Parameters and ranges of values used in the FLEX-Topo model
Parameter . | Range . | Description . |
---|---|---|
FDD | [1,8] | Degree day factor defining the melted water per day per Celsius degree above Tt |
Tt | [−2.5,2.5] | Air temperature threshold above which snow melts |
Pt | [5,35] | Threshold parameter indicating occurrence of HOF in hydrological upland |
SumaxB | [5,500] | Maximum soil moisture capacity in the root zone of hydrological upland |
PmaxB | [0.1,10] | Maximum percolation of hydrological upland |
DB | [0,1] | Splitter to separate preferential flow from recharge in hydrological upland |
Tlag | [0,5] | Time lag between storm and fast runoff generation |
KfB | [2,50] | Timescale of the runoff from fast reservoir in hydrological upland |
ImaxFH | [1,10] | Daily maximum interception capacity of sunny hillslope |
Ce | 0.5 | A ratio above which the actual evaporation is equal to potential evaporation |
SumaxFH | [100,1,000] | Maximum soil moisture capacity in the root zone of sunny hillslope |
βFH | [0.1,5] | Parameter used to calculate runoff coefficient in sunny hillslope |
D | [0,1] | Parameter separating the generated surface runoff on hydrological upland into the splitter to separate preferential flow from recharge in sunny and shady hillslope |
Kf | [2,50] | Timescale of the runoff from fast reservoir in sunny and shady hillslope |
ImaxGH | [0,10] | Daily maximum interception capacity of shady hillslope |
SumaxGH | [50,1,000] | Maximum soil moisture capacity in the root zone of shady hillslope class |
βGH | [0.1,5] | Parameter used to calculate runoff coefficient in shady hillslope |
ImaxW | [0.1,10] | Daily maximum interception capacity of hydrological lowland |
SumaxW | [5,1,000] | Maximum soil moisture capacity in the root zone of hydrological lowland |
βW | [0.1,5] | Parameter used to calculate runoff coefficient in hydrological lowland |
KW | [1,9] | Timescale of runoff from fast reservoir in hydrological lowland |
Ks | 90 | Timescale of the runoff from slow reservoir |
CRmax | [0,5] | Parameter indicating a constant amount of capillary rise |
Parameter . | Range . | Description . |
---|---|---|
FDD | [1,8] | Degree day factor defining the melted water per day per Celsius degree above Tt |
Tt | [−2.5,2.5] | Air temperature threshold above which snow melts |
Pt | [5,35] | Threshold parameter indicating occurrence of HOF in hydrological upland |
SumaxB | [5,500] | Maximum soil moisture capacity in the root zone of hydrological upland |
PmaxB | [0.1,10] | Maximum percolation of hydrological upland |
DB | [0,1] | Splitter to separate preferential flow from recharge in hydrological upland |
Tlag | [0,5] | Time lag between storm and fast runoff generation |
KfB | [2,50] | Timescale of the runoff from fast reservoir in hydrological upland |
ImaxFH | [1,10] | Daily maximum interception capacity of sunny hillslope |
Ce | 0.5 | A ratio above which the actual evaporation is equal to potential evaporation |
SumaxFH | [100,1,000] | Maximum soil moisture capacity in the root zone of sunny hillslope |
βFH | [0.1,5] | Parameter used to calculate runoff coefficient in sunny hillslope |
D | [0,1] | Parameter separating the generated surface runoff on hydrological upland into the splitter to separate preferential flow from recharge in sunny and shady hillslope |
Kf | [2,50] | Timescale of the runoff from fast reservoir in sunny and shady hillslope |
ImaxGH | [0,10] | Daily maximum interception capacity of shady hillslope |
SumaxGH | [50,1,000] | Maximum soil moisture capacity in the root zone of shady hillslope class |
βGH | [0.1,5] | Parameter used to calculate runoff coefficient in shady hillslope |
ImaxW | [0.1,10] | Daily maximum interception capacity of hydrological lowland |
SumaxW | [5,1,000] | Maximum soil moisture capacity in the root zone of hydrological lowland |
βW | [0.1,5] | Parameter used to calculate runoff coefficient in hydrological lowland |
KW | [1,9] | Timescale of runoff from fast reservoir in hydrological lowland |
Ks | 90 | Timescale of the runoff from slow reservoir |
CRmax | [0,5] | Parameter indicating a constant amount of capillary rise |