In fluid dynamics, circulation is the path integral around a closed curve of the fluidvelocity. Circulation is normally denoted Γ. If is the fluid velocity and the closed curve is denoted C:
For a body in an inviscid flow field, lift is equal to the product of the circulation about the body, the air density, and the velocity. Circulation is often used in computational fluid dynamics as an intermediate variable to calculate forces on an airfoil or other body. The circulation around an airfoil can be finite, but the vorticity of the fluid outside of the airfoil can be zero.
In fluiddynamics, vorticity is the curl of the fluid velocity.
For a fluid having locally a "rigid rotation" around an axis (i.e., moving like a rotating cylinder), vorticity is twice the angular velocity of a fluid element.
Since the atmospheric circulation is nearly horizontal, the (3 dimensional) vorticity is nearly vertical, and it is common to talk use the vertical component as the scalar vorticity.