AP Calculus BC Unit 9 Notes: Learning Parametric Curves from First Principles

Defining and Differentiating Parametric Equations

What a parametric equation is (and why you’d use one)

A parametric curve describes a path in the plane by giving both coordinates as functions of a third variable called a parameter (usually tt). Instead of defining yy directly as a function of xx (like y=f(x)y = f(x)), you define

x=x(t)x = x(t)

y=y(t)y = y(t)

As tt changes, the point (x(t),y(t))\big(x(t), y(t)\big) moves—so you can think of the curve as a “motion picture” of a point traveling through the plane.

This matters because many curves are awkward or impossible to describe cleanly as yy in terms of xx. Parametric equations let you:

  • Model motion naturally (position depends on time).
  • Describe curves that fail the vertical line test (loops, sideways curves).
  • Keep track of direction and time along the curve, not just the shape.

A key mindset shift: with parametrics, tt is not just a trick; it carries information about where you are on the curve and how fast you’re moving.

Interpreting the curve: shape, direction, and time

When you graph a parametric curve, you are really graphing the set of points

{(x(t),y(t)):t in some interval}\{(x(t), y(t)) : t \text{ in some interval}\}

Two important interpretive ideas:

  1. Direction (orientation): As tt increases, the point traces the curve in a specific direction. Two different parameterizations can trace the same geometric curve but in opposite directions.

  2. Speed along the curve: If tt is time, then dxdt\frac{dx}{dt} and dydt\frac{dy}{dt} describe how the coordinates change per unit time. Even if the curve’s shape is the same, different parameterizations can move along it at different speeds.

Eliminating the parameter (when you can, and what you lose)

Sometimes you can rewrite the parametric equations to remove tt and get a relationship between xx and yy.

Example idea (not a full worked problem yet): if x=costx = \cos t and y=sinty = \sin t, then eliminating tt gives x2+y2=1x^2 + y^2 = 1.

This is useful for recognizing the shape. But you lose information about:

  • which point corresponds to a specific tt,
  • the direction of travel,
  • how quickly the point moves.

So on AP questions, eliminating tt can help identify a curve, but you often still need derivatives with respect to tt to answer calculus questions.


Differentiating parametric equations: finding dydx\frac{dy}{dx}

To find slope on a parametric curve, you want dydx\frac{dy}{dx}. But you are not given yy as a function of xx; you are given both as functions of tt. The key idea is the Chain Rule:

If y=y(t)y = y(t) and x=x(t)x = x(t), then

dydx=dydtdxdt\frac{dy}{dx} = \frac{\frac{dy}{dt}}{\frac{dx}{dt}}

as long as dxdt0\frac{dx}{dt} \ne 0.

Why this formula makes sense

Over a tiny change Δt\Delta t, you get approximate changes

ΔydydtΔt\Delta y \approx \frac{dy}{dt}\Delta t

ΔxdxdtΔt\Delta x \approx \frac{dx}{dt}\Delta t

So the slope ΔyΔx\frac{\Delta y}{\Delta x} becomes approximately

dydtΔtdxdtΔt=dydtdxdt\frac{\frac{dy}{dt}\Delta t}{\frac{dx}{dt}\Delta t} = \frac{\frac{dy}{dt}}{\frac{dx}{dt}}

The Δt\Delta t cancels, which is exactly the intuition: slope depends on the _relative_ rates of change of yy and xx.

Tangent lines and normals

Once you compute dydx\frac{dy}{dx} at a specific parameter value t=at = a, you can write the tangent line in point-slope form:

  • Point on curve: (x(a),y(a))\big(x(a), y(a)\big)
  • Slope: m=dydxt=am = \left.\frac{dy}{dx}\right|_{t=a}

Equation:

yy(a)=m(xx(a))y - y(a) = m\big(x - x(a)\big)

A normal line is perpendicular to the tangent line, so its slope is

mnormal=1mm_{\text{normal}} = -\frac{1}{m}

provided m0m \ne 0.

Horizontal and vertical tangents (common AP targets)

Because dydx=(dy/dt)(dx/dt)\frac{dy}{dx} = \frac{(dy/dt)}{(dx/dt)}:

  • Horizontal tangent: dydx=0\frac{dy}{dx} = 0 happens when

dydt=0\frac{dy}{dt} = 0

and dxdt0\frac{dx}{dt} \ne 0.

  • Vertical tangent: slope is undefined when

dxdt=0\frac{dx}{dt} = 0

and dydt0\frac{dy}{dt} \ne 0.

