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Sine and cosine

Sine and cosine are fundamental in , originally defined as ratios of sides in a right-angled triangle—sine of an θ as the opposite side over the , and cosine as the adjacent side over the —and later generalized as the y- and x-coordinates, respectively, of a point on circle at an θ radians from the positive x-axis. These functions are periodic with a period of 2π, meaning sin(θ + 2π) = sin(θ) and cos(θ + 2π) = cos(θ) for all real θ, and they satisfy the Pythagorean identity sin²θ + cos²θ = 1, which underscores their geometric foundation. Their range is the interval [-1, 1], reflecting the bounded nature of coordinates on circle. The historical development of sine and cosine traces back to ancient astronomy and , where early trigonometric concepts arose from calculations involving in circles. of (c. 190–120 BCE) is credited as the founder of , compiling the first known tables of lengths for a circle of radius 60 units to aid astronomical computations. (c. 100–170 ) advanced this work in his , producing a comprehensive table and recognizing the identity equivalent to sin²θ + cos²θ = 1, with calculations accurate to six decimal places for small angles. The explicit sine function emerged in around 500 with , who used the term jya (meaning ) in sine tables for planetary positions, later refined by Arab mathematicians like Abu al-Wafāʾ al-Būzjānī (c. 940–998 ), who introduced the double-angle formula sin(2θ) = 2 sinθ cosθ. By the 16th century, European scholars such as and Rheticus standardized sine and cosine tables, with modern notation (sin and cos) abbreviated by in 1624. Beyond their geometric and historical roots, sine and cosine are indispensable in modeling periodic and oscillatory phenomena across science and engineering. In physics, they describe simple harmonic motion, such as the displacement of a mass on a spring or a pendulum, where position x(t) = A cos(ωt + φ), with A as amplitude, ω as angular frequency, and φ as phase shift. In electrical engineering, these functions underpin alternating current (AC) circuits and signal processing, forming the basis of Fourier analysis to decompose complex waveforms into sums of sines and cosines. Applications extend to navigation, where sine and cosine compute positions via spherical trigonometry, and to computer graphics for rotations and transformations. Their derivatives—cosθ for sine and -sinθ for cosine—further enable analysis of rates of change in dynamic systems.

Elementary Definitions

Right-Angled Triangle Definition

In a right-angled triangle, the sine of an acute θ is defined as the of the of the side opposite to θ to the of the . Similarly, the cosine of θ is the of the of the side adjacent to θ to the of the . These definitions are commonly remembered using the mnemonic "SOH CAH TOA," where SOH stands for sine equals opposite over , CAH for cosine equals adjacent over , and TOA for equals opposite over adjacent. Consider a 30-60-90 , a with angles measuring 30°, 60°, and 90°, and side lengths in the ratio 1 : √3 : 2, where the side opposite the 30° angle is 1, the side opposite the 60° angle is √3, and the is 2. For the 30° angle, the sine is the opposite side (1) divided by the (2), yielding sin(30°) = 1/2; the cosine is the adjacent side (√3) divided by the (2), yielding cos(30°) = √3/2. For the 60° angle, the sine is √3/2 and the cosine is 1/2. The definitions also reveal a between complementary in a , where the two acute sum to 90°. Specifically, the sine of one acute equals the cosine of the other, so sin(θ) = cos(90° - θ). These definitions apply to measured in degrees and provide a foundation for understanding measure, defined as the of to on a . This geometric approach using can be extended to all via the unit .

Unit Circle Definition

The unit circle is defined as the circle centered at the origin (0,0) in the Cartesian plane with a radius of 1. For an angle \theta measured counterclockwise from the positive x-axis, consider the point where the terminal side of the angle intersects the unit circle; the coordinates of this point are (\cos \theta, \sin \theta), where \cos \theta is the x-coordinate and \sin \theta is the y-coordinate. This geometric construction provides a definition of the sine and cosine functions that extends to all real numbers \theta, unlike the right-triangle approach limited to acute angles. The angle \theta is typically measured in radians, the standard unit for trigonometric functions, defined as the ratio of the arc length subtended by the angle at the center of the circle to the radius of the circle. On the unit circle, where the radius is 1, one radian corresponds to an arc length of 1, which is approximately 57.3 degrees. This unit circle perspective also interprets sine and cosine as the components of a unit vector pointing in the direction of the angle \theta from the positive x-axis. Since the unit circle is periodic with a full rotation every $2\pi radians, the functions satisfy \sin(\theta + 2\pi) = \sin \theta and \cos(\theta + 2\pi) = \cos \theta, establishing a period of $2\pi for both. The range of both \sin \theta and \cos \theta is the closed interval [-1, 1], as these are the possible x- and y-coordinates on a circle of radius 1. For acute angles between 0 and \pi/2, this definition aligns with the right-triangle ratios, where the hypotenuse is taken as 1, serving as a special case of the more general approach.

Fundamental Properties

Special Angle Values

The exact values of sine and cosine for certain standard angles, known as special angles, are derived from the side ratios of right triangles and can be expressed algebraically without approximation. These values, including those for 0°, 30°, 45°, 60°, and 90° (with radian equivalents 0, π/6, π/4, π/3, and π/2), are fundamental for computations and memorization in trigonometry. Consider the 45°-45°-90° triangle, an isosceles with legs of equal length, say 1, and √2 obtained via the . The ratios yield sin(45°) = opposite/ = 1/√2 = √2/2 and cos(45°) = adjacent/ = √2/2, reflecting the geometric symmetry of the triangle. For the 30°-60°-90° triangle, construct an of side 1 and bisect it to form a with angles 30°, 60°, and 90°; the side ratios are 1 : √3 : 2 (opposite 30° : opposite 60° : ). Thus, sin(30°) = 1/2, cos(30°) = √3/2, sin(60°) = √3/2, and cos(60°) = 1/2, directly from these proportions. The values for 0° and 90° follow from the unit circle definition, where the angle 0° aligns with the positive x-axis at (1, 0), giving sin(0°) = 0 and cos(0°) = 1, while 90° aligns with the positive y-axis at (0, 1), yielding sin(90°) = 1 and cos(90°) = 0. On the unit , these special angles correspond to key positions: 0° at (1, 0), 30° at (√3/2, 1/2), ° at (√2/2, √2/2), ° at (1/2, √3/2), and 90° at (0, 1), where the coordinates are (cos θ, sin θ). The signs of sine and cosine vary by quadrant: sine is positive in the first and second quadrants (0° to 180°), negative in the third and fourth (180° to 360°); cosine is positive in the first and fourth quadrants (0° to 90° and 270° to 360°), negative in the second and third (90° to 270°).
Angle (degrees)Angle (radians)sin θcos θ
001
30°π/61/2√3/2
45°π/4√2/2√2/2
60°π/3√3/21/2
90°π/210

