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The versine or versed sine is a trigonometric function found in some of the earliest (Sanskrit Aryabhatia,[1] Section I) trigonometric tables. The versine of an angle is 1 minus its cosine.

There are several related functions, most notably the coversine and haversine. The latter, half a versine, is of particular importance in the haversine formula of navigation.

A unit circle with trigonometric functions.[2]

Overview

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The versine[3][4][5][6][7] or versed sine[8][9][10][11][12] is a trigonometric function already appearing in some of the earliest trigonometric tables. It is symbolized in formulas using the abbreviations versin, sinver,[13][14] vers, or siv.[15][16] In Latin, it is known as the sinus versus (flipped sine), versinus, versus, or sagitta (arrow).[17]

Expressed in terms of common trigonometric functions sine, cosine, and tangent, the versine is equal to

There are several related functions corresponding to the versine:

  • The versed cosine,[18][nb 1] or vercosine, abbreviated vercosin, vercos, or vcs
  • The coversed sine or coversine[19] (in Latin, cosinus versus or coversinus), abbreviated coversin, covers,[20][21][22] cosiv, or cvs[23]

Special tables were also made of half of the versed sine, because of its particular use in the haversine formula used historically in navigation.

  • The haversed sine[24] or haversine (Latin semiversus),[25][26] abbreviated haversin, semiversin, semiversinus, havers, hav,[27][28] hvs,[nb 2] sem, or hv.[29] It is defined as

History and applications

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Versine and coversine

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Sine, cosine, and versine of angle θ in terms of a unit circle with radius 1, centered at O. This figure also illustrates the reason why the versine was sometimes called the sagitta, Latin for arrow.[17][30] If the arc ADB of the double-angle Δ = 2θ is viewed as a "bow" and the chord AB as its "string", then the versine CD is clearly the "arrow shaft".
Graphs of historical trigonometric functions compared with sin and cos – in the SVG file, hover over or click a graph to highlight it

The ordinary sine function (see note on etymology) was sometimes historically called the sinus rectus ("straight sine"), to contrast it with the versed sine (sinus versus).[31] The meaning of these terms is apparent if one looks at the functions in the original context for their definition, a unit circle:

For a vertical chord AB of the unit circle, the sine of the angle θ (representing half of the subtended angle Δ) is the distance AC (half of the chord). On the other hand, the versed sine of θ is the distance CD from the center of the chord to the center of the arc. Thus, the sum of cos(θ) (equal to the length of line OC) and versin(θ) (equal to the length of line CD) is the radius OD (with length 1). Illustrated this way, the sine is vertical (rectus, literally "straight") while the versine is horizontal (versus, literally "turned against, out-of-place"); both are distances from C to the circle.

This figure also illustrates the reason why the versine was sometimes called the sagitta, Latin for arrow.[17][30] If the arc ADB of the double-angle Δ = 2θ is viewed as a "bow" and the chord AB as its "string", then the versine CD is clearly the "arrow shaft".

In further keeping with the interpretation of the sine as "vertical" and the versed sine as "horizontal", sagitta is also an obsolete synonym for the abscissa (the horizontal axis of a graph).[30]

In 1821, Cauchy used the terms sinus versus (siv) for the versine and cosinus versus (cosiv) for the coversine.[15][16][nb 1]

The trigonometric functions can be constructed geometrically in terms of a unit circle centered at O.

As θ goes to zero, versin(θ) is the difference between two nearly equal quantities, so a user of a trigonometric table for the cosine alone would need a very high accuracy to obtain the versine in order to avoid catastrophic cancellation, making separate tables for the latter convenient.[12] Even with a calculator or computer, round-off errors make it advisable to use the sin2 formula for small θ.

Another historical advantage of the versine is that it is always non-negative, so its logarithm is defined everywhere except for the single angle (θ = 0, 2π, …) where it is zero—thus, one could use logarithmic tables for multiplications in formulas involving versines.

In fact, the earliest surviving table of sine (half-chord) values (as opposed to the chords tabulated by Ptolemy and other Greek authors), calculated from the Surya Siddhantha of India dated back to the 3rd century BC, was a table of values for the sine and versed sine (in 3.75° increments from 0 to 90°).[31]

The versine appears as an intermediate step in the application of the half-angle formula sin2(θ/2) = 1/2versin(θ), derived by Ptolemy, that was used to construct such tables.

