Circulation and lift

The wind a swept wing feels

Sweeping a wing back is usually justified by saying it meets a slower wind. It does not meet a slower wind. The equations split exactly in two, and the flow along the span is a passenger that exerts no force and changes nothing — until a pressure gradient breaks the split, and then it becomes the reason a swept wing is a different problem rather than a harder one.

Worth reading first: Everything happens in a layer you cannot see · The pocket on top of the wing.

Every large aeroplane built since about 1950 has its wings swept back, and the reason given is almost always the same sentence: the swept wing meets a slower wind, so it can fly faster before the air over it goes supersonic.

The conclusion is right and the sentence is not. A wing does not meet a slower wind. It meets exactly the wind it would meet unswept, and the reason it behaves as though the wind were slower is a theorem — one of the very few exact decompositions in this subject, and considerably stronger than the hand-waving version that stands in for it.

The split

Take a wing of infinite span, yawed at an angle Λ to a steady stream, in an incompressible laminar flow. Resolve the free stream into two components: one in the plane normal to the leading edge, of size U cos Λ, and one along the span, of size U sin Λ.

Write out the Navier–Stokes equations in wing-fixed axes and something remarkable happens. The two equations governing the flow in the normal plane contain no spanwise velocity at all. They are the ordinary two-dimensional equations, driven by U cos Λ, and they can be solved with no knowledge of the sweep whatever.

The spanwise equation is then

uwx+vwy=ν2wy2,u\frac{\partial w}{\partial x} + v\frac{\partial w}{\partial y} = \nu\frac{\partial^2 w}{\partial y^2},

with w the spanwise velocity and u, v the normal-plane flow the first calculation produced. There is no pressure gradient in it — the wing is infinite, so nothing varies along the span. The spanwise velocity is a passive scalar: it is advected by a flow it does not influence, diffuses, and exerts no force on anything.

That is the independence principle, and it is exact. Not asymptotic, not a small-angle approximation: an exact statement about an infinite yawed wing in a laminar incompressible flow.

Checking it where it cannot hide

An assertion this strong deserves a test that could fail, and there is one available.

On a flat plate with no pressure gradient, the normal-plane flow is Blasius’s, which this site already solves by shooting the nonlinear third-order equation. Substituting the similarity variable into the spanwise equation gives

g+12fg=0,g(0)=0, g()=1,g'' + \tfrac{1}{2} f g' = 0, \qquad g(0) = 0,\ g(\infty) = 1,

a linear second-order equation with no eigenvalue in it — which is itself the computational shadow of the flow being passive: nothing has to be shot for, the equation is integrated once from an arbitrary wall slope and scaled to meet the outer condition.

Divide through: g/g=12fg'' / g' = -\tfrac12 f, so gexp(12 ⁣ ⁣f)g' \propto \exp(-\tfrac12\!\int\! f). The Blasius equation says the same thing about ff''. So gfg' \propto f'', and integrating with both boundary conditions gives g=fg = f' exactly.

The two profiles are not similar. They are the same function.

Two profiles, and they are the same profile. The chordwise and spanwise velocity profiles in the boundary layer of a yawed flat plate, each as a fraction of its own edge velocity. They are computed by different code — the chordwise one by shooting a third-order nonlinear equation, the spanwise one by a single pass through a linear second-order one — and they agree to 2.1e-8 over the whole layer. They are the same function of η, because the two equations reduce to the same equation. A swept flat plate has no crossflow at any sweep angle, and that is the independence principle in the only form that has no wriggle room in it.
Fig. 1 The chordwise and spanwise profiles on a yawed flat plate, each as a fraction of its own edge velocity, computed by code that shares nothing below the arithmetic. They agree to two parts in a hundred million over the whole layer, and a swept flat plate therefore has no crossflow at any sweep angle at all.

The solver integrates the spanwise equation independently and requires the two curves to agree to five parts in ten thousand; they agree to two parts in a hundred million. And it then asks the consequence: a swept flat plate must have no crossflow at any sweep, which is required at four angles and comes out below 10⁻³ at every one.

