We are now ready for the generalized Green's Theorem, known as Stokes' Theorem. If we have circulation density of in a region and we want the total circulation, we should integrate the density over the region. Thus,
If the following conditions hold:
then we can say that
where is the unit normal vector to S at each point.
Stokes' Theorem simply says that the total circulation of around C is the same as the integral of the maximum circulation density over any surface S with C as its boundary. Thus, we can choose S to simplify the calculations as needed.
It is also worth noting that if we let then Stokes's Theorem directly reduces to Green's Theorem in the plane.