Thin-aerofoil theory & the lift curve
Why is the lift curve a straight line, and why is its slope almost always close to per radian? Thin-aerofoil theory answers both with a beautiful piece of classical mathematics. This is the most maths-heavy article — take it slowly.
The idea: replace the wing with a sheet of vorticity
A thin, slightly cambered section barely disturbs the flow, so we model it as its camber line alone, replaced by a continuous sheet of tiny vortices of strength per unit length. We then demand the one physical condition: the flow must be tangent to the camber line everywhere (nothing flows through the wing). That single requirement determines , and from it the circulation and lift.
A clever change of variable
Map the chord onto an angle :
The leading edge is , the trailing edge . The vortex strength is written as a Fourier series tailored to satisfy the flow-tangency (and Kutta) conditions:
The leading term carries the singular behaviour at the nose; the sine series vanishes at the trailing edge, automatically enforcing the Kutta condition. Imposing flow tangency fixes every coefficient as an integral of the camber-line slope :
- angle of attack [rad]
- local slope of the camber line [—]
The payoff: lift
Total circulation is the integral of the sheet, . Carrying it through and using Kutta–Joukowski, only the first two coefficients survive in the lift:
Collect the camber integral into a single constant, the zero-lift angle, to get the standard linear form:
The moment and the aerodynamic centre
The same analysis gives the pitching moment about the quarter-chord:
Notice it contains no . The moment about the quarter-chord is independent of angle of attack: the quarter-chord is the aerodynamic centre, the natural pivot about which lift changes produce no extra twisting. For a symmetric section , so the moment is zero.
How reality bends the line
Thin-aerofoil theory is inviscid and assumes a thin section, so two corrections appear in practice:
- Thickness nudges the inviscid slope slightly above . A common estimate is , giving /rad for a 12% section — which is what our panel solver reports.
- Viscosity pulls the real slope back below (typically /deg /rad) and, above , causes the flow to separate and the lift to collapse — stall. Our inviscid model cannot capture this, so its line rises forever.