Trigonometry

What you will be able to do

Given an angle, the learner can locate it on the unit circle and give exact values for the special angles; given an identity, can derive it from the circle's equation or the angle-addition formulas rather than recalling it; and given a trigonometric equation, can find every solution in a stated interval and express the general solution.

Orientation

Past the right triangle

Sine and cosine are usually met as ratios in a right triangle: opposite over hypotenuse, adjacent over hypotenuse. That definition works and then stops working. A right triangle has no angle of 120 ° , so cos ⁡ ( 2 π / 3 ) has no meaning under it, and neither does a negative angle, nor one past a full turn.

The unit circle removes the ceiling. Walk θ units counterclockwise around the circle x 2 + y 2 = 1 starting from ( 1 , 0 ) ; the point you reach has coordinates ( cos ⁡ θ , sin ⁡ θ ) . Every real number names a point, so every real number has a sine and a cosine.

Almost everything else then follows from the picture rather than from memory. The values cannot leave [ − 1 , 1 ] , because a point on the circle has coordinates no larger than its radius. The functions repeat every 2 π , because the walk returns to where it began. Tangent is undefined at π / 2 , because the first coordinate is zero there and the quotient sin ⁡ / cos divides by it.

The Pythagorean identity is the clearest case: cos 2 ⁡ θ + sin 2 ⁡ θ = 1 is not a theorem to learn but the circle's own equation with the coordinates renamed. It cannot fail without the point leaving the circle.

What the circle does not supply is exact values, and those come from two triangles, the half-square and the half-equilateral, which between them fix every entry in the table calculus uses throughout.

Definition

What the definition settles, and why radians

Why the circle definition is the general one. The triangle definition reads a ratio of side lengths, and side lengths are positive, so it can only produce values for acute angles with positive sines and cosines. The circle definition reads coordinates, which carry signs, so obtuse and reflex angles work without amendment: at 2 π / 3 the point sits in the second quadrant, giving cos = − 1 2 and sin = + 3 2 .

The two agree wherever both apply. For an acute θ the point ( cos ⁡ θ , sin ⁡ θ ) is the corner of a right triangle with hypotenuse 1, so the coordinates are the ratios.

Why radians and not degrees. The angle θ in the definition is an arc length along a circle of radius 1. A pure number, not a count of arbitrary subdivisions. That matters beyond tidiness: the limit lim θ → 0 sin ⁡ θ θ = 1 holds in radians and fails in degrees, where the same limit is π 180 ≈ 0.01745 . Every derivative formula depends on it, so d d x sin ⁡ x = cos ⁡ x is false for x in degrees.

A degree measure would force a constant into every subsequent formula, which is why analysis fixes radians and treats degrees as a conversion.

Why sin 2 ⁡ θ is written that way. sin 2 ⁡ θ abbreviates ( sin ⁡ θ ) 2 . The value squared. It does not mean sin ⁡ ( θ 2 ) . The notation is a compression that avoids parentheses in the identities, and misreading it inverts the order of operations: at θ = 2 , ( sin ⁡ 2 ) 2 ≈ 0.827 while sin ⁡ ( 4 ) ≈ − 0.757 .

Why the range is exactly [ − 1 , 1 ] . The coordinates of a point at distance 1 from the origin satisfy | x | ≤ 1 and | y | ≤ 1 , with equality at the axis crossings. So sin ⁡ θ = 2 is not merely hard to solve. It has no solution, because no point on the unit circle has second coordinate 2.

Why tangent has period π , not 2 π . Advancing by π sends ( cos ⁡ θ , sin ⁡ θ ) to ( − cos ⁡ θ , − sin ⁡ θ ) , the diametrically opposite point. Both coordinates change sign, so their quotient is unchanged. Sine and cosine need a full revolution to return; their ratio needs only half.

Why the identity list is short. The Pythagorean identity restates x 2 + y 2 = 1 . The double-angle formulas are angle addition with β = α . The reciprocal identities 1 + tan 2 = sec 2 follow by dividing the Pythagorean identity by cos 2 ⁡ θ . Only the angle-addition formulas themselves require separate proof, so the material to remember is one equation and one pair of formulas, everything else is derived in a line.

Representation

Circle and graph, read side by side

an angle on the circle is a position along the graph

The same two functions support two pictures, drawn here in two separate frames because their horizontal axes mean different things: on the circle it is cos ⁡ θ , on the graph it is θ . Each answers questions the other cannot.

QuestionUnit circleGraph
value at one anglecoordinates of one pointheight of one point
why | sin ⁡ | ≤ 1 radius is 1curve between two lines
periodicitythe walk returnsthe pattern repeats
sign by quadrantposition of the pointsign of the height
how many solutionsline crosses circleline crosses curve
behaviour over an intervalone angle at a timevisible at a glance

A worked reading, sin ⁡ θ = 1 2 . Both pictures answer it, and they answer differently. The circle gives the reason there are two solutions: the horizontal line at height 1 2 meets a circle twice, and the two meeting points are mirror images across the vertical axis, which is why the second solution is π − θ 0 rather than a separate discovery. The graph gives the count: two crossings per period, forever.

Exactly: sin ⁡ π 6 = 1 2 and sin ⁡ 5 π 6 = 1 2 , and since sin has period 2 π the full solution set is θ = π 6 + 2 π k or θ = 5 π 6 + 2 π k for integer k .

Where they disagree in usefulness. The equation sin ⁡ θ = 2 is settled by either, but only the circle says why: no point at distance 1 from the origin has a coordinate of 2.

For tangent the graph is the clearer of the two. Its asymptotes at π / 2 + k π mark angles where the function has no value: as θ → π / 2 the ratio sin ⁡ θ / cos ⁡ θ has numerator tending to 1 and denominator tending to 0, so it grows without bound. The circle shows only that one coordinate is approaching zero.

Translating between them. An angle on the circle is a horizontal position on the graph; a coordinate on the circle is a height. Moving fluently between the two is what makes a trigonometric question answerable from whichever side is easier.

Derivation

Two triangles, one equation, and everything else

The 45-45-90 triangle. Cut a unit square along its diagonal. The two legs are 1 and 1 , and the hypotenuse h satisfies 1 2 + 1 2 = h 2 , so h = 2 , checked: ( 2 ) 2 = 2.0000000000 .

The two acute angles are equal and sum to 90 ° , so each is 45 ° = π / 4 . Scaling the triangle to hypotenuse 1 divides every side by 2 :

sin ⁡ π 4 = cos ⁡ π 4 = 1 2 = 2 2 ≈ 0.7071067812 .

Confirmed: sin ⁡ ( π / 4 ) = 0.7071067812 .

The 30-60-90 triangle. Take an equilateral triangle of side 2 and drop a perpendicular from one vertex. It bisects both the opposite side and the angle, leaving a right triangle with hypotenuse 2, short leg 1, and long leg ℓ where 1 2 + ℓ 2 = 2 2 , so ℓ = 3 , checked: 1 + 3 = 4 = 2 2 .

The angles are 30 ° and 60 ° , and dividing by the hypotenuse 2 gives

sin ⁡ π 6 = 1 2 , cos ⁡ π 6 = 3 2 , sin ⁡ π 3 = 3 2 , cos ⁡ π 3 = 1 2 .

Confirmed: sin ⁡ ( π / 6 ) = 0.5000000000 and sin ⁡ ( π / 3 ) = 0.8660254038 = 3 / 2 .

Every entry in the special-angle table comes from these two pictures. Nothing else is memorised.

The Pythagorean identity, in one line. The definition places ( cos ⁡ θ , sin ⁡ θ ) on the circle x 2 + y 2 = 1 . Substituting the coordinates:

cos 2 ⁡ θ + sin 2 ⁡ θ = 1 .

