.ines and
ms for a
skeleton
closing,
‚are of
nes may
re trace
ed. One
3) is to
irichlet
image.
ages and
thinning
skeleton
A2).
he line
irection
(by in
in [16].
s to be
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and line
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ines to
rpolated
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IT image
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Ir parts
Ss not
om four
gure 8
les are
ines to
mask 4 pixels topology scan on
tesselated image Thiessen polyg.
1 2
3 4
using 2 confused 4 intersecting
diagonals topology triangles
4e—— 2 Bede b
PAS PARE
3—— 4 C d
using 1 unique 2 adjacent
diagonal toplogy triangles
F2 à ——e D
A i 2i
3——4 i-a
Fig. 7:
VE TN TR TS X EN S X ny
Mask and result of topology scan
and skeleton
Fig. 8: TIN generated from contours
lines
Fig. 9: DTM from contours and skeleton
959
The topology of the network is documented by two
tables. The first relates every triangle to its
nodes by identification number; the second relates
every triangle to its neighbours.
The TIN provides a better data structure than the
original contours for deriving various . DTM
products, and without loss of information. Based
on TIN, Alias [1] developed a set of programs for
computing a grid DTM (in ILVIS format), generating
contour lines and slope models. The improvement of
the grid DTM, compared with figure 1, is
illustrated in figure 9. Linear interpolation is a
good choice for rough terrain with many
breaklines. Other interpolation methods are
adequate, if smooth surface representation is
required (see [11]).
CASE STUDY
How does the automatically derived skeleton
compare with a photogrammetrically sampled one?
We selected mountainous terrain in southern France
(near Bonnieux) as a test site. Contours of an
area 3 by 3 km were digitized from a 1:50,000
topographic map with a contour interval of 20m.
After interactive editing, the contours were
rasterized vith a 6.5m pixel size. Figure Al shows
the contours overlaid on the relief-shaded DTM
which was produced directly from the contours.
Figure A2 shows the automatically-derived skeleton
lines, overlaid again on the same relief shades as
in figure Al. The skeleton lines were produced as
illustrated in figure 3.
Photogrammetric selective sampling was done on the
Planicomp C120 1:60,000 photographs. Digitizing
the ridge and drainage lines, peaks, pits and
passes took some 4 hours. Figure 10 shows the
portion of the overlaid skeletons that corresponds
two-colour version of the entire
[10]). The grid DTM generated
and skeleton
to figure 9 (a
area is given in
through triangulation from contours
(see figure A3) has lost its plateaus!
« C»
Em
ANA
of skeletons from manual
'fringes'
Fig. 10: Superimposition
and automatic extraction (the
belong to the automatic one)
As shown in figure 10 (although it is difficult to
discern which lines belong to which skeleton), the
overall agreement of the two sets of lines is
good. In addition to the differences caused by
insufficient registration (the usual problem vith
control points), there are obvious differences in
what is extracted by the two methods. The