Model direct runoff with dimensionless and triangular hydrographs. Compare peak discharge, lag, and base time. Clear outputs support watershed planning and stormwater design decisions.
Enter watershed and storm values below. Results appear above this form after submission.
Use these sample scenarios to test the calculator quickly.
| Scenario | Method | Area (km²) | Excess (cm) | Duration (hr) | Lag (hr) | Base Factor | Approx. Tp (hr) | Approx. Qp (m³/s) |
|---|---|---|---|---|---|---|---|---|
| Small rural catchment | Triangular | 45 | 1.0 | 2.0 | 3.0 | 2.67 | 4.00 | 23.40 |
| Mixed land use basin | SCS | 62 | 1.2 | 1.5 | 4.0 | 2.67 | 4.75 | 32.59 |
| Broad watershed check | Triangular | 110 | 0.9 | 3.0 | 5.0 | 3.10 | 6.50 | 27.34 |
V = A × 10,000 × Pe
A is basin area in km², Pe is effective rainfall in cm, and V is runoff volume in m³.
Tp = (Lag + D / 2) × Ft
Lag is basin lag, D is excess duration, and Ft is the optional time adjustment factor.
Qp = 2V / (Tb × 3600)
Tb = Fb × Tp
Fb is the base time factor. The triangular hydrograph preserves the runoff volume exactly.
Qp = 2.08 × A × Pe / Tp
This form uses A in km², Pe in cm, and Tp in hours. Ordinates follow a standard dimensionless SCS shape.
A unit hydrograph represents direct runoff caused by one unit depth of effective rainfall over a basin during a specified duration. It helps convert rainfall excess into a runoff response curve.
Only effective rainfall contributes to direct runoff. Losses such as infiltration, interception, and surface storage should be removed before using this calculator.
Use the triangular method for preliminary sizing, quick checks, or when you need a simple runoff shape with direct control over base time.
The SCS option is useful when you want a smoother, more realistic hydrograph shape based on a standard dimensionless runoff pattern commonly used in drainage studies.
Use a time step that matches your reporting interval or routing model. Smaller steps improve curve smoothness but also create larger tables.
The difference comes from numerical integration and the selected time step. Finer sampling usually reduces the volume error shown in the results summary.
Yes. Enter 1.0 cm for effective rainfall. The computed ordinates will then represent a one-centimeter unit hydrograph for the selected basin and duration.
No. This tool supports screening studies and design estimates. Detailed projects should still verify basin parameters, losses, routing assumptions, and observed hydrograph data.
Important Note: All the Calculators listed in this site are for educational purpose only and we do not guarentee the accuracy of results. Please do consult with other sources as well.