Time of Concentration Calculator (Kirpich Method)
Calculate the Time of Concentration (Tc) for a watershed using the Kirpich Formula. This metric is essential for hydrologic modeling and calculating peak discharge using the Rational Method.
Estimated Time of Concentration (Tc)
Minutes
What is Time of Concentration?
In hydrology, the Time of Concentration (Tc) represents the time required for water to travel from the hydraulically most distant point in a watershed to the point of interest (usually the drainage outlet). Understanding Tc is critical for predicting how a watershed will respond to a rain event.
Understanding the Kirpich Formula
The Kirpich Equation is one of the most widely used empirical formulas for calculating flow time in small, agricultural, or urban watersheds. The formula is expressed as:
Tc = 0.0078 × L0.77 × S-0.385
- Tc: Time of concentration in minutes.
- L: Length of the flow path in feet.
- S: Average slope of the flow path (ft/ft).
Why is Tc Important?
- Rational Method: Tc is directly used to determine the rainfall intensity (I) from Intensity-Duration-Frequency (IDF) curves.
- Flood Risk: Shorter Tc values usually indicate faster runoff and higher peak flow rates, increasing flash flood potential.
- Infrastucture Design: Civil engineers use this data to size culverts, storm drains, and detention ponds appropriately.
Step-by-Step Calculation Example
Assume you have a small drainage area with the following characteristics:
- Flow Length (L): 1,200 feet
- Elevation Drop: 24 feet
- Slope (S): 24 / 1,200 = 0.02 ft/ft (or 2%)
Applying the formula:
1. Tc = 0.0078 × (1200)0.77 × (0.02)-0.385
2. Tc = 0.0078 × 235.15 × 4.50
3. Tc ≈ 8.26 Minutes