Superelevation of the Water Surface in a Channel Bend

Also known as Δd = V² T / (g Rc) · water surface superelevation in a bend · channel bend superelevation · super-elevation of flow around a curve · rise of the water on the outside of a bend · freeboard in a curved ditch · outer bank water level · HEC-22 equation 6.6 · HDS 4 equation 4.33 · centrifugal tilt of the water surface · difference in water surface between inner and outer bank · curved channel water surface rise

Δd=V2 Tg Rc\Delta d = \frac{V^{2}\,T}{g\,R_c}
sig figs

Worked example: HDS 4 Example 4.7 SI: V 3.4 m/s, T = 12 - 8 = 4 m, Rc 10 m → 0.47 m. Press Try an example to run it live, then adjust anything.

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Where Superelevation of the Water Surface in a Channel Bend fits

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See also

Froude Number (Open Channel): The relation holds for subcritical flow, so check the Froude number is below 1 before using it.Manning's Equation for Velocity: Gives the average velocity V that goes in here, from the channel's roughness, hydraulic radius and slope.Specific Energy in an Open Channel: The energy of the flow at a section, for the depth and velocity this page assumes are steady through the bend.Superelevation Rate for a Horizontal Curve: The banking of a road curve, which is a different thing from the tilt of a water surface in a bend.
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Superelevation of the Water Surface in a Channel Bend explained

RcVplansectionΔdTinner bankouter bank

Water forced round a bend does not turn by itself. Its own inertia pushes it toward the outside bank, and the surface tilts across the channel until the slope of the water balances that push. The tilt is the answer here: Δd\Delta d is how much higher the water stands at the outer bank than at the inner bank. The ratio V2/RcV^{2}/R_c measures how sharply the flow has to be turned, dividing by gg turns it into a slope, and multiplying by the surface width TT gives the rise across the whole channel.

Use the radius to the centreline for RcR_c, and give TT and RcR_c in the same length unit. The outer bank sits half of Δd\Delta d above the water level at the centreline and the inner bank half of it below, so a designer adds half the difference to the normal depth to find the depth at the outside of the bend, and sets freeboard and lining height above that. The same effect puts a lining in a bend under more shear than one in a straight reach. Gravity is standard, 9.80665 m/s² (32.174 ft/s²); the manuals round it to 9.81 and 32.2. This is the water surface in a curved channel, not the banking of a road.

The relation is published in the Federal Highway Administration's urban drainage manual (HEC-22, fourth edition, equation 6.6) and in its companion Introduction to Highway Hydraulics (HDS 4, equation 4.33), which writes the surface width as the outer radius less the inner radius. It holds for subcritical flow only, so check that the Froude number is below 1: in supercritical flow a bend raises standing waves and oblique jumps that this relation does not describe. HDS 4 adds that the equation assumes a uniform velocity and uniform curvature, so it gives a value somewhat lower than a natural channel shows, generally within 10 percent, and that for a lined canal with strong curvature and large velocities its more detailed equation 4.34 should be used instead.

HDS 4 works it as Example Problem 4.7. With V=3.4V = 3.4 m/s, an outer radius of 12 m, a centreline radius of 10 m and an inner radius of 8 m, the width is T=12−8=4T = 12 - 8 = 4 m. The page gives 11.56×4/(9.80665×10)=0.4715211.56 \times 4 / (9.80665 \times 10) = 0.47152 m, which agrees with the manual's printed 0.47 m to 0.01 m. In English units, with V=11.15V = 11.15 ft/s, T=13.12T = 13.12 ft and Rc=32.81R_c = 32.81 ft, the manual prints 1.54 ft.

Superelevation of the Water Surface in a Channel Bend formula

Δd=V2 Tg Rc\Delta d = \frac{V^{2}\,T}{g\,R_c}
Where
  • Δd\Delta d= Difference in water surface level between the outer and inner banks (m)
  • VV= Average velocity (m/s)
  • TT= Surface width of the channel (m)
  • RcR_c= Radius to the centreline of the bend (m)
Where this comes from
  • US Department of Transportation, Federal Highway Administration, Urban Drainage Design, Hydraulic Engineering Circular No. 22 (HEC-22), Fourth Edition, publication FHWA-HIF-24-006, February 2024, section 6.1.5 Superelevation in Bends, equation 6.6 (printed pages 64 and 65): the difference in water surface elevation is V^2 T / (g Rc), valid for subcritical flow, with the outer bank at half of it above and the inner bank half below the centreline level. US federal work, public domain. Read it
  • US Department of Transportation, Federal Highway Administration, Introduction to Highway Hydraulics, Hydraulic Design Series No. 4 (HDS 4), Fourth Edition, publication FHWA-NHI-08-090, June 2008, section 4.6.5 Subcritical Flow in Bends, equation 4.33 (printed page 4-35) and Example Problem 4.7 in SI and English units (pages 4-36 to 4-38). US federal work, public domain. Read it
Revised 31 October 2026
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formula.expert. (2026, October 31). Superelevation of the Water Surface in a Channel Bend Calculator. https://formula.expert/solvers/superelevation-of-water-surface-in-channel-bend