. explicit implicit 
automation 
degree medium high 
complexity medium low 
  
2.1 Data Acquisition 
Essentially, both methods sample the surface. The fly- 
ing height of existing ALR systems—typically less than 
1000 m—is quite limited, compared to photogramme- 
try. The sampling size (ground pixel size in case of pho- 
togrammetry, footprint size in case of ALS) is consider- 
ably smaller in photogrammetry when the same flying 
height is assumed. For H = 1000 m and f = 0.15 m we 
have a pixel size on the ground of 15 cm, but a footprint 
size of 1 m, for example. In ALR systems the average dis- 
tance between samples is several times larger than the 
footprint size, resulting in an irregular sampling pattern 
with gaps. On the other hand, photogrammetry provides 
continuous ground coverage. 
The smaller swath angle of laser scanning systems and 
the limited flying height cause much longer flying times 
for covering the same area. Baltsavias (1999) mentions 
a factor of three to five. Since the initial equipment cost 
and the shorter life time result in substantially higher 
amortization cost, the data acquisition with ALR is quite 
a bit more expensive. Now, this is partially compensated 
by the much less stringent weather conditions for ALR 
missions; the waiting time for crew and equipment is 
certainly much longer in photogrammetry. 
Another interesting aspect in this comparison is the sur- 
face characteristic. It is clear that photogrammetric sur- 
face reconstruction methods require a reasonable image 
function, that is, good contrast or texture. Sand, snow, 
ice, or water bodies defy photogrammetric methods. In- 
terestingly enough, ALR works very well in these condi- 
tions. 
2.2 Surface Reconstruction 
In this section we briefly compare ALR and photogram- 
metry in terms of surface reconstruction. Fig. 1 illus- 
trates the principle of determining a surface point by 
ALR. Although grossly simplified, it captures the basic 
notion of establishing relationships between different 
coordinate systems. Let us begin with what we may call 
the laser beam coordinate system (x', y', z') whose ori- 
International Archives of Photogrammetry and Remote Sensing, Vol. 32, Part 3W14, La Jolla, CA, 9-11 Nov. 1999 
gin is at the center of the laser's firing point and whose 
Z'—axis is oriented opposite to the direction of the laser 
beam. In this system, point P on the surface is expressed 
by the range vector r = [0,0,7]" with r the measured 
distance (range). 
  
Figure 1: Relationship of local laser coordinate sys- 
tems and object space reference system for transform- 
ing range data to surface points. 
Obviously, the laser beam system changes with every 
new range measured. Let us transform it into the laser 
reference system, denoted by x, y, z. Its origin is also 
at the laser's firing point. The orientation depends on 
the particular system; for example, in nutating mirror 
systems, the z — axis would be collinear with the rotation 
axis and the x — axis points to the starting position of 
the rotating mirror; in the case of a scanning system, the 
X — z plane would be identical to the scan plane with z 
indicating scan angle zero. 
The transformation from the beam system to the refer- 
ence system is accomplished by the rotation matrix R; 
since there is only a rotation involved. R; is determined 
by the laser system. In the case of a profiler, R; is the 
identity matrix; for a scanning system, the rotation ma- 
trix is determined by the scan angle; two angles are nec- 
essary to determine R; for a nutating mirror system. Let 
us call the relationship of an individual laser beam with 
respect to the reference system the interior orientation 
of the laser system. 
To establish a relationship of the laser system to the ob- 
ject space, the exterior orientation is required. Thus, we 
obtain for the position of the center of the laser footprint 
p=c+ReRjir (1) 
In this equation, c expresses the positional and R, the 
angular component (attitude) of the exterior orientation 
(see also Fig. 1). These two components are usually ob- 
tained from GPS and inertial measurements. We omit 
here the details of establishing the relationship between 
the platform orientation system and the laser system 
     
   
  
    
     
   
   
   
    
  
  
  
  
   
   
  
  
   
  
  
   
   
  
  
   
  
  
  
    
   
   
  
   
  
   
   
    
  
   
   
  
   
  
  
   
   
  
   
   
  
   
  
    
  
  
  
  
   
   
    
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