5.1 Polar Coordinates and the Jacobian
A double integral is a refined sum over cells. In rectangular coordinates the cells are congruent little squares, each of area , and nobody thinks twice. But regions with a center — disks, rings, anything round — beg to be chopped along rings and rays instead, and then something changes: the cells are not congruent. Every cell in one ring matches its neighbors, but the rings themselves widen as they move outward. The area element must record that widening, and the figure lets you measure it before any formula claims it.
Explore in 3D (opens in a new tab)A flat red disk meshed by a coarse polar grid of 11 rings and 11 wedges, each cell split by a diagonal, whose cells visibly widen toward the rim, beneath a dome-shaped paraboloid carrying the same coarse polar mesh, shaded from blue at its rim to red at its top. A Cartesian wireframe of the same paraboloid, with equal square cells, is hidden in this view; it can be shown by opening the figure in XYZ 3D, where it covers the square from minus 2 to 2 in x and y and dips below the disk to a depth of 4 at the square's corners.
Explore
- Orbit until you look straight down the -axis, so the flat grid reads like a dartboard. Count the cells in the innermost ring and in the outermost. Same count — same size?
- Each cell is approximately a rectangle, one side running radially and one side running along the arc. Moving from center to rim, which side length stays fixed and which one grows?
- Write, before touching anything, a formula for the approximate area of a cell at radius with radial step and angular step .
- Now interrogate the mesh: press Open in XYZ 3D ↗ under the figure, and in the editor's object list retype the flat grid's Resolution field (the first Param Surface row) from
12to24, then64, then128. At every fineness, cells within one ring stay congruent, and cell area keeps growing in proportion to — compare a cell near with one near at each level and watch the ratio stay locked near . The factor of is a property of polar coordinates, not of any particular mesh. - Set the resolution back to
12. Turn on the hidden Cartesian-mesh paraboloid (the Surface row) with its eye toggle (hide the two Param Surface rows for a clean look) and orbit straight down: every Cartesian cell is an identical square, so needs no correction. Explain why summing over the polar cells — with no — would overweight the cells near the center. - Turn the two Param Surface rows back on. The colored dome is the integrand riding the same grid: each cell contributes height times of volume. Set up the volume both ways — the example below finishes the story.
One cell, measured exactly
The cell between radii and , spanning an angle , is a slice of a ring. Its exact area is the difference of two circular sectors:
which is up to a vanishing correction — arc length times radial step , exactly what steps 2 and 3 measured. Refining the mesh turns the sum into the integral . The extra is the local area-scaling of the map — its Jacobian, a name the next section grows into a general tool.
The area-scaling factor of , computed from the map itself rather than read off the ring-slice picture. It is the same the mesh above made you count, and the same that turns into . ( stands for .)
The pivot step of the volume computation, integrated exactly by the computer algebra system: the from the area element rides along, and the inner integral lands on the exact value the worked example reads off as . Multiply by the -integral's and the dome's volume follows.
An original work of XYZ Homework, built around interactive XYZ 3D figures. Aligned to OpenStax Calculus Volume 3 (Strang & Herman), © OpenStax (Rice University), licensed CC BY-NC-SA 4.0; no OpenStax content is reproduced, and this work is not affiliated with or endorsed by OpenStax or Rice University. License: CC-BY-NC-SA-4.0.