Research Article
Prioritization of Susceptible Watershed to Sediment Yield and Evaluation of Best Management Practice: A Case Study of Awata River, Southern Ethiopia
Table 6
Streamflow calibration parameters and their sensitivity rank.
| Rank | Parameter | Description of parameter | Range value | t-stat | value |
| 1 | R_CN2.mgt | SCS runoff curve number | ±0.2 | −16.81 | 0 | 2 | V_HRU_SLP.hru | Average slope steepness | 0-1 | −15.94 | 0 | 3 | V_RCHRG_DP.gw | Deep aquifer percolation fraction | 0-1 | −15.51 | 0 | 4 | V_CANMX.hru | Maximum canopy storage | 0–100 | 7.63 | 0 | 5 | V_ALPHA_BF.gw | Baseflow alpha factor | 0-1 | 6.73 | 0 | 6 | R_SOL_K.sol | Saturated hydraulic conductivity | ±0.25 | −5.72 | 0 | 7 | R_SLSUBBSN.hru | Average slope length | ±0.25 | 4.4 | 0 | 8 | R_SOL_AWC.sol | Available water content of soil | ±0.25 | −2.41 | 0.02 | 9 | V_GW_DELAY.gw | Groundwater delay | 100–500 | 1.38 | 0.17 | 10 | V_CH_N2.rte | Manning’s “n” value for the main channel | −0.01–0.3 | 1.25 | 0.21 | 11 | V_CH_K2.rte | Effective hydraulic conductivity of main channel alluvium | −0.01–500 | −0.67 | 0.5 | 12 | V_SURLAG.bsn | Surface runoff lag time | 0.05–24 | −0.67 | 0.5 | 13 | V_GW_REVAP.gw | Groundwater revap coefficient | 0.02–0.2 | 0.52 | 0.61 | 14 | V_GWQMN.gw | Threshold depth of water in the shallow aquifer for return flow to occur | 3500–5000 | −0.46 | 0.65 | 15 | V_REVAPMN.gw | Threshold depth of water in the shallow aquifer for revap to occur | 100–500 | 0.35 | 0.72 | 16 | V_OV_N.hru | Manning’s “n” value for overland flow | 0-1 | 0.31 | 0.76 | 17 | V_EPCO.bsn | Plant uptake compensation factor | 0-1 | 0.26 | 0.79 | 18 | R_SOL_Z.sol | Soil depth (for each layer) | ±0.25 | −0.1 | 0.92 | 19 | V_ESCO.bsn | Soil evaporation compensation factor | 0-1 | −0.06 | 0.95 |
|
|