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Calculus IIIUniversity

Double Integrals in Polar Coordinates

A rigorous, example-driven guide to double integrals in polar coordinates, including hypotheses, method choice, verification, and practice.

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The central idea

Under $x=r\cos\theta$, $y=r\sin\theta$ with $r\ge0$, area transforms as $dA=r\,dr\,d\theta$. Thus $\iint_Df(x,y)dA=\iint_{D^*}f(r\cos\theta,r\sin\theta)r\,dr\,d\theta$. The extra $r$ is the absolute Jacobian determinant and must be included.

Definitions, hypotheses, and notation

Regions offset from the origin can require radial bounds from solving a polar equation, such as $r=2\cos\theta$ for a shifted circle. Negative radial bounds are usually avoided in change-of-variables integrals by choosing angles and $r\ge0$ that cover the region once. The coordinate map is singular at $r=0$, but that single point has zero area and causes no problem for ordinary integrable functions.

Order $drd\theta$ describes rays; order $d\theta dr$ describes arcs at fixed radius and may require splitting a region differently. Choose bounds from geometry rather than copying a standard disk pattern.

Conceptual meaning

A small polar cell is approximately a sector rectangle with radial thickness $dr$ and arc length $r d\theta$, so its area is $rdrd\theta$. Polar coordinates fit disks, annuli, sectors, and radial integrands naturally.

A dependable method and decision rule

  1. Sketch the planar region and choose an angular interval without repeated coverage.
  2. Write radial bounds along each ray.
  3. Convert every occurrence of $x,y$, especially $x^2+y^2$.
  4. Multiply the transformed integrand by the Jacobian factor $r$.
  5. Integrate and compare with area or symmetry estimates.

Fully worked example

Common mistakes and why they fail

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