Haversine

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The haversine, in particular, was important in navigation because it appears in the haversine formula, which is used to reasonably accurately compute distances on an astronomic spheroid (see issues with the Earth's radius vs. sphere) given angular positions (e.g., longitude and latitude). One could also use sin2(θ/2) directly, but having a table of the haversine removed the need to compute squares and square roots.[12]

An early utilization by José de Mendoza y Ríos of what later would be called haversines is documented in 1801.[14][32]

The first known English equivalent to a table of haversines was published by James Andrew in 1805, under the name "Squares of Natural Semi-Chords".[33][34][17]

In 1835, the term haversine (notated naturally as hav. or base-10 logarithmically as log. haversine or log. havers.) was coined[35] by James Inman[14][36][37] in the third edition of his work Navigation and Nautical Astronomy: For the Use of British Seamen to simplify the calculation of distances between two points on the surface of the Earth using spherical trigonometry for applications in navigation.[3][35] Inman also used the terms nat. versine and nat. vers. for versines.[3]

Other high-regarded tables of haversines were those of Richard Farley in 1856[33][38] and John Caulfield Hannyngton in 1876.[33][39]

The haversine continues to be used in navigation and has found new applications in recent decades, as in Bruce D. Stark's method for clearing lunar distances utilizing Gaussian logarithms since 1995[40][41] or in a more compact method for sight reduction since 2014.[29]

Modern uses

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While the usage of the versine, coversine and haversine as well as their inverse functions can be traced back centuries, the names for the other five cofunctions appear to be of much younger origin.

One period (0 < θ < 2π) of a versine or, more commonly, a haversine waveform is also commonly used in signal processing and control theory as the shape of a pulse or a window function (including Hann, Hann–Poisson and Tukey windows), because it smoothly (continuous in value and slope) "turns on" from zero to one (for haversine) and back to zero.[nb 2] In these applications, it is named Hann function or raised-cosine filter.

Mathematical identities

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Definitions

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[4]
[4]
[18]
[4]

Circular rotations

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The functions are circular rotations of each other.

Derivatives and integrals

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[42] [4][42]
[19] [19]
[24] [24]

Inverse functions

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Inverse functions like arcversine (arcversin, arcvers,[8] avers,[43][44] aver), arcvercosine (arcvercosin, arcvercos, avercos, avcs), arccoversine (arccoversin, arccovers,[8] acovers,[43][44] acvs), arccovercosine (arccovercosin, arccovercos, acovercos, acvc), archaversine (archaversin, archav, haversin−1,[45] invhav,[46][47][48] ahav,[43][44] ahvs, ahv, hav−1[49][50]), archavercosine (archavercosin, archavercos, ahvc), archacoversine (archacoversin, ahcv) or archacovercosine (archacovercosin, archacovercos, ahcc) exist as well:

[43][44]
[43][44]
[43][44][45][46][47][49][50]

Other properties

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These functions can be extended into the complex plane.[42][19][24]

Maclaurin series:[24]

[8]
[8]

Approximations

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Comparison of the versine function with three approximations to the versine functions, for angles ranging from 0 to 2π
Comparison of the versine function with three approximations to the versine functions, for angles ranging from 0 to π/2

When the versine v is small in comparison to the radius r, it may be approximated from the half-chord length L (the distance AC shown above) by the formula[51]

Alternatively, if the versine is small and the versine, radius, and half-chord length are known, they may be used to estimate the arc length s (AD in the figure above) by the formula This formula was known to the Chinese mathematician Shen Kuo, and a more accurate formula also involving the sagitta was developed two centuries later by Guo Shoujing.[52]

A more accurate approximation used in engineering[53] is

Arbitrary curves and chords

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The term versine is also sometimes used to describe deviations from straightness in an arbitrary planar curve, of which the above circle is a special case. Given a chord between two points in a curve, the perpendicular distance v from the chord to the curve (usually at the chord midpoint) is called a versine measurement. For a straight line, the versine of any chord is zero, so this measurement characterizes the straightness of the curve. In the limit as the chord length L goes to zero, the ratio 8v/L2 goes to the instantaneous curvature. This usage is especially common in rail transport, where it describes measurements of the straightness of the rail tracks[54] and it is the basis of the Hallade method for rail surveying.

