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โˆซCalculus I Unit 1 Review

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1.3 Trigonometric Functions

1.3 Trigonometric Functions

Written by the Fiveable Content Team โ€ข Last updated August 2025
Written by the Fiveable Content Team โ€ข Last updated August 2025
โˆซCalculus I
Unit & Topic Study Guides

Angle Measurements and Trigonometric Functions

Trigonometric functions connect angles to ratios, and they show up constantly in calculus. They're the main tool for describing anything periodic: circular motion, waves, oscillations. Before diving into derivatives and integrals of trig functions later in the course, you need a solid handle on how angles are measured, how the six trig functions work, and how their graphs behave.

Degree vs. Radian Measurements

A degree divides a full circle into 360 equal parts, so 360โˆ˜360^\circ is one complete rotation. You've used degrees your whole life for compass directions, weather, etc.

A radian is defined by the unit circle: 1 radian is the angle created when the arc length equals the radius of the circle. A full circle has an arc length of 2ฯ€r2\pi r, so a full rotation is 2ฯ€2\pi radians.

Why do we care about radians in calculus? Because the derivative and integral formulas for trig functions only work cleanly in radians. For example, the derivative of sinโก(x)\sin(x) is cosโก(x)\cos(x) only when xx is in radians. If you use degrees, an ugly conversion factor appears. So from here on out, radians are the default.

Conversion formulas:

  • Degrees to radians: radians=degreesร—ฯ€180\text{radians} = \text{degrees} \times \frac{\pi}{180}
  • Radians to degrees: degrees=radiansร—180ฯ€\text{degrees} = \text{radians} \times \frac{180}{\pi}

Common angles to memorize:

DegreesRadians
30โˆ˜30^\circฯ€6\frac{\pi}{6}
45โˆ˜45^\circฯ€4\frac{\pi}{4}
60โˆ˜60^\circฯ€3\frac{\pi}{3}
90โˆ˜90^\circฯ€2\frac{\pi}{2}
180โˆ˜180^\circฯ€\pi
360โˆ˜360^\circ2ฯ€2\pi

Trigonometric Functions in Triangles and Circles

Right triangle definitions (SOH-CAH-TOA):

For an acute angle ฮธ\theta in a right triangle:

  • sinโก(ฮธ)=oppositehypotenuse\sin(\theta) = \frac{\text{opposite}}{\text{hypotenuse}}
  • cosโก(ฮธ)=adjacenthypotenuse\cos(\theta) = \frac{\text{adjacent}}{\text{hypotenuse}}
  • tanโก(ฮธ)=oppositeadjacent\tan(\theta) = \frac{\text{opposite}}{\text{adjacent}}

These definitions work great for angles between 00 and ฯ€2\frac{\pi}{2}, but they break down for larger or negative angles. That's where the unit circle comes in.

Unit circle definitions:

Place a circle of radius 1 centered at the origin. For any angle ฮธ\theta measured counterclockwise from the positive xx-axis, the point where the terminal side of the angle meets the circle has coordinates (cosโกฮธ,โ€‰sinโกฮธ)(\cos\theta,\, \sin\theta). This means:

  • cosโก(ฮธ)=x-coordinate\cos(\theta) = x\text{-coordinate}
  • sinโก(ฮธ)=y-coordinate\sin(\theta) = y\text{-coordinate}
  • tanโก(ฮธ)=sinโก(ฮธ)cosโก(ฮธ)=yx\tan(\theta) = \frac{\sin(\theta)}{\cos(\theta)} = \frac{y}{x}

The unit circle definition handles any angle, positive or negative, well beyond 360โˆ˜360^\circ. It also makes clear why sinโก\sin and cosโก\cos are always between โˆ’1-1 and 11: the point never leaves the unit circle.

Degree vs radian measurements, Converting Between Degrees and Radians | Precalculus II

Properties of Trigonometric Functions

Each trig function has a specific domain (valid inputs), range (possible outputs), and period (how often it repeats).

  • Sine: Domain is all real numbers. Range is [โˆ’1,1][-1, 1]. Period is 2ฯ€2\pi.
  • Cosine: Domain is all real numbers. Range is [โˆ’1,1][-1, 1]. Period is 2ฯ€2\pi.
  • Tangent: Domain is all real numbers except ฮธ=ฯ€2+nฯ€\theta = \frac{\pi}{2} + n\pi (where cosโกฮธ=0\cos\theta = 0). Range is (โˆ’โˆž,โˆž)(-\infty, \infty). Period is ฯ€\pi.

Trigonometric Identities and Graphs

Degree vs radian measurements, MrAllegretti - Trigonometric Functions - B1

Trigonometric Identities

Trig identities are equations that hold true for all valid angles. You'll use these constantly in calculus to simplify expressions before differentiating or integrating.

