Misplaced Pages

Van der Grinten projection: Difference between revisions

Article snapshot taken from Wikipedia with creative commons attribution-sharealike license. Give it a read and then ask your questions in the chat. We can research this topic together.
Browse history interactively← Previous editNext edit →Content deleted Content addedVisualWikitext
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 ]. 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, though the polar regions are subject to extreme distortion. The projection was the first of four proposed by ] in 1904, and, unlike perspective projections, is an arbitrary geometric construction on the plane. It was made famous when the ] adopted it as their reference map of the world from 1922 until 1988.<ref>''Flattening the Earth: Two Thousand Years of Map Projections'', John P. Snyder, 1993, pp.258-262, ISBN 0-226-76747-7.</ref> 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}}


=== Sources === ==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

Van der Grinten projection of the world.

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:

x = ± π ( A ( G P 2 ) + A 2 ( G P 2 ) 2 ( P 2 + A 2 ) ( G 2 P 2 ) ) P 2 + A 2 y = ± π ( P Q A ( A 2 + 1 ) ( P 2 + A 2 ) Q 2 ) P 2 + A 2 {\displaystyle {\begin{aligned}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}}}\\y&={\frac {\pm \pi \left(PQ-A{\sqrt {\left(A^{2}+1\right)\left(P^{2}+A^{2}\right)-Q^{2}}}\right)}{P^{2}+A^{2}}}\end{aligned}}}

where x takes the sign of λλ0, y takes the sign of φ and

A = 1 2 | π λ λ 0 λ λ 0 π | G = cos θ sin θ + cos θ 1 P = G ( 2 sin θ 1 ) θ = arcsin | 2 φ π | Q = A 2 + G {\displaystyle {\begin{aligned}A&={\frac {1}{2}}\left|{\frac {\pi }{\lambda -\lambda _{0}}}-{\frac {\lambda -\lambda _{0}}{\pi }}\right|\\G&={\frac {\cos \theta }{\sin \theta +\cos \theta -1}}\\P&=G\left({\frac {2}{\sin \theta }}-1\right)\\\theta &=\arcsin \left|{\frac {2\varphi }{\pi }}\right|\\Q&=A^{2}+G\end{aligned}}}

Should it occur that φ = 0, then

x = ( λ λ 0 ) y = 0 {\displaystyle {\begin{aligned}x&=\left(\lambda -\lambda _{0}\right)\\y&=0\end{aligned}}}

Similarly, if λ = λ0 or φ = ±⁠π/2⁠, then

x = 0 y = ± π tan θ 2 {\displaystyle {\begin{aligned}x&=0\\y&=\pm \pi \tan {\frac {\theta }{2}}\end{aligned}}}

In all cases, φ is the latitude, λ is the longitude, and λ0 is the central meridian of the projection.

See also

References

  1. ^ Flattening the Earth: Two Thousand Years of Map Projections, John P. Snyder, 1993, pp.258-262, ISBN 0-226-76747-7.
  2. Map Projections - A Working Manual, USGS Professional Paper 1395, John P. Snyder, 1987, pp.239-242.

Bibliography

External links

Map projection
By surface
Cylindrical
Mercator-conformal
Equal-area
Pseudocylindrical
Equal-area
Conical
Pseudoconical
Azimuthal
(planar)
General perspective
Pseudoazimuthal
By metric
Conformal
Equal-area
Bonne
Bottomley
Cylindrical
Tobler hyperelliptical
Equidistant in
some aspect
Gnomonic
Loxodromic
Retroazimuthal
(Mecca or Qibla)
By construction
Compromise
Hybrid
Perspective
Planar
Polyhedral
See also
Stub icon

This cartography or mapping term article is a stub. You can help Misplaced Pages by expanding it.

Categories: