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The results for the cell morphometric parameters are listed in Table 1.
The model based and model independent morphometric parameters are comparable with measurements using other characterisation techniques.
The methodologies adopted for the computation of morphometric parameters are given in Table 2 and results are presented in Table 3.
The watershed is delineated and the morphometric parameters are derived from analyzing the SRTM3 Digital Elevation Model (DEM) using Geographic Information System GISS) to construct a hydrological model.
Inferring from the Terrain Mapping Camera-Digital Elevation Model (TMC-DEM), the morphometric parameters are estimated (350 m in height, 9.62 km in diameter), and accordingly the rheological parameters are also estimated.
Morphometric parameters are important and useful to identify various hydraulic characteristics of drainage basin, i.e., patterns, shape, stage of stream, permeability of bed rock, health of streams, as well as help to correlate with lithological characteristics (Yadav et al. 2014).
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The prioritization based on different morphometric parameters is time consuming.
Overall, twenty-seven morparametersparameters were computed for Agula watershed and for each of the sub-watersheds.
Other morphometric parameters were calculated using the equations as described in Table 1.
Linear, areal and relief aspects of the morphometric parameters were calculated in the study.
Morphometric parameters were evaluated from four perspectives: drainage network, watershed geometry, drainage texture, and relief characteristics.
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