Reciprocal identities define three additional trig functions:

  • cscโก(ฮธ)=1sinโก(ฮธ)\csc(\theta) = \frac{1}{\sin(\theta)}
  • secโก(ฮธ)=1cosโก(ฮธ)\sec(\theta) = \frac{1}{\cos(\theta)}
  • cotโก(ฮธ)=1tanโก(ฮธ)=cosโก(ฮธ)sinโก(ฮธ)\cot(\theta) = \frac{1}{\tan(\theta)} = \frac{\cos(\theta)}{\sin(\theta)}

Pythagorean identities come directly from the equation of the unit circle, x2+y2=1x^2 + y^2 = 1:

  • sinโก2(ฮธ)+cosโก2(ฮธ)=1\sin^2(\theta) + \cos^2(\theta) = 1
  • 1+tanโก2(ฮธ)=secโก2(ฮธ)1 + \tan^2(\theta) = \sec^2(\theta)
  • 1+cotโก2(ฮธ)=cscโก2(ฮธ)1 + \cot^2(\theta) = \csc^2(\theta)

The second and third identities are just the first one divided by cosโก2(ฮธ)\cos^2(\theta) and sinโก2(ฮธ)\sin^2(\theta), respectively. You don't need to memorize all three if you remember how to derive them from the first.

Graphs of Basic Trigonometric Functions

Sine y=sinโก(ฮธ)y = \sin(\theta):

  • Starts at 0, rises to 1 at ฯ€2\frac{\pi}{2}, returns to 0 at ฯ€\pi, drops to โˆ’1-1 at 3ฯ€2\frac{3\pi}{2}, and completes the cycle at 2ฯ€2\pi
  • Range: [โˆ’1,1][-1, 1]
  • Odd function: sinโก(โˆ’ฮธ)=โˆ’sinโก(ฮธ)\sin(-\theta) = -\sin(\theta) (symmetric about the origin)

Cosine y=cosโก(ฮธ)y = \cos(\theta):

  • Starts at 1, drops to 0 at ฯ€2\frac{\pi}{2}, reaches โˆ’1-1 at ฯ€\pi, returns to 0 at 3ฯ€2\frac{3\pi}{2}, and completes the cycle at 2ฯ€2\pi
  • Range: [โˆ’1,1][-1, 1]
  • Even function: cosโก(โˆ’ฮธ)=cosโก(ฮธ)\cos(-\theta) = \cos(\theta) (symmetric about the yy-axis)

Notice that cosine is just sine shifted left by ฯ€2\frac{\pi}{2}: cosโก(ฮธ)=sinโกโ€‰โฃ(ฮธ+ฯ€2)\cos(\theta) = \sin\!\left(\theta + \frac{\pi}{2}\right).

Tangent y=tanโก(ฮธ)y = \tan(\theta):

  • Period of ฯ€\pi (repeats twice as fast as sine and cosine)
  • Range: (โˆ’โˆž,โˆž)(-\infty, \infty)
  • Vertical asymptotes at ฮธ=ฯ€2+nฯ€\theta = \frac{\pi}{2} + n\pi for any integer nn, because cosโก(ฮธ)=0\cos(\theta) = 0 at those points
  • Odd function: tanโก(โˆ’ฮธ)=โˆ’tanโก(ฮธ)\tan(-\theta) = -\tan(\theta)

Effects of Parameters on Trigonometric Graphs

The general form is y=Asinโก(Bฮธ+C)+Dy = A\sin(B\theta + C) + D (same idea applies to cosine). Each parameter controls a different transformation:

  • Amplitude โˆฃAโˆฃ|A|: Stretches the graph vertically. The function oscillates between โˆ’โˆฃAโˆฃ+D-|A| + D and โˆฃAโˆฃ+D|A| + D. If AA is negative, the graph also flips over the horizontal axis.
  • Period 2ฯ€โˆฃBโˆฃ\frac{2\pi}{|B|}: Controls horizontal compression or stretching. A larger โˆฃBโˆฃ|B| means more cycles squeezed into the same interval. For example, y=sinโก(2ฮธ)y = \sin(2\theta) completes a full cycle in ฯ€\pi instead of 2ฯ€2\pi.
  • Phase shift โˆ’CB-\frac{C}{B}: Shifts the graph horizontally. A positive result shifts right; a negative result shifts left. Be careful with the sign here: in y=sinโก(2ฮธโˆ’ฯ€)y = \sin(2\theta - \pi), the phase shift is ฯ€2\frac{\pi}{2} to the right, not ฯ€\pi.
  • Vertical shift DD: Moves the entire graph up (D>0D > 0) or down (D<0D < 0). The midline of the wave becomes y=Dy = D instead of y=0y = 0.

Quick example: For y=3sinโก(2ฮธโˆ’ฯ€)+1y = 3\sin(2\theta - \pi) + 1, you have amplitude 3, period 2ฯ€2=ฯ€\frac{2\pi}{2} = \pi, phase shift ฯ€2\frac{\pi}{2} to the right, and midline at y=1y = 1.

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