Full text: Proceedings of the Symposium on Progress in Data Processing and Analysis

372 
Real -Time Correction Of Geometric Distorsions in Airborne Remote 
Sensing Systems 
H. Hirsch, J. Nopirakowski, M. Scheele, Th. Terzibaschian 
Institut for Space Researche, Berlin 
Rudower Chaussee 5 
Berlin 
1199 
Dr. F. Plischke 
INTERFLUG, Betrieb Fernerkundung, Industrie und Forschungsflug 
Berlin-Schoenefeld 
1189 
Images, produced by an airborne electro-optical line scanner, 
show geometrical distorsions. They have to be corrected in a 
strong way line by line with respect to the airplane motion. 
These disturbances can lead to displacements between neighbouring 
lines of the recordered images. They are eompareable with the 
image-pixel size. The topic of this report is to present a 
possibility to correct it by using attitude-measurements, 
especially measurments of the angular motion around the three 
body axes or measurments of the three tilt angles yaw, pitch and 
roll. These angular motions are connected with typical image 
distorsions. The roll-angle produces a lateral shift of image 
lines and decreases so the usable swath-width. The yaw motion 
rotates the image lines and the pitch-angle produces varying 
distances between neighbouring image lines. The rather complex 
angular airplane motion produces ergo rather complex geometric 
distorsions./1/ The authors' aim is the development of inteligent 
real-time onboard control algorithms for elctro-optical line 
scanners. It shall be demonstrated studying the pitch-angle 
related distorsions. One way to correct the pitch-effects is a 
control of the line's sample time. Because of the velocity v, 
the altitude h and the pitch motion the projection of a sensor 
pixel onto the earth moves during a discrete time interval AT 
over a distance Ax : 
Supposing quadratic pixels and realistic pitch-angles of about 
some degrees, the right sample period AT 1 , the time between two 
following read outs of the sensor line, can be derived using 
formula 1. It is possible to aproxímate 
Here isAT^the normal sample period under ideal conditions, i.e. 
M ) 
дх s v дт + h• tonfi-AT) 
tan (*S• ДТ) 
Thats why formula 2 is :
	        
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