The term sagitta (often abbreviated sag) is used similarly in optics, for describing the surfaces of lenses and mirrors.

See also

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Notes

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References

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Further reading

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Revisions and contributorsEdit on WikipediaRead on Wikipedia
from Grokipedia
The versine, also known as the versed sine, is a trigonometric function defined as \vers(θ)=1cos(θ)\vers(\theta) = 1 - \cos(\theta) for an angle θ\theta, geometrically representing the —the perpendicular distance from the of a chord to the of the corresponding arc on a . This function, along with related variants like the haversine \hav(θ)=1cos(θ)2\hav(\theta) = \frac{1 - \cos(\theta)}{2}, provides an alternative to standard for certain computations, particularly where differences from unity simplify calculations. Historically, the versine emerged in Hindu around 500 CE, as documented in Aryabhata's work, where it was treated as a chord segment length rather than a pure , alongside in astronomical tables. It gained prominence in Islamic mathematics by the , with scholars like employing it for angles exceeding 90° to avoid negative sine values, and Abul exploring related identities around 980 CE. By the 14th century, Jewish Levi ben Gerson integrated versine into his De Sinibus, Chordis et Arcubus, using it to derive precise sine and chord values at 15-minute intervals for solar and planetary motion. European adoption followed in the , appearing in Regiomontanus's tables, though it gradually faded from mainstream use with the rise of logarithmic by the 17th century. The versine's applications spanned astronomy for planetary positioning and eclipse predictions, navigation via the haversine formula for great-circle distances on spherical Earth models, and surveying for arc measurements. In modern contexts, it persists in engineering fields like railway track alignment to quantify curvature via sagitta and in optics for lens design, underscoring its enduring utility in precise geometric modeling.

Introduction

Definition

The versine, also known as the versed sine, is a trigonometric function defined mathematically as \versin(θ)=1cos(θ)\versin(\theta) = 1 - \cos(\theta), where θ\theta is an angle in radians. This function originates from the geometric interpretation in a unit circle, where it represents the sagitta—the perpendicular distance from the midpoint of a chord subtended by the arc of central angle 2θ2\theta to the midpoint of the arc itself. Geometrically, in a unit circle with the arc from (1,0)(1,0) to (cos(2θ),sin(2θ))(\cos(2\theta),\sin(2\theta)), the sagitta measures 1cos(θ)1 - \cos(\theta), capturing the deviation from the chord to the arc. Equivalently, for an arc of angle θ\theta from the positive x-axis to (cosθ,sinθ)(\cos \theta, \sin \theta), the versine corresponds to the length along the diameter from the initial point (1,0)(1,0) to the foot of the perpendicular from the endpoint to the diameter, which is 1cos(θ)1 - \cos(\theta). The versine exhibits several basic properties inherent to its definition. It is an even function, satisfying \versin(θ)=\versin(θ)\versin(-\theta) = \versin(\theta), because the cosine is even. Additionally, it is periodic with period 2π2\pi, as \versin(θ+2π)=\versin(θ)\versin(\theta + 2\pi) = \versin(\theta), mirroring the periodicity of the cosine. The range of the versine is the closed interval [0,2][0, 2], since the cosine varies between 1-1 and $1,making, making 1 - \cos(\theta) nonnegative and bounded above by &#36;2. Visually, in a diagram, the versine can be illustrated by drawing a chord connecting the endpoints of the arc subtended by 2θ2\theta from the positive x-axis; the is then the from the chord's to the circle's arc at its , emphasizing the function's role in describing circular deviations. A related function is the coversine, defined as \coversin(θ)=1sin(θ)\coversin(\theta) = 1 - \sin(\theta), which provides a complementary geometric measure analogous to the versine but aligned with the sine, representing the in a configuration rotated by 9090^\circ. The haversine, briefly, is half the versine.