Graphs and Periodicity

The sine function, denoted \sin \theta, produces a smooth, symmetric wave that oscillates indefinitely along the horizontal axis. It begins at the origin (0,0), rises to a maximum of $1at\theta = \pi/2, crosses the axis again at \pi, reaches a minimum of -1at3\pi/2, and returns to $0 at $2\pi. This shape reflects its odd symmetry, where the graph is a mirror image across the origin for positive and negative arguments. Special values such as \sin 0 = 0 and \sin(\pi/2) = 1 mark key intercepts and peaks on this graph. The cosine function, \cos \theta, shares the same oscillatory pattern but is phase-shifted by \pi/2 relative to sine, such that \cos \theta = \sin(\theta + \pi/2). It starts at (0,1), descends to $0at\pi/2, reaches -1at\pi, returns to $0 at $3\pi/2, and peaks again at $1at2\pi.[2] Unlike sine, cosine exhibits [even symmetry](/page/Symmetry), appearing identical when reflected across the [vertical axis](/page/Axis), as \cos(-\theta) = \cos \theta.[2] Meanwhile, \sin(-\theta) = -\sin \theta$ confirms sine's . Both functions are periodic with a fundamental period of $2\pi, meaning \sin(\theta + 2\pi) = \sin \theta and \cos(\theta + 2\pi) = \cos \theta for all \theta. Their amplitude is $1, bounding the waves between -1 and $1 inclusive. Zeros of sine occur at integer multiples of \pi, i.e., \theta = k\pi for k \in \mathbb{Z}, while cosine zeros are at odd multiples of \pi/2, \theta = \pi/2 + k\pi. Maxima for sine are at \pi/2 + 2k\pi (value $1), and minima at 3\pi/2 + 2k\pi(value-1); for cosine, maxima are at 2k\pi (value $1), and minima at (2k+1)\pi (value -1). General transformations modify these base graphs: vertical scaling by amplitude a yields a \sin \theta or a \cos \theta, altering the height while preserving the ; frequency adjustment via \omega \sin(\omega \theta + \phi) changes the to $2\pi / \omega and introduces a shift \phi. Sine and cosine are continuous everywhere and bounded within [-1, 1], ensuring their graphs form unbroken, confined waves without discontinuities or unbounded growth.

Differentiation and Integration

The sine and cosine functions are continuous and infinitely differentiable everywhere on the real line, belonging to the class of smooth functions C^\infty(\mathbb{R}). The first derivative of \sin \theta is \cos \theta, and the first derivative of \cos \theta is -\sin \theta. These results can be established using the limit definition of the derivative. To derive \frac{d}{d\theta} \sin \theta = \cos \theta, \frac{d}{d\theta} \sin \theta = \lim_{\Delta \theta \to 0} \frac{\sin(\theta + \Delta \theta) - \sin \theta}{\Delta \theta}. Using the angle addition formula, \sin(\theta + \Delta \theta) = \sin \theta \cos \Delta \theta + \cos \theta \sin \Delta \theta, this becomes \sin \theta \left( \frac{\cos \Delta \theta - 1}{\Delta \theta} \right) + \cos \theta \left( \frac{\sin \Delta \theta}{\Delta \theta} \right). Taking the limit as \Delta \theta \to 0, using the known limits \lim_{h \to 0} \frac{\sin h}{h} = 1 and \lim_{h \to 0} \frac{\cos h - 1}{h} = 0, yields \cos \theta. A similar derivation, applying the cosine addition formula, gives \frac{d}{d\theta} \cos \theta = -\sin \theta. Higher-order derivatives of sine and cosine follow a cyclic every four differentiations due to the repeated application of these rules. Specifically, the second derivative of \sin \theta is -\sin \theta, the third is -\cos \theta, and the fourth returns to \sin \theta. For \cos \theta, the second derivative is -\cos \theta, the third is \sin \theta, and the fourth is \cos \theta. This periodicity reflects the functions' oscillatory nature and holds for all orders. The indefinite integrals are the antiderivatives obtained by reversing the differentiation rules: \int \sin \theta \, d\theta = -\cos \theta + C and \int \cos \theta \, d\theta = \sin \theta + C, where C is the constant of integration. These follow directly from the fundamental theorem of calculus, as differentiation of the right-hand sides recovers the integrands. Definite integrals of sine and cosine over full periods exhibit symmetry properties leading to zero values. For example, \int_0^{2\pi} \sin \theta \, d\theta = [-\cos \theta]_0^{2\pi} = -\cos(2\pi) + \cos(0) = -1 + 1 = 0, and similarly \int_0^{2\pi} \cos \theta \, d\theta = 0. This arises from the functions' equal positive and negative areas over one period. These and properties make sine and cosine fundamental solutions to simple linear equations, such as the second-order equation y'' + y = 0. The r^2 + 1 = 0 has roots \pm i, yielding the general solution y(\theta) = A \sin \theta + B \cos \theta, where A and B are constants determined by initial conditions. Substituting verifies that both \sin \theta and \cos \theta satisfy the equation, as their second derivatives are negatives of themselves.

