Rational Method peak flow
Peak runoff from a small drainage area — the feed value for the pipe-sizing, detention, and outlet calculators below. Rainfall intensity comes from the local IDF curve; it is regional and is not built in.
Peak flow Q
—cfs
Time of concentration Tc
—min
Method & References
Q (cfs) = C · i · A
Tc (min) = 0.0078 · L^0.77 · S^−0.385 (Kirpich; S in ft/ft)
Variables & units: C — runoff coefficient (dimensionless); i — rainfall intensity, in/hr, from the local IDF curve at the design return period and Tc; A — drainage area, acres; L — longest flow path, ft; S — mean flow-path slope, ft/ft.
| Typical C values (Industry Approximation — Verify with PE) | C |
|---|---|
| Pavement / asphalt / concrete | 0.85–0.95 |
| Roofs | 0.85–0.95 |
| Gravel | 0.40–0.70 |
| Lawn, flat (sandy → heavy soil) | 0.10–0.25 |
| Lawn, steep (sandy → heavy soil) | 0.15–0.35 |
| Composite site — area-weight the parts | ΣCᵢAᵢ / ΣAᵢ |
Assumptions & limitations: small, hydrologically simple areas (commonly capped near 100–200 acres by agency policy); uniform rainfall over the whole area for a duration ≥ Tc; C constant over the storm. Intensity–duration–frequency data are regional — this tool does not hardcode an IDF curve, so i must be read from the governing agency's curves at the computed Tc. Many agencies apply a Tc floor of 5–10 min. Kirpich was calibrated on small rural Tennessee watersheds; check the governing manual's preferred Tc method for paved sites.
Source: Rational Method per FHWA HEC-22 (Urban Drainage Design Manual), Ch. 3; Kirpich (1940). C values are generic textbook ranges (e.g. HEC-22 Table 3-1) — use the governing agency's table.