Revision as of 13:48, 22 November 2016 editBrandmeister (talk | contribs)Autopatrolled, Extended confirmed users, Pending changes reviewers38,017 edits →top: wikilink← Previous edit | Revision as of 15:37, 28 November 2016 edit undo2602:306:c445:6719:716d:a28d:a206:712c (talk) wiki style; minor clarifNext edit → | ||
Line 1: | Line 1: | ||
] | ] | ||
The '''van der Grinten projection''' is a compromise ] that is neither ] nor ] |
The '''van der Grinten projection''' is a compromise ] that is neither ] nor ].<ref name="snyder">''Flattening the Earth: Two Thousand Years of Map Projections'', John P. Snyder, 1993, pp.258-262, ISBN 0-226-76747-7.</ref> | ||
==History== | |||
In 1904, the projection was the first of four proposed by ].<ref name="snyder" /> | |||
In 1922, the projection was made famous when the ] adopted it as their reference map of the world.<ref name="snyder" /> | |||
In 1988, 66 years later, it was supplanted by the ].<ref name="snyder" /> | |||
==Strengths and weaknesses== | |||
Unlike perspective projections, is an arbitrary geometric construction on the plane.<ref name="snyder" /> | |||
Areas of a fixed size at a distance from the equator look smaller than they do on a ] but larger than a ]. It projects the entire Earth into a circle, although the polar regions are subject to extreme distortion.<ref name="snyder" /> | |||
== Geometric construction== | == Geometric construction== | ||
The geometric construction given by van der Grinten can be written algebraically:<ref>, ] Professional Paper 1395, John P. Snyder, 1987, pp.239-242</ref> | The geometric construction given by van der Grinten can be written algebraically:<ref>, ] Professional Paper 1395, John P. Snyder, 1987, pp.239-242.</ref> | ||
:<math>\begin{align} x &= \frac {\pm \pi \left(A\left(G - P^2\right) + \sqrt {A^2 \left(G - P^2\right)^2 - \left(P^2 + A^2\right)\left(G^2 - P^2\right)}\right)} {P^2 + A^2} \\ | :<math>\begin{align} x &= \frac {\pm \pi \left(A\left(G - P^2\right) + \sqrt {A^2 \left(G - P^2\right)^2 - \left(P^2 + A^2\right)\left(G^2 - P^2\right)}\right)} {P^2 + A^2} \\ | ||
Line 30: | Line 42: | ||
==See also== | ==See also== | ||
{{Portal|Atlas}} | {{Portal|Atlas}} | ||
* |
*] | ||
*] (successor) | |||
==References== | ==References== | ||
{{reflist}} | {{reflist}} | ||
== |
==Bibliography== | ||
* {{cite web|url=http://www.progonos.com/furuti/MapProj/Normal/ProjOth/projOth.html|title=Projections by Van der Grinten, and variations}} | * {{cite web|url=http://www.progonos.com/furuti/MapProj/Normal/ProjOth/projOth.html|title=Projections by Van der Grinten, and variations}} | ||
==External links== | |||
{{Map Projections}} | {{Map Projections}} |
Revision as of 15:37, 28 November 2016
The van der Grinten projection is a compromise map projection that is neither equal-area nor conformal.
History
In 1904, the projection was the first of four proposed by Alphons J. van der Grinten.
In 1922, the projection was made famous when the National Geographic Society adopted it as their reference map of the world.
In 1988, 66 years later, it was supplanted by the Robinson projection.
Strengths and weaknesses
Unlike perspective projections, is an arbitrary geometric construction on the plane.
Areas of a fixed size at a distance from the equator look smaller than they do on a Mercator map but larger than a globe. It projects the entire Earth into a circle, although the polar regions are subject to extreme distortion.
Geometric construction
The geometric construction given by van der Grinten can be written algebraically:
where x takes the sign of λ − λ0, y takes the sign of φ and
Should it occur that φ = 0, then
Similarly, if λ = λ0 or φ = ±π/2, then
In all cases, φ is the latitude, λ is the longitude, and λ0 is the central meridian of the projection.
See also
- List of map projections
- Robinson projection (successor)
References
- ^ Flattening the Earth: Two Thousand Years of Map Projections, John P. Snyder, 1993, pp.258-262, ISBN 0-226-76747-7.
- Map Projections - A Working Manual, USGS Professional Paper 1395, John P. Snyder, 1987, pp.239-242.
Bibliography
External links
This cartography or mapping term article is a stub. You can help Misplaced Pages by expanding it. |