06·ToolsArcheve AIPNEW · Hydrology

Time of
concentration.

Kirpich and FAA computed side by side from one set of inputs — so you can see the spread before you pick a design value.

Longest hydraulic flow path, outlet to remotest point
Total fall along the path ÷ length
Same C as your Rational Method calculation
Kirpich T꜀
FAA T꜀
Spread
Suggested design value
Branded A4 sheet — inputs, results & section diagram. Drop it straight into your report appendix.
Most municipal criteria impose a minimum T꜀ of 5–10 minutes regardless of computed value — the calculator floors the suggested value at 10 min. Preliminary aid — verify against project criteria.

T꜀ in hand. Take it to the Rational Method calculator — or have us build the full hydrology study, gauge to hydrograph.

Brief us →

The two methods

Kirpich (1940): T꜀ = 0.0195 · L0.77 · S−0.385 (minutes, L in m, S in m/m). Derived from small agricultural watersheds with defined channels; tends to run fast — short T꜀, conservative (higher) intensities. The default for natural and channelised rural catchments, including wadi tributaries.

FAA (1970): T꜀ = 1.8 · (1.1 − C) · Lft0.5 / S%1/3 (the calculator converts units internally). Developed for airfield drainage — essentially sheet flow over uniform surfaces. The standard pick for paved urban sub-catchments, car parks and roofs-to-gutter paths.

Which value to design with

T꜀ sets the storm duration for intensity lookup — in the Gulf that lookup is its own minefield; see rainfall design criteria for Saudi Arabia. Then feed Q = CiA in the Rational Method calculator and capacity-check with Manning's equation.