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.

ParameterDefinitionHydrologic process or variable affectedRankValue

Alpha_BfBaseflow recession constantBaseflow10.084
Cn2Moisture condition curve numberSurface runoff230~92
Ch_K2Effective hydraulic conductivity in main channel alluvium (mm/h)Concentration of channel310
EscoSoil evaporation compensation factorSoil water and soil evaporation40.6
Sol_KSaturated hydraulic conductivity of first layer (mm/h)Infiltration and soil water50~2000
Sol_ZDepth from soil surface to bottom of layer (mm)Soil water60~3500
CanmxMaximum canopy storage (mm)Interception70~10
Sol_AwcAvailable soil water capacity (mm/mm)Soil water80.0125~0.5