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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
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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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VariableParameterFrequencyNotes
PETPotential evapotranspirationtime-step
xExcess rainfalltime-stepsee Figure 1
INFInfiltrationtime-stepEstimated from (1-H’)x (see Figure 1)
r1Direct runofftime-stepsee Figure 1
r2Rainfall in excess of infiltration capacity (Hortonian runoff)time-stepsee Figure 1
r3Moisture in excess of soil moisture capacity discharged to streamtime-stepsee Figure 1
r9Moisture in excess of soil moisture capacity recharging (percolating to) groundwatertime-stepsee Figure 1
rsGenerated surface runofftime-stepsee Figure 1
QOUTsurfRouted surface runoff (from gamma function)time-stepsee Figure 1
QOUTgwRouted groundwater runofftime-stepsee Figure 1
SMStotSoil moisture store contents (total of all layers)time-stepsee Figure 1Layers 1...etcList of soil moisture store layersone-off itemsee Figure 1

Reference list

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