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The second simulation consisted of removing all of upper Marx Creek's stream cells located upstream of its confluence with the extension stream (stream cells 1 14), and leaving the extension stream in the model.
Table 4 Morphometric parameters using prioritization of the stream Stream number Bifurcation ratio (R b) Stream length L u/S u Rank 1 10 8 1 I 2 6 4 7 II 3 5 5 6 III 4 9 3 7 IV Open image in new window Fig. 8 Prioritization classes map of study area.
The results achieved in this study proposes that morphometric attributes defining basin geometry as well as shape, length of stream, stream network topology and topography dissection can be well retrieved from ASTER-DEM and accomplished to generate data on stream number and basin relief.
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This apart, geometry of ephemeral nets obeys the laws of drainage composition that apply to perennial streams: stream length, stream number, channel width, and water discharge can be expressed as exponential functions of stream order, and drainage area and channel slope as power functions, whereas slope and discharge can be expressed as power functions of width and drainage area.
Streams, stream sequences, and the related sets are defined as follows.
The fundamental parameters, namely, number of streams, stream length, area, perimeter and basin length were derived from the drainage layer.
The geomorphologic parameters were computed graphically by plotting number of streams, stream length and stream area versus the order of the stream and finding the slope of the best fit equation.
Information on number of different orders of streams, stream length and corresponding basin area etc. were extracted from the vectorized maps.
The input parameters for present study such as area, perimeter, stream order, number of streams, stream length, elevation and basin length were derived from digitized stream network and contour map in GIS environment.
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