A subtle but important caution: if both dxdt=0\frac{dx}{dt} = 0 and dydt=0\frac{dy}{dt} = 0, then the point may be a cusp, corner, or a moment where the motion “stops”—and you cannot conclude “vertical tangent” from dxdt=0\frac{dx}{dt} = 0 unless you also check dydt\frac{dy}{dt}.


Worked Example 1: slope and tangent line

Let

x=t21x = t^2 - 1

y=t3+ty = t^3 + t

Find dydx\frac{dy}{dx} and the tangent line at t=1t = 1.

Step 1: Differentiate each with respect to tt.

dxdt=2t\frac{dx}{dt} = 2t

dydt=3t2+1\frac{dy}{dt} = 3t^2 + 1

Step 2: Use the parametric derivative formula.

dydx=3t2+12t\frac{dy}{dx} = \frac{3t^2 + 1}{2t}

Step 3: Evaluate at t=1t = 1.

Point:

x(1)=121=0x(1) = 1^2 - 1 = 0

y(1)=13+1=2y(1) = 1^3 + 1 = 2

Slope:

dydxt=1=3(1)2+12(1)=42=2\left.\frac{dy}{dx}\right|_{t=1} = \frac{3(1)^2 + 1}{2(1)} = \frac{4}{2} = 2

Step 4: Write the tangent line.

y2=2(x0)y - 2 = 2(x - 0)

So

y=2x+2y = 2x + 2


Worked Example 2: horizontal and vertical tangents

Let

x=t2+tx = t^2 + t

y=t33ty = t^3 - 3t

Find parameter values where the curve has horizontal or vertical tangents.

Step 1: Compute derivatives.

dxdt=2t+1\frac{dx}{dt} = 2t + 1

dydt=3t23=3(t21)\frac{dy}{dt} = 3t^2 - 3 = 3(t^2 - 1)

Horizontal tangents: set dydt=0\frac{dy}{dt} = 0 and require dxdt0\frac{dx}{dt} \ne 0.

3(t21)=03(t^2 - 1) = 0

t2=1t^2 = 1

t=1,1t = 1, -1

Check dxdt\frac{dx}{dt}:

dxdt(1)=30\frac{dx}{dt}(1) = 3 \ne 0

dxdt(1)=10\frac{dx}{dt}(-1) = -1 \ne 0

So both t=1t = 1 and t=1t = -1 give horizontal tangents.

Vertical tangents: set dxdt=0\frac{dx}{dt} = 0 and require dydt0\frac{dy}{dt} \ne 0.

2t+1=02t + 1 = 0

t=12t = -\frac{1}{2}

Check dydt\frac{dy}{dt}:

dydt(12)=3(141)=3(34)=940\frac{dy}{dt}\left(-\frac{1}{2}\right) = 3\left(\frac{1}{4} - 1\right) = 3\left(-\frac{3}{4}\right) = -\frac{9}{4} \ne 0

So t=12t = -\frac{1}{2} gives a vertical tangent.


Exam Focus
  • Typical question patterns
    • “Given x(t)x(t) and y(t)y(t), find dydx\frac{dy}{dx} at t=at = a and write the tangent line equation.”
    • “Find all points where the curve has a horizontal/vertical tangent on a given tt-interval.”
    • “Eliminate the parameter to identify the curve, then use calculus in parametric form to answer slope/velocity questions.”
  • Common mistakes
    • Forgetting that dydx\frac{dy}{dx} is a _ratio_ and writing dydx=dydt\frac{dy}{dx} = \frac{dy}{dt}.
    • Declaring “vertical tangent” when dxdt=0\frac{dx}{dt} = 0 without checking dydt0\frac{dy}{dt} \ne 0.
    • Plugging in tt too early (before simplifying) and missing cancellations or sign errors.

Second Derivatives of Parametric Equations

What the second derivative means in parametric form

The second derivative d2ydx2\frac{d^2y}{dx^2} measures how the slope dydx\frac{dy}{dx} changes as xx changes. Geometrically, it tells you the curve’s **concavity** (concave up vs concave down) when you view yy as changing with xx.

In parametric problems, you still care about concavity for the same reasons as in regular functions:

  • identifying concavity changes (inflection behavior),
  • understanding curve shape beyond just tangent lines,
  • modeling motion (it also connects to acceleration when combined with vector ideas).

But since yy is not explicitly given as y(x)y(x), you must compute d2ydx2\frac{d^2y}{dx^2} carefully using the chain rule again.