Both triangles follow from that one construction. Confirmed at 17 ° , 133 ° and 271 ° , each giving 1.000000000000000 , and it holds for every real θ , since every θ names a point on the circle.

Dividing it gives two more. Dividing through by cos 2 ⁡ θ (where nonzero):

1 + tan 2 ⁡ θ = sec 2 ⁡ θ ,

and dividing by sin 2 ⁡ θ gives cot 2 ⁡ θ + 1 = csc 2 ⁡ θ . Neither is a new fact.

Double angles from angle addition. Taking β = α in sin ⁡ ( α + β ) = sin ⁡ α cos ⁡ β + cos ⁡ α sin ⁡ β :

sin ⁡ 2 α = 2 sin ⁡ α cos ⁡ α ,

and in the cosine formula, cos ⁡ 2 α = cos 2 ⁡ α − sin 2 ⁡ α .

Confirmed at α = 23 ° : sin ⁡ 46 ° = 0.719339800339 and 2 sin ⁡ 23 ° cos ⁡ 23 ° = 0.719339800339 ; cos ⁡ 46 ° = 0.694658370459 and cos 2 ⁡ 23 ° − sin 2 ⁡ 23 ° = 0.694658370459 . At α = 77 ° and α = 150 ° the agreement is identical to twelve places.

A new exact value from the old ones. 75 ° = 30 ° + 45 ° , so

sin ⁡ 75 ° = sin ⁡ 30 ° cos ⁡ 45 ° + cos ⁡ 30 ° sin ⁡ 45 ° = 1 2 ⋅ 2 2 + 3 2 ⋅ 2 2 = 2 + 6 4 .

Confirmed: sin ⁡ 75 ° = 0.965925826289 and ( 6 + 2 ) / 4 = 0.965925826289 . Angle addition extends the table to every angle expressible as a sum or difference of special ones.

Worked example

Five computations, from the circle outward

1. An exact value outside the first quadrant: cos ⁡ 2 π 3 .

The angle 2 π / 3 = 120 ° places the point in the second quadrant, where the first coordinate is negative and the second positive. Its reference angle, the acute angle to the horizontal axis, is π − 2 π / 3 = π / 3 .

From the 30-60-90 triangle, cos ⁡ ( π / 3 ) = 1 2 and sin ⁡ ( π / 3 ) = 3 2 . Applying the quadrant's signs:

cos ⁡ 2 π 3 = − 1 2 , sin ⁡ 2 π 3 = + 3 2 .

Check: cos ⁡ ( 2 π / 3 ) = − 0.5000000000 and sin ⁡ ( 2 π / 3 ) = + 0.8660254038 = 3 / 2 .

No sign rule was memorised. The quadrant supplied it.

2. One function from another: given cos ⁡ t = 3 5 with sin ⁡ t > 0 , find sin ⁡ t and tan ⁡ t .

From the Pythagorean identity,

sin 2 ⁡ t = 1 − cos 2 ⁡ t = 1 − 9 25 = 16 25 ⟹ sin ⁡ t = ± 4 5 .

The stated condition sin ⁡ t > 0 selects sin ⁡ t = 4 5 . Then

tan ⁡ t = sin ⁡ t cos ⁡ t = 4 / 5 3 / 5 = 4 3 .

Check: cos 2 + sin 2 = 1.000000000000000 and 4 / 3 = 1.3333333333 .

The sign condition is not decoration: without it both values are possible, and the identity alone cannot choose.

3. A new exact value by angle addition: sin ⁡ 75 ° .

Write 75 ° = 30 ° + 45 ° and apply sin ⁡ ( α + β ) = sin ⁡ α cos ⁡ β + cos ⁡ α sin ⁡ β :

sin ⁡ 75 ° = 1 2 ⋅ 2 2 + 3 2 ⋅ 2 2 = 2 4 + 6 4 = 2 + 6 4 .

Check: sin ⁡ 75 ° = 0.965925826289 and ( 6 + 2 ) / 4 = 0.965925826289 .

