19
plotter. Absolute orientation was performed using thirty control
points which resulted in a CMAS of .2 meter earth scale, with
the photo scale being 1/15000. No attempt was made to correct
for atmospheric refraction lens distortion, or film shrinkage.
Profiles were spaced at .75mm in the model and points recorded
every .25mm along the profile. Profiling was done automatically,
using the correlator on the AS-11B-1, producing 187 profiles
in about 5 hours. The total elevation range in the area covered
by the orthophoto was about 4mm at a model scale of 1/15,000.
Profiling accuracy at the 90% confidence level was one meter
at ground scale.
The orthophoto was produced from a portion of the model
at 2X using a nominal print width of 1mm. (Figure 8) Forty-
four photogrammetrie ground targets were then measured on the
AS-11B-1. The orthophoto target coordinates were rotated,
translated, and scaled to the NRC supplied ground control by
a least-squares adjustment. The residuals produced a CMAS of
33 microns referred to the input photography thus confirming
the general accuracy level achieved in the first test. One
might expect the first test to yield smaller residuals than the
second since model control was used instead of absolute ground
control. Thirty (30) reseaus randomly selected from the Sudbury
model did indeed produce a CMAS of only 30u, when fit to their
corresponding model coordinates. It should be noted however,
that the California model contained more relief than Sudbury
and that the California orthophoto was printed at a 2mm print
width while Sudbury was done at 1mm. The latter essentially
decreased the control available for the printer.
3. Other Tests.
A stereomate was made from the same photo used in
printing the Sudbury orthophoto (Figure 9). Elevations were
calculated from x parallex measurements made on the orthophoto-
stereomate. The error in these elevations when compared to
ground control resulted in a standard deviation of .9 meters.
Marty Alice and J. Abshier of Bendix Research Labs
have also evaluated a stereomate and orthophoto (Figures 10 and 11)
which were produced from 1/50,000 6 inch focal length photo
graphy over Fort Sill, Oklahoma. The model contained an
elevation range of 4mm. The same photo was used for printing
both the orthophoto and the stereomate. The resultant standard
deviation of the elevation error derived from the orthophoto-
stereomate was 2.2 meters. Bendix also evaluated their ortho
photo in a manner similar to the California model and obtained
a CMAS of 40 microns referred to the input photography. Tables
1 and 2 give a summary of the orthophoto and stereomate tests
to date.