Relation to Other Trigonometric Functions

The versine function is fundamentally linked to the cosine through its primary definition: versin(θ) = 1 - cos(θ). This relation stems from the geometric interpretation of the versine as the length of the versed chord in a . Equivalently, using the half-angle formula for cosine, which rearranges to 1 - cos(θ) = 2 sin²(θ/2), the versine can be expressed as versin(θ) = 2 sin²(θ/2). This identity highlights the versine's connection to the via half-angles, facilitating computations in certain trigonometric contexts. The coversine function complements the versine, defined as coversin(θ) = 1 - sin(θ). It relates directly to the versine through the complementary angle identity: coversin(θ) = versin(π/2 - θ). This equivalence arises because cos(π/2 - θ) = sin(θ), so 1 - cos(π/2 - θ) = 1 - sin(θ). Together, versine and coversine form a pair analogous to sine and cosine, emphasizing their roles in complementary trigonometric pairs. Versine belongs to a broader class of chord functions in historical trigonometry, which includes the exsecant, defined as exsec(θ) = sec(θ) - 1 = 1/cos(θ) - 1, and the excosecant, excsc(θ) = csc(θ) - 1 = 1/sin(θ) - 1. These functions, like the versine, measure excesses over unity in reciprocal trigonometric ratios, often appearing in early tables for chord length calculations. To illustrate these relations, the following table compares the values of sine, cosine, versine, and coversine for selected angles in the interval [0, π], computed using standard trigonometric definitions (values rounded to four decimal places for clarity):
θ (radians)sin(θ)cos(θ)versin(θ) = 1 - cos(θ)coversin(θ) = 1 - sin(θ)
00.00001.00000.00001.0000
π/60.50000.86600.13400.5000
π/30.86600.50000.50000.1340
π/21.00000.00001.00000.0000
2π/30.8660-0.50001.50000.1340
5π/60.5000-0.86601.86600.5000
π0.0000-1.00002.00001.0000
This comparison demonstrates the symmetry between versine and coversine relative to , particularly around θ = π/2.

Historical Context

Origins in Ancient Astronomy

The versine, known as utkrama-jya in , first emerged in ancient as a key trigonometric tool for chord calculations essential to modeling celestial motions. In Aryabhata's Āryabhaṭīya, composed around 499 CE, the function is defined and applied within the context of a sine table, where it represents the versed sine (R - R cos θ, with radius R typically 3438 units) to facilitate computations of planetary positions and arcs on the . This innovation built on earlier chord-based methods, enabling more precise determinations of angular distances in astronomical tables divided into 225-minute intervals. Possible precursors to the versine appear in Greek astronomy through chord tables, which approximated arc lengths for celestial calculations. Ptolemy's , from the 2nd century CE, features a comprehensive table of chords subtending angles from 0.5° to 180° in a of 60 parts, used to derive positions of , , and the sun by converting angular measures to linear distances in right triangles. These chords, equivalent to twice the sine of half-angles, laid foundational geometric techniques that influenced later developments, including the versine's role in approximations for small arcs. In medieval Islamic astronomy, the versine concept was adopted and refined through translations and syntheses of Indian and Greek works. Al-Battani (c. 858–929 CE), in his Kitāb al-Zīj, integrated —including and related functions derived from chord methods—to enhance the accuracy of planetary ephemerides and solar-lunar motions beyond Ptolemy's values. His observations over four decades produced refined zij tables that employed these functions for computing eccentricities and anomalies in the . Around 980 CE, Abul Wafa explored trigonometric identities related to the versine, further advancing its application in astronomical computations. By the , the versine was integrated into European mathematics by Jewish scholar Levi ben Gerson in his De Sinibus, Chordis et Arcubus, where it was used to derive precise values at 15-minute intervals for solar and planetary motion calculations. European adoption continued in the with Regiomontanus's , which included versine values, though it gradually faded from mainstream use with the rise of logarithmic functions by the 17th century. Prior to the dominance of in modern , the versine proved invaluable for estimating distances and elevations on the , particularly in predictions and visibility calculations. This astronomical utility later extended to navigational applications in subsequent centuries.