The companion computation gives cos ⁡ 75 ° = cos ⁡ 30 ° cos ⁡ 45 ° − sin ⁡ 30 ° sin ⁡ 45 ° = 6 − 2 4 ≈ 0.258819045103 , with the minus sign that the cosine formula carries.

4. A double angle: sin ⁡ 46 ° from α = 23 ° .

sin ⁡ 2 α = 2 sin ⁡ α cos ⁡ α ⟹ sin ⁡ 46 ° = 2 sin ⁡ 23 ° cos ⁡ 23 ° .

Check: both sides give. Likewise cos ⁡ 46 ° = cos 2 ⁡ 23 ° − sin 2 ⁡ 23 ° = 0.694658370459 , matching directly.

These are angle addition with β = α , not separate formulas.

5. A periodic equation: solve 2 sin ⁡ θ = 1 on [ 0 , 2 π ) , then in general.

Divide first: sin ⁡ θ = 1 2 . The second coordinate equals 1 2 at two points of the circle, one in the first quadrant and one in the second, mirror images across the vertical axis:

θ = π 6 and θ = π − π 6 = 5 π 6 .

Check: 2 sin ⁡ ( π / 6 ) = 1.0000000000 and 2 sin ⁡ ( 5 π / 6 ) = 1.0000000000 .

The general solution adds whole revolutions to each:

θ = π 6 + 2 k π or θ = 5 π 6 + 2 k π , k ∈ Z .

Check at k = 1 and k = 2 : every value returns 2 sin ⁡ θ = 1.0000000000 .

Reporting only π / 6 would answer a different question. Periodicity makes the solution set infinite, and the interval, when one is given, is what makes the answer finite.

Example

The angles worth knowing on sight

The first-quadrant table. Every entry comes from one of the two reference triangles:

θ 0 π / 6 π / 4 π / 3 π / 2
cos ⁡ θ 1 3 2 2 2 1 2 0
sin ⁡ θ 0 1 2 2 2 3 2 1

Each verified to ten decimal places against the circle. Cosine descends while sine climbs, which is the point travelling counterclockwise from ( 1 , 0 ) to ( 0 , 1 ) .

θ = 2 π / 3 (second quadrant). Reference angle π / 3 , first coordinate negative: cos = − 1 2 , sin = + 3 2 . The magnitudes repeat from the first quadrant; only the signs change.

θ = 7 π / 6 (third quadrant). Reference angle π / 6 , both coordinates negative: cos = − 3 2 , sin = − 1 2 . Check: sin ⁡ ( 7 π / 6 ) = − 0.5000000000 .

θ = 11 π / 6 (fourth quadrant). Reference angle π / 6 , first coordinate positive and second negative: cos = + 3 2 , sin = − 1 2 . Check: sin ⁡ ( 11 π / 6 ) = − 0.5000000000 .

These two share a sine and differ in cosine, which is why sin ⁡ θ = − 1 2 has exactly these two solutions per revolution.

θ = π / 12 , from 45 ° − 30 ° . Not a special angle itself, but a difference of two:

sin ⁡ π 12 = sin ⁡ 45 ° cos ⁡ 30 ° − cos ⁡ 45 ° sin ⁡ 30 ° = 6 − 2 4 ≈ 0.258819045103 .

Check: sin ⁡ ( π / 12 ) = 0.258819045103 . Angle addition extends the table indefinitely.

θ = π / 2 for tangent. Undefined, because cos ⁡ ( π / 2 ) = 0 and the quotient divides by it. The computed cosine is 6.1 × 10 − 17 , zero to machine precision, and the tangent values nearby climb 10,381 , 158,058 , 3,060,023 at 1.5707 , 1.57079 , 1.570796 . The function has no value there, and the same holds at every π / 2 + k π .

θ beyond a revolution: 13 π 6 . Subtract 2 π to get π / 6 , the same point on the circle, so the values are identical: sin = 1 2 , cos = 3 2 . Periodicity means any angle can be reduced to [ 0 , 2 π ) before evaluating.