Trigonometric Identities

Basic Identities

The Pythagorean trigonometric identity states that for any angle \theta, \sin^2 \theta + \cos^2 \theta = 1. This identity arises directly from the unit circle definition, where a point on the circle has coordinates (\cos \theta, \sin \theta) and satisfies the equation x^2 + y^2 = 1, substituting yields the relation. Alternatively, using the right-angled triangle definition with hypotenuse 1, the opposite side is \sin \theta and the adjacent side is \cos \theta; applying the gives (\sin \theta)^2 + (\cos \theta)^2 = 1^2. Special values of \theta, such as multiples of \pi/6 and \pi/4, satisfy this identity exactly. The reciprocal identities define the cosecant, , and cotangent functions in terms of and : \csc \theta = \frac{1}{\sin \theta}, \quad \sec \theta = \frac{1}{\cos \theta}, \quad \cot \theta = \frac{\cos \theta}{\sin \theta}. These follow from the basic definitions of the in a , where cosecant is the over the opposite side, secant is the over the adjacent side, and cotangent is the adjacent over the opposite. The function is similarly defined as the ratio \tan \theta = \frac{\sin \theta}{\cos \theta}. These reciprocal and quotient identities hold wherever the denominators are defined. The cofunction identities relate sine and cosine through complementary angles: \sin \theta = \cos\left(\frac{\pi}{2} - \theta\right), \quad \cos \theta = \sin\left(\frac{\pi}{2} - \theta\right). In a right triangle, if \theta is one acute angle, its complement \frac{\pi}{2} - \theta swaps the roles of the opposite and adjacent sides relative to the hypotenuse, leading to the equality. On the unit circle, the point for \frac{\pi}{2} - \theta has coordinates (\sin \theta, \cos \theta), confirming the relation. These identities have domain restrictions: \csc \theta and \cot \theta are undefined where \sin \theta = 0 (i.e., \theta = k\pi for integer k), while \sec \theta and \tan \theta are undefined where \cos \theta = 0 (i.e., \theta = \frac{\pi}{2} + k\pi).

Laws of Sines and Cosines

The law of sines states that in any triangle with sides a, b, c opposite angles A, B, C respectively, the ratios of the side lengths to the sines of their opposite angles are equal: \frac{a}{\sin A} = \frac{b}{\sin B} = \frac{c}{\sin C} = 2R, where R is the circumradius of the triangle. This relation holds for both acute and obtuse triangles, providing a direct link between the trigonometric functions and the geometry of the circumscribed circle. A standard derivation of the law of sines begins with the area formulas for the triangle. The area can be expressed as \frac{1}{2}bc \sin A = \frac{1}{2}ca \sin B = \frac{1}{2}ab \sin C. Dividing the first equality by bc and rearranging yields \frac{\sin A}{a} = \frac{\sin B}{b} = \frac{\sin C}{c}, which inverts to the law of sines. The constant $2R arises from the extended law of sines, where each side subtends an inscribed angle at the circumference and a central angle at the circumcenter; the side length equals $2R \sin \theta for central angle $2\theta. The provides a relationship for the sides and the cosine of an included angle: c^2 = a^2 + b^2 - 2ab \cos C, with cyclic permutations for the other forms. This formula generalizes the , reducing to c^2 = a^2 + b^2 when C = 90^\circ since \cos 90^\circ = 0. One derivation uses the . Consider vectors \mathbf{u} and \mathbf{v} along sides b and a, with |\mathbf{u} - \mathbf{v}| = c. Then, c^2 = |\mathbf{u} - \mathbf{v}|^2 = |\mathbf{u}|^2 + |\mathbf{v}|^2 - 2 \mathbf{u} \cdot \mathbf{v} = a^2 + b^2 - 2ab \cos C, since the \mathbf{u} \cdot \mathbf{v} = ab \cos C. Alternatively, a approach aligns one side with an and projects the adjacent side onto it, yielding the -2ab \cos C term as the adjustment for the angle. This interpretation connects to the unit circle definition of cosine, where \cos \theta represents the horizontal of a point on the unit circle. These laws enable the given partial information about sides and angles. The applies to angle-side- (), angle--side (), and side-side- () configurations, while the suits side--side () and side-side-side (). In the case, known as the ambiguous case, multiple triangles may satisfy the conditions: none if the given is acute and the opposite side is too short to reach the other side; exactly one if the opposite side is long enough or the angle is obtuse; or two possible triangles if the relative to the given side allows the opposite side to intersect twice. To resolve ambiguity, compute the possible second using \sin^{-1} and consistency with the third summing to $180^\circ.

Sum and Product Identities

The sum and difference identities for sine and cosine express the sine or cosine of the sum or difference of two in terms of and cosines of the individual . These identities are for simplifying trigonometric expressions and solving equations involving multiple . They can be derived geometrically using the unit circle and distance formula, where the length between points corresponding to \alpha and \beta is equated after . The sine addition formula is \sin(\alpha + \beta) = \sin \alpha \cos \beta + \cos \alpha \sin \beta, and the sine difference formula is \sin(\alpha - \beta) = \sin \alpha \cos \beta - \cos \alpha \sin \beta. Similarly, the cosine addition formula is \cos(\alpha + \beta) = \cos \alpha \cos \beta - \sin \alpha \sin \beta, and the cosine difference formula is \cos(\alpha - \beta) = \cos \alpha \cos \beta + \sin \alpha \sin \beta. These hold for all real angles \alpha and \beta. A geometric proof involves placing points on the unit circle at angles \alpha and \beta, computing the distance between them using the in the triangle formed, and applying the Pythagorean identity to match the chord length expressions. Alternatively, a brief proof uses complex exponentials via , where \sin \theta = \frac{e^{i\theta} - e^{-i\theta}}{2i} and \cos \theta = \frac{e^{i\theta} + e^{-i\theta}}{2}, leading to the addition formulas by expanding the exponential product e^{i(\alpha + \beta)} = e^{i\alpha} e^{i\beta}. These identities trace back to chord tables and were formalized by Persian astronomers around 950 AD. A special case of the sum identities yields the double-angle formulas, obtained by setting \beta = \alpha. Thus, \sin 2\theta = 2 \sin \theta \cos \theta and \cos 2\theta = \cos^2 \theta - \sin^2 \theta = 2\cos^2 \theta - 1 = 1 - 2\sin^2 \theta. These can be derived directly from the sum formulas, for example, \cos 2\theta = \cos(\theta + \theta) = \cos \theta \cos \theta - \sin \theta \sin \theta. Another geometric approach uses on a inscribed in the unit circle, where the product of diagonals equals the sum of products of opposite sides, leading to the double-angle relations after substituting chord lengths proportional to sines. The product-to-sum identities convert products of sines and cosines into sums, facilitating and simplification. Key formulas include: \sin \alpha \cos \beta = \frac{1}{2} [\sin(\alpha + \beta) + \sin(\alpha - \beta)], \sin \alpha \sin \beta = \frac{1}{2} [\cos(\alpha - \beta) - \cos(\alpha + \beta)], \cos \alpha \cos \beta = \frac{1}{2} [\cos(\alpha + \beta) + \cos(\alpha - \beta)], \cos \alpha \sin \beta = \frac{1}{2} [\sin(\alpha + \beta) - \sin(\alpha - \beta)]. These are derived by applying the sum identities to the right-hand sides and solving, or using the formulas from early trigonometric tables. Half-angle formulas express sine and cosine of half an in terms of the full angle, useful for nested radicals in exact values. The sine half-angle formula is \sin \frac{\theta}{2} = \pm \sqrt{\frac{1 - \cos \theta}{2}}, and the cosine half-angle formula is \cos \frac{\theta}{2} = \pm \sqrt{\frac{1 + \cos \theta}{2}}, where the sign depends on the quadrant of \frac{\theta}{2}. These follow from solving the double-angle formulas for the half-angle terms, such as starting with \cos \theta = 1 - 2 \sin^2 \frac{\theta}{2} and isolating the .

