Watershed Area
161.95 km²
Final ArcSWAT watershed corresponding closely to the Hare Weir catchment.
HARE Revisited · Continuous watershed modelling
The SWAT model provides the continuous-watershed component of the HARE Irrigation Project hydrological reassessment. Watershed delineation, HRU development, climate preparation and two continuous simulations have now been completed for the approximately 161.95 km² Hare River catchment.
The current analysis examines daily and seasonal streamflow, watershed water balance, evapotranspiration, surface runoff, lateral flow, groundwater contribution, upland erosion and sediment transport and deposition.
161.95 km²
Final ArcSWAT watershed corresponding closely to the Hare Weir catchment.
17
Hydrologically connected subbasins generated from the DEM-derived drainage network.
2020–2025
Daily NASA POWER climate forcing represented by 16 spatial weather points.
2020
The first simulation year is used for model initialization.
2021–2025
Principal period used for hydrological and sediment assessment.
2
Two successful daily SWAT simulations with similar overall watershed response.
1665.5 mm
Mean annual precipitation reported by the Simulation 2 SWAT Error Checker.
267.63 mm
Basin-average annual surface runoff from Simulation 2.
182.06 mm
Simulated groundwater contribution to the stream system.
211.6 m³/s
Largest current SWAT daily outlet flow, simulated on 15 April 2024.
58.4 Mg/ha
Basin-average upland sediment yield in Simulation 2.
96.23%
SWAT diagnostic indicating very strong simulated in-stream sediment deposition.
Daily NASA POWER precipitation, temperature, solar radiation, relative humidity and wind-speed forcing for 2020–2025, represented by a 16-point spatial weather grid.
Status: Completed
Climate →DEM processing, flow direction, flow accumulation, stream definition, outlets and the final 17-subbasin watershed.
Status: Completed
Watershed →Full land-use, soil and five-class slope overlay with zero-percent elimination thresholds and HRU-scale runoff and erosion assessment.
Status: Completed
HRUs →Water balance, seasonal response, daily outlet flow, groundwater contribution, erosion hotspots, sediment yield and channel deposition.
Status: Active interpretation
Results →Historical 1980–1990 Hare River observations are available, but matching historical climate forcing is still required before formal same-period calibration.
Status: Framework prepared
Calibration →The HARE reassessment uses HEC-HMS and SWAT for different but complementary purposes.
| Model | Primary Role | Current Status |
|---|---|---|
| HEC-HMS | Event-based rainfall-runoff modelling and design-flood hydrograph estimation at the Hare diversion weir. | Completed |
| SWAT | Continuous watershed water balance, streamflow, groundwater, erosion and sediment-routing assessment. | Simulation completed; results under interpretation |
The models should not be expected to return identical discharge values. HEC-HMS resolves individual design-flood events, while the present SWAT analysis represents continuous daily watershed behaviour.
One of the strongest findings from the SWAT assessment is the importance of sediment production and deposition within the Hare River system.
Simulation 2 indicates an average upland sediment yield of approximately 58.4 Mg/ha, identifies localized high-erosion HRUs and indicates strong net deposition within the stream network.
Current field photographs and video of the Hare diversion structure independently show substantial gravel, sand and finer sediment accumulation both upstream and downstream of the weir.
DEM + Drainage Network
↓
17 Subbasins
↓
Land Use + Soil + Slope
↓
HRUs
↓
NASA POWER Climate 2020–2025
↓
Continuous SWAT Simulation
↓
Hydrology + Streamflow + Sediment
↓
Field Evidence + Historical Comparison
↓
Calibration and Engineering Interpretation