Four quadrants supply four sign patterns for the same magnitudes, angle addition reaches the gaps between special angles, and periodicity reduces everything else to one revolution. The table is five columns; the reachable values are unlimited.

Procedure

Evaluating and solving

To evaluate at an angle.

  1. Reduce to [ 0 , 2 π ) by adding or subtracting whole revolutions. 13 π / 6 becomes π / 6 ; − π / 4 becomes 7 π / 4 .
  2. Identify the quadrant, which fixes the signs of both coordinates.
  3. Find the reference angle. The acute angle to the horizontal axis: θ in the first quadrant, π − θ in the second, θ − π in the third, 2 π − θ in the fourth.
  4. Read the magnitude from the special-angle table, if the reference angle is special.
  5. Apply the quadrant's signs.

For tangent, compute sin ⁡ / cos , and check first whether cos ⁡ θ = 0 , in which case it is undefined rather than large.

To find one function from another. Use cos 2 ⁡ θ + sin 2 ⁡ θ = 1 to get the magnitude, then use the stated quadrant or sign condition to choose between + and − . The identity alone never determines the sign, so a problem that omits the condition has two answers.

To prove or simplify an identity. Work on one side only and transform it into the other. Useful moves, in rough order of frequency:

  • Replace cos 2 by 1 − sin 2 , or the reverse, to reach a single function.
  • Rewrite tan , sec , csc and cot in terms of sin and cos .
  • Combine fractions over a common denominator.
  • Recognise a double angle as angle addition with β = α .

Do not manipulate both sides of a claimed identity simultaneously, which can prove a false statement.

To solve a trigonometric equation.

  1. Isolate the function: get to sin ⁡ θ = c , cos ⁡ θ = c or tan ⁡ θ = c .
  2. Check feasibility: for sine and cosine, no solution exists unless | c | ≤ 1 .
  3. Find the reference angle from the magnitude of c .
  4. Locate every solution in one period. Sine takes a given value twice per revolution, at θ 0 and π − θ 0 ; cosine twice, at θ 0 and 2 π − θ 0 ; tangent once per period of π .
  5. Add the period's multiples for the general solution: + 2 k π for sine and cosine, + k π for tangent.
  6. Restrict to the stated interval, if one is given.

Checks. Substitute each solution back, for 2 cos ⁡ x + 1 = 0 at x = 2 π / 3 and 4 π / 3 , both give 0 to machine precision. Count solutions against the graph: a horizontal line crossing a wave twice per period should yield two per period, and finding only one usually means the second quadrant case was missed.

Non-example

Notation and reasoning that go wrong

sin 2 ⁡ θ is not sin ⁡ ( θ 2 ) . The notation abbreviates ( sin ⁡ θ ) 2 : the value squared, not the angle. At θ = 2 :

( sin ⁡ 2 ) 2 ≈ 0.8268218104 , sin ⁡ ( 4 ) ≈ − 0.7568024953 .

Different numbers, and different signs. Read under the wrong convention, the Pythagorean identity would claim sin ⁡ ( θ 2 ) + cos ⁡ ( θ 2 ) = 1 , which fails at once: at θ = 2 that sum is sin ⁡ 4 + cos ⁡ 4 ≈ − 1.4104 , not 1.

A reference angle is not the answer. For cos ⁡ ( 2 π / 3 ) the reference angle is π / 3 with cos ⁡ ( π / 3 ) = 1 2 , but the angle lies in the second quadrant where first coordinates are negative. The value is − 1 2 . Reporting + 1 2 uses the magnitude and discards the position.

The Pythagorean identity does not fix a sign. Given cos ⁡ t = 3 5 , the identity gives sin 2 ⁡ t = 16 25 , so sin ⁡ t = ± 4 5 . Both are consistent with it, one in the first quadrant and one in the fourth. Choosing requires the extra condition, and a problem stating none has two answers rather than one.

tan ⁡ ( π / 2 ) is undefined, not infinite. The quotient sin ⁡ / cos divides by cos ⁡ ( π / 2 ) = 0 . The nearby values grow without bound, reaching 10,381 at 1.5707 and 3,060,023 at 1.570796 , but the function has no value at π / 2 . Writing tan ⁡ ( π / 2 ) = ∞ names a number that is not one.

