Stokes’ theorem is the 3D generalization of Green’s circulation form. It states: the circulation of around a closed curve equals the flux of through any oriented surface whose boundary is .

Statement

Let be a piecewise-smooth oriented surface in with piecewise-smooth boundary curve , oriented compatibly with by the right-hand rule (thumb along the surface normal , fingers curl in the direction of ). Let be a vector field on a region containing . Then

A 1D boundary controls a 2D surface in 3D — one dimension is consumed by the curl on the right side. This is the unifying structure of the FTC family.

Special case: planar surface gives Green’s

If is a flat region in the -plane with , then , and Stokes’ reduces to Green’s circulation form. Green’s is the planar case of Stokes’.

Why Stokes’ is true (sketch)

Subdivide into many small patches , each oriented compatibly with . For each patch , the local circulation-density interpretation of curl says

where is a point inside the patch and is the patch normal. Sum over all patches:

The right side is a Riemann sum that converges to as the patches shrink.

The left side: shared edges between adjacent patches cancel pairwise. If patches and share an edge, that edge gets traversed once in and once in . Because both patches are oriented compatibly with , the shared edge is traversed in opposite directions in the two boundaries — so the line-integral contributions cancel. After all internal cancellations, the only edges that survive are the ones not shared with any neighboring patch — and those are exactly the edges that make up the outer boundary . So

Combining the two halves: in the limit. The detailed verification of the “circulation ≈ curl·area” approximation on each patch reduces to Green’s theorem applied locally (in a coordinate chart on the surface).

The cancellation idea is the same telescoping that proves the FTC: pair up adjacent contributions, internal terms cancel, only boundary contributions survive.

Surface-independence

Two different oriented surfaces sharing the same boundary give the same flux of :

Huge in practice: given a complicated surface, swap it for a simpler one with the same boundary. For example, replacing a paraboloid by the flat disk that has the same circular boundary.

Curl-free ⇒ conservative on simply connected regions

If throughout a simply connected region , then for any closed curve , we can find an oriented surface with , and by Stokes’,

Every closed-loop circulation vanishes, so is conservative on .

This finishes the 3D version of the conservative-iff-curl-free criterion. The condition that is simply connected is exactly what lets us fill in any closed loop with an oriented surface lying in .

Curl as local circulation density

Apply Stokes’ to a tiny disk of area centered at a point with normal :

So is the circulation per unit area around an infinitesimal loop with that normal direction. The vector at each point has direction maximizing this density.

This is the precise statement of “curl = local rotation” that’s invoked when introducing curl heuristically.

Worked example: hemisphere

, upper unit hemisphere , , unit circle in -plane counterclockwise viewed from above.

Left side: parameterize by , , . Dot: . .

Right side: . By surface-independence, swap the hemisphere for the flat disk in the -plane: , so . Flux . ✓

Trading complicated surfaces for simple ones

, paraboloid with , oriented upward.

Boundary : the circle in , counterclockwise.

By Stokes’, . Parameterize by . Compute as a line integral; result .

Direct computation of the paraboloid flux would have been substantially nastier. Use Stokes’ to deform the surface to its simplest equivalent.

Connection to FTC family

TheoremBoundaryInterior
FTC
FTLI
Green’s (circ)
Stokes’
Divergence

Stokes’ is one rung on the ladder. Each says “integral of derivative on interior = boundary integral on boundary.”