Series Representations

Power Series Expansions

The expansions, also known as centered at zero (Maclaurin series), provide analytic representations of the sine and cosine functions that are valid for all real arguments. These series express \sin \theta and \cos \theta as infinite sums of powers of \theta, facilitating approximations, numerical computations, and proofs of various properties. The for \sin \theta around \theta = 0 is derived by repeatedly differentiating the function and evaluating at zero, leveraging the cyclic nature of the derivatives: \frac{d}{d\theta} \sin \theta = \cos \theta, \frac{d^2}{d\theta^2} \sin \theta = -\sin \theta, and so on, with higher even derivatives yielding zero at zero due to \sin 0 = 0 and derivatives yielding \pm 1 or zero based on \cos 0 = 1. This process yields the coefficients as the reciprocals with alternating signs for powers: \sin \theta = \sum_{n=0}^{\infty} \frac{(-1)^n}{(2n+1)!} \theta^{2n+1} = \theta - \frac{\theta^3}{3!} + \frac{\theta^5}{5!} - \frac{\theta^7}{7!} + \cdots Similarly, for \cos \theta, the derivatives cycle as \frac{d}{d\theta} \cos \theta = -\sin \theta, \frac{d^2}{d\theta^2} \cos \theta = -\cos \theta, etc., with even powers at zero giving \pm 1 and odd powers zero, resulting in: \cos \theta = \sum_{n=0}^{\infty} \frac{(-1)^n}{(2n)!} \theta^{2n} = 1 - \frac{\theta^2}{2!} + \frac{\theta^4}{4!} - \frac{\theta^6}{6!} + \cdots These series converge to \sin \theta and \cos \theta for all real \theta, as the is infinite, confirmed by the where the limit of consecutive term ratios approaches zero. Chebyshev polynomials offer a related representation tied directly to , useful for approximations and . The Chebyshev of the first kind, T_n(x), satisfies T_n(\cos \theta) = \cos(n\theta) for x = \cos \theta, where T_n is a of n. The second kind, U_n(x), relates via U_n(\cos \theta) \sin \theta = \sin((n+1)\theta). These identities stem from multiple-angle formulas for cosine and sine, allowing trigonometric functions to be expressed in terms of polynomials in \cos \theta. For practical approximations, the alternating signs in the series enable error estimation using the alternating series theorem, which bounds the remainder after k terms by the absolute value of the next term. For \sin \theta truncated after the (2m+1)-th power term, the error |R_{2m+2}(\theta)| < \frac{|\theta|^{2m+3}}{(2m+3)!}, providing a tight bound that decreases rapidly for moderate \theta. This estimation is particularly effective near \theta = 0 but holds globally due to the series' convergence properties.

Fourier Series Applications

Fourier series provide a powerful method for representing periodic functions using infinite sums of sine and cosine terms, leveraging the periodic nature of these trigonometric functions to decompose complex waveforms into simpler harmonic components. The general form of a Fourier series for a periodic function f(\theta) with period $2\pi is given by f(\theta) = \frac{a_0}{2} + \sum_{n=1}^\infty \left( a_n \cos(n\theta) + b_n \sin(n\theta) \right), where the coefficients a_n and b_n are determined by integrals over one period. This representation is particularly effective because sine and cosine functions form a complete orthogonal basis for the space of square-integrable periodic functions on [0, 2\pi], allowing any such function to be uniquely expressed as a linear combination of these basis elements. The orthogonality properties of sines and cosines are fundamental to this decomposition. Specifically, over the interval [0, 2\pi], \int_0^{2\pi} \sin(m\theta) \cos(n\theta) \, d\theta = 0 for all positive integers m and n, and more generally, \int_0^{2\pi} \sin(m\theta) \sin(n\theta) \, d\theta = \begin{cases} \pi & m = n \neq 0, \\ 0 & m \neq n, \end{cases} with analogous results for cosines (replacing \pi with $2\pi for the n=0 cosine term). These relations ensure that the projections onto each basis function are independent, enabling the computation of coefficients without interference from other terms. The coefficients are thus a_n = \frac{1}{\pi} \int_0^{2\pi} f(\theta) \cos(n\theta) \, d\theta \quad (n \geq 0), \quad b_n = \frac{1}{\pi} \int_0^{2\pi} f(\theta) \sin(n\theta) \, d\theta \quad (n \geq 1). A classic example is the square wave, defined as f(\theta) = 1 for $0 < \theta < \pi and f(\theta) = -1 for \pi < \theta < 2\pi, extended periodically. As an odd function, its Fourier series contains only sine terms: f(\theta) = \frac{4}{\pi} \sum_{k=1,3,5,\dots}^\infty \frac{1}{k} \sin(k\theta), where the odd harmonics dominate, and higher terms contribute finer details to approximate the sharp transitions. Similarly, the sawtooth wave, defined as f(\theta) = \frac{\theta}{\pi} for -\pi < \theta < \pi and extended periodically, is an odd function and thus relies only on sine terms: f(\theta) = \frac{2}{\pi} \sum_{n=1}^\infty \frac{(-1)^{n+1}}{n} \sin(n\theta), illustrating how the series captures the linear ramp and reset through decreasing amplitude harmonics. In cases where cosine series are used, such as for even extensions of sawtooth-like functions in half-range expansions, the representation shifts to emphasize phase alignment with the waveform's symmetry. For the series to converge pointwise to the original function, the function must satisfy the Dirichlet conditions: it is periodic with period $2\pi, absolutely integrable over one period, has a finite number of maxima and minima, and possesses a finite number of discontinuities (each of finite jump size) in any finite interval. Under these conditions, the series converges to f(\theta) at points of continuity and to the average of the left and right limits at discontinuities. In signal analysis, Fourier series enable the breakdown of periodic signals into their frequency components, facilitating tasks such as noise filtering, spectral estimation, and data compression by isolating dominant harmonics. This mathematical framework underpins broader applications in engineering, where it ties into the modeling of periodic phenomena like vibrations, though the focus here remains on the representational power of sines and cosines.

