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The generalization of braided sections of rivers needs further investigation,
as the first attempts did not produce satisfactory results. In one of our sam-
ple datasets the presence of too many flat edges inside braided sections of
rivers caused the river course reconstruction to fail; the only viable solu-
tion was then to exclude these sections from the pruning.
Source
Generalized
Length
Density
River sections
9786
6290
2112
1474
River courses
5674
2530
2053
1091
Total length (meters)
3420245
2720324
299766
400155
Average length per section (meters) 349
432
142
366
Table 3: results of the generalization process; the third and fourth columns indicate
respectively the numbers relative to the rivers pruned by length and density thresholds.
Figure 9: results of the generalization: left source data, right generalized data (only re-
classified, not pruned).
This was achieved finding the cycles in the hydrography graph (the edges
forming a cycle are part of a braided stream). The braided parts of the
rivers then are not pruned but only re-classified. We are currently investi-
gating a generalization strategy that detects the areas enclosed between the
branches of a braided river and typifies the clusters of these areas either by
collapsing each area to a line, or by merging neighboring ones.
4- Conclusions and future plans
In this paper a complete process for model generalization of a hydro-
graphic network was described.
 
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