Research Article
Hydrologic Responses to Land Use Change in the Loess Plateau: Case Study in the Upper Fenhe River Watershed
Table 4
The results of parameter sensitivity analysis and calibration.
| Parameter | Definition | Hydrologic process or variable affected | Rank | Value |
| Alpha_Bf | Baseflow recession constant | Baseflow | 1 | 0.084 | Cn2 | Moisture condition curve number | Surface runoff | 2 | 30~92 | Ch_K2 | Effective hydraulic conductivity in main channel alluvium (mm/h) | Concentration of channel | 3 | 10 | Esco | Soil evaporation compensation factor | Soil water and soil evaporation | 4 | 0.6 | Sol_K | Saturated hydraulic conductivity of first layer (mm/h) | Infiltration and soil water | 5 | 0~2000 | Sol_Z | Depth from soil surface to bottom of layer (mm) | Soil water | 6 | 0~3500 | Canmx | Maximum canopy storage (mm) | Interception | 7 | 0~10 | Sol_Awc | Available soil water capacity (mm/mm) | Soil water | 8 | 0.0125~0.5 |
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