d NUS Sn
Figure 3: ERS-2 Intensity image
(information provided by ESA). The lengths of these
components satisfy the wish to have a limited baseline
decorrelation.
The window that is selected from the images reflects an
area in the central part of the Netherlands. The area
consists of a relative new polder with large agriculture fields,
a developed moor land including reed fields, an area with
small agriculture fields on the "old" land and parcels with
forest. The old and the new land are separated by a lake. In
the area there are no relief differences, it is a very flat
terrain.
2.2 Field data collection
In order to classify the images, samples were taken that are
supposed to be representative of the various types of land
cover, and, at the same time, in order to check the accuracy
and reliability of the classification another independent set
of samples was acquired. Field data was acquired a few
weeks later than the image acquisition dates. The eight
classes that are selected did not change between the
acquisition date and the field check. Only some grass field
may have been cut in that period and some stubble fields
plowed.
The following classes are recognized :
. Bare soil.
. Sugar beets.
. Stubbles.
. Forest.
. Maize.
. Grass.
. Water.
. Reed.
o 100120 mw -—
2.3 SPOT georeferencing
The Spot image is georeferenced using the ILWIS image
processing software applying an affine transformation
including a nearest neighbor "interpolation". The overall
accuracy, expressed in RMSE, of the reference points used
for the creation of the transformation polygons was less
than 1 pixel.
2.4 ERS1/2 intensity images
From the SLC images, intensity images are created. The
one with the highest number of clearly visible objects (in this
case the ERS-1) is selected to support the registration of
the coherence map to the SPOT image.
2.5 Coherence map creation
The coherence map (figure 4) is created using software
developed at DLR in Oberpfaffenhofen, Germany. The
interferometric software requires some information which is
available in the leader file.
Figure 4: Coherence map
For an accurate registration of two SLC data sets it is
necessary to measure the shifts between the images in
azimuth and range direction which is done in the intensity
images. These shifts are introduced in the data processing
for a coarse registration. The WGS84 is chosen as
reference system for the resampling of the second scene.
To inspect the coarse registration, the fringes and the
coherence map are calculated from the coarse registered
images. If the registered images cannot produce a sufficient
number of fringes, the coarse registration has to be
repeated with more accurate shifts. The next step is the fine
registration of the images. This is one of the most important
steps during the whole data processing because it is the
basis for the quality of the later derived interferometric
products. The master image remains unchanged while the
slave image is fitted to the master. To reduce unwanted
variation in the coherence map, a window of 20 azimuth * 2
range elements is used for the computation of the
correlation. Based on this filtered map the interferogram is
calculated, i.e., the resulting fringes are also corrected
under assumption that the Earth is flat.
2.6 Coherence map registration
The coherence map and the ERS-1 image have apart from
minor shifts, which are caused by the slightly different orbits
of the ERS-1 and the ERS-2, the same geometry. So
registration of the coherence map and ERS-1 image will
follow the same transformation steps. The following steps
are performed, partly with ILWIS and partly with PCI's
EASI/PACE.
- resample the intensity image to an azimuth resolution of
20 meter by averaging five columns elements into one.
- select the sub image of the ERS-1 that covers
approximately the same area as the SPOT sub image.
- transform the image from slant range into ground range
International Archives of Photogrammetry and Remote Sensing. Vol. XXXI, Part B2. Vienna 1996
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