Theory 1

Polar coordinates are pairs of numbers which identify points in the plane in terms of distance to origin and angle from -axis:

Converting


Polar coordinates have many redundancies: unlike Cartesian which are unique!

  • For example:
    • And therefore also (negative can happen)
  • For example: for every
  • For example: for any

Polar coordinates cannot be added: they are not vector components!

  • For example
  • Whereas Cartesian coordinates can be added:

The transition formulas require careful choice of .

  • The standard definition of sometimes gives wrong
    • This is because it uses the restricted domain ; the polar interpretation is: only points in Quadrant I and Quadrant IV (SAFE QUADRANTS)
  • Therefore: check signs of and to see which quadrant, maybe need -correction!
    • Quadrant I or IV: polar angle is
    • polar angle is


Equations (as well as points) can also be converted to polar.

For , look for cancellation from .

For , try to keep inside of trig functions.

  • For example:

Theory 2

To draw the polar graph of some function, it can help to first draw the Cartesian graph of the function. (In other words, set and , and draw the usual graph.) By tracing through the points on the Cartesian graph, one can visualize the trajectory of the polar graph.

This Cartesian graph may be called a graphing tool for the polar graph.


A limaçon is the polar graph of .

Any limaçon shape can be obtained by adjusting in this function (and rescaling):

Limaçon satisfying : unit circle.

Limaçon satisfying : ‘outer loop’ circle with ‘dimple’:

Limaçon satisfying : ‘cardioid’ ‘outer loop’ circle with ‘dimple’ that creates a cusp:

Limaçon satisfying : ‘dimple’ pushes past cusp to create ‘inner loop’:

Limaçon satisfying : ‘inner loop’ only, no outer loop exists:

Limaçon satisfying : ‘inner loop’ and ‘outer loop’ and rotated :


Transitions between limaçon types, :

Notice the transition points at and :

The flat spot occurs when

  • Smaller gives convex shape

The cusp occurs when

  • Smaller gives dimple (assuming )
  • Larger gives inner loop

Theory 3

Roses are polar graphs of this form:

The pattern of petals:

  • (even): obtain petals
    • These petals traversed once
  • (odd): obtain petals
    • These petals traversed twice
  • Either way: total-petal-traversals: always