Complex Extensions

Euler's Formula

Euler's formula establishes a profound connection between exponential functions and trigonometric functions in the complex plane, stating that for any real number θ, e^{i\theta} = \cos \theta + i \sin \theta. This equality reveals that the exponential function with an imaginary argument generates rotations in the complex plane, unifying algebraic and geometric interpretations of periodic phenomena. The formula can be derived by comparing the Taylor series expansions of the exponential function, sine, and cosine around zero. The series for the exponential is \exp(z) = \sum_{n=0}^{\infty} \frac{z^n}{n!} = 1 + z + \frac{z^2}{2!} + \frac{z^3}{3!} + \frac{z^4}{4!} + \cdots, while those for cosine and sine are \cos \theta = \sum_{k=0}^{\infty} (-1)^k \frac{\theta^{2k}}{(2k)!} = 1 - \frac{\theta^2}{2!} + \frac{\theta^4}{4!} - \cdots, \sin \theta = \sum_{k=0}^{\infty} (-1)^k \frac{\theta^{2k+1}}{(2k+1)!} = \theta - \frac{\theta^3}{3!} + \frac{\theta^5}{5!} - \cdots. Substituting z = iθ into the exponential series yields e^{i\theta} = 1 + i\theta + \frac{(i\theta)^2}{2!} + \frac{(i\theta)^3}{3!} + \frac{(i\theta)^4}{4!} + \cdots = 1 + i\theta - \frac{\theta^2}{2!} - i \frac{\theta^3}{3!} + \frac{\theta^4}{4!} + \cdots, which separates into real and imaginary parts matching exactly the series for cos θ and sin θ, respectively. A direct consequence of Euler's formula is De Moivre's theorem, which states that for any integer n and real θ, (\cos \theta + i \sin \theta)^n = \cos (n\theta) + i \sin (n\theta). This follows by raising both sides of Euler's formula to the power n, since (e^{i\theta})^n = e^{in\theta} = \cos (n\theta) + i \sin (n\theta). De Moivre originally formulated this identity in the early 18th century as a tool for computing powers of complex numbers expressed trigonometrically. Euler's formula also underpins the polar form of complex numbers, where any complex number z can be written as z = r (cos θ + i sin θ), with r = |z| the modulus and θ = arg(z) the argument. Equivalently, z = r e^{iθ}, facilitating multiplication and exponentiation in the complex domain by adding arguments and multiplying moduli./08%3A_Further_Applications_of_Trigonometry/8.05%3A_Polar_Form_of_Complex_Numbers) Leonhard Euler first introduced the formula in his 1748 treatise Introductio in analysin infinitorum, specifically in Volume I, Chapter VIII, where he explores infinite series and their applications to trigonometric functions.

Complex Sine and Cosine Functions

The complex sine and cosine functions extend the real trigonometric functions to the entire complex plane via the exponential function, which serves as the basis for their definitions derived from Euler's formula. For any complex number z, these functions are defined as \sin z = \frac{e^{iz} - e^{-iz}}{2i}, \quad \cos z = \frac{e^{iz} + e^{-iz}}{2}. When z = x + iy with x, y \in \mathbb{R}, explicit expressions in terms of real sine, cosine, and hyperbolic functions can be obtained, though the primary utility lies in the exponential form for analysis. These definitions reveal connections to hyperbolic functions: \sin(iz) = i \sinh z and \cos(iz) = \cosh z for real z, linking trigonometric and hyperbolic behaviors through imaginary arguments. The complex sine and cosine are periodic with fundamental period $2\pi, satisfying \sin(z + 2\pi) = \sin z and \cos(z + 2\pi) = \cos z, but they exhibit exponential growth along the imaginary axis and are unbounded throughout the complex plane. Many real trigonometric identities persist in the complex domain; for instance, the Pythagorean identity \sin^2 z + \cos^2 z = 1 holds for all complex z, as does the addition formula \sin(z_1 + z_2) = \sin z_1 \cos z_2 + \cos z_1 \sin z_2. The sine function has simple zeros precisely at z = k\pi for integers k, while both sine and cosine are entire functions—holomorphic everywhere in the complex plane with no poles—due to the entire nature of the exponential function.