Development in Navigation

The haversine function, defined as hav(θ) = versin(θ)/2, emerged as a practical tool in during the , building on earlier uses of the versine in . Scottish mathematician James Gregory employed the versed sine (versin(θ) = 1 - cos(θ)) in his 1670s work on geometric and trigonometric series, providing foundational methods for calculating arcs and angles relevant to astronomical observations at sea. This laid groundwork for more specialized functions in maritime computations. Tobias Mayer further advanced its application in the 1750s through his precise lunar tables, which facilitated the lunar distance method for determining . Mayer's tables, submitted to the British Board of Longitude in 1755 and later incorporated into the starting in 1767, relied on spherical trigonometric identities involving the versine to clear observed angular distances between the and , enabling navigators to compute time differences with errors reduced to under half a degree. The haversine played a pivotal role in , allowing computation of the shortest path between two points on Earth's surface. The key formula is hav(Δσ) = hav(Δφ) + hav(Δλ) cos(φ₁) cos(φ₂), where Δσ is the , Δφ the difference in latitudes, and Δλ the difference in longitudes at latitudes φ₁ and φ₂; this equation avoids singularities in logarithmic tables and minimizes rounding errors during manual calculations. In the , haversine tables were published to streamline these computations, with early versions appearing in works by José de Mendoza y Ríos in 1801 and James Andrew in 1805. By the 1830s, such tables were integrated into nautical almanacs, including the British Nautical Almanac, where the term "haversine" was formalized by James Inman in his 1835 . These tables, providing haversine values to high precision, significantly reduced computational errors in great-circle and sight reductions, often cutting calculation time by half compared to cosine-based methods. The reliance on haversine declined after the with the widespread adoption of electronic calculators and computers, which favored direct cosine-rule implementations for spherical distances due to their in programming. Nonetheless, the haversine's legacy persists in foundational formulas and modern geospatial software.

Core Mathematical Properties

Fundamental Identities

The versine function, defined as \versinθ=1cosθ\versin \theta = 1 - \cos \theta, satisfies a fundamental half-angle identity that relates it directly to the sine function: \versinθ=2sin2(θ2).\versin \theta = 2 \sin^2 \left( \frac{\theta}{2} \right). This identity arises from the half-angle formula for cosine, cosθ=12sin2(θ/2)\cos \theta = 1 - 2 \sin^2 (\theta/2), rearranged accordingly. The haversine is defined as half the versine: \hav(θ)=\versinθ2=sin2(θ2)\hav(\theta) = \frac{\versin \theta}{2} = \sin^2 \left( \frac{\theta}{2} \right). For double angles, the versine can be expressed using the double-angle formula for cosine, cos2θ=2cos2θ1\cos 2\theta = 2 \cos^2 \theta - 1, which yields \versin2θ=1cos2θ=2(1cos2θ)=2sin2θ.\versin 2\theta = 1 - \cos 2\theta = 2 (1 - \cos^2 \theta) = 2 \sin^2 \theta. Substituting cosθ=1\versinθ\cos \theta = 1 - \versin \theta provides a reduction solely in terms of the versine: \versin2θ=2[1(1\versinθ)2]=4\versinθ2(\versinθ)2.\versin 2\theta = 2 \left[1 - (1 - \versin \theta)^2 \right] = 4 \versin \theta - 2 (\versin \theta)^2. This relation facilitates power reduction and simplification in expressions involving even multiples of angles.

Differentiation and Integration

The derivative of the versine function is ddθ\versin(θ)=sin(θ).\frac{d}{d\theta} \versin(\theta) = \sin(\theta). This result follows from the relation \versin(θ)=1cos(θ)\versin(\theta) = 1 - \cos(\theta), as the derivative of the constant 1 is 0 and the derivative of cos(θ)-\cos(\theta) is sin(θ)\sin(\theta). Using the chain rule, the derivative of a composite versine function \versin(u(θ))\versin(u(\theta)) is sin(u(θ))u(θ)\sin(u(\theta)) \cdot u'(\theta). For instance, if u(θ)=kθu(\theta) = k\theta for constant kk, then ddθ\versin(kθ)=ksin(kθ)\frac{d}{d\theta} \versin(k\theta) = k \sin(k\theta). This property simplifies computations in contexts involving scaled angles, such as in periodic phenomena. The second derivative is d2dθ2\versin(θ)=cos(θ),\frac{d^2}{d\theta^2} \versin(\theta) = \cos(\theta), obtained by differentiating sin(θ)\sin(\theta). Higher-order derivatives cycle through cos(θ)\cos(\theta), sin(θ)-\sin(\theta), and cos(θ)-\cos(\theta), mirroring the derivatives of the cosine function but offset by one differentiation. The indefinite integral of the versine function is \versin(θ)dθ=θsin(θ)+C,\int \versin(\theta) \, d\theta = \theta - \sin(\theta) + C, derived by integrating 1cos(θ)1 - \cos(\theta) term by term, yielding θ\theta minus the integral of cos(θ)\cos(\theta), which is sin(θ)\sin(\theta). For a definite integral example, consider 0π\versin(θ)dθ=[θsin(θ)]0π=π\int_0^\pi \versin(\theta) \, d\theta = [\theta - \sin(\theta)]_0^\pi = \pi. The integral of the versine function relates to the parametric equations of the , where the vertical coordinate is y=a\versin(θ)y = a \versin(\theta) for radius aa, linking the function's to the curve's horizontal progression x=a(θsin(θ))x = a(\theta - \sin(\theta)).

