2-2 Density Transformation Method
The following four typos of density
transformation functions were examined to
SPOT data of Japan and Peru.
(1) Linear contrast stretch function
(2) Multi-zonal linear functions
(3) logarithmic function
(4) Histogram flattening function
Data distribution of Peru scene was rather
normal but mostly below level 70. Simple
linear function to stretch gray level
range to full 256 levels gave very clear
image. On the other hand. Japan data was
irregular as bi modal distribution.
Therefore, single linear function could
not correct whole range of data.
Different slope linear functions are
necessary for each lumps of data. Then,
dual linear "contrast stretch function was
adopted and gave good result.
it is supposed to give good result that
original gray level is divided into a few
zones according to "data. histogram : and
different linear functions are adopted to
each zone.
3. PLOTTING ACCURACY
SPOT data is stated to be applicable for
1:50,000 scale topographic mapping. |n
accordance with the specification adopted
in international cooperation project of
Japan, planimetric error should not exceed
35m and altimetric error should not exceed
7m in class À mapping of. the scale. of
1:50,000. Since the pixel size of SPOT
data is 10m, 35m planimetric accuracy is
seemed to be accomplished in most cases.
However, 7m altimetric accuracy might be
rather hard to be achieved. Therefore,
height measurement accuracy of SPOT stereo
pair was examined.
3.1 Examination
Three SPOT images of Mt. Fuji area were
used as test images. The specifications
of the images are as follows.
Column-Low 929-279
Observed date Mar. 7, 1986 (Center)
Mar. 8, 1986 (Left)
Mar.17. 1986 (Right)
Off nadir angle 4.0 East (Conter)
24.1 West (Loft)
15.7 East (Right)
Mode Panchromatic
Processed level 1A
SPOT image orientation and measurement was
carried out by using PLANICOMP C=100
analytical plotter and the SPOT plotting
software "BINGO". 32 GCPs were selected
from 1:25,000 scale topographic maps for
orientation of images.
9km of
every
images
the two test sites of 3km by
and mountainous area, DEM of
were measured from oriented
compared to DEM measured from aerial
Furthermore, contour line of
was drawn at the scale of
At
flat
100m
and
photographs.
40m interval
337
1:50.000 and compared to 1: 50.000
topographic map.
3.2 Height measurement accuracy
Orientation accuracy at the 32 OOPs was
such that planimetric accuracy is 5m both
in Center-Right pair and Left-Right pair,
and altimetric accuracy were bm and 4m in
Center-Right and Left-Right respectively.
Orientation accuracy is rather constantly
good as decreasing number of control
points. Required orientation accuracy is
seemed to be achieved if there exist some
ten control points.
Table 3-1 shows the result of DEM
comparison. Root mean square of elevation
errors were within 7m tolerance except the
of mountainous area of Center-Right
case
pair, but quite close to 7m tolerance in
other cases. From this result. it is
hardly to say that 1:50,000 scale maps can
constantly be produced out of SPOT images.
1:100,000 scale maps with 40m interval
contour lines are supposed to suit to SPOT
data mapping.
Table 3-1 Residuals at DEM points
area pair | B/H | RMS max.
plain C-R | 0.52 | 5. 5m | -24. 7m
plain L-R 0.72! 5.8n |. 22.4n
mountain | C-R | 0.52 | 9.6m | 62. 7m
mountain | L-R | 0.72 | 6.9n | 31. Im
Figure 3-1 of the next page shows the
contour lines drawn from the SPOT stereo
pair, while figure 3-2 shows the |:50.000
scale topographic map of the corresponding
area. Through the visual inspection of
two figures. it was. convinced that
principal terrain features as main ridges
and valleys were correctly plotted as
sufficient for 1:100,000 scale topographic
maps.
4. CONTROL POINT EXTRACTION METHOD
In aerial photogrammetric mapping process,
anti-photo signals were set at
triangulation points before photographing.
On the other hand, in the case of SPOT
mapping, pt. Ise quite difficult to set
anti-photo signals in advance of imaging.
Therefore, it is necessary to develop
practical method to extract ground control
points out of given SPOT images.
technique
much higher
required in
image
GCP extraction
in remote sensing.
accuracy of GCP coordinates
mapping than in remote
registration.
is quite common
However,
is
sensing
points for mapping must
geodetic coordinates and
identified on an image.
available, geodetic
coordinates can easily be obtained any
place in the world. The difficulty ..is
that there can not always exist clearly
identifiable and pointable ground object
around where we need a GCP. Here, two
control
correct
should be clearly
Since GPS got
Ground
have