How to compute d2ydx2\frac{d^2y}{dx^2}

Start with

dydx=dydtdxdt\frac{dy}{dx} = \frac{\frac{dy}{dt}}{\frac{dx}{dt}}

This is a function of tt. To find how it changes with xx, you can think in two stages:

  1. Differentiate the slope with respect to tt to get ddt(dydx)\frac{d}{dt}\left(\frac{dy}{dx}\right).
  2. Convert “per unit tt” to “per unit xx” by dividing by dxdt\frac{dx}{dt}.

That gives the parametric second derivative formula:

d2ydx2=ddt(dydx)dxdt\frac{d^2y}{dx^2} = \frac{\frac{d}{dt}\left(\frac{dy}{dx}\right)}{\frac{dx}{dt}}

This formula is easy to misuse if you forget what it’s saying: you’re doing the chain rule with xx as an intermediate variable.

Why dividing by dxdt\frac{dx}{dt} appears again

If dydx\frac{dy}{dx} is a function of tt, then

ddx(dydx)=ddt(dydx)dxdt\frac{d}{dx}\left(\frac{dy}{dx}\right) = \frac{\frac{d}{dt}\left(\frac{dy}{dx}\right)}{\frac{dx}{dt}}

This mirrors the first-derivative logic: “rate of change with respect to xx” equals “rate of change with respect to tt” divided by “rate of change of xx with respect to tt.”

Interpreting concavity and points to be careful about
  • If d2ydx2>0\frac{d^2y}{dx^2} > 0, the curve is concave up at that parameter value.
  • If d2ydx2<0\frac{d^2y}{dx^2} < 0, the curve is concave down.

However, concavity is about how yy bends as xx increases. If the curve doubles back (not one-to-one in xx), concavity descriptions can still be made locally, but you must be careful interpreting “up” and “down” in a global way.

Also, note the second-derivative formula requires dividing by dxdt\frac{dx}{dt}. If dxdt=0\frac{dx}{dt} = 0 at a point (a vertical tangent or cusp possibility), d2ydx2\frac{d^2y}{dx^2} may be undefined there, even if the curve exists.


Worked Example 1: computing d2ydx2\frac{d^2y}{dx^2} and concavity

Let

x=t2+1x = t^2 + 1

y=t33ty = t^3 - 3t

Find d2ydx2\frac{d^2y}{dx^2} and determine concavity at t=1t = 1.

Step 1: First derivatives with respect to tt.

dxdt=2t\frac{dx}{dt} = 2t

dydt=3t23\frac{dy}{dt} = 3t^2 - 3

Step 2: Compute dydx\frac{dy}{dx}.

dydx=3t232t\frac{dy}{dx} = \frac{3t^2 - 3}{2t}

You can simplify to reduce algebra errors:

dydx=3(t21)2t\frac{dy}{dx} = \frac{3(t^2 - 1)}{2t}

Step 3: Differentiate dydx\frac{dy}{dx} with respect to tt.

Using quotient rule on 3t232t\frac{3t^2 - 3}{2t} is straightforward:

Let u=3t23u = 3t^2 - 3 and v=2tv = 2t.

u=6tu' = 6t

v=2v' = 2

Then

ddt(dydx)=uvuvv2=(6t)(2t)(3t23)(2)(2t)2\frac{d}{dt}\left(\frac{dy}{dx}\right) = \frac{u'v - uv'}{v^2} = \frac{(6t)(2t) - (3t^2 - 3)(2)}{(2t)^2}

Simplify:

ddt(dydx)=12t26t2+64t2=6t2+64t2=3(t2+1)2t2\frac{d}{dt}\left(\frac{dy}{dx}\right) = \frac{12t^2 - 6t^2 + 6}{4t^2} = \frac{6t^2 + 6}{4t^2} = \frac{3(t^2 + 1)}{2t^2}

Step 4: Divide by dxdt\frac{dx}{dt} to get d2ydx2\frac{d^2y}{dx^2}.

d2ydx2=3(t2+1)2t22t=3(t2+1)4t3\frac{d^2y}{dx^2} = \frac{\frac{3(t^2 + 1)}{2t^2}}{2t} = \frac{3(t^2 + 1)}{4t^3}

Step 5: Evaluate at t=1t = 1.

d2ydx2t=1=3(2)4=32\left.\frac{d^2y}{dx^2}\right|_{t=1} = \frac{3(2)}{4} = \frac{3}{2}

Since 32>0\frac{3}{2} > 0, the curve is concave up at t=1t = 1.


Worked Example 2: noticing where the second derivative can fail

Let

x=t3x = t^3

y=t2y = t^2

Compute dydx\frac{dy}{dx} and discuss what happens at t=0t = 0.

