How it works
Q = C·i·A / 360 — Q in m³/s, C the dimensionless runoff coefficient, i the design rainfall intensity (mm/hr) at a duration equal to the catchment's time of concentration, and A the area in hectares. With multiple surfaces, the composite coefficient is the area-weighted mean: Cw = ΣC·A / ΣA.
Runoff coefficient C — typical values
| Surface | C |
|---|---|
| Roofs | 0.85 – 0.95 |
| Asphalt / concrete pavement | 0.80 – 0.95 |
| Gravel surfaces | 0.40 – 0.60 |
| Urban landscape / irrigated gardens | 0.15 – 0.35 |
| Desert / sparse natural ground (Gulf) | 0.30 – 0.60 |
| Steep rocky wadi slopes | 0.50 – 0.80 |
Gulf caution: arid soils crust and shed water far more aggressively than temperate lookup tables assume — municipal criteria (MOMRAH, Abu Dhabi DMT) often mandate minimum C values for desert catchments. Our note on Saudi rainfall design criteria covers selecting the intensity i defensibly.
When the Rational Method stops being enough
Beyond ~80 ha, with significant storage, or where flow paths interact — peak-only methods miss timing and volume effects that govern the design. That's hydrograph and 2D territory: stormwater modelling in HEC-HMS, HEC-RAS 2D or InfoWorks ICM. Capacity-check the receiving pipe or channel with the Manning calculator.