The image quality of modern orthophoto systems combined with stereo
orthophoto interpretation, and the measuring and plotting facilities
introduced by the National Research Council of Canada will without
doubt result in an increased use of orthophotos. The possibility of
a precise determination of X, Y and Z coordinates offered by the stereo-
orthophoto technique, will extend the use of orthophotos to the measure-
ment of terrain profiles, spot elevations, and heights of terrain
features such as buildings and trees. Contour lines, representing the
same amount of detail as obtained from conventional-type photogrammetric
methods, can be plotted directly from the stereo-orthophotos. The
stereo-orthophoto technique will therefore take an important place in
transferring orthophotographs into orthophoto maps and line maps.
‚The accuracy of vertical terrain information obtained from stereo-
orthophotos has been evaluated theoretically and it was proven that
the elevation errors are considerably smaller than the usual plani-
metric error of orthophotographs (Ref.: Blachut, van Wijk 1970).
Lately a number of large-scale mapping experiments, based on the
stereo-orthophoto technique, have been undertaken. Some of the
results obtained from this work are described here.
The basic principles of the stereo-orthophoto technique
o
À stereo-orthophoto pair consists of an orthophoto and a stereomate,
produced by differential rectificatios of two adjacent photographs
which form the stereoscopic model. The stereomáte is produced in
such a way that it contains image shifts proportional to the terrain
heights and parallel to the flight direction. When the orthophoto
and the stereo-mate are viewed stereoscopically, the terrain surface
appears three-dimensional because of the x-parallaxes introduced by
the image shifts in the stereomate. Terrain features which are not
Sübject to the differential rectification process, such as buildings
amd trees, will be projected with their original parallaxes with
respect to the tegrain, and they also appear three-dimensional.
In order to create a smooth, three-dimensional model from stereoscopic
orthophotos it is important that the artificial differential parallaxes
be compatible with the basic parallax equation. In this case the
vertical appearance of the three-dimensional model will not be affected
by approximations in the rectification process, such as caused by
dimensions of the scanning slit.
Orthophotos and their stereomates should be produced simultaneously or
' based on the same profile information to make the technique economically
attractive. Moreover, simultaneous production is required in order to
assure optimum accuracy (Ref.: Collins 1968).
An instrument in which this principle has been realized is presently in
an advanced state of completion at the N.R.C. This instrument, called
the Orthocartograph, is based on simultaneous optical transfer of
corresponding aerial photographs on two separate photographic emulsions
(Ref.: Blachut 1971).
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