DrainageCalculators

Vegetated Swale Calculator

Calculate vegetated swale hydraulics including normal depth, velocity, and capacity using Manning's equation with variable roughness based on vegetation retardance.

What This Solves

Sizes a grass-lined or vegetated open channel (swale) to convey stormwater at non-erosive velocities using Manning's equation with vegetation-adjusted roughness.

Best Used When

  • You are designing a vegetated stormwater conveyance channel for a parking lot, roadway, or low-impact development site
  • You need to calculate flow depth, velocity, and residence time for a grass swale
  • You want to verify that flow velocities are low enough to prevent erosion and allow pollutant settling

Do NOT Use When

Key Assumptions

  • Flow is uniform and steady along the swale length
  • Vegetation is healthy and maintained at the specified height and density
  • Manning's roughness is based on empirical correlations for grass retardance classes
  • The cross-section (bottom width, side slopes) is constant along the swale
  • Infiltration during flow is not accounted for (conservative for capacity)

Input Quality Notes

Vegetation type and grass height directly affect roughness. Use conservative (higher) roughness values for design, and verify that the selected vegetation can be established and maintained on-site.

Calculate Vegetated Swale Hydraulics

For educational purposes only. Not a substitute for professional engineering judgment.

Input Parameters

Design Requirements

cfs

Peak flow rate the swale must convey

ft

Total length for residence time calculation (optional)

Channel Geometry

Channel slope along flow direction (ft/ft or m/m)

:1

Horizontal to vertical ratio (e.g., 4 means 4:1)

ft

Width of flat bottom (0 for triangular section)

Cross-sectional shape of the swale

Vegetation Properties

Type of grass/vegetation lining the swale

ft/s

Override default velocity limit for erosion control

Vegetated Swale Design Overview

Vegetated swales convey stormwater while providing filtration and infiltration. Design uses Manning's equation with variable roughness coefficients that depend on flow depth, velocity, and grass retardance.

  • Normal Depth - Uniform flow depth for design flow
  • Velocity Check - Must be below permissible velocity for erosion control
  • Froude Number - Flow regime indicator (subcritical preferred)
  • Residence Time - Contact time for water quality treatment

Vegetation Retardance Classes

Vegetation TypeClassHeight Range
Bermuda GrassC6-12 inches
Buffalo GrassC3-6 inches
Kentucky BluegrassC4-10 inches
Tall FescueB8-18 inches
Native Grass MixB12-24 inches
Unmowed/Dense GrassA> 24 inches
Short Mowed GrassD2-4 inches

Source: Chow (1959) Open-Channel Hydraulics, Table 5-6

Manning's n Values by Retardance Class

ClassLow VRMedium VRHigh VRDescription
A0.500.250.150Very high retardance - dense, tall vegetation
B0.350.150.080High retardance - tall grass (18-24 in)
C0.250.100.050Moderate retardance - medium grass (6-12 in)
D0.150.060.035Low retardance - short grass (2-6 in)
E0.080.040.025Very low retardance - very short grass

VR = Velocity x Hydraulic Radius. Source: HEC-22 Table 7-6

Permissible Velocities (ft/s)

Retardance ClassSlope 0-5%Slope 5-10%Slope > 10%
Class A8.07.06.0
Class B7.06.05.0
Class C6.05.04.0
Class D5.04.03.0
Class E4.03.02.5

For erosion-resistant soils. Source: HEC-22 Table 7-5

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Last verified: February 2026