(2)
be de-
m the
mined,
m the
rmina-
meas-
tion is
vident
Ally in
it such
taken
ys from
y inter-
allaxes
correc-
tation.
allaxes
lax is
)ancies
deter-
marily
nd the
~oordi-
we the
t upon
in the
ng in-
stances
tween
different sources of errors and the re-
sulting errors in the coordinate deter-
mination were known, it would be
possible to determine numerical cor-
rections to the elements of orientation
of the cameras; so that the discrepan-
cies would vanish in the same number
of control points as the number of
orientation elements which are as-
sumed to have an influence upon the
coordinate determination. But if there
are more control points than the used
elements of orientation, there are
superfluous observations, and conse-
quently one has the problem of dis-
tributing the discrepancies which can-
not be compensated by the available
elements of orientation. In such cases
the method of least squares is normally
used. The corrections to the elements
of the orientation are to be deter-
mined so that the square sum of the
residuals or corrections to the measure-
ments of image coordinates is a mini-
mum. This principle means that one
assumes the discrepancies, which can-
SYMPOSIUM—NON-TOPOGRAPHIC PHOTOGRAMMETRY
‘YA
A
LC
04 b 02
7 +X
AL
7 c Ic
Ca I
x xul. 1
P, (PR) H, PH,
Hi H;
Iz, Zl
Came ;
R X ] hy
Frc. 3.—The normal case of terrestrial
stereophotogrammetry. The principles for the
determination of the coordinates x, y and z are
indicated.
not be corrected by the elements of orientation, to depend primarily upon the
errors of the image coordinate measurements. The principles of the least square
method furthermore permits one to determine the standard error of the meas-
urements, to determine the accuracy of the elements, and to study the error
propagation to the determination of the coordinates of arbitrary points.
These general principles will be applied to the most important case of terres-
trial photogrammetry, the stereophotogrammetric normal case, Figure 3.
The pictures are assumed to have been photographed at the stations O; and
O, with the same camera, or with equal cameras having the same principal
distances c and free from distortion. If distortion is present, the measurements
must be corrected; this is no real problem. The camera axes are perpendicular
to the base and horizontal. A phototheodolite and a stereocamera are shown in
Figures 4 and 5.
À coordinate system is assumed to have the origin at the left camera station,
the + x-axis horizontal towards the right station, the +y-axis in the left camera
axis and the +z axis upwards. The image coordinates are denoted x', x", z/, z//.
The coordinates of an arbitrary point can be determined from the following
expressions which can easily be derived. See Figure 3.
bc
y LI
x! —
yx’
x= —
C
ys
21 = — =
bc
uf f (3)
x p
ba’
ox. (4)
?
bz’
— (Sa)
—————————
EE
eget:
pt EE