Step 1: First derivatives.

dxdt=3t2\frac{dx}{dt} = 3t^2

dydt=2t\frac{dy}{dt} = 2t

Step 2: First derivative dydx\frac{dy}{dx}.

dydx=2t3t2=23t\frac{dy}{dx} = \frac{2t}{3t^2} = \frac{2}{3t}

At t=0t = 0, this is undefined. That doesn’t mean the curve disappears—rather, it signals a vertical tangent or cusp-type behavior. If you eliminate the parameter for insight:

From x=t3x = t^3, you get t=x1/3t = x^{1/3}, so

y=t2=x2/3y = t^2 = x^{2/3}

The graph y=x2/3y = x^{2/3} has a cusp at the origin with a vertical tangent behavior, matching the undefined slope.

This example shows why you must treat points where dxdt=0\frac{dx}{dt} = 0 with extra care—both for dydx\frac{dy}{dx} and for d2ydx2\frac{d^2y}{dx^2}.


Exam Focus
  • Typical question patterns
    • “Given parametric equations, find d2ydx2\frac{d^2y}{dx^2} at t=at = a and determine concavity.”
    • “Find where the curve changes concavity on a parameter interval (often by analyzing the sign of d2ydx2\frac{d^2y}{dx^2}).”
    • “At a time/value where dxdt=0\frac{dx}{dt} = 0, interpret what happens to slope/concavity.”
  • Common mistakes
    • Computing ddt(dydx)\frac{d}{dt}\left(\frac{dy}{dx}\right) and stopping, forgetting to divide by dxdt\frac{dx}{dt}.
    • Plugging into the second-derivative formula at a value where dxdt=0\frac{dx}{dt} = 0 without discussing that d2ydx2\frac{d^2y}{dx^2} may be undefined.
    • Algebra/quotient-rule errors inside ddt(dydx)\frac{d}{dt}\left(\frac{dy}{dx}\right); simplifying dydx\frac{dy}{dx} first often reduces mistakes.

Arc Lengths of Parametric Curves

What arc length is and why parametrics make it natural

Arc length is the distance traveled along a curve between two points. For straight lines, distance is easy. For curves, you approximate by lots of tiny straight segments and take a limit (an integral).

Parametric equations are especially well-suited for arc length because they already describe a moving point. If tt is time, arc length over t[a,b]t \in [a,b] is literally “total distance traveled” during that time interval.

Deriving the arc length formula (from the distance formula)

Over a tiny change dtdt, the point moves from (x(t),y(t))\big(x(t), y(t)\big) to approximately (x(t)+dx,y(t)+dy)\big(x(t)+dx, y(t)+dy\big). The tiny distance traveled is approximately the hypotenuse of a right triangle:

ds(dx)2+(dy)2ds \approx \sqrt{(dx)^2 + (dy)^2}

Divide by dtdt to convert to rates:

dsdt=(dxdt)2+(dydt)2\frac{ds}{dt} = \sqrt{\left(\frac{dx}{dt}\right)^2 + \left(\frac{dy}{dt}\right)^2}

This quantity dsdt\frac{ds}{dt} is the **speed** (magnitude of velocity) if tt represents time.

Integrating speed gives total distance (arc length):

L=ab(dxdt)2+(dydt)2dtL = \int_a^b \sqrt{\left(\frac{dx}{dt}\right)^2 + \left(\frac{dy}{dt}\right)^2}\,dt

When the formula works nicely (and when it doesn’t)

This integral is guaranteed to represent arc length for a smooth curve, but it may not be easy to compute exactly. On AP problems, the functions are often chosen so that the square root simplifies (frequently using a Pythagorean identity or a perfect square).

Be aware of two common “gotchas”:

  • Parameter interval matters. The arc length depends on t[a,b]t \in [a,b]; the same geometric curve traced multiple times would accumulate extra length.
  • Direction does not matter for length. Reversing direction changes signs of derivatives, but the squares make the integrand nonnegative.
Notation connection: arc length and speed

It helps to recognize these equivalent interpretations:

QuantityMeaningFormula
dsdssmall piece of arc lengthds=(dx)2+(dy)2ds = \sqrt{(dx)^2 + (dy)^2}
dsdt\frac{ds}{dt}speed along curvedsdt=(dxdt)2+(dydt)2\frac{ds}{dt} = \sqrt{\left(\frac{dx}{dt}\right)^2 + \left(\frac{dy}{dt}\right)^2}
LLarc length on [a,b][a,b]L=ab(dxdt)2+(dydt)2dtL = \int_a^b \sqrt{\left(\frac{dx}{dt}\right)^2 + \left(\frac{dy}{dt}\right)^2}\,dt

This is a powerful bridge: arc length is a geometry concept, but in parametric form it becomes a motion concept.


