WEBVTT

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Let me tell you what
Stokes' theorem actually says.

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It is one sentence.

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Not a page of conditions,
not a machine you turn a handle on.

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One sentence, which then
gets written down three times,

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in three different numbers of dimensions,
and picks up a different name each time.

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Before the sentence,
put its three regions side by side.

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A chunk of the number line, a path through
the plane, and a two dimensional patch.

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These regions have different dimensions,

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but each has an edge
one dimension smaller.

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Start with the chunk of line.

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Its edge is two dots, one at each end.

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Those two endpoints are the complete
boundary of the interval from a to b.

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The path has the same kind of boundary.

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Its edge is the point P
where the journey starts,

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together with the point Q where it stops.

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The patch is different.

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Its edge is not a pair of points.

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It is the closed curve running
all the way around the outside,

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walked in one direction.

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Now look at the pattern.

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The edge of a piece
of line is a couple of points.

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The edge of a path is its two endpoints.

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The edge of a blob is a curve.

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In every case the edge
is one dimension smaller,

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and here is the sentence
all three theorems share:

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add up how fast something
changes inside a region,

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and the answer depends only on its edge.

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And here is that sentence
written in symbols.

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This is Stokes' theorem.

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The whole of it, on one line.

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You are not supposed
to be able to read that yet.

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I only want you to have seen it once.

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Omega is the region,
whatever it happens to be.

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Del Omega is its edge. And the line says:

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what you get by integrating
inside is decided on the edge.

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And you have almost certainly met
that line three times already,

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under three different names.

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The fundamental theorem of calculus.

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The fundamental theorem
for line integrals.

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And Green's theorem.

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So let's take them one at a time.

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One dimension, then a curve

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through the plane, then a flat patch, and
watch the same line come back every time.

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Start in one dimension, where you
have known this theorem the longest.

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Here is the question it actually answers.

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You know how fast something
is changing at every moment:

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you're driving, and you can watch
the speedometer the whole way.

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How far did you go?

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The fundamental theorem of calculus
says this. If you integrate the derivative

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of f from a to b, you don't get anything
complicated. You get f at b, minus f at a.

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Read that out loud in words.

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Add up all the little changes over the
whole interval, and you get the net change

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from one end to the other.

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The speedometer tells you the odometer.

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Let's make that concrete,

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because a number you can check
beats a formula you can only nod at.

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Take f of x equal to x squared over four.

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Its derivative is x over two,
which is this blue line.

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Fix the left end at one, and let
the right endpoint b start at two.

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The left hand side
is the shaded area from one to b.

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Now slide b out to four.

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The region grows with it, and the running
total up in the corner counts all the way

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to three point seven five.

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Now check the other side.

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f of four is four.

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f of one is a quarter.

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Four minus a quarter
is three point seven five.

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Same number, obviously.

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But here is the thing I
really want you to notice.

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The right hand side never
looks inside the interval at all.

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It only asks two questions.

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What is f at the right end,
and what is f at the left end?

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Everything in the middle cancels.

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So here is the piece of language you need.

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The interval from a to b is the region.
Its boundary is just the two endpoints.

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That word, boundary, is the whole lecture.

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The boundary is not the number b minus a.

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It is a formal sum of two points:

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plus b at the right hand end, together
with negative a at the left hand end.

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Those signs are exactly why
the answer is f of b minus f of a.

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That sign is orientation,
the direction in which you travel.

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Watch the traveller move from the negative
endpoint to the positive endpoint.

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Keep that direction in mind.

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It comes straight back in Green's theorem.

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Now go up a dimension.

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Same sentence, new region.

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This time the region is not
a chunk of the number line.

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It is a route, drawn through the plane,
from a point P to a point Q.

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And instead of a function
of one variable, there are now two.

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Picture it as a hill: f of x, y is the
height of the ground above the point x, y.

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These grey rings are its contour lines.

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A contour is the set of places
at one particular height.

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So put a walker on the ring where f
is nine, and send it the whole way round.

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It climbs nothing at all, because every
point of that ring is at the same height.

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Here is theorem one again, so you
can see what is coming. Integrate

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the derivative across the region,
and read the answer off the two ends.

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And here is theorem two. Integrate
the gradient of f along the curve C,

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and what you get is f at Q minus f at P.

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Look at those two lines together.

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It is the same sentence twice.

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Read the left side as, add up every
little bit of climbing as you walk.

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Read the right side as,

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the height where you finished
minus the height where you started.

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It is the odometer story again, on a hill.

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And that hands you
something genuinely useful.

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The route does not matter.

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Take hold of it here, in the middle,

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and bend it wherever you like,
keeping P and Q where they are.

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Up over the shoulder of the hill.

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Or down round the bottom instead.

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The climb you total up
is the same number every single time,

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because the right hand side
never mentions the route at all.

