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Rational Method (Q = CIA)

The simplest peak-runoff equation. Best for drainage areas under 200 acres — pipe sizing, ditch design, parking-lot drainage. Not appropriate for runoff hydrograph generation or large watersheds.

— (0.10 to 0.95)
in/hr
acres
cfs

In US customary units, the equation is Q = CIA exactly because 1 acre·in/hr = 1.008 cfs ≈ 1 cfs (Mulvany's coincidence).

$$ Q = C \, I \, A \quad \text{(US customary, Q in cfs)} $$
$$ Q = \frac{C \, I \, A}{360} \quad \text{(SI, Q in m³/s, I in mm/hr, A in ha)} $$
Q peak flow rate · C dimensionless runoff coefficient (fraction of rainfall that becomes runoff) · I rainfall intensity for storm duration equal to time of concentration · A drainage area.

Runoff coefficient C

C is the most uncertain parameter. Standard values from ASCE Manual 77:

For mixed-cover watersheds, compute an area-weighted composite C: Cw = Σ(Ci × Ai) / Σ(Ai).

Rainfall intensity I

I is the average rainfall intensity for a storm duration equal to the watershed's time of concentration. Look up I from local IDF (intensity-duration-frequency) curves — NOAA Atlas 14 in the US is the common source. The design recurrence interval is selected by code: 10-year for residential streets, 25- to 50-year for arterials, 100-year for floodplain crossings.

Use the right time of concentration

The Rational Method assumes the entire watershed contributes to peak flow simultaneously, which only happens for storm durations ≥ tc. Use the time of concentration calculator to estimate tc, then read I off the IDF curve at that duration.

Limitations

Reference: ASCE Manual 77 — Design and Construction of Urban Stormwater Management Systems. Original: Mulvany, T.J. (1851), Kuichling, E. (1889).

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