Reporting one solution to a periodic equation. sin ⁡ θ = 1 2 has solutions π / 6 and 5 π / 6 in [ 0 , 2 π ) , and infinitely many overall. Giving π / 6 alone omits the second-quadrant solution, which is the most common error in solving these, since the calculator's arcsin returns one value from a restricted range and says nothing about the rest.

An equation with no solution. sin ⁡ θ = 2 has none, because no point on the unit circle has second coordinate 2. Applying arcsin regardless produces an error rather than an answer, and the check | c | ≤ 1 catches it before any work is done.

Degrees where radians are required. d d x sin ⁡ x = cos ⁡ x is false for x in degrees; the correct derivative carries a factor of π / 180 ≈ 0.01745 . The same constant spoils lim x → 0 sin ⁡ x x = 1 , which becomes 0.01745 . Analysis uses radians for exactly this reason, and a degree-mode calculator silently produces wrong derivatives.

Proving an identity by working both sides. Transforming the left and right simultaneously until they meet can establish a false statement, since the steps need not be reversible. The sound method transforms one side into the other.

Optional enrichment (1)

Application

Where periodic functions are the model

Anything that repeats. A quantity oscillating with period T , amplitude A and phase φ is written A sin ⁡ ( 2 π T t + φ ) , alternating current, a pendulum's displacement, a sound pressure wave, a tide, a seasonal sales figure. The three parameters are read directly off the graph: amplitude is half the peak-to-trough distance, period is the repeat length, phase is the horizontal shift.

That single form is why trigonometry is the language of periodic phenomena rather than one topic among several.

Fourier analysis. The orthogonality unit computes ⟨ sin , cos ⟩ = 0 and ⟨ sin , sin ⟩ = π , making { 1 , sin ⁡ x , cos ⁡ x , sin ⁡ 2 x , … } an orthogonal set. Projecting a function onto that basis gives its Fourier coefficients, so any periodic signal decomposes into these functions. The integrals involved are evaluated using the product-to-sum forms of the angle-addition formulas derived here.

Everything from audio compression to image codecs rests on that decomposition.

Complex numbers and rotation. Polar form writes z = r ( cos ⁡ θ + i sin ⁡ θ ) , and multiplying two such numbers adds their angles, which is the angle-addition formula, appearing as the arithmetic of complex multiplication. De Moivre's theorem is that formula applied n times, and Euler's identity e i θ = cos ⁡ θ + i sin ⁡ θ makes the connection exact.

In the plane, the rotation matrix ( cos ⁡ θ − sin ⁡ θ sin ⁡ θ cos ⁡ θ ) carries the same content: composing two rotations multiplies the matrices, and the entries of the product are the angle-addition formulas.

Triangulation and navigation. Measuring an inaccessible distance from two angles and a baseline uses the law of sines; GPS trilateration and surveying are the same computation at scale. The special triangles supply the exact cases against which numerical answers are sanity-checked.

In calculus. d d x sin ⁡ x = cos ⁡ x holds because of the limit lim x → 0 sin ⁡ x x = 1 , which the limits unit establishes by squeezing between cos ⁡ x and 1. Both depend on radian measure and on the unit circle definition, in degrees the derivative acquires a factor of π / 180 .

The simple-harmonic differential equation y ″ = − y has sin and cos as its solutions, which is why they describe every undamped oscillation: the equation says acceleration is proportional to displacement and opposite in sign, and these are the functions that satisfy it.

The through-line. Sine and cosine are the coordinates of a point going around a circle. Every application above is something that goes around, literally, as with rotation, or in the sense of returning to its starting state, as with a wave or a season.

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