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Because the formula only
ever looks at the endpoints.

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There is that word again.

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The boundary of a curve is its two ends,
and the answer depends on nothing else.

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Which hands you a corollary
that falls straight out.

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Suppose the route is a closed
loop, like this circle Gamma.

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You finish exactly where you started,

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so the start point and the end
point are the same point.

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So the endpoint term is f of P

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minus f of P.

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The two copies cancel,
and the result is zero.

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Around any closed loop,
a gradient field integrates to zero.

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You can see it coming without computing
anything: closed curve, gradient field,

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nothing to do.

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Same theorem. Region, boundary, done.

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Now the one that looks
hardest and really isn't.

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So, the flat case.

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Green's theorem. This is the one that
looks frightening the first time you meet

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it, and it is the same sentence again.

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Our region is now genuinely two
dimensional: a flat patch R in the plane,

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carrying a field of arrows.

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The rectangle keeps the boundary easy
to read, but the theorem does not depend

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on that shape.

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Its boundary is the closed curve
that runs all the way around the outside.

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We write it as del R.

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Orientation matters, exactly as the plus
and minus mattered on the interval.

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Travel counterclockwise,
so the region stays on your left.

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Starting here, one complete trip
comes back to the point it left.

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That choice of direction
is the same choice as the plus sign

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on the interval's right hand end.

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Here is the statement.

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The double integral over every point
of the region lives on the left.

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One line integral around
its boundary lives on the right.

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Inside on the left, edge on the right.

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Read the left side as the total
swirl at all points inside R.

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Read the right side

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as the total push along one
counterclockwise trip around del R.

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Every arrow inside contributes to the
first count; the rim supplies the second.

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Green's theorem says
those two numbers are equal.

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Total swirl inside equals total push
around the rim. That is the whole theorem.

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Now for the reason.

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Chop R into little tiles.

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Each tile contributes
a walk around its own boundary.

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Choose this tile.

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Its contribution
includes this little edge.

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Adding the tiles means reading that edge
once from each tile that touches it.

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One tile walks the shared edge upward.

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Its neighbour walks
the very same edge downward.

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The geometric edge is one object, but
its two induced directions are opposites.

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Those two contributions cancel.

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The same happens at every shared edge, so
the entire interior grid deletes itself.

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Only edges with no neighbour remain:

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the outside of R.

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Their induced walk is the surviving
boundary, with the region on its left.

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That is Green's theorem.

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The equality now reads
from the region to its surviving boundary.

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The derivative is integrated

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over R on the left; the original field
is integrated over del R on the right.

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If a line integral around a closed curve
is horrible, read the equality backward.

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Swap the loop integral to the left
and the double integral to the right.

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Often that reversal is the whole

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difference between an integral
you can do and one you cannot.

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Put the three theorems side by side
with the three regions we started from.

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For each theorem, name its region
and then its complete boundary.

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For the fundamental theorem of calculus,
the region is the interval from a to b.

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Its boundary is the two endpoints a and b.

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For line integrals, the region is the
curve C. Its boundary is the point P

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where the curve starts
and the point Q where it ends.

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For Green's theorem,
the region is the patch R.

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Its boundary is the closed loop del R,
walked with the region on the left.

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Now read the two right hand columns.

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This one names the region
being integrated over.

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This one names its boundary,
always one dimension smaller.

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Every row is saying the same thing.

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And that shared structure
is the line I showed you at the start.

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Here it is again, and this time
it should read as ordinary English.

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Omega names the region,
whatever dimension it has.

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Del Omega names its boundary,
always one dimension smaller.

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The symbol d means take the appropriate
derivative: an ordinary derivative

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on an interval, a gradient along
a curve, or curl over a patch.

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It is the operation

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that turns the original
quantity into the inside quantity.

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The left side integrates
that derivative over the region.

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The right side integrates
the original quantity over the boundary.

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Read at three different dimensions,
this one line is all three theorems.

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And notice what that line does not say.

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It never says how many
dimensions the region has.

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So take one more: a surface in space,
a sheet of it hanging in the air.

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Let me turn it round,

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because a curved sheet and a flat one
look exactly alike until something moves.

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Now you can see it is bowed upward,
like a cloth held up by its four corners.

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Its boundary is the closed curve running
round the rim, walked so that the surface

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stays on your left.

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A region, and an edge
one dimension smaller.

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The same two things
as every other picture today.

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Read that same line over a surface like
this one, and what you get is the theorem

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that actually carries Stokes' name.

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Read it one dimension higher again
and it is the divergence theorem.

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Nobody had to invent a new
idea for either of them.

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So there it is.

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That line is Stokes' theorem.

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Omega is whatever region you have,
del Omega is its edge, and adding

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up the change inside always leaves you
something that was settled on that edge.