Advanced Relations and Approximations

Rotational and Inverse Properties

The versine function demonstrates through its periodicity, satisfying versin(θ + 2π) = versin(θ) for all real θ, a direct consequence of the 2π-periodicity of the cosine function from which it is defined as versin(θ) = 1 - cos(θ). This periodicity reflects the circular nature of the underlying trigonometric relation, allowing the function to repeat identically after a full . Additionally, the versine exhibits reflection symmetries consistent with its even nature and periodic structure. Specifically, versin(-θ) = versin(θ), making it an even function symmetric about the y-axis, and versin(2π - θ) = versin(θ), providing symmetry about θ = π. These properties arise from the even of cosine and its behavior under reflection across the unit circle. For rotations by an arbitrary angle α, the versine can be expanded using addition formulas derived from the cosine sum identity: versin(θ + α) = 1 - cos(θ + α) = 1 - [cos θ cos α - sin θ sin α] = versin(θ) cos α + sin θ sin α + versin(α). This expression highlights how versine combines with terms under angular shifts, though full derivations rely on standard trigonometric expansions. The inverse versine, denoted arversin(x) or versin⁻¹(x), is defined as the angle θ such that versin(θ) = x, equivalently θ = arccos(1 - x), with domain x ∈ [0, 2] corresponding to the range of versin over [0, π]. Graphically, arversin(x) is a strictly increasing function from (0, 0) to (2, π), concave down, mirroring the shape of the versine curve inverted over the line y = x in the principal branch; its derivative, where defined, follows from the chain rule applied to the arccosine relation. To solve versin(θ) = k for k ∈ [0, 2], the general solution accounts for the function's evenness and periodicity: θ = 2πn ± arversin(k), where n ∈ ℤ. This multi-valued yields infinitely many solutions spaced by 2π, with pairs symmetric about multiples of π due to the reflection properties.

Approximation Formulas

The expansion for the versine function, centered at θ = 0, is derived from the corresponding series for the cosine function. Specifically, versin(θ) = ∑{n=1}^∞ (-1)^{n+1} θ^{2n} / (2n)!, which begins as versin(θ) = θ²/2! - θ⁴/4! + θ⁶/6! - θ⁸/8! + ⋯. This even-powered series arises because versin(θ) = 1 - cos(θ), and subtracting the cosine series (cos(θ) = ∑{n=0}^∞ (-1)^n θ^{2n} / (2n)!) yields the form above, with the constant term canceling out. For small angles θ (in radians), the leading term provides a useful : versin(θ) ≈ θ²/2. This follows directly from truncating the after the first term, as higher-order terms become negligible when |θ| ≪ 1. The absolute in this approximation is bounded by the term, approximately θ⁴/24 for small θ, leading to a relative on the order of θ²/12. This approximation is particularly valuable in computations where θ is small, avoiding numerical cancellation issues inherent in evaluating 1 - cos(θ) directly. The haversine function, defined as hav(θ) = versin(θ)/2 = sin²(θ/2), shares a similar small-angle behavior and is prominent in navigational applications. For small θ, hav(θ) ≈ (θ/2)², derived from the sin(φ) ≈ φ with φ = θ/2. This simplifies distance calculations on spheres, such as great-circle distances, where the θ is often small for nearby points. The versine series offers advantages in convergence for certain arc-related computations, particularly near θ = 0, compared to the cosine or sine series, due to its avoidance of subtractive cancellation and focus on even powers starting quadratically. The table below compares the first few terms of the versine, cosine, and sine series (all in radians, centered at 0) to illustrate the structural differences:
FunctionSeries Expansion (first four nonzero terms)
versin(θ)θ²/2 - θ⁴/24 + θ⁶/720 - θ⁸/40320
cos(θ)1 - θ²/2 + θ⁴/24 - θ⁶/720
sin(θ)θ - θ³/6 + θ⁵/120 - θ⁷/5040

