International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XXXV, Part B4. Istanbul 2004
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Xo 7 | long,lato, ho, ^ lon, 4, lat, 4,09 ,, 00 p. Co, (9)
Yo aX tX (10)
new
In equation 9, there are no derivation terms to óh, ,, which is
the height of ground point.
Since the inverse f; g;, f» and g» are set of functions, some of
which are iterative functions, their partial derivatives in A
cannot be directly derived. They are instead analytically
computed.
With the initial A; of tie points to 0, /on;,lat; of both tie points
and ground point calculated from equation 2, and 3 coefficients
to 0, X can be solved with equation 8. Then the initial values are
replaced with the new values X,,,, with equation 10. The least
square estimation is repeated until Æ is stabilised to a minimal.
4. IMAGE ORTHORECTIFICATION
The original sensor model of PAN and the refined sensor model
of XS images are used to orthorectified PAN and XS images
respectively. As mentioned earlier, the look angles between the
PAN and XS Image for SPOT 5 HRG instrument is 1.06?. This
is equivalent to a B/H ratio of less than 0.02. If the error in the
DEM used is 100m in height, the relief displacement error
between the PAN and XS images will be about 2m, less than a
PAN pixel size. This insensitivity to DEM accuracy suggests
that a coarse orthorectification with the km gridded GLOBE or
SRTM will be accurate enough for removing the relative
displacement error to sub pixel accuracies.
5. COLOR MERGING
Merging of the high resolution colour imagery is performed by
multiplying each spectral band with a sharpening factor
computed from the intensity values of the panchromatic image
and the corresponding pixels of the multispectral images. The
equation for merging is described below:
Lan
la m 1 (11)
merge I lys
XS
where i =the band index of SPOTS imagery
Li and IS = intensity of panchromatic and
multispectral imagery, respectively
Ly and I, = grey value of each band in
merge =
multispectral and merged imagery, respectively
The factor ( /
pon td fc) 18 referred to as the sharpening factor.
Since the spectral range of the PAN image overlaps only the
RED and GREEN bands of the XS image, we compute the
T by taking averaging of pixel values of only the RED and
XN
GREEN bands. The non-overlapping bands (NIR band and
SWIR band) can either be sharpened with the same sharpening
factor or merely resampled to the resolution of the
panchromatic imagery. The pseudo-natural colour SPOT 5
imagery can also be merged with the panchromatic imagery in
the same way.
6. TEST IMAGERY AND RESULTS
To test the method developed, we chose a site in Bandung,
Indonesia, where there are sullen volcanoes and the terrain
height variation from a few tens to more than 3000 meters. A
pair of 2.5m PAN and 10m XS SPOT 5 images taken from the
same instrument were selected over the area. Figure 2 and
Figure 4 show the overview of level 1A images of PAN and XS
respectively. Parts of the full resolution images are shown in
Figure 3 and 5.
The edges of PAN imagery detected by Canny detector are
shown in Figure 6 in grey, while the corners detected by Harris
corner detector are shown in black in the same figure. Total 40
image patches have been matched and the tie points selected
automatically for the sensor model refinement. The rms
residual after least squares solution of the refined XS sensor
model is 0.7 pixel (PAN image pixel size).
Figure 7 shows the overview of orthorectified PAN image after
applying its sensor model. And Figure 8 shows the overview of
orthorectified XS image after applying its refined sensor model.
The final merged 2.5m pixel pseudo-natural color imagery
(merged from both orthorectified PAN and XS images) is show
in Figure 9 in overview and Figure 10 in full resolution.
7. CONCLUSION
image registration method
and corners) and
To conclude, an automated relative
based on feature information (edges
refinement of XS sensor model relative to the PAN sensor
model is described. The GLOBE or SRTM DEM used in
orthorectification was sufficient to eliminate the relative relief
displacement to better than one PAN pixel. The PAN and XS
orthorectified images generated can then be merged to produce
a high resolution multispectral image, that has the high
resolution of PAN and colour information of XS. The method
has been tested on a few SPOTS PAN and XS image pairs of
various incidence angles and various relief situations. The
results were consistent.
We expect the automatic matching method to have problems in
imagery where there are too much clouds or water. In such
situations, the program may not be able to find enough image
patches with good edges and corners content. An option has
been provided to manually provide the corresponding image
Intern.
MIEL IE
registi
locate
refinit
way.
Refer
Bergh
patter
pp. 72
Canny
IEEE
PAMI
Christ
quinci
Geosc
Harris
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189-1