# Winkel tripel projection

(Redirected from Winkel Tripel Projection)
Winkel tripel projection of the world. 15° graticule.
The Winkel tripel projection with Tissot's indicatrix of deformation

The Winkel tripel projection (Winkel III), a modified azimuthal map projection of the world, is one of three projections proposed by Oswald Winkel in 1921. The projection is the arithmetic mean of the equirectangular projection and the Aitoff projection:[1] The name Tripel (German for "triple") refers to Winkel's goal of minimizing three kinds of distortion: area, direction, and distance.[2]

## Algorithm

{\displaystyle {\begin{aligned}x&={\frac {1}{2}}\left(\lambda \cos \varphi _{1}+{\frac {2\cos \varphi \sin {\frac {\lambda }{2}}}{\operatorname {sinc} \alpha }}\right)\\y&={\frac {1}{2}}\left(\varphi +{\frac {\sin \varphi }{\operatorname {sinc} \alpha }}\right)\end{aligned}}}

where λ is the longitude minus that of the central meridian of the projection, φ is the latitude, φ1 is the standard parallel for the equirectangular projection, and

${\displaystyle \alpha =\arccos \left(\cos \varphi \cos {\frac {\lambda }{2}}\right)}$

sinc α is the unnormalized cardinal sine function (with the discontinuity removed). In his proposal, Winkel set :

${\displaystyle \varphi _{1}=\arccos {\frac {2}{\pi }}\,}$

A closed-form inverse mapping does not exist, and computing the inverse numerically is somewhat complicated.[3]

## Comparison with other projections

David M. Goldberg and J. Richard Gott III show that the Winkel tripel fares well against several other projections analyzed against their measures of distortion, producing small distance errors, small combinations of Tissot indicatrix ellipticity and area errors, and the smallest skewness of any of the projections they studied.[4] By a different metric, Capek’s "Q", the Winkel tripel ranked ninth among a hundred map projections of the world, behind the common Eckert IV projection and Robinson projections.[5]

In 1998, the Winkel tripel projection replaced the Robinson projection as the standard projection for world maps made by the National Geographic Society.[2] Many educational institutes and textbooks followed National Geographic's example in adopting the projection, and most of those still use it.[6][7]