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[[File:Winkel triple projection SW.jpg|300px|thumb|Winkel tripel projection of the world. 15° graticule.]]
[[File:Tissot indicatrix world map Winkel Tripel proj.svg|thumb|300px|The Winkel tripel projection with [[Tissot's indicatrix]] of deformation]]
 
The '''Winkel tripel projection''' ('''Winkel III'''), a modified azimuthal [[map projection]], 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]]:<REF name="Snyder"/>  The name ''Tripel'' (German for "triple") refers to Winkel's goal of minimizing three [[Map projection#Metric properties of maps|kinds of distortion]]: area, direction and distance.<REF name="winkel.org"/>
 
==Algorithm==
:<math>x = \frac{1}{2}\left[\lambda \cos \varphi_1 + \frac{2 \cos \varphi\sin \frac{\lambda}{2}}{\mathrm{sinc}\,\alpha}\right]</math>
 
:<math>y = \frac{1}{2}\left[\varphi + \frac{\sin \varphi}{\mathrm{sinc}\,\alpha}\right]</math>
 
where <math>\lambda</math> is the longitude minus that of the central meridian of the projection, <math>\varphi</math> is the latitude, <math>\varphi_1</math> is the standard parallel for the [[equirectangular projection]], and
 
:<math>\alpha = \arccos\left[\cos\varphi \cos \frac{\lambda}{2} \right]</math>
 
<math>\mathrm{sinc}\,\alpha</math> is the [[sinc function|unnormalized cardinal sine]] function (with the discontinuity removed). In his proposal, Winkel set :
 
:<math>\varphi_1 = \arccos \frac{2}{\pi}\,</math>
 
A [[Closed-form expression|closed-form]] [[Inverse function|inverse mapping]] does not exist, and computing the inverse numerically is somewhat complicated.<ref name="Ipbüker"/>
 
==Comparison with other projections==
Goldberg and [[J. Richard Gott|Gott]] 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's indicatrix|Tissot indicatrix]] ellipticity and area errors, and the smallest [[skewness]] of any of the projections they studied.<ref name="Goldberg-Gott"/>
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 projection]]s.<ref name="Capek"/>
 
In 1998, the Winkel tripel projection replaced the [[Robinson projection]] as the standard projection for world maps made by the [[National Geographic Society]]. Many educational institutes and textbooks followed National Geographic's example in adopting the projection, and most of those still use it.<ref>{{cite web|title=NG Maps Print Collection - World Political Map (Bright Colored)|url=http://maps.nationalgeographic.com/maps/print-collection/world-map-bright.html|publisher=National Geographic Society|accessdate=1 October 2013|quote=This latest world map … features the Winkel Tripel projection to reduce the distortion of land masses as they near the poles.}}</ref><ref>{{cite web|title=Selecting a Map Projection - National Geographic Education|url=http://education.nationalgeographic.com/education/media/selecting-map-projection/?ar_a=1|publisher=National Geographic Society|accessdate=1 October 2013}}</ref>
 
==See also==
{{Portal|Atlas}}
* [[List of map projections]]
 
== References ==
{{Reflist|refs=
<ref name="Snyder">{{cite book
  | title      = Flattening the Earth:  Two Thousand Years of Map Projections
  | last      = Snyder
  | first      = John P.
  | authorlink = John P. Snyder
  | year      = 1993
  | publisher  = University of Chicago Press
  | location  = Chicago
  | isbn      = 0-226-76747-7
  | pages      = 231–232
  | url        = http://books.google.com/books?id=0UzjTJ4w9yEC&pg=PA282&dq=winkel
  | accessdate = 2011-11-14
  }}</ref>
<ref name="winkel.org">{{cite web
  | url        = http://www.winkel.org/other/Winkel%20Tripel%20Projections.htm
  | title      = Winkel Tripel Projections
  | work      = Winkel.org
  | accessdate = 2011-11-14
  }}</ref>
<ref name="Goldberg-Gott">{{cite journal
  | url        = http://www.physics.drexel.edu/~goldberg/projections/goldberg_gott.pdf
  | title      = Flexion and Skewness in Map Projections of the Earth
  | year      = 2007
  | first1    = David M.
  | last1      = Goldberg
  | first2    = J. Richard
  | last2      = Gott III
  | journal    = Cartographica
  | volume    = 42
  | issue      = 4
  | pages      = 297–318
  | accessdate = 2011-11-14
  }}</ref>
<ref name="Capek">{{cite journal
  | last      = Capek
  | first      = Richard
  | year      = 2001
  | url        = http://icaci.org/documents/ICC_proceedings/ICC2001/icc2001/file/f24014.doc
  | title      = Which is the best projection for the world map?
  | journal    = Proceedings of the 20th International Cartographic Conference
  | location  = Beijing, China
  | volume    = 5
  | pages      = 3084–93
  | accessdate = 2011-11-14
  }}</ref>
<ref name="Ipbüker">{{cite journal
  | last      = Ipbüker and Bildirici
  | first      = Cengizhan and I.Öztug
  | year      = 2002
  | url        = http://atlas.selcuk.edu.tr/paperdb/papers/130.pdf
  | title      = A GENERAL ALGORITHM FOR THE INVERSE TRANSFORMATION OF MAP PROJECTIONS USING JACOBIAN MATRICES
  | journal    = Proceedings of the Third International Symposium Mathematical & Computational Applications
September 4-6, 2002. Konya, Turkey
  | location  = Selcuk, Turkey
  | pages      = 175–182
  }}</ref>
}}
 
 
== External links ==
* [http://www.radicalcartography.net/?projectionref Table of common projections]
 
{{Map Projections}}
 
[[Category:Cartographic projections]]

Revision as of 07:39, 19 January 2014

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, 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

x=12[λcosφ1+2cosφsinλ2sincα]
y=12[φ+sinφsincα]

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

α=arccos[cosφcosλ2]

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

φ1=arccos2π

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

Comparison with other projections

Goldberg and Gott 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. Many educational institutes and textbooks followed National Geographic's example in adopting the projection, and most of those still use it.[6][7]

See also

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References

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Template:Map Projections

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