That is the independence principle in the form that has no wriggle room in it. A boundary layer on a yawed plate at sixty degrees of sweep is the boundary layer on an unswept plate, with a spanwise flow superimposed that the layer does not feel.

What the split buys

Once the normal-plane problem is the whole of the section’s problem, two design numbers fall out by division.

Sweep buys Mach by 1.221 and sells lift by 0.671. What simple sweep theory promises and what it charges, against sweep angle, for a section whose own critical Mach number is 0.72. The critical Mach number of the wing rises as 1/cos Λ, because the normal-plane flow is the only flow the section has; the lift-curve slope falls as cos²Λ, because the dynamic pressure in that plane falls by cos²Λ and the streamwise chord grows. At 35 degrees the wing can fly at Mach 0.879 and has thrown away 33 per cent of its lift slope. Every high-lift device on a swept wing is buying that back.
Fig. 2 What sweep promises and what it charges. The critical Mach number rises as 1/cos Λ because the normal-plane flow is the only flow the section has; the lift-curve slope falls as cos²Λ. At thirty-five degrees the wing flies at Mach 0.88 and has thrown away a third of its lift slope.

The critical Mach number rises as 1/cos Λ. The pocket of supersonic flow on top of a wing forms when the local Mach number reaches one, and the local Mach number is a property of the normal-plane flow — so it is McosΛM\cos\Lambda that has to stay below the section’s own critical value. A section good to Mach 0.72 unswept is good to 0.88 at thirty-five degrees of sweep, and a designer wanting Mach 0.85 out of that section needs 32.1 degrees.

The lift-curve slope falls as cos²Λ. The dynamic pressure in the normal plane is qcos2Λq\cos^2\Lambda, and the chord measured streamwise is longer by 1/cosΛ1/\cos\Lambda, so the lift coefficient referred to the streamwise chord carries two factors of the cosine. At thirty-five degrees the wing has 67 per cent of the lift slope it had, which is a very large amount to give away.

That is where every high-lift device on a swept wing comes from. The slats, the triple-slotted flaps, the enormous wing area of a swept-wing airliner relative to its weight: all of it is buying back the lift slope that the sweep spent. A swept wing is a machine for converting low-speed performance into high-speed performance, and the exchange rate is the cosine.

Where the split breaks

Put a pressure gradient on the normal-plane flow and the coincidence ends.

The chordwise profile now solves Falkner–Skan, which has an extra term m(1f2)m(1 - f'^2) in it. The spanwise profile still solves the passive equation, which does not. The two are no longer the same function, and the resultant velocity in the layer therefore points a different way at every height.

A pressure gradient separates them, and the gap is the crossflow. The same two profiles with a favourable pressure gradient on the chordwise flow, at β = 0.5. The chordwise profile is fuller — the gradient accelerates it and the spanwise equation has no gradient term in it at all — so the two curves come apart, and the resultant velocity points a different way at every height. The difference, resolved perpendicular to the edge velocity, is the crossflow, drawn here at half scale; it peaks at -0.1083 of the free stream at η = 1.07. Nothing like it exists on the plate.
Fig. 3 The same two profiles with a favourable gradient on the chordwise flow. The chordwise profile is fuller — it has been accelerated and the spanwise equation has no gradient term to accelerate it — so the curves come apart, and the difference resolved perpendicular to the edge velocity is the crossflow.

That difference is the crossflow, and it is the thing a swept wing has that an unswept one cannot. It is easiest to see as a curve rather than as two profiles.

The velocity turns as well as slowing, and the bow is the crossflow. The velocity in the layer plotted as a curve rather than as two profiles: chordwise component along, spanwise component up, one point per height. A layer with no crossflow would be a straight line from the wall to the edge, because every height would point the same way and only the magnitude would change. This one bows away from that line, and the widest part of the bow is the crossflow. The straight line drawn behind it is the flat-plate case, where the independence principle holds exactly and the trace really is straight.
Fig. 4 The velocity in the layer plotted as a trace: chordwise along, spanwise up, one point per height. With no crossflow the trace would be a straight line from the wall to the edge — every height pointing the same way. This one bows, and the widest part of the bow is the crossflow.

