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Therefore, the high relief difference was scored with 5 and the flat area (low relief class) was scored with 0. Table 3 The correlation between slope and relief (van Zuidam, 1986) Slope Relief (m/km2) Classification 0 2 <5 Flat 2 7 5–25 Gently slope 7 15 25–75 Sloping 15 30 75 200 Moderately steep 30 70 200 500 Steep 70 140 500–1000 Very steep >140 >1000 Extremely steep.
This anomaly is due to diversity of slope, relief and structural conditions prevailing in the watershed.
The relations among slope, relief, and landform class are depicted in Table 5.
The circularity ratio is influenced by the slope, relief geologic structure of the basin and landuse/landcover.
The watershed boundaries were demarcated on the basis of contour value, slope, relief, and drainage flow directions and DEM.
The central portion of the range exhibits the highest slope, relief and steepness of river longitudinal profiles.
Similar(50)
The water availability can be described by the relief-dependent (influenced by the exposition, slope and relief position) climatic water balance within the period from May to October and the available water capacity in the upper 1 m of the ground.
Longitudinal profiles and geomorphometric indices, such as slope, local relief and channel steepness reveal that the Qilian Shan was developed as a local plateau with high-relief steep marginal ranges, and interior low-relief topography.
This is mainly due to the diversity of slope and relief pattern of the basin.
There were five facets with homogeneous terrain conditions was divided using topographical map based on slope inclination, relief (elevation difference), and slope direction.
Moreover, the slope and relief of the area were extracted from the same data source using spatial analyst tool in ArcGIS 10 software.
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