Applications in Complex Analysis

In complex analysis, the sine function exemplifies the Weierstrass factorization theorem, which enables the representation of entire functions as infinite products incorporating their zeros and exponential factors for convergence. The theorem, developed by Karl Weierstrass, guarantees that any entire function f(z) with prescribed zeros \{a_n\} (counting multiplicity) can be factored as f(z) = z^m e^{g(z)} \prod_{n=1}^\infty E_{p_n}(z/a_n, \lambda_n), where E_p are primary factors, m accounts for a zero at the origin, and g(z) is entire. For the sine function, this yields the canonical infinite product \sin(\pi z) = \pi z \prod_{n=1}^\infty \left(1 - \frac{z^2}{n^2}\right), reflecting its simple zeros at all integers and no essential singularity at infinity. This representation, originally derived by Euler and rigorously justified via Weierstrass's methods, is pivotal for studying the growth order of entire functions and analytic continuation. The cotangent function's partial fraction expansion further illustrates applications of trigonometric functions in residue calculus and meromorphic function theory. Specifically, \pi \cot(\pi z) = \frac{1}{z} + \sum_{n=1}^\infty \left( \frac{1}{z-n} + \frac{1}{z+n} \right), or equivalently in symmetric form \cot(\pi z) = \frac{1}{z} + \sum_{n \neq 0} \left( \frac{1}{z-n} + \frac{1}{n} \right), where the sum is over all nonzero integers. This expansion arises from considering the principal parts at the simple poles of \cot(\pi z) at integer points and ensuring convergence by subtracting the constant $1/n term. It is indispensable for evaluating contour integrals, such as sums over residues, and underpins techniques in number theory and physics via the Poisson summation formula. Conformal mappings involving the sine function are essential for transforming domains to solve boundary value problems, particularly for Laplace's equation. The mapping w = \sin z conformally maps the infinite horizontal strip |\Im z| < \pi/2 onto the complex plane minus the rays (-\infty, -1] \cup [1, \infty), preserving angles and facilitating the solution of Dirichlet problems in simply connected regions. This property stems from the analyticity of sine and its derivative \cos z \neq 0 in the strip interior, ensuring local invertibility. Such mappings are routinely applied to model electrostatic potentials or fluid flows in strip-like geometries, converting irregular boundaries to straight lines for easier harmonic function construction. The Mittag-Leffler theorem extends these ideas by prescribing the expansion of any meromorphic function as a sum of its principal Laurent parts at poles plus an entire function, with trigonometric functions providing key examples. For instance, the expansions of \pi \cot(\pi z) and \pi \csc(\pi z) are direct applications, where the simple poles at integers yield terms like $1/(z - n), and the theorem guarantees uniform convergence on compact sets avoiding poles via auxiliary entire functions. This framework allows the construction of meromorphic functions with specified singularities, aiding in the approximation of general meromorphic functions and the study of their global behavior. Complex sine and cosine functions play a crucial role in solving linear differential equations with complex coefficients, where real-variable methods fail due to non-real characteristic roots. Consider the second-order equation y'' + 2\alpha y' + \beta y = 0 with complex \alpha, \beta; the solutions are y(z) = e^{-\alpha z} \sin(\gamma z + \phi) or analogous cosine forms, where \gamma = \sqrt{\beta - \alpha^2} is complex, leveraging the entire nature of \sin z and \cos z for analytic solutions across the complex plane. This approach exploits the addition formulas and periodicity of complex trigonometric functions to express general solutions compactly, particularly useful in quantum mechanics and control theory with complex parameters.

Applications

Geometric and Mensuration Uses

In geometry, sine and cosine functions are essential for computing arc lengths and chord lengths in circles. The arc length s subtended by a central angle \theta (measured in radians) in a circle of radius r is given by the formula s = r \theta, which directly arises from the definition of the radian as the ratio of arc length to radius. For chord lengths, the straight-line distance between two points on the circle separated by angle \theta is $2r \sin(\theta/2), derived from the geometry of the isosceles triangle formed by the radii and the chord, where the half-angle bisector creates a right triangle with opposite side r \sin(\theta/2). These functions also play a key role in mensuration formulas for areas. The area of a triangle with sides a and b and included angle C is \frac{1}{2} ab \sin C, which follows from the height of the triangle being b \sin C and the base a. Similarly, the area of a circular sector with radius r and central angle \theta in radians is \frac{1}{2} r^2 \theta, representing the proportional fraction of the full circle's area \pi r^2. In spherical geometry, sine and cosine extend to the spherical law of cosines for triangles on a sphere's surface, where sides a, b, c are angular distances and angles A, B, C are dihedral. The formula is \cos c = \cos a \cos b + \sin a \sin b \cos C, accounting for the sphere's curvature and enabling calculations of great-circle distances. For mensuration of volumes, the volume of a sphere of radius r is \frac{4}{3} \pi r^3, obtained via triple integration in : \int_0^{2\pi} \int_0^\pi \int_0^r \rho^2 \sin \phi \, d\rho \, d\phi \, d\theta, where the \sin \phi factor arises from the Jacobian determinant in the coordinate transformation. An example of these applications is resolving vectors in polygons, such as in the closed polygon method for vector addition, where each side vector is decomposed into components using \cos \theta and \sin \theta relative to a reference axis, allowing summation of x- and y-components to find the resultant and verify closure. The laws of sines and cosines serve as foundational tools for such geometric computations in non-right triangles.

Physical and Engineering Applications

Sine and cosine functions are fundamental in describing simple harmonic motion, which models oscillatory systems such as pendulums, springs, and molecular vibrations. The position of an object undergoing simple harmonic motion can be expressed as x(t) = A \cos(\omega t), where A is the amplitude, \omega = \sqrt{k/m} is the angular frequency with spring constant k and mass m, assuming the motion starts at maximum displacement with zero initial velocity. The corresponding velocity is the time derivative, given by v_x(t) = -A \omega \sin(\omega t), illustrating how the velocity is maximum at equilibrium and zero at extrema. Alternatively, if the motion begins at equilibrium with initial velocity, the position uses the sine form x(t) = B \sin(\omega t), with B = v_{x,0}/\omega, and velocity v_x(t) = B \omega \cos(\omega t). These representations highlight the periodic nature of the motion, with sine and cosine capturing the phase-dependent displacement and its rate of change. In electrical engineering, sine and cosine model alternating current (AC) circuits, where voltages and currents vary sinusoidally with time. The voltage across a source is typically v(t) = V_m \sin(\omega t + \phi), with peak amplitude V_m, angular frequency \omega = 2\pi f, and phase \phi. In a purely resistive circuit, the current follows the same form i(t) = I_m \sin(\omega t + \phi), in phase with the voltage. However, reactive components introduce phase shifts: for a capacitor, current leads voltage by 90°, so if v(t) = V_m \sin(\omega t), then i(t) = I_m \cos(\omega t); for an inductor, current lags by 90°, yielding i(t) = I_m (-\cos(\omega t)). These phase relationships, analyzed via phasors as complex numbers V = V_m \angle \phi, determine power transfer and circuit behavior in applications like power distribution and filters. Solutions to the one-dimensional wave equation, \frac{\partial^2 u}{\partial t^2} = c^2 \frac{\partial^2 u}{\partial x^2}, often involve and for standing waves in bounded media like strings or pipes. The general solution is u(x,t) = f(x - ct) + g(x + ct), where f and g represent right- and left-propagating waves, but interference of equal-amplitude waves y_1(x,t) = A \sin(kx - \omega t) and y_2(x,t) = A \sin(kx + \omega t) produces a standing wave y(x,t) = 2A \sin(kx) \cos(\omega t). Here, \sin(kx) fixes the spatial pattern with nodes at x = n\pi/k (n integer) and antinodes at maxima, while \cos(\omega t) governs temporal oscillation at frequency \omega = ck. This form arises from the trigonometric identity \sin a + \sin b = 2 \sin\left(\frac{a+b}{2}\right) \cos\left(\frac{a-b}{2}\right) and models phenomena such as acoustic resonances in musical instruments. In signal processing, sine and cosine serve as orthogonal basis functions for representing and manipulating periodic signals. A continuous signal can be expressed as s(t) = A \sin(\omega t - \theta), and its discrete counterpart as s = A \sin(2\pi k n / N), enabling decomposition into frequency components via Fourier methods. These functions underpin modulation techniques, where a carrier sine wave is multiplied by the message signal—equivalent to convolving in the frequency domain—to shift spectra for transmission, as in amplitude or frequency modulation. The sampling theorem connects to their periodicity, stating that a bandlimited signal with maximum frequency f_{\max} can be reconstructed from samples if the sampling rate f_s > 2 f_{\max}, preventing in digital representations of sinusoidal content. Engineering applications in utilize sine and cosine in matrices to describe and end-effector orientations. For a 2D by \theta about the z-axis, the matrix is \begin{pmatrix} \cos \theta & -\sin \theta \\ \sin \theta & \cos \theta \end{pmatrix}, transforming coordinates from one to another while preserving distances. In 3D manipulators, such matrices compose via , for example, the z-y-x convention yields ^jR_i = \begin{pmatrix} c_\alpha c_\beta & c_\alpha s_\beta s_\gamma - s_\alpha c_\gamma & c_\alpha s_\beta c_\gamma + s_\alpha s_\gamma \\ s_\alpha c_\beta & s_\alpha s_\beta s_\gamma + c_\alpha c_\gamma & s_\alpha s_\beta c_\gamma - c_\alpha s_\gamma \\ -s_\beta & c_\beta s_\gamma & c_\beta c_\gamma \end{pmatrix}, where c and s denote cosine and sine, facilitating forward in serial chains. These elements, derived from direction cosines between basis vectors, enable precise path planning and control in robotic arms.

