Open main menu
Home
Random
Recent changes
Special pages
Community portal
Preferences
About Wikipedia
Disclaimers
Incubator escapee wiki
Search
User menu
Talk
Dark mode
Contributions
Create account
Log in
Editing
Gudermannian function
(section)
Warning:
You are not logged in. Your IP address will be publicly visible if you make any edits. If you
log in
or
create an account
, your edits will be attributed to your username, along with other benefits.
Anti-spam check. Do
not
fill this in!
{{Short description|Mathematical function relating circular and hyperbolic functions}} [[File:Gudermannian function.png|thumb|upright=1.5|The Gudermannian function relates the area of a [[circular sector]] to the area of a [[hyperbolic sector]], via a common [[stereographic projection]]. If twice the area of the blue hyperbolic sector is {{math|''Ο''}}, then twice the area of the red circular sector is {{math|''Ο'' {{=}} gd ''Ο''}}. Twice the area of the purple triangle is the stereographic projection {{math|''s'' {{=}} tan {{sfrac|1|2}}''Ο'' {{=}} tanh {{sfrac|1|2}}''Ο''.}} The blue point has coordinates {{math|(cosh ''Ο'', sinh ''Ο'')}}. The red point has coordinates {{math|(cos ''Ο'', sin ''Ο'').}} The purple point has coordinates {{math|(0, ''s'').}} ]] [[File:Gudermannian graph.png|thumb|right|upright=1.4|[[Graph of a function|Graph]] of the Gudermannian function.]] [[File:Inverse Gudermannian graph.png|thumb|right|upright=1.2|Graph of the inverse Gudermannian function.]] In mathematics, the '''Gudermannian function''' relates a [[hyperbolic angle]] measure <math display=inline>\psi</math> to a [[angle|circular angle]] measure <math display=inline>\phi</math> called the ''gudermannian'' of <math display=inline>\psi</math> and denoted <math display=inline>\operatorname{gd}\psi</math>.<ref>The symbols <math display=inline>\psi</math> and <math display=inline>\phi</math> were chosen for this article because they are commonly used in [[geodesy]] for the [[Latitude#Isometric latitude|isometric latitude]] (vertical coordinate of the [[Mercator projection]]) and [[Geodetic coordinates|geodetic latitude]], respectively, and geodesy/cartography was the original context for the study of the Gudermannian and inverse Gudermannian functions.</ref> The Gudermannian function reveals a close relationship between the [[circular function]]s and [[hyperbolic function]]s. It was introduced in the 1760s by [[Johann Heinrich Lambert]], and later named for [[Christoph Gudermann]] who also described the relationship between circular and hyperbolic functions in 1830.<ref>Gudermann published several papers about the trigonometric and hyperbolic functions in [[Crelle's Journal]] in 1830β1831. These were collected in a book, {{harvp|Gudermann|1833}}.</ref> The gudermannian is sometimes called the '''hyperbolic amplitude''' as a [[limiting case (mathematics)|limiting case]] of the [[Jacobi elliptic functions#am|Jacobi elliptic amplitude]] <math display=inline>\operatorname{am}(\psi, m)</math> when parameter <math display=inline>m=1.</math> The [[real number|real]] Gudermannian function is typically defined for <math display=inline>-\infty < \psi < \infty</math> to be the integral of the hyperbolic secant<ref>{{harvp|Roy|Olver|2010}} [http://dlmf.nist.gov/4.23#viii Β§4.23(viii) "Gudermannian Function"]; {{harvp|Beyer|1987}}</ref> :<math> \phi = \operatorname{gd} \psi \equiv \int_0^\psi \operatorname{sech} t \,\mathrm{d}t = \operatorname{arctan} (\sinh \psi).</math> The real inverse Gudermannian function can be defined for <math display=inline>-\tfrac12\pi < \phi < \tfrac12\pi</math> as the [[integral of the secant function|integral of the (circular) secant]] :<math> \psi = \operatorname{gd}^{-1} \phi = \int_0^\phi \operatorname{sec} t \,\mathrm{d}t = \operatorname{arsinh} (\tan \phi). </math> The hyperbolic angle measure <math>\psi = \operatorname{gd}^{-1} \phi</math> is called the ''anti-gudermannian'' of <math>\phi</math> or sometimes the '''lambertian''' of <math>\phi</math>, denoted <math>\psi = \operatorname{lam} \phi.</math><ref>{{harvp|Kennelly|1929}}; {{harvp|Lee|1976}}</ref> In the context of [[geodesy]] and [[navigation]] for latitude <math display=inline>\phi</math>, <math>k \operatorname{gd}^{-1} \phi</math> (scaled by arbitrary constant <math display=inline>k</math>) was historically called the '''meridional part''' of <math>\phi</math> ([[French (language)|French]]: ''latitude croissante''). It is the vertical coordinate of the [[Mercator projection]]. The two angle measures <math display=inline>\phi</math> and <math display=inline>\psi</math> are related by a common [[stereographic projection]] :<math>s = \tan \tfrac12 \phi = \tanh \tfrac12 \psi,</math> and this identity can serve as an alternative definition for <math display=inline>\operatorname{gd}</math> and <math display=inline>\operatorname{gd}^{-1}</math> valid throughout the [[complex plane]]: :<math>\begin{aligned} \operatorname{gd} \psi &= {2\arctan}\bigl(\tanh\tfrac12 \psi \,\bigr), \\[5mu] \operatorname{gd}^{-1} \phi &= {2\operatorname{artanh}}\bigl(\tan\tfrac12 \phi \,\bigr). \end{aligned}</math> __TOC__ {{clear}}
Edit summary
(Briefly describe your changes)
By publishing changes, you agree to the
Terms of Use
, and you irrevocably agree to release your contribution under the
CC BY-SA 4.0 License
and the
GFDL
. You agree that a hyperlink or URL is sufficient attribution under the Creative Commons license.
Cancel
Editing help
(opens in new window)