Full text: Proceedings, XXth congress (Part 2)

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International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XXXV, Part B2. Istanbul 2004 
2. METHODOLOGY 
The proposed method comprises two major parts. The first part 
is to build up the satellite orientation by using the ground 
control points. The second part is to use the orbit parameters to 
perform the orthorectification, in which a “Patch 
Backprojection" method is proposed. The model error of 
*Patch Backprojection" will also be evaluated in this section. 
2.1 Orbit Modeling 
In the modeling of orientation parameters, the position vectors 
and the attitudes of the satellite are expressed with low order 
polynomials in terms of sampling time. Due to the extremely 
high correlation between two groups of orbital parameters and 
attitude data, we only adjust the orbital parameters followed by 
a collocation procedure to compensate for the local systematic 
errors. Two steps are included in the orientation modeling. 
The first step is to initialize the orientation parameters using on- 
board ephemeris data. We then fit the orbital parameters with 
low order polynomials using GCPs (Chen and Teo, 2002). 
Once the trend functions of the orbital parameters are 
determined, the fine-tuning of an orbit is performed by using 
Least Squares Filtering technique (Mikhail and Ackermann, 
1982). 
2.2 Image Orthorectification 
The objective of image orthorectification is to determine the 
corresponding image pixel for a ground element. In addition to 
providing the traditional pixel-by-pixel procedure, we proposed 
a "Patch Backprojection" method and a patch size optimization 
approach as well. It is demonstrated that the indirect method 
performs better than the direct method in terms of quality and 
efficiency (Kim et al, 2001). Thus, we select the indirect 
method to determine the corresponding image pixels from a 
ground element. 
2.2.1  Pixel-by-pixel Backprojection 
Figure 1 shows the geometry of indirect method. Given a 
ground point A, we can create a vector r(t) from ground point A 
to image point a. The vector r(t) vector is located on the 
principle plane and n(t) is the normal vector on the principal 
plane. The mathematics show that, at time t, r(t) is orthogonal 
to the normal vector n(t). When r(t) is perpendicular to n(t), 
the inner product of r(t) and n(t) is zero. The function f(t) is 
defined to characterize the coplanarity condition. 
ft)»r(t) in(t )20 (1) 
We apply Newton-Raphson method to solve the nonlinear 
equation (1), and to determine the sampling time t for ground 
point A. Using the trigonometric calculation, the image 
coordinate respect to ground point can be determinate from the 
principal plane. After determining the corresponding image 
point for ground element, the grey value on the orthoimage is 
calculated by image resampling, while the orthoimage is done 
by pixel-by-pixel backprojection. 
587 
Satellite Orbit after precision normal vector n(t) Projection Center 
correction 
       
Satellite CCD array 
scanning surface 
    
Principal 
plane 
Ground surface 
X 
Figure 1. Illustration of indirect method 
2.2.2 Patch Backprojection 
The indirect method in pixel-by-pixel way is very time 
consuming. Thus, we proposed a “Patch Backprojection” 
method to minimize the orthorectification computation load 
with negligible model error. The proposed method is based on 
the following two assumptions: (1) the relief displacements in a 
small area with moderate terrain variations are linear, and (2) 
the mapping geometry between image coordinates and object 
coordinates may be expressed by affine transformation when a 
small area is considered. 
The procedure of the patch backprojection is illustrated in 
Figure 2. We first divide the area of interest into a number of 
equal-sized tiles. Selecting the lowest elevation in the tile, the 
corners of the tile are projected on the image to form a set of 
anchor points. Another set of anchor points with the highest 
elevation are generated in the same manner. Assuming that the 
relief displacement in a small tile is linear, a groundel within 
the tile is projected into the image space according to the 
groundel elevation and the two associated anchor point sets. 
  
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Figure 2. Illustration of patch backprojection 
(a) Tiles with equal size 
(b) Anchor point generation for the top layer 
(c) Anchor point generation for the bottom layer 
(d) Interpolation 
 
	        
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