Applications and Generalizations

Uses in Navigation and Astronomy

In navigation, the haversine function plays a central role in computing great-circle distances between two points on Earth's surface, given their latitudes and longitudes. The formula for the angular central angle Δσ is derived from spherical trigonometry as hav(Δσ) = hav(Δφ) + cos(φ₁) cos(φ₂) hav(Δλ), where φ₁ and φ₂ are the latitudes, Δφ is the difference in latitudes, and Δλ is the difference in longitudes (all angles in radians). The great-circle distance d is then d = R arccos(1 - 2 hav(Δσ)), where R is Earth's mean radius (approximately 6371 km); this form leverages the identity cos(Δσ) = 1 - 2 hav(Δσ) for numerical stability in calculations, especially on early computing devices or with logarithmic tables. To apply it, convert latitudes and longitudes to radians, compute the haversines of the differences, adjust for the cosine terms, and solve for Δσ before scaling by R to obtain d. This method, popularized in the 19th century through haversine tables, enabled precise route planning for transoceanic voyages by avoiding errors in small-angle approximations inherent in cosine-based formulas. The method, employed extensively from the late 18th to the , relied on versine and haversine tables to correct observed angular separations between the and a reference body (such as the Sun or stars) for determining at . Observers measured the apparent with a , then "cleared" it—adjusting for horizontal , , and the bodies' semi-diameters—using versine-based computations to obtain the true geocentric angle. For instance, José de Mendoza y Ríos's versine method (published around 1801) simplified these corrections by expressing and effects in terms of versines, reducing the need for iterative logarithmic solutions and minimizing computational errors on board ships. These tables, integral to the from 1767 onward, allowed navigators to derive from the cleared distance and almanac predictions, yielding estimates accurate to within a few minutes of arc under favorable conditions. In astronomy, the versine facilitates computations involving small angular displacements, where approximations like versin(θ) ≈ (θ²)/2 (with θ in radians) model the quadratic deviations from true positions. These applications, rooted in 18th- and 19th-century tabular methods, enhanced the accuracy of ephemerides for both and work. A notable example is Tobias Mayer's lunar tables from the 1760s, which dramatically improved determination via the lunar distance method. Prior trials with earlier tables yielded errors up to 1 degree (60 arcminutes), but Mayer's refinements—incorporating Euler's perturbations and corrections—reduced typical errors to half a degree (30 arcminutes) in sea trials, as verified by the British Board of Longitude; his widow received £3000 in posthumous recognition for this advancement.

Extensions to Arbitrary Curves

The versine of an arbitrary is defined as the , the perpendicular distance from the of a chord connecting two points on the curve to the curve itself at its midpoint. This measure quantifies the local deviation due to , generalizing the beyond circular arcs to assess how the path bows away from the straight-line connection. In and parabolas, the versine is computed parametrically as the sagitta for segments of these conic sections. For elliptical orbits in Keplerian paths, the sagitta represents the deviation from a chord along the orbital , aiding in analysis. In parabolic curves, such as those used in vertical alignments for roads and railways, the versine measures the offset from the chord to ensure gradual grade changes; for instance, railway standards limit the vertical versine to 30 mm over a 10-m chord in parabolic sections to maintain ride comfort. Applications in often involve versine measurements for beam deflection curves, where it quantifies the deviation from the straight, unloaded position to evaluate structural under load. In , versine data from multiple chords along the track curve enables precise alignment corrections, with the estimated as Rl28vR \approx \frac{l^2}{8v}, where ll is the chord length and vv is the versine. In , the versine relates directly to the of the , the circle best approximating the curve at a point with matching and . For a small chord of ll, the versine vv approximates vl28Rv \approx \frac{l^2}{8R}, where R=1κR = \frac{1}{\kappa} is the and κ\kappa is the . This connection facilitates , where the curve segment ss is given by sl+8v23ls \approx l + \frac{8v^2}{3l} for small deviations, providing a practical tool for estimating path lengths from measured versines.

References

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