2-3-2 INTERPOLATION WITH POINT BY POINT
It is necessary to select new reference points
while a point is inserted by this method. The
principle of this method is shown in Figure 4.
At the first, we define the effective area for
DTM sampling that means what area will be
sampled or not. For deciding the interval of
interpolation, all intersections of each scan
line and defined area should be determined,
before interpolation is processing . As
mentioned above, there are N reference points
to be selected in neighborhood of sampling
point. Then suitable interpolation model is
used according to accuracy criterion, e.g.
weighted moving average method, bilinear
interpolation, two-order polynomials and linear
least squares prediction etc. Although the
result of surface modelling is more feasible,
description of terrain features is still worse
due to grid DTM. And it is time-consuming
especially as the number of reference points is
increasing.
Figure 4 The principle of interpolation with
point by point
2-4 CASE STUDY
The case study is based on a topographic map
used for the design of a golf court. The: shape
of study area is irregular. There are total
514 random points in the area which is gained
by digitizing contour lines. The Delauney
triangulated network for a set of 514 random
points is shown in Figure 5. Figure 6 is the
original contour map of the study area. The
polygon of the area is constituted with 166
vertices. Then a 65x65 grid DTM is generated
by the methods mentioned above, i.e. TIN and
point by point methods. Heights outside the
study area are given by negative values and are
not processed. Fig. 7 shows the contour map
which is the result of TIN method and Fig. 8
shows the result of point by point method with
least squares prediction.
Figure 5 The Delaunay triangulated network for
a set of 514 points
904
Figure 6
Figure 7 The contour map obtained from the
result of TIN
Figure 8 The contour map obtained from the
result of point by point with least
squares prediction method
III. EXTRACTION OF TERRAIN FEATURES FROM DTM
The extraction of terrain features from DTM can
be done by either raster or vector methods. In
fact, extracting terrain features and display
the result by raster method is simpler than
vector method. ' Moreover, raster display has
better effect in landscape visualization.
Slope gradient and aspect in each grid can be
computated with DTM data[13). Feature lines of
terrain, such as ridges and valleys, are
the important factors of describing the
characteristics of terrain. They are helpful
for interpretation of streams and watersheds
and can be used as reference features for image
matching [ 16, 3, 6 JJ. For example, a 3x3
operating mask is used to decide ridges. If
the central pixel P contents with following
three criterions, then pixel P is a ridge:
1. Height of pixel P is not the lowest when
it compare to heights of neighboring 8
points, see Figure 9.
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