Orientation Element Différences
to Investigate Error Causes in Aerial Triangulation
Robert B. Forrest
Photogrammetrist
Cornell University, Arecibo Ionospheric Observatory
Arecibo, Puerto Rico
For many years, photogrammetrists have been subjected to dozens of
papers on theories of errors and error propagation in aerial triangulation. Some
of these hypotheses are in direct opposition - yet they flourish in the absence
of empirical evidence that would confirm or refute the opposing theories.
The research that I am discussing today is empirical rather than theoreti
cal. I did this work because - after reading some theoretical studies - I was
curious to see some real orientation errors for an actual strip triangulation.
After determining these orientation errors, I made graphs of the errors in
successive photographs to show the actual error propagation of orientation
errors for a real triangulation.
I repeated this determination of orientation errors for several triangulations
to find to what extent the error pattern of each orientation element is a function
of the triangulation process. The error graphs of each orientation element for
the several triangulations provide some information on the actual propagation
of orientation element errors. In addition to these graphs, I performed some
further work which shows the importance of relative orientation errors in the
final residual coordinate errors of the triangulated points.
I will now describe in more detail the materials and procedure that I used
in this empirical work.
Materials — A 37 exposure strip of Wild RC-7 glass plate photography (Aviogon
objective, f=100 mm., 14 x 14 cm. format) was used for this work. The strip
was taken in October, 1954, as part of a research project of the I.S.P. Stato-
scope data was obtained during the photographic mission. The flying height
was 6,100 m. above terrain, and the strip length is 106 km. Approximate photo
graphic scale thus is 1/60,000 and the base-height ratio is 0.5. Relative
relief ranged up to 13 per cent of the flying height above mean terrain. Over
20Ô geodetic control points are available for this strip, an average of 12 per
photograph.
Triangulations - Three instrumental triangulations of the entire strip were
performed, triangulations 1 and 2 by aerial polygons, and triangulation 3
(performed in 1959 by another operator) by aerial levelling. Triangulation 4 was
performed for the first nine models by aerial polygons. Triangulation 5 was
started by changing photograph 10 to the left projector and setting in the orien
tation elements determined for photograph 10 during triangulation 4. The
optical train was adjusted to obtain an erect stereoscopic model, but With left
and right reversed. Triangulation 6 was performed for photographs 24 through
37, starting with the elements of photograph 24 set to the orientation elements
determined in triangulation 2. Triangulations 1 through 6 were performed at
1/15,000 using the Wild A7 Autograph of the Ohio State University. Later an
analytical triangulation also was performed running from photographs 7 through