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The disrupted former drainage system of southwest Western Australia has already been referred to, and remnants of similar old stream networks occur in the Amadeus depression, on the Nullarbor Plain, and in the Great Victoria Desert.
Table 1 summarizes the comparison of stream networks and catchments.
This helps increase the degree of agreement between stream networks delineated from the DEM and the input vector stream networks (Hellweger 1996).
If required, the algorithm will generate cyclic and/or split stream networks.
These stream networks were monitored for both their DOC concentration and export (flux per unit area).
The DEM was used for delineating the study area's watershed and stream networks.
Open image in new window Fig. 1 Location map of the study area with stream networks.
Later, the stream networks within each of the watersheds were digitized using ArcGIS.
The stream networks were used to generate the drainage density of the study area.
The development of stream networks depends on geology, rainfall of the area.
In the Diamare piedmont (northern Cameroon) they are particularly well developed within stream networks.
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