Polar Coordinates - Comprehensive Notes

Polar Coordinates: Basics

  • Key idea: In polar coordinates, a point is given by (r, θ), where r is the distance from the origin (the pole) and θ is the angle from the polar axis (positive x-axis).
  • Core relationships to Cartesian:
    • x=rcos⁡θx = r \cos \theta
    • y=rsin⁡θy = r \sin \theta
    • r2=x2+y2r^2 = x^2 + y^2
    • tan⁡θ=yx\tan \theta = \frac{y}{x}
  • Important nuance: r can be negative. When r < 0, the point lies in the direction opposite to θ, i.e., the angle effectively shifts by π.
  • Practical note: Sketching polar graphs often involves recognizing circles from r = a cos θ or r = a sin θ, and lines from θ = constant.

Converting Between Polar and Cartesian

  • From polar to Cartesian (given r, θ):
    • x=rcos⁡θ,y=rsin⁡θx = r \cos \theta, \quad y = r \sin \theta
    • Example: The polar point (−2,5π6)(-2, \frac{5\pi}{6}) →
    • x=−2cos⁡5π6=−2(−32)=3x = -2 \cos \frac{5\pi}{6} = -2\left(-\frac{\sqrt{3}}{2}\right) = \sqrt{3}
    • y=−2sin⁡5π6=−2(12)=−1y = -2 \sin \frac{5\pi}{6} = -2\left(\frac{1}{2}\right) = -1
    • Cartesian: (3,−1)(\sqrt{3}, -1).
  • From Cartesian to polar (given x, y):
    • r=x2+y2r = \sqrt{x^2 + y^2} (with r ≥ 0 by convention)
    • θ=atan2⁡(y,x)\theta = \operatorname{atan2}(y, x) which places θ in [0,2π)[0, 2\pi) (adjusting for the correct quadrant)
    • Example: Cartesian (−3,−3)(-3, -3) →
    • r=(−3)2+(−3)2=18=32r = \sqrt{(-3)^2 + (-3)^2} = \sqrt{18} = 3\sqrt{2}
    • θ=arctan⁡(y/x)=arctan⁡(1)=π4\theta = \arctan(y/x) = \arctan(1) = \tfrac{\pi}{4} but in QIII, so θ=5π4\theta = \tfrac{5\pi}{4}
  • Negative radius interpretation:
    • A point with (r,θ)(r, θ) is equivalent to (∣r∣,θ)(|r|, θ) if you add π to θ when r < 0, or keep r negative with a corresponding angle. Both representations refer to the same Cartesian point.
  • Quick check example (from above): polar (−2,5π6)(-2, \tfrac{5\pi}{6}) equals Cartesian (3,−1)(\sqrt{3}, -1).
  • Practice: Given a Cartesian point (−3,−3)(-3, -3), the polar form with r>0r>0 is (32,5π4)(3\sqrt{2}, \tfrac{5\pi}{4}); a representation with r<0r<0 could be ( −32,5π4−π)(\, -3\sqrt{2}, \tfrac{5\pi}{4} - \pi). The key is to ensure θ lies in [0,2π)[0, 2\pi) when required.

Sketching Polar Graphs: Key Shapes

  • Circle from r=acos⁡θr = a \cos\theta:
    • Circle of diameter ∣a∣|a|; center at (a/2,0)(a/2, 0), on the right if a>0a>0 and on the left if a<0a<0.
  • Circle from r=asin⁡θr = a \sin\theta:
    • Circle of diameter ∣a∣|a|; center at (0,a/2)(0, a/2).
  • Lines from θ=constant\theta = \text{constant}:
    • A straight line through the origin at angle θ0; slope is tan⁡(θ0)\tan(\theta_0).
  • Practical visualization:
    • If you plug in a few θ-values for r=acos⁡θr = a \cos\theta or r=asin⁡θr = a \sin\theta, you recover the circle through polar coordinates with the claimed center and radius.
  • Desmos/graphing tip:
    • To graph a polar point in Desmos, input as Cartesian coordinates: (x,y)=(rcos⁡θ,rsin⁡θ)(x, y) = (r\cos\theta, r\sin\theta). If plotting with a function r=f(θ)r = f(\theta), use the parametric form x(θ)=f(θ)cos⁡θx(\theta) = f(\theta)\cos\theta, y(θ)=f(θ)sin⁡θy(\theta) = f(\theta)\sin\theta.

