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[[File:Hammer projection SW.jpg|300px|thumb|Hammer projection of the world]]
The '''Hammer projection''' is an equal-area [[map projection]] described by [[Ernst Hammer (cartographer)|Ernst Hammer]] in 1892. Using the same 2:1 elliptical outer shape as the [[Mollweide projection]], Hammer intended to reduce distortion toward the outer limbs, where it is extreme in the Mollweide.
 
==Development==
Directly inspired by the [[Aitoff projection]], Hammer suggested the use of the equatorial form of the [[Lambert azimuthal equal-area projection]] instead of Aitoff's use of the [[azimuthal equidistant projection]]:
 
:<math>x = \mathrm{laea}_x\left(\frac\lambda 2, \phi\right)</math>
 
:<math>y = \frac 1 2\mathrm{laea}_y\left(\frac\lambda 2, \phi\right)</math>
 
where <math>\mathrm{laea}_x</math> and <math>\mathrm{laea}_y</math> are the x and y components of the equatorial Lambert azimuthal equal-area projection. Written out explicitly:
 
:<math>x = \frac{2 \sqrt 2 \cos(\phi)\sin\left(\frac\lambda 2\right)}{\sqrt{1 + \cos(\phi)\cos\left(\frac\lambda 2\right)}}</math>
 
:<math>y = \frac{\sqrt 2\sin(\phi)}{\sqrt{1 + \cos(\phi) \cos\left(\frac\lambda 2\right)}}</math>
 
The inverse is calculated with the intermediate variable
:<math>z \equiv \sqrt{1 - \left(\frac1 4 x\right)^2 - \left(\frac1 2 y\right)^2}</math>
 
The longitude and latitudes can then be calculated by
:<math>
\begin{align}
\lambda &= 2 \arctan \left[\frac{zx}{2(2z^2 - 1)}\right] \\
\phi &= \arcsin(zy)
\end{align}
</math>
 
where <math>\lambda</math> is the [[longitude]] from the central meridian and <math>\phi</math> is the [[latitude]].<ref>''Flattening the Earth: Two Thousand Years of Map Projections'', John P. Snyder, 1993, pp.&nbsp;130–133, ISBN 0-226-76747-7.</ref><ref>Weisstein, Eric W. [http://mathworld.wolfram.com/Hammer-AitoffEqual-AreaProjection.html "Hammer–Aitoff Equal-Area Projection." From MathWorld—A Wolfram Web Resource]</ref>
 
Visually, the Aitoff and Hammer projections are very similar.  The Hammer has seen more use because of its equal-area property.  The [[Mollweide projection]] is another equal-area projection of similar aspect, though with straight parallels of latitude, unlike the Hammer's curved parallels.
 
===Briesemeister===
William A. Briesemeister presented a variant of the Hammer in 1953. In this version, the central meridian is set to 10°E, the coordinate system is rotated to bring the 45°N parallel to the center, and the resulting map is squashed horizontally and reciprocally stretched vertically to achieve a 1.75:1.0 aspect ratio instead of the 2:1 of the Hammer. The purpose is to present the land masses more centrally and with lower distortion.<ref name="Album">
{{cite book
|last = Snyder
|first = John P.
|title = An Album of Map Projections
|page = 162
|date = 1989
|url = http://upload.wikimedia.org/wikipedia/commons/d/d8/AnAlbumOfMapProjections.pdf
}}</ref>
 
===Nordic===
Before projecting to Hammer, John Bartholomew rotated the coordinate system to bring the 45° north parallel to the center, leaving the prime meridian as the central meridian. He called this variant the "Nordic" projection.<ref name="Album" />
 
==See also==
{{Portal|Atlas}}
* [[List of map projections]]
*[[Mollweide projection]]
*[[Aitoff projection]]
 
==References==
{{reflist}}
 
==External links==
{{Commonscat|Hammer projection}}
*[http://www.radicalcartography.net/?projectionref Table of common projections]
*[http://www.uff.br/mapprojections/HammerAitoff_en.html An interactive Java Applet to study the metric deformations of the Hammer–Aitoff Projection].
 
{{Map Projections}}
 
[[Category:Cartographic projections]]
[[Category:Equal-area projections]]

Latest revision as of 15:25, 26 June 2013

Hammer projection of the world

The Hammer projection is an equal-area map projection described by Ernst Hammer in 1892. Using the same 2:1 elliptical outer shape as the Mollweide projection, Hammer intended to reduce distortion toward the outer limbs, where it is extreme in the Mollweide.

Development

Directly inspired by the Aitoff projection, Hammer suggested the use of the equatorial form of the Lambert azimuthal equal-area projection instead of Aitoff's use of the azimuthal equidistant projection:

where and are the x and y components of the equatorial Lambert azimuthal equal-area projection. Written out explicitly:

The inverse is calculated with the intermediate variable

The longitude and latitudes can then be calculated by

where is the longitude from the central meridian and is the latitude.[1][2]

Visually, the Aitoff and Hammer projections are very similar. The Hammer has seen more use because of its equal-area property. The Mollweide projection is another equal-area projection of similar aspect, though with straight parallels of latitude, unlike the Hammer's curved parallels.

Briesemeister

William A. Briesemeister presented a variant of the Hammer in 1953. In this version, the central meridian is set to 10°E, the coordinate system is rotated to bring the 45°N parallel to the center, and the resulting map is squashed horizontally and reciprocally stretched vertically to achieve a 1.75:1.0 aspect ratio instead of the 2:1 of the Hammer. The purpose is to present the land masses more centrally and with lower distortion.[3]

Nordic

Before projecting to Hammer, John Bartholomew rotated the coordinate system to bring the 45° north parallel to the center, leaving the prime meridian as the central meridian. He called this variant the "Nordic" projection.[3]

See also

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References

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External links

Template:Commonscat

Template:Map Projections

  1. Flattening the Earth: Two Thousand Years of Map Projections, John P. Snyder, 1993, pp. 130–133, ISBN 0-226-76747-7.
  2. Weisstein, Eric W. "Hammer–Aitoff Equal-Area Projection." From MathWorld—A Wolfram Web Resource
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    My blog: http://www.primaboinca.com/view_profile.php?userid=5889534