Worked Example 1: arc length with simplification

Let

x=3costx = 3\cos t

y=3sinty = 3\sin t

Find the arc length from t=0t = 0 to t=πt = \pi.

Step 1: Compute derivatives.

dxdt=3sint\frac{dx}{dt} = -3\sin t

dydt=3cost\frac{dy}{dt} = 3\cos t

Step 2: Build the integrand.

(dxdt)2+(dydt)2=9sin2t+9cos2t\sqrt{\left(\frac{dx}{dt}\right)^2 + \left(\frac{dy}{dt}\right)^2} = \sqrt{9\sin^2 t + 9\cos^2 t}

Use sin2t+cos2t=1\sin^2 t + \cos^2 t = 1:

9(1)=3\sqrt{9(1)} = 3

Step 3: Integrate over the parameter interval.

L=0π3dt=3πL = \int_0^\pi 3\,dt = 3\pi

Interpretation: the curve is a circle of radius 3 traced from angle 0 to π\pi, which is a semicircle. Its arc length should be half the circumference:

12(2πr)=πr=3π\frac{1}{2}(2\pi r) = \pi r = 3\pi

So the parametric arc length matches the geometry, which is a good reasonableness check.


Worked Example 2: arc length of a polynomial parameterization

Let

x=t2x = t^2

y=23t3y = \frac{2}{3}t^3

Find arc length from t=0t = 0 to t=1t = 1.

Step 1: Differentiate.

dxdt=2t\frac{dx}{dt} = 2t

dydt=2t2\frac{dy}{dt} = 2t^2

Step 2: Form the speed.

(2t)2+(2t2)2=4t2+4t4\sqrt{\left(2t\right)^2 + \left(2t^2\right)^2} = \sqrt{4t^2 + 4t^4}

Factor inside:

4t2(1+t2)=2t1+t2\sqrt{4t^2(1 + t^2)} = 2|t|\sqrt{1+t^2}

On [0,1][0,1], t=t|t| = t, so the integrand is

2t1+t22t\sqrt{1+t^2}

Step 3: Integrate.

L=012t1+t2dtL = \int_0^1 2t\sqrt{1+t^2}\,dt

Let u=1+t2u = 1+t^2, so du=2tdtdu = 2t\,dt. When t=0t=0, u=1u=1. When t=1t=1, u=2u=2.

L=12udu=12u1/2duL = \int_1^2 \sqrt{u}\,du = \int_1^2 u^{1/2}\,du

L=23u3/212=23(23/21)L = \left.\frac{2}{3}u^{3/2}\right|_1^2 = \frac{2}{3}\left(2^{3/2} - 1\right)

You can also write 23/22^{3/2} as 222\sqrt{2}:

L=23(221)L = \frac{2}{3}\left(2\sqrt{2} - 1\right)


A common conceptual trap: arc length vs straight-line distance

Arc length is not the distance between endpoints. Even if you find the endpoints (x(a),y(a))\big(x(a),y(a)\big) and (x(b),y(b))\big(x(b),y(b)\big), using the distance formula gives the chord length, not the arc length.

If an AP question asks for “distance traveled” by a particle with position (x(t),y(t))\big(x(t),y(t)\big), that is arc length, so you should think immediately of

ab(dxdt)2+(dydt)2dt\int_a^b \sqrt{\left(\frac{dx}{dt}\right)^2 + \left(\frac{dy}{dt}\right)^2}\,dt

not

(x(b)x(a))2+(y(b)y(a))2\sqrt{(x(b)-x(a))^2 + (y(b)-y(a))^2}


Exam Focus
  • Typical question patterns
    • “Find the length of the curve for tt from aa to bb (often chosen so the radical simplifies).”
    • “A particle moves with position (x(t),y(t))\big(x(t),y(t)\big); find total distance traveled on [a,b][a,b].”
    • “Compute arc length and interpret it geometrically (circle, cycloid-like segments, etc.).”
  • Common mistakes
    • Forgetting to square both derivatives inside the square root, or forgetting the square root entirely.
    • Dropping absolute values incorrectly when simplifying (for example, replacing t2\sqrt{t^2} with tt on an interval that includes negatives).
    • Computing endpoint distance instead of integrating speed (confusing displacement with distance traveled).