Historical Context

Etymology

The word sine traces its origins to the term jya, meaning "" or "bowstring," which denoted the length of a subtending an in ancient astronomical calculations. This concept was transmitted to scholars in the , where jya was rendered as jiba, retaining the sense of a . During the 12th-century of texts into Latin, jiba was misread as jaib—an word for "pocket" or "bay"—and translated as sinus, the Latin term for "bay," "fold," or "." Consequently, the sine derives directly from this Latin sinus. The term cosine was introduced by English mathematician Edmund Gunter in his 1620 publication Canon triangulorum, where he abbreviated it as "co." or "co-sine" to signify the sine of the complementary angle (90° minus the given angle). This innovation complemented the existing sine and facilitated tabular computations in trigonometry. Among related trigonometric functions, tangent originates from the Latin tangens, the present participle of tangere meaning "to touch," reflecting the geometric property of a tangent line touching a circle at a single point. Similarly, secant comes from the Latin secans, from secare meaning "to cut," as the secant line intersects a circle at two points. The adoption of these terms spread across European languages via Latin intermediaries; in French, it appears as sinus, borrowed from Latin sinus denoting a curve or fold, while in German, it is Sinus, directly from Latin sinus in its mathematical sense of an arc or curve.

Historical Development

The development of the concepts of sine and cosine originated in ancient astronomy and geometry, where they were initially expressed through chord lengths in circles. Hipparchus, around 140 BCE, created the first known table of chords for a circle of radius 60, laying the foundation for trigonometry as a tool for astronomical calculations. Ptolemy, in the 2nd century CE, advanced this in his Almagest by compiling a table of chords that effectively functioned as a sine table, using a circle of radius 60 and demonstrating identities such as the Pythagorean relation for sine and cosine as well as the sine addition formula. In , trigonometric ideas evolved further with a focus on sine values derived from half-chords. , in the 5th century CE, introduced sine tables based on differences (jya-vyavahāra) for computing positions in astronomical tables, marking an early systematic approach to . By the 14th century, discovered infinite series expansions equivalent to the for sine and cosine, providing a precursor to calculus-based approximations centuries before European developments. Islamic scholars refined and expanded these tables for greater precision in astronomy. , spanning the 9th and 10th centuries, improved sine and cosine tables with higher accuracy. The double-angle formula sin(2θ) = 2 sin θ cos θ was introduced by Abu'l-Wafa around 980 CE to aid computations. , in the 13th century, shifted from chords to direct sine functions in his commentary on Ptolemy's , introducing techniques for sine tables and contributing to the in . During the European Renaissance, trigonometry transitioned toward plane applications independent of astronomy. , in his 1464 treatise De triangulis omnimodis (published 1533), treated as a fundamental function for solving triangles, establishing it as a core element of plane . In the 18th century, Leonhard Euler connected and to complex numbers through his formula e^{ix} = + i , published in 1748, which unified trigonometric and exponential functions. The 19th century saw sine and cosine integrated into analysis and physics. , in his 1822 Théorie analytique de la chaleur, developed series expansions using sines and cosines to represent periodic functions, revolutionizing heat conduction and wave theory. extended these functions to the in the mid-19th century, analyzing their analytic continuations and multi-valued nature on Riemann surfaces, which deepened their role in . A key milestone was the adoption of radian measure, first employed implicitly by James Gregory in the 1670s for infinite series derivations of , standardizing arguments in radians for compatibility.