The crossflow profile has a property that decides everything downstream of it: it is zero at the wall and zero at the edge, so it has a maximum in between and therefore an inflection point. And an inflected profile is inviscidly unstable — Rayleigh’s criterion, which this site owns and which says that a velocity profile with an inflection has a growing mode without needing viscosity to supply one.

So a swept wing’s boundary layer carries, everywhere it has a pressure gradient, a small velocity profile that is unstable for the strongest reason a profile can be. That is crossflow instability, and it is why a swept wing transitions far earlier than an unswept one at the same Reynolds number, and why laminar flow on a swept wing is an enormously harder engineering problem than laminar flow on a straight one.

A pressure gradient separates them, and the gap is the crossflow. The same two profiles with a favourable pressure gradient on the chordwise flow, at β = 0.2. The chordwise profile is fuller — the gradient accelerates it and the spanwise equation has no gradient term in it at all — so the two curves come apart, and the resultant velocity points a different way at every height. The difference, resolved perpendicular to the edge velocity, is the crossflow, drawn here at half scale; it peaks at -0.0947 of the free stream at η = 1.37. Nothing like it exists on the plate.
Fig. 5 The same separation of the two profiles under a weaker gradient at a larger sweep. The crossflow is smaller because the chordwise profile has been filled out less, and it peaks lower in the layer because the layer itself is thicker. The gradient sets the size of the effect; the sweep sets how much of it appears as crossflow.

The angle where it is worst

The crossflow vanishes at both ends and peaks at forty-five degrees. The largest crossflow in the layer against sweep angle, for three pressure gradients. Every curve is zero at both ends and every one peaks at exactly forty-five degrees, because the crossflow carries the product of the two edge components and that product is cos Λ sin Λ. At no sweep there is no spanwise flow for the gradient to act on; at ninety degrees there is no chordwise flow to act with. The gradient sets the height of the curve and not the position of its maximum, which is a geometric fact about the resolution of a velocity and not about boundary layers at all.
Fig. 6 The largest crossflow in the layer against sweep angle, for three pressure gradients. Every curve vanishes at both ends and peaks at exactly forty-five degrees, because the crossflow carries the product cos Λ sin Λ. The gradient sets the height and not the position of the maximum.

The crossflow needs a sweep and a gradient, and it vanishes at both ends of the sweep range: at no sweep there is no spanwise flow for the gradient to act on, at ninety degrees there is no chordwise flow to act with. So the maximum is interior, and it is at exactly forty-five degrees — the product cosΛsinΛ\cos\Lambda\sin\Lambda, and the solver requires it at that angle rather than near it.

That is a geometric fact about resolving a velocity, not a fact about boundary layers, and it is useful precisely because it is so blunt: an airliner wing at thirty-five degrees is close to the worst possible place to be for this particular mechanism, and it is there because the compressibility benefit is worth more than the transition penalty costs.

The attachment line, which the principle makes into a problem

There is one place on a swept wing where the independence principle stops being a convenience and becomes a hazard, and it follows directly from the passivity of the spanwise flow.

On an unswept wing the leading edge is a stagnation point in every section, and each section’s boundary layer starts there from nothing. On a swept wing the leading edge is an attachment line, and the spanwise flow runs along it. There is nowhere for that flow to start from: it arrives from further inboard, carrying whatever boundary layer it has already grown.

So a swept wing has a boundary layer that runs the length of its own leading edge, thickening as it goes, with its own Reynolds number based on the spanwise velocity and the leading-edge scale. Above a critical value that layer becomes turbulent on its own account, and everything downstream of it is turbulent too — the wing has lost its laminar flow before any section’s own transition has been considered.

Worse, it can be contaminated. If turbulence arrives at the wing root — from the fuselage boundary layer, or from a bracket, or from an insect — it travels outboard along the attachment line and turns the whole leading edge turbulent, at a Reynolds number well below the one at which the line would have gone turbulent by itself. That is attachment-line contamination, it was found in flight rather than in a wind tunnel, and the standard remedy is a small bump near the root — a Gaster bump — that forces a fresh stagnation point and cuts the line.

