The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences. Vol. XXXVII. Part Bl. Beijing 2008
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workstation. Operators of the Photogrammetry and Remote
Sensing Department of Shanxi Bureau of Surveying and
Mapping have manually collected 1489 well-distributed
checking points in study area. We computed the differences as
these points minus the interpolated heights from our generated
DTM. The accuracy of the DTM is between 3.6 - 4.5m
depending on the terrain relief and landform. Since the DTM
generation and point measurement procedure share the same
image orientation results, the errors of the DTM would be from
ME derived from stereo image matching, which is directly relate
to the matching accuracy. Detailed accuracies are shown in
Table 1 downside.
According to the experiment results, the following conclusions
can be made: (a) DEM at 1:50,000 scale can be generated
automatically from SPOT-5 HRS/HRG stereo/triplet-stereo
images by using the automatic DTM generation approach
proposed in this paper. The elevation accuracy can roughly be
50% better than requirements of the Chinese national surveying
regulation; (b) simultaneously matching SPOT-5 HRS/HRG
triplet stereo strips and matching both feature points and
feature-lines are quite necessary for deeply incensed
mountainous area and rugged terrain, such as arid and semi-arid
broken mountains in northern part and rugged mountain ranges
in southern part of the study area; (c) the proposed automatic
DTM generation approach can largely increase the working
efficiency, however, careful manually stereoscopic checking and
editing are still necessary to remove some small matching
blunders, which are in most cases within shadow and gully/rill/
steep-valley well-developed areas.
Table 1: DTM accuracy evaluation results with SPOT-5 HRS/HRG imagery
Reference
data
Map
sheets
Num. of
check points
Height accuracy
(RMSE)
Accuracy requirements of
1:50,000 scale l st /2 nd level DTM
Type of terrain
GPS points
3
99
6.7 m
14.0 m/19.0 m
Mountainous area
1
26
3.6 m
8.0 m/11.0 m
Mountainous area
2
64
1.7 m
5.0 m/ 7.0 m
Hilly area
3
127
2.8 m
3.0 m/ 4.0 m
Flat/hilly area
Manually
measured
points
47
937
3.6 m
5.0 m/ 7.0 m
Hilly area
21
367
4.5 m
8.0 m/11.0 m
Mountainous area
8
185
4.4 m
14.0 m/19.0 m
Mountainous area
3.2 DSM Generation from 23 IRS-P5 Stereo Images over
Beijing Test-field
The test-field is an area around the city of Beijing, China. It
consists of a steep mountainous region in the north-western part
and flat regions in the middle and southern parts. The city of
Beijing is located in the lower part of the study area. The whole
area is about 70 x 210 km 2 . The site has an average terrain
height of 300m and an elevation range of more than 1100 m.
Totally there are 23
scenes of IRS-P5
stereo images
involved in the
Beijing test field,
after the re-mosaic
procedure which
mention in the text,
3 long IRS-P5
stereo strips are
used for subsequent
processing.
Fig. 6: In Beijing test-field, there are 23 scenes of IRS-P5
stereo images. In order to facilitate the subsequent
processing, we use the re-mosaic procedure based on
metadata to combine these 23 stereo images into 3 long
stereo strips.
Over the test area, totally 23 scenes of IRS-P5 stereo images
were acquired. The ground resolution of IRS-P5 images is 2.5m,
and each scene covers about 30 x 30km 2 . In order to precisely
georeference these images, with the cooperation of the l rd
Institute of Surveying and Mapping of Heilongjiang SBSM,
about 66 well-distributed GCPs were collected with differential
GPS in 2006. The measurement accuracy was better than 0.5m
in planimetry and lm in height. The GCPs are well-distributed in
the test area, their ground intervals are about 30km, and half of
them are located at the center of road intersection which can be
precisely measurement both in image and object space.
Normally, we could commercially get so-called IRS-P5
“standard scene” of images, which have 12000 x 12000 pixels
and cover 30 x 30km 2 . Basically the standard scenes could be
sub-images of a long IRS-P5 strip. They are just subdivided
from a long IRS-P5 strip for commercial reason and normally
they have 5%-15% overlap between adjacent scenes. This
situation will cause difficulties or complicate the sub-sequent
processing. To avoid these problems, we develop a procedure to
re-mosaic adjacent IRS-P5 standard scenes into a long stereo
strip (Fig. 6) in condition that these scenes are sub-images of the
original long IRS-P5 strip. After this re-mosaic procedure, 23
IRS-P5 scenes of the Beijing test-field are re-mosaic into only 3
IRS-P5 long stereo strips.
With aids of 66 GCPs, block-adjustment was made and the
orientation accuracy is about 1.7m in planimetry and 2m in
height. After the block-adjustment, the proposed DSM/DTM
generation approach was applied to 3 re-mosaic IRS-P5 stereo
image strips simultaneously. As a result, 12.5m grid-spacing
DSM of the study area has been generated automatically. Since
our DSM/DTM generation approach not only generates a large
number of mass points but also produces line features, which are
necessary for the modeling the rugged mountainous terrain.
Parts of DSM results are shown in Fig. 7, the resulted 12.5 m
DSM reproduced quite well not only the general features of the
terrain relief but also small geomorphological and other features
visible in the IRS-P5 images. The DSM shows many
topographic details and features such as small valleys in the
mountains, detailed patterns related to streets and buildings in
suburban and urban areas, linear features related to highways
and main road networks, sparse trees, small clusters of houses
and forest areas. Checking by GCPs measured by differential
GPS shows that the accuracy of the DSM is 3.7 m and it meet
the requirements from the Chinese Surveying and Mapping
regulations for 1:50000 topographic maps.