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Figure 6. Inspection of FWF-ALS echoes in vegetated areas
with dense understory (red points) and TLS point cloud (green).
Next to the examination of the echoes that belong to one line of
sight, the influence of low vegetation on the FWF information
is analysed. One example for this study is displayed in Figure 6.
In the upper part of the figure dense brushwood can be found
below a tree (marked by a yellow rectangle). In the middle of
the figure a more detailed view of the understory area with the
red ALS points attached on the TLS observations can be found.
In the lower part of the figure the digitised FWF information for
one representative ALS point is displayed in a graph. Compared
to other echoes from planar extended targets (compare for
example the echoes of the tree trunk in Figure 4) it can clearly
be seen that the understory leads to an enlarged echo width.
This increase of the echo width is caused by the reflection of a
sequence of small reflecting surface elements at different
heights and provides therefore a good basis for the automated
detection of influence of these low vegetation cover on the
resulting ALS points. In these areas, points that are affected by
understory will typically lie slightly above the terrain. Without
the additional knowledge from FWF-ALS these points are very
As ALS constantly finds new fields of application, special
demands are increasingly made on the results. Archaeology for
example needs a high quality separation of terrain and off-
terrain points to derive detailed DTMs displaying micro-
topographic variation even under forest canopies. Biology and
forestry are interested to extract individual trees from the point-
clouds. During the last years, FWF-ALS turned out to have a
high potential to meet many of these requirements. However, an
in-depth understanding of the FWF-information is essential to
enhance the quality of the DTM and to allow a reliable
automated interpretation of the acquired data.
This paper aimed to start the investigation of the complex
interaction of the laser beam with different types of vegetation
cover. Part of a forest was scanned by airborne and terrestrial
laser scanning (Riegl LMS-Q680 and Riegl VZ-400). The
combined data acquisition took place simultaneously on a calm
day. Using tachymetry, the data sets were geo-referenced and
the differences between the ALS and TLS data sets were
minimized by an adjustment using planar control and tie
patches.
The investigation of each individual FWF echo together with
the derived FWF parameters and the digitised waveform could
be done within the context of the object that is provided from
the TLS data. In that way, we could gain interesting results
especially from densely vegetated areas, which will help to
improve algorithms for the advanced usage of FWF
information.
In the future we want to quantify the accuracy of the geo-
referencing of the ALS and TLS data in more detail.
Furthermore, we aim to study the interaction of the laser beam
with the terrain and the attached objects by further advanced
visualisations (e.g. by the direct visualisation of the FWF signal
and the FWF parameters in the 3D view).
REFERENCES
Briese, C., 2010. Extraction of Digital Terrain Models. In:
Airborne and Terrestrial Laser Scanning, Whittles Publishing,
ISBN: 978-1904445876, pp. 135-167.
Doneus, M. und Briese, C., 2006. Digital terrain modelling for
archaeological interpretation within forested areas using full-
waveform laserscanning. In: M. Ioannides, D. Arnold, F.
Niccolucci und K. Mania (Editors), The 7th International
Symposium on Virtual Reality, Archaeology and Cultural
Heritage VAST, pp. 155-162.
Doneus, M., Briese, C., Fera, M. und Jänner, M., 2008.
Archaeological prospection of forested areas using full-
waveform airborne laser scanning. Journal of Archaeological
Science, 35, pp. 882-893.