A Guide to Parametric & Polar Coordinates
Instead of defining a path with $y$ in terms of $x$, we use a third variable, $t$ (think of it as time). A point's location is given by its coordinates $(x(t), y(t))$. This lets us trace complex paths, like the flight of a projectile or a path that crosses itself.
To see the underlying path, we try to eliminate the parameter $t$.
Even with this new way of defining curves, we can still find slopes and lengths. We just need to adapt our formulas.
The slope $\frac{dy}{dx}$ is found by the ratio of how $y$ changes with respect to $t$ and how $x$ changes with respect to $t$.
To find the length of a path from $t=a$ to $t=b$, we integrate the "speed" along the curve. This comes from a version of the Pythagorean theorem.
Instead of a rectangular grid $(x, y)$, we navigate with a distance from the origin, $r$, and an angle, $\theta$. A point is given by $(r, \theta)$. This is perfect for describing things with circular or rotational symmetry.
These are the formulas you need to translate between Cartesian and Polar coordinates.
$x = r \cos(\theta)$
$y = r \sin(\theta)$
$r^2 = x^2 + y^2 \implies r = \sqrt{x^2 + y^2}$
$\tan(\theta) = \frac{y}{x}$
We can also measure area and length using polar coordinates. The key is to think in terms of wedge-shaped sectors instead of rectangles.
To find the area swept out by a polar curve $r = f(\theta)$ from angle $\alpha$ to $\beta$, we use the following integral.
This is one of the most important formulas to remember for polar coordinates.
This formula looks a bit like the parametric version, but adapted for polar variables $r$ and $\theta$.