HARE Revisited · Continuous watershed modelling

SWAT

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.

Current model status

Hare River SWAT Model

Watershed Area

161.95 km²

Final ArcSWAT watershed corresponding closely to the Hare Weir catchment.

Subbasins

17

Hydrologically connected subbasins generated from the DEM-derived drainage network.

Climate Period

2020–2025

Daily NASA POWER climate forcing represented by 16 spatial weather points.

Warm-up

2020

The first simulation year is used for model initialization.

Interpretation Period

2021–2025

Principal period used for hydrological and sediment assessment.

Continuous Runs

2

Two successful daily SWAT simulations with similar overall watershed response.

Current results

Key Findings from the First SWAT Simulations

Mean Annual Precipitation

1665.5 mm

Mean annual precipitation reported by the Simulation 2 SWAT Error Checker.

Surface Runoff

267.63 mm

Basin-average annual surface runoff from Simulation 2.

Groundwater Return Flow

182.06 mm

Simulated groundwater contribution to the stream system.

Largest Daily Outlet Flow

211.6 m³/s

Largest current SWAT daily outlet flow, simulated on 15 April 2024.

Average Upland Sediment Yield

58.4 Mg/ha

Basin-average upland sediment yield in Simulation 2.

Channel Deposition

96.23%

SWAT diagnostic indicating very strong simulated in-stream sediment deposition.

Calibration status: the present SWAT model is functioning successfully and provides useful preliminary hydrological and sediment information, but it is not yet formally calibrated against an observed same-period discharge record.
SWAT technical record

Completed Model Components

Climate

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 →

Watershed

DEM processing, flow direction, flow accumulation, stream definition, outlets and the final 17-subbasin watershed.

Status: Completed

Watershed →

HRUs

Full land-use, soil and five-class slope overlay with zero-percent elimination thresholds and HRU-scale runoff and erosion assessment.

Status: Completed

HRUs →

Results

Water balance, seasonal response, daily outlet flow, groundwater contribution, erosion hotspots, sediment yield and channel deposition.

Status: Active interpretation

Results →

Calibration & Verification

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 →
Complementary hydrological models

HEC-HMS and SWAT

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.

Engineering interpretation

Emerging Importance of Sediment Management

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.

Current engineering implication: sediment exclusion, flushing, scour facilities and desilting should be considered important elements in the reassessment of the Hare diversion headworks.

View SWAT hydrology and sediment results →

Current SWAT workflow

Model Development Sequence

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