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
| Theorem | Boundary | Interior |
|---|---|---|
| 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.”