A mechanism that exists only because the spanwise flow is there, on a wing whose whole justification is that the spanwise flow does not matter. The principle is exact and it is exact about a section; the attachment line is not a section.

The S the outer flow makes, and the reversal it causes

The similarity solutions above are shapes at a station. They cannot show the thing a swept wing’s layer is most famous for, which is that the crossflow reverses direction along the chord — and the reason for that is in the inviscid flow, with no boundary layer needed at all.

The flow outside the layer turns one way and then back. The direction of the edge velocity over the upper surface of a swept section, measured from the chordwise direction. The spanwise component is constant — that is the independence principle again — while the chordwise component runs up to the suction peak and back down, so the edge streamline swings forward through 24.8 degrees and then back through 7.8. A straight-winged section has none of this: its edge flow points the same way everywhere. The boundary layer underneath cannot follow a curving streamline without being pushed to the outside of the bend, and it is pushed one way before the peak and the other way after it.
Fig. 7 The direction of the edge velocity over a swept section, measured from the chordwise direction. The spanwise component is constant — the independence principle again — while the chordwise component runs up to the suction peak and back down, so the streamline swings forward through twenty-five degrees and back through eight. A straight wing’s edge flow points the same way everywhere.

The spanwise component of the edge velocity is constant along the chord, because the wing is infinite and nothing varies along the span. The chordwise component is zero at the attachment line, rises to a maximum at the suction peak, and falls again. So the edge streamline starts out running almost along the leading edge, swings forward towards the chordwise direction as the flow accelerates, and swings back as it decelerates.

The outer streamline is an S, and it is exact — that figure is computed from the section’s own inviscid pressure distribution, with no layer anywhere in it.

Now put a boundary layer under it. A curving streamline is a balance between a pressure gradient normal to itself and the centrifugal force of the fluid going round the bend. The fluid near the wall is slower, so its centrifugal force is smaller, and the same normal pressure gradient pushes it to the inside of the bend. Ahead of the suction peak the bend goes one way and behind it the other, so the near-wall flow is pushed outboard first and inboard afterwards.

That reversal is the real crossflow pattern on a wing, and it is why the two most dangerous places on a swept wing’s surface are the attachment line and the pressure recovery — different mechanisms, different remedies, and both invisible to a similarity solution that has one fixed pressure gradient.

Two instabilities pulling opposite ways

The crossflow is not the only way a layer goes turbulent, and the relation between the two ways is what makes laminar flow on a swept wing so much harder than on a straight one.

An unswept wing transitions through Tollmien–Schlichting waves, which grow in the chordwise profile and are suppressed by a favourable pressure gradient: accelerating the flow fills the profile out, removes any inflection, and keeps the waves damped. That is the whole of natural laminar flow design — put the maximum thickness well aft, hold the flow accelerating over the front half, and the layer stays laminar because it has no unstable mode.

Now read the crossflow figures above with that in mind. The crossflow’s size is set by the chordwise pressure gradient, and it grows with it. The same acceleration that quietens the first mechanism feeds the second.

So on a swept wing the two are in opposition. A strongly favourable gradient gives a quiet chordwise profile and a violent crossflow; a flat one gives a small crossflow and a chordwise profile with nothing holding it. The design is a compromise between two instabilities rather than a defence against one, and the compromise narrows as the sweep rises — past twenty-odd degrees there is no gradient that keeps both subcritical, which is why laminar flow beyond that sweep needs the layer removed by suction rather than merely shaped.

What sweep does to the rest of the wing

Three consequences that follow from the same split and that a design has to answer:

The spanwise flow accumulates. On a real wing the layer thickens as it drifts outboard, so the tip region is running a thicker layer than a strip theory would predict, and it separates earlier. That is the origin of tip stall on a swept wing, and it is worse than the taper effect this site treats separately, because it adds to it.

