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ParameterDescriptionUnitsDefaultRange
CEvaporation coefficientnone00-1
Gused to estimate the proportion of moisture in excess of soil moisture storage capacity recharging groundwater (and also discharged to the stream)none00-1
Hused to estimate the proportion of rainfall excess contributing to the generated runoff as saturation excess runoff or the Dunne runoffnone00-1
KgTime lag parameter for groundwater routingnone0.010.01-200
nSurface runoff hydrograph ‘shape’ parameter (i.e. number of linear reservoirs)none11-10
nKSurface runoff hydrograph ‘scale’ parameter (i.e. time lag parameter in Nash cascade model)none11-10
TRatio of potential evapotranspiration to pan evaporationnone00-1
YInfiltration capacity of the soilmm.d-100-100
ZEffective moisture storage capacity of the soil contributing to the runoff generation mechanismsmm02000-125


Info
iconfalse
Note: the number of soil layers is determined from "Z" (Soil Moisture Storage Capacity) and a constant in the code which is 25 mm (the depth of each of the "groundwater"/soil layers in mm of water).

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