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Rational Method Runoff Calculator

The peak stormwater runoff from a catchment — the rational method, Q = C i A — from the surface type, the design rainfall intensity and the area, in cubic metres and litres per second.

The rational method assumes that at the peak the whole catchment contributes: peak flow equals a runoff coefficient (the share of rain that runs off — near 0.

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Results
Peak runoff
0.278 m³/s
In litres per second
Per hectare
Pipe that carries it at 1 m/s (rough)
Volume in a 30-minute storm at this rate
Reviewed September 2026. Planning arithmetic is universal; the rates are local and yours to set. ONS publishes density by output area; local plans under the NPPF set housing and land-use policy.
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About rational method runoff

How the rational method runoff calculator works

The rational method assumes that at the peak the whole catchment contributes: peak flow equals a runoff coefficient (the share of rain that runs off — near 0.9 for roofs and asphalt, 0.2–0.3 for lawns) times rainfall intensity times area. With intensity in mm/h and area in hectares, dividing by 360 gives m³/s. It suits small catchments up to a few tens of hectares; larger ones need routing.

Formula: Q (m³/s) = C × i (mm/h) × A (ha) ÷ 360

Worked examples

InputsPeak runoffNote
Suburban mix, 80 mm/h, 2.5 ha0.278 m³/s0.278 m³/s
A 1 ha car park at 120 mm/h0.283 m³/s0.283 m³/s
10 ha of parkland at 50 mm/h0.347 m³/s0.347 m³/s

Frequently asked questions

What intensity do I use?

The design storm for your standard — a 10- or 20-year event for minor drainage, 100-year for major — at a duration equal to the catchment’s time of concentration (often 5–15 minutes for a small site). Intensity–frequency–duration tables are published by the national weather service.

Why do the coefficients vary?

They combine how much rain soaks in with how fast the rest runs off: roofs and asphalt shed nearly everything, lawns absorb most of a moderate storm. Steep or saturated ground pushes the coefficient up; use the higher end of the range for big storms.

What are the method’s limits?

It gives a peak, not a hydrograph; it assumes uniform rain over the whole catchment for at least the time of concentration; and it becomes unreliable above a few tens of hectares or where storage and routing matter.

How do I size the pipe properly?

The 1 m/s row is only a first estimate. Pipe capacity depends on slope and roughness (Manning’s equation) and codes require minimum velocities for self-cleansing; a drainage engineer sizes it.

Where these figures come from

Last checked: September 2026. Default per-capita rates are mid-range figures from national statistical agencies and utility reports; every one is an input you should replace with the local figure.