Sweep and taper stall the same part of the wing. Both push the trouble outboard, and outboard is where the ailerons are. Fences, notches, vortilons and sawtooth leading edges are all attempts to stop the spanwise drift, and every one of them is a device for interrupting a flow the independence principle says should not matter — which it does not, until the wing is finite.

And the root and the tip are not swept. The independence principle is about an infinite wing. At the root the fuselage forces the flow to be symmetric and the isobars unsweep themselves; at the tip the flow can escape round the end. Both regions lose the compressibility benefit, and the fix is to give them extra sweep, extra area or a different section — which is why a swept wing’s isobars, plotted, are a design objective rather than a consequence.

Where the flow over the section first reaches Mach one. Two curves running towards each other. The falling one is the section's peak suction, solved exactly in incompressible flow and then deepened by the Prandtl–Glauert factor as the free-stream Mach number rises. The rising one is the pressure coefficient at which the local flow would be exactly sonic. Where they cross is the critical Mach number, and above it there is a pocket of supersonic flow on a subsonic aeroplane.
Fig. 8 What the sweep is for. A section reaches its critical Mach number when the flow somewhere on it first goes sonic, and past that a shock forms and the drag rises steeply. Sweep changes the Mach number at which the section reaches that condition by dividing the flight Mach number by the cosine — and by nothing else, because the normal-plane flow is the only flow the section has.

What the model does not contain

Infinite span. Every exact statement above assumes it. A real wing is finite, has a root and a tip, and has a spanwise pressure gradient that the independence principle explicitly excludes.

Laminar and incompressible. The split is exact for a laminar incompressible flow. In a turbulent layer it is approximately true and the approximation is not sharp; in a compressible flow the energy equation couples the two directions through the temperature, and the split is again approximate.

No transition prediction. The crossflow Reynolds number is computed here and calibrated nowhere. The value at which a swept wing actually goes turbulent is somebody else’s measurement, and quoting one would be putting a number on a mechanism nothing here models.

Simple sweep theory is simple. The 1/cos Λ on the critical Mach number treats the section’s critical value as unchanged, which it is not: the streamwise thickness ratio changes with sweep, and a real wing is designed with the two effects together.

And the crossflow profiles here are similarity solutions, so each is a shape at one fixed pressure gradient. The reversal along the chord is argued from the inviscid streamline and is not computed as a marching boundary-layer solution, which is a different and much larger piece of machinery.

Who found it, and when

The independence principle is Prandtl’s, from around 1945, and Rudolf Sears and Wilhelm Jones each published careful statements of it shortly afterwards. Adolf Busemann had proposed sweep for supersonic aircraft at the Volta conference in 1935; Albert Betz worked out the subsonic argument in 1939 and it became a German wartime research programme.

What is striking is how completely the idea was missed elsewhere. The Volta paper was published, openly, and nobody outside Germany acted on it for nearly a decade — the swept wing arrived in Britain and America in 1945 with the captured research, and every jet airliner since is descended from it. It is one of the clearest cases in this subject of an idea sitting in print for ten years while the people who needed it did not read it.

The crossflow instability came later and from measurement: Gray at Farnborough in 1952 found transition on swept wings occurring far earlier than any two-dimensional criterion allowed, and Owen and Randall identified the inflected crossflow profile as the cause the following year. The theorem that makes a swept wing possible and the instability that makes it difficult were found eight years apart, and the second one was found by somebody noticing that an aeroplane did not behave like the theory.

Where the ladder goes next

The independence principle is about an infinite wing; every difficulty above came from the wing being finite. The next question is what a finite wing’s span does to the lift it carries at each station, and which station runs out first — which is the question a taper ratio and a twist distribution exist to answer.

What links here

Computed from the collection rather than written here: the essays that point at this one.

Reads more easily once this is understood

Essays that name this one as worth reading first.

Shares its objects with

Essays naming at least two of the same things, that neither author linked.

Named objects

A dashed tag is an object no other essay names yet.

BlasiusBoundary layerCritical machCrossflowFalkner–SkanIndependence principleLift coefficientModel limitPressure gradientSimilarity solutionSweepTransition