Numerical Computation

Algorithms for Evaluation

To compute sine and cosine for arbitrary real arguments, numerical algorithms first perform argument reduction to map the input θ to a smaller equivalent within a principal , leveraging the functions' periodicity and symmetries. The periodicity of sine and cosine, with period 2π, allows reduction of θ to the interval [0, 2π) via θ mod 2π = θ - 2π ⌊θ / 2π⌋, where ⌊·⌋ denotes the floor function; this step handles large inputs by approximating π with high precision (typically to more bits than the floating-point mantissa) to minimize error accumulation. Further symmetry reductions exploit identities such as cos(θ) = sin(π/2 - θ), sin(π - θ) = sin(θ), and cos(π - θ) = -cos(θ) to map the to [0, π/2], where approximations are most efficient due to the functions' monotonicity and positive values in this . For small angles in [0, π/2], the provides a direct : sin(θ) ≈ ∑{k=0}^n (-1)^k θ^{2k+1} / (2k+1)! and cos(θ) ≈ ∑{k=0}^n (-1)^k θ^{2k} / (2k)!, truncated at degree n. The error from truncation is bounded by the Lagrange remainder term R_{n+1}(θ) = f^{(n+1)}(ξ) θ^{n+1} / (n+1)! for some ξ between 0 and θ, where |f^{(n+1)}(ξ)| ≤ 1 for f = or cos since derivatives cycle through ± and ±cos. For example, with n=5, the for (θ) with θ < π/2 is less than θ^7 / 7! ≈ 0.0002 for θ=1, ensuring double-precision accuracy for small θ. This method converges rapidly for |θ| < 1 but requires argument reduction for larger values to avoid numerical instability from high powers. The CORDIC (COordinate Rotation DIgital Computer) algorithm offers an efficient alternative, particularly for hardware, by iteratively rotating a unit vector using only shifts and adds to compute sin(θ) and cos(θ) simultaneously. Starting from the initial vector (1, 0), each iteration i applies a micro-rotation by angle α_i = atan(2^{-i}): x_{i+1} = x_i - d_i y_i 2^{-i}, y_{i+1} = y_i + d_i x_i 2^{-i}, z_{i+1} = z_i - d_i α_i, where d_i = sign(z_i) = ±1 to align the accumulated angle z with θ; after n iterations, x_n ≈ cos(θ) / K and y_n ≈ sin(θ) / K, with scaling factor K = ∏_{i=0}^{n-1} (1 + 2^{-2i})^{1/2} ≈ 0.607. This shift-add structure avoids multiplications, enabling O(n) time complexity suitable for fixed-point implementations with n ≈ 16 for single-precision accuracy. Polynomial approximations, such as minimax designs, often outperform truncated Taylor series by minimizing the maximum error over [0, π/2]. The minimax polynomial of degree m for sin(θ) is the unique polynomial p_m(θ) such that max_{θ ∈ [0, π/2]} |sin(θ) - p_m(θ)| is minimized, equioscillating at m+2 points per the equioscillation theorem; these are computed via the Remez exchange algorithm and yield smaller uniform errors than Taylor truncations for the same degree. For instance, a degree-5 minimax polynomial for sin(θ) achieves a maximum absolute error of approximately 6.8 × 10^{-5} over [0, π/2], compared to the Taylor polynomial's maximum error of about 4.4 × 10^{-3}, making it preferable for balanced computational cost. Rational approximations, combining polynomials in numerator and denominator, can further reduce degree for equivalent accuracy but introduce pole avoidance challenges. Error analysis in these algorithms must account for floating-point precision, as per IEEE 754 standards, which recommend implementing sin and cos with correctly rounded results (error ≤ 0.5 ulp) where feasible, though not strictly required unlike basic arithmetic operations. Argument reduction introduces the primary error source due to π approximation inaccuracies, potentially amplifying to several ulps for large θ without extended-precision intermediates; CORDIC errors stem from finite iterations and scaling, while series and minimax methods suffer rounding in summations. Overall, modern implementations achieve <1 ulp error across the range by combining techniques, with rigorous bounds verified via interval arithmetic.

Software Implementations

Sine and cosine functions are implemented in the standard libraries of many programming languages, typically accepting arguments in radians and returning results in double-precision floating-point format. In the C programming language, the <math.h> header provides sin(double x) and cos(double x) functions, which compute the sine and cosine of x radians, respectively, adhering to the standard for to ensure portability and accuracy across compliant systems. Similarly, Python's math module includes math.sin(x) and math.cos(x), which operate on radians and are built on the platform's C library implementations, with error bounds typically under 1 ulp (unit in the last place) for arguments in the normal range. In Java, the java.lang.Math class offers Math.sin(double a) and Math.cos(double a), also using radians, and leveraging the host system's math while guaranteeing results within 1 ulp of the correctly rounded value. For applications requiring higher precision beyond standard double-precision, the MPFR library provides arbitrary-precision implementations of sine and cosine, supporting computations to thousands of decimal digits. MPFR's mpfr_sin and mpfr_cos functions employ advanced algorithms such as asymptotically fast methods based on for efficient evaluation or polynomial approximations with precomputed tables for specific precision levels, ensuring rigorous error control relative to the working precision. These methods allow for configurable precision, making MPFR suitable for scientific computing where standard floating-point accuracy is insufficient, such as in numerical simulations or cryptographic applications involving trigonometric identities. An alternative to radian-based implementations emphasizes intuitive periodicity by using turns, where angles are fractions of a full circle, and τ = 2π serves as the circumference constant. This approach, advocated in the Tau Manifesto by Bob Palais and further popularized by Michael Hartl in his Tau Manifesto, suggests expressing functions as sin(τ t) and cos(τ t) for a parameter t in [0,1), which aligns directly with modular arithmetic for angles and simplifies code for periodic phenomena like animations or signal processing. While not standard in most libraries, some custom implementations and educational tools adopt this for better conceptual clarity, though it requires conversion from radians in legacy code. Performance-oriented implementations leverage vectorized instructions for parallel computation of sine and cosine on multiple data elements. For instance, Intel's AVX () instruction set includes approximations like _mm256_sin_ps in optimized libraries such as Intel's Short Vector Math Library (SVML), which processes 8 single-precision values simultaneously with latencies around 20-30 cycles, achieving throughputs up to 4 values per cycle on modern CPUs for applications like rendering or . These SIMD variants reduce overhead in loops but may trade slight accuracy for speed, with errors bounded by 2-3 ulps in typical ranges. Portability issues arise across systems due to varying floating-point behaviors; for example, results may differ slightly between x86 and architectures because of instruction rounding modes, necessitating tests with standards like for consistent behavior in . A common preliminary step in these implementations is angle reduction to a principal , such as [-π/4, π/4] for efficiency. The following illustrates a basic reduction formula using Payne-Hanek or similar range reduction, often preceding the core approximation:
function reduce_angle(x):
    // Reduce x modulo 2π to [-π, π]
    pi = 3.141592653589793
    twopi = 2 * pi
    x = x - [floor](/page/Floor)(x / twopi) * twopi  // Basic [modulo](/page/Modulo), improved with [hi/lo](/page/Hi-Lo) precision in practice
    if x > pi:
        x = x - twopi
    else if x < -pi:
        x = x + twopi
    return x
This step minimizes the argument size before applying series expansions or table lookups, with full implementations incorporating higher-precision constants to avoid accumulated errors.

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