Lift generation results from circulation around an object, quantified by the Kutta-Joukowski theorem: L = ρVΓ, where Γ is circulation. The Magnus effect on spinning objects, airfoil lift at angle of attack, and wind turbine forces all rely on circulation. At the trailing edge of an airfoil, the Kutta condition enforces smooth flow separation, creating a bound vortex and a wake vortex that satisfy the theorem. Vortex shedding in cylindrical bodies and bluff bodies creates periodic lift fluctuations.
From your study of rotating flow, you know that circulation Γ is the line integral of velocity around a closed path: Γ = ∮ v · ds. A non-zero circulation means the fluid is, on average, rotating around the object. The Kutta-Joukowski theorem then states a surprising result: for a two-dimensional body in a uniform flow of density ρ and speed V, the lift per unit span is exactly L = ρVΓ. Lift is not fundamentally about pressure difference or Bernoulli — it is about how much net circulation the body induces in the flow. The pressure and velocity explanations are consequences; circulation is the cause.
How does an airfoil generate circulation? A symmetric airfoil at zero angle of attack generates none — flow is symmetric above and below. Tilt the airfoil to an angle of attack, or use a cambered (curved) airfoil, and the geometry forces flow to travel farther over the upper surface. The Kutta condition is the physical constraint that does the work: real viscous flow cannot turn a sharp corner, so it must leave the trailing edge smoothly. This requirement uniquely determines the circulation — there is exactly one value of Γ that places the rear stagnation point at the sharp trailing edge. Nature selects that value automatically. A higher angle of attack requires more circulation to satisfy the Kutta condition, generating more lift, until the flow separates and the airfoil stalls.
Kelvin's circulation theorem says circulation in an inviscid fluid is conserved, so when the airfoil acquires a bound vortex with circulation +Γ, an equal and opposite starting vortex of circulation −Γ is shed into the wake. This is not a mathematical trick — you can see starting vortices in experiments with flapping wings. The bound vortex "lives" on the airfoil; the starting vortex is left behind at takeoff. The Magnus effect is the same physics applied to spinning objects: a rotating cylinder or baseball drags fluid around itself through viscosity, creating net circulation and therefore lift perpendicular to the flow. This is why a topspin tennis ball curves downward and a backspin shot floats.
Vortex shedding is what happens on bluff bodies — cylinders, chimneys, bridge cables — that cannot maintain smooth attached flow. Vortices shed alternately from each side, forming the Kármán vortex street. Each shed vortex briefly deflects lift in one direction before the next vortex appears on the other side, creating periodic oscillating forces at the Strouhal frequency f = St · V/D, where St ≈ 0.2 for cylinders. These periodic forces can drive resonance in structures — the Tacoma Narrows bridge collapsed partly due to aeroelastic coupling with vortex shedding. In design, either the shedding frequency is kept far from structural natural frequencies, or helical strakes are added to cylinders to disrupt coherent shedding.