Polar–Cartesian Inverse Relations (and Practice)

  • Important identities to memorize:

    • x = r \cos \theta, \quad y = r \sin \theta,

    r^2 = x^2 + y^2,

    \tan \theta = \frac{y}{x}

  • Converting a Cartesian point to polar and choosing a representative with 0≤θ<2π0 \le \theta < 2\pi:

    • Example: Cartesian (−3,−3)(-3, -3) gives r=32r = 3\sqrt{2} and θ=5π4\theta = \tfrac{5\pi}{4} (in [0,2π)[0, 2\pi)).
  • Quick check of consistency:

    • The polar point (r,θ)=(18,5π4)(r, \theta) = (\sqrt{18}, \tfrac{5\pi}{4}) produces Cartesian (x,y)=(rcos⁡θ,rsin⁡θ)=(−3,−3)(x, y) = (r\cos\theta, r\sin\theta) = ( -3, -3 ) after substitution.
  • When converting from Cartesian to polar, be mindful of quadrant; you may also represent the same point with a negative rr and a different angle.

Slope of a Polar Curve (dy/dx)

  • If a polar curve is given by r=r(θ)r = r(\theta), then with
    • x=r(θ)cos⁡θ,y=r(θ)sin⁡θx = r(\theta) \cos \theta, \quad y = r(\theta) \sin \theta
    • and with r′=drdθr' = \dfrac{dr}{d\theta},
  • Then the derivatives with respect to θ\theta are:
    • dydθ=r′(θ)sin⁡θ+r(θ)cos⁡θ\frac{dy}{d\theta} = r'(\theta) \sin\theta + r(\theta) \cos\theta
    • dxdθ=r′(θ)cos⁡θ−r(θ)sin⁡θ\frac{dx}{d\theta} = r'(\theta) \cos\theta - r(\theta) \sin\theta
  • Therefore the slope of the tangent is:
    • dydx=dydθdxdθ=r′(θ)sin⁡θ+r(θ)cos⁡θr′(θ)cos⁡θ−r(θ)sin⁡θ\frac{dy}{dx} = \frac{\dfrac{dy}{d\theta}}{\dfrac{dx}{d\theta}} = \frac{r'(\theta) \sin\theta + r(\theta) \cos\theta}{r'(\theta) \cos\theta - r(\theta) \sin\theta}
  • Example (conceptual, not fully simplified here): find the slope of the curve r(θ)=1+sin⁡θr(\theta) = 1 + \sin\theta at θ=π4\theta = \tfrac{\pi}{4}.
    • r=1+sin⁡(π4)=1+22r = 1 + \sin(\tfrac{\pi}{4}) = 1 + \tfrac{\sqrt{2}}{2}
    • r′=cos⁡(π4)=22r' = \cos(\tfrac{\pi}{4}) = \tfrac{\sqrt{2}}{2}
    • sin⁡θ=cos⁡θ=22\sin\theta = \cos\theta = \tfrac{\sqrt{2}}{2}
    • Compute dydθ\dfrac{dy}{d\theta} and dxdθ\dfrac{dx}{d\theta} using the formulas above, then take their ratio.
    • Result (numerical): approximately −2.414-2.414 (negative slope), illustrating the need to evaluate with both rr and r′r'.
  • Takeaways:
    • The slope is well-defined except where dxdθ=0\dfrac{dx}{d\theta} = 0 (vertical tangent) or dydθ=0\dfrac{dy}{d\theta} = 0 (horizontal tangent).

