where
( X, Y, Z ) : ground coordinate of target P
( X(L),Y(L),Z(L) ) : ground coordinate of the position of
sensor on scan band L
{ m it }
scan band ( L = MOD( J, 6 )
assumed prinei pa 1 dis tance
1 )
components of rotation matrix on scan band L
The position and attitude of sensor are expressed as functions
of scan band L since they are ever changing. The concept of scan
band is used because LANDSAT MSS scans six lines at a time. It was
experimentally found out that the position and the attitude could
be expressed by monomials and by trinomials, respectively as below.
Angle deviation ( u ) caused by the irregularity of scan mirror
rotation is also expressed by a trinomial of pixel number.
Xq — a j -P b j L
2 0 —+ b L
<P=a À + bL+c L +dV
co—a. -P b L -Pc L -p d L
5 5 5 5
(4)
~ a c>+ b 6 L +c e L
V = d 7 I (/ — N/ 2 ) (/-/V)
Totally 19 orientation parameters have to be determined. They
are solved from the image coordinates and ground coordinates of
GCPs and the approximations of the position and attitude of sensor,
it was found out from experiments that more than 11 GCPs was
necessary for sufficient accuracy when they were well distributed.
The s
accuracy c
Here is int
imagery an
size from
with the ac
in the same
bird's eye
procedure.
south with
atellite imagery corrected
an be superimposed on other
roduced a bird's eye view o
d DEM. Elevation data were
250m grid. Geometric correc
curacy of less than a pixel
grid size of DEM. Both dat
view by parallel proje
Photo. 1 shows the result
the depression angle of 30
geometrically with sufficient
geographical informations,
f Mt. Fuji using LANDSAT MSS
interpolated into 56m grid
tion of MSS imagery was done
, and the data were resampled
a were processed to produce a
ction through hidden point
which was projected from the
degrees.
3. Geometric Correction of MOS-1 VT1R imagery
The
ied ou
ttle d
earth
r large
dinate
n g t h i
¡ensor
ty of
issary.
2 ) is
geometric correction of MOS-1 VT
t utilizing photogrammetric princ
ifferent from that of LANDSAT MSS
curvature is not negligible sin
area. The exterior orientation i
system and the earth is represen
s effect into account. Both the p
are expressed by binomials of tin
scan mirror rotation and the cone
Consequently the equation (1) is
replaced by line number J.
802
IR imagery can be also
iples. But the method is
imagery. The effect of
ce VTIR imagery covers
s made on the geocentric
ted by an ellipsoid for
osition and the attitude
e number J. The irregu-
ept of scan band are not
modified into (5) and L
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