ina
na
lization.
obstacles
>s can be
xtraction.
ng wind
0 hedges
Different
tion, are
by their
nshine.
3). Prior
le open
) extract
potential
ed work
ion and
terest in
n field
of wind
rwards,
'stacles,
*b, line
will be
d wind
on 4 to
Finally,
d wind
gery as
IS-data
ape of
Ige and
e from
w. The
International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XXXV, Part B3. Istanbul 2004
non-vegetation areas in CIR images are removed by NDVI and
CIE L*a*b. Afterwards, edges of tree rows and hedges are
extracted with Canny edge extraction algorithm followed by line
linking, grouping and matching. Lines belong to non-interested
regions such as urban, forests in the stereo imagery are masked
out by GIS-data. DSM is also integrated into line grouping
approach because of usually short distance and low contrast in
NDVI and CIE L*a*b information of pixels between hedge and
tree row. Then the matched lines are projected onto the landscape
with known camera parameters. 3D information provided by
DSM is used to verify the potential wind erosion obstacles since
they are always higher than the landscape. Finally, the objects of
interest, wind erosion obstacles, are described by their
characteristics and appearance in an overall context with other
neighboring and influencing objects.
2.0 Data sources
~
The GIS data with accuracy of about 3 m consists of scene
description of the German ATKIS DLMBasis (Authoritative
Topographic Cartographic Information System, basic digital
landscape model) (Butenuth 2003). Since only wind erosion
obstacles are of interest, regions where no wind erosion obstacles
exist (e.g. urban, water, forest) in the imagery can be masked out
by the available GIS-data. Furthermore, the GIS-objects road,
river and railway represent the approximate geometric position of
parts of the field boundaries. They also represent potential search
areas for wind erosion obstacles, which are usually located
parallel and near to them. Figure 1 shows the GIS data
superimposed on the aerial image in the open landscape. Roads
and field boundaries are depicted in yellow, buildings in white
and forests in green. A representative region of interest is
represented in dashed white lines, separately shown in figure 2.
Fig. 1. Open landscape with superimposed GIS data
CIR images (with ground resolution of 0.5m in this paper) are
generated in early autumn when the vegetation is in an advanced
period of growth. The color is almost fully green for wind erosion
785
obstacles, while for example light yellow for crops. This
information is advantageous for automatic vegetation extraction.
Therefore, the color space RGB, which presents the raw stereo
CIR images, is transformed into a device type independent color
space CIE L*a*b since it is powerful in image segmentation. The
CIR aerial image is classified into vegetation and non-vegetation
regions. Furthermore, classifying with NDVI is also possible. The
two approaches are both used to segment the images into
vegetation and non-vegetation areas. Of course, there are other
objects than wind erosion obstacles, which will appear in green
color such as grassland. That means GIS-data and CIR imagery
are not enough to extract wind erosion obstacles.
Fig.2 Selected region of interest
Fig. 3. DSM superimposed with orthoimage
Additionally, corresponding DSM with 0.5 m ground resolution
of the interested open landscape is obtained with VirtuoZo, which
is developed by Supresoft Inc. The DSM is not precise because