Area Inside a Polar Curve

  • General formula (polar area):
    • A=12∫<em>θ</em>1θ2[r(θ)]2  dθA = \frac{1}{2} \int<em>{\theta</em>1}^{\theta_2} [r(\theta)]^2 \; d\theta
  • Rationale: A small sector with radius rr and angle dθd\theta has area approximately (\tfrac{1}{2} r^2 d\theta).
  • Key steps:
    • Determine the angular interval that sweeps the region.
    • Integrate [r(θ)]2[r(\theta)]^2 over that interval and multiply by (1/2).
  • Example 1: Area in the first and fourth quadrants bounded by r=3r = 3 (a circle of radius 3)
    • angular span from −π4-\tfrac{\pi}{4} to π4\tfrac{\pi}{4}
    • A=12∫<em>−π/4π/432  dθ=92[θ]</em>−π/4π/4=92⋅π2=9π4A = \tfrac{1}{2} \int<em>{-\pi/4}^{\pi/4} 3^2 \; d\theta = \tfrac{9}{2} \left[ \theta \right]</em>{-\pi/4}^{\pi/4} = \tfrac{9}{2} \cdot \tfrac{\pi}{2} = \frac{9\pi}{4}
  • Example 2: One petal of r=sin⁡(2θ)r = \sin(2\theta)
    • A rose with 4 petals; one petal occurs for θ\theta from 00 to π2\tfrac{\pi}{2} (where r≥0r \ge 0)
    • A<em>petal=12∫</em>0π/2sin⁡2(2θ)  dθA<em>{\text{petal}} = \tfrac{1}{2} \int</em>{0}^{\pi/2} \sin^2(2\theta) \; d\theta
    • Using sin⁡2u=1−cos⁡2u2\sin^2 u = \frac{1 - \cos 2u}{2} with u=2θu = 2\theta gives
    • A<em>petal=12⋅12∫</em>0π/2(1−cos⁡4θ) dθ=14[θ−sin⁡4θ4]0π/2=π8≈0.3927A<em>{\text{petal}} = \frac{1}{2} \cdot \frac{1}{2} \int</em>{0}^{\pi/2} (1 - \cos 4\theta) \, d\theta = \frac{1}{4} \Big[ \theta - \frac{\sin 4\theta}{4} \Big]_{0}^{\pi/2} = \frac{\pi}{8} \approx 0.3927
  • Example 3: Area between curves r=2cos⁡θr = 2\cos\theta and r=3r = \sqrt{3}
    • Intersections satisfy 2cos⁡θ=32\cos\theta = \sqrt{3} => cos⁡θ=3/2\cos\theta = \sqrt{3}/2 => θ=±π/6\theta = \pm \pi/6 (within [−π/2,π/2][-\pi/2, \pi/2] where both are nonnegative)
    • For θ∈[−π/6,π/6]\theta \in [-\pi/6, \pi/6], the outer radius is R(θ)=2cos⁡θR(\theta) = 2\cos\theta and the inner radius is r(θ)=3r(\theta) = \sqrt{3}
    • Area
    • A=12∫−π/6π/6[(2cos⁡θ)2−(3)2]dθA = \frac{1}{2} \int_{-\pi/6}^{\pi/6} \left[(2\cos\theta)^2 - (\sqrt{3})^2\right] d\theta
    • Simplify: (2cos⁡θ)2−3=4cos⁡2θ−3=2(1+cos⁡2θ)−3=−1+2cos⁡2θ(2\cos\theta)^2 - 3 = 4\cos^2\theta - 3 = 2(1+\cos 2\theta) - 3 = -1 + 2\cos 2\theta
    • A=12∫<em>−π/6π/6[−1+2cos⁡(2θ)] dθ=12[−θ+sin⁡(2θ)]</em>−π/6π/6=−π6+32≈0.342A = \frac{1}{2} \int<em>{-\pi/6}^{\pi/6} [-1 + 2\cos(2\theta)]\, d\theta = \frac{1}{2}\left[ -\theta + \sin(2\theta)\right]</em>{-\pi/6}^{\pi/6} = -\frac{\pi}{6} + \frac{\sqrt{3}}{2} \approx 0.342
    • Note: one can double a symmetric half to simplify the calculation, if preferred.
  • Quick tips for area problems:
    • Always identify the correct radial function(s) over the interval(s) of interest.
    • If curves intersect, split the integral at intersection angles and subtract as needed when one curve lies outside another.

Polar to Cartesian Equation (Another View)

  • Example: Convert r=cos⁡θ+sin⁡θr = \cos\theta + \sin\theta to Cartesian.
    • Multiply both sides by rr: r2=rcos⁡θ+rsin⁡θr^2 = r\cos\theta + r\sin\theta.
    • Replace with Cartesian variables: x2+y2=x+yx^2 + y^2 = x + y.
    • Complete the square to see the circle form:
    • x2−x+y2−y=0x^2 - x + y^2 - y = 0 → (x−12)2+(y−12)2=12(x - \tfrac{1}{2})^2 + (y - \tfrac{1}{2})^2 = \tfrac{1}{2}.
  • Key takeaway: The polar form r=f(θ)r = f(\theta) and the Cartesian form can describe the same curve; sometimes one form is easier to analyze for geometry (center, radius) and integration.

Practice Notes and Takeaways

  • Core identities to memorize:
    • x = r \cos \theta, \quad y = r \sin \theta, \
      r^2 = x^2 + y^2, \
      \tan \theta = \frac{y}{x}.
  • When converting Cartesian to polar, ensure the angle θ lies in the requested interval (often [0,2π)[0, 2\pi)).
  • When plotting polar curves, remember the sign of r affects the quadrant of the plotted point. You may prefer to adjust to a positive r with a shifted angle for clarity, especially when interpreting graphs.
  • Real-world relevance: Polar coordinates are natural for problems with radial symmetry, circular motion, or angular measurements from a fixed axis; they complement Cartesian views and can simplify area, length, and intersection analyses.
  • Desmos/graphing tip: Represent a polar curve parametrically via x(θ)=r(θ)cos⁡θx(\theta) = r(\theta) \cos \theta, y(θ)=r(θ)sin⁡θy(\theta) = r(\theta) \sin \theta to visualize it accurately.

Connection to Prior Topics

  • Builds on pre-calc/trigonometry ideas (sine/cosine relationships, unit circle geometry).
  • Uses calculus concepts (area via integration, slope via derivatives) in a coordinate system best suited to rotational symmetry.
  • Bridges geometric intuition (circles, lines) with algebraic manipulation (substituting x=rcos⁡θx = r\cos\theta and y=rsin⁡θy = r\sin\theta).

Quick Summary of Key Formulas (for quick review)

  • Cartesian from polar:
    • x = r \cos \theta, \quad y = r \sin \theta, \
      r^2 = x^2 + y^2, \
      \tan \theta = \frac{y}{x}
  • Polar from Cartesian:
    • r=x2+y2,θ=atan2⁡(y,x)∈[0,2π)r = \sqrt{x^2 + y^2}, \quad \theta = \operatorname{atan2}(y, x) \in [0, 2\pi)
  • Slope of polar curve:
    • Let r′=drdθr' = \dfrac{dr}{d\theta}; then
    • dydx=r′sin⁡θ+rcos⁡θr′cos⁡θ−rsin⁡θ\frac{dy}{dx} = \frac{r' \sin \theta + r \cos \theta}{r' \cos \theta - r \sin \theta}
  • Area in polar coordinates:
    • A=12∫<em>θ</em>1θ2[r(θ)]2  dθA = \tfrac{1}{2} \int<em>{\theta</em>1}^{\theta_2} [r(\theta)]^2 \; d\theta

End of Notes