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The '''van der Grinten projection''' is a compromise ] that is neither ] nor ]. 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 Alphons J. van der Grinten in 1904, and, unlike most 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 ]. 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 Alphons J. van der Grinten in 1904, and, unlike most 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 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>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> :<math>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>

Revision as of 09:53, 10 March 2013

Van der Grinten projection of the world.

The van der Grinten projection is a compromise map projection that is neither equal-area nor conformal. 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 Alphons J. van der Grinten in 1904, and, unlike most projections, is an arbitrary geometric construction on the plane. It was made famous when the National Geographic Society adopted it as their reference map of the world from 1922 until 1988.

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 {\displaystyle 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 = ± π ( P Q A ( A 2 + 1 ) ( P 2 + A 2 ) Q 2 ) P 2 + A 2 {\displaystyle 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}}}}

where x {\displaystyle x\,} takes the sign of λ λ 0 {\displaystyle \lambda -\lambda _{0}\,} , y {\displaystyle y\,} takes the sign of ϕ {\displaystyle \phi \,} and

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

Should it occur that ϕ = 0 {\displaystyle \phi =0\,} , then

x = ( λ λ 0 ) {\displaystyle x=\left(\lambda -\lambda _{0}\right)\,}
y = 0 {\displaystyle y=0\,}

Similarly, if λ = λ 0 {\displaystyle \lambda =\lambda _{0}\,} or ϕ = ± π / 2 {\displaystyle \phi =\pm \pi /2\,} , then

x = 0 {\displaystyle x=0\,}
y = ± π tan θ / 2 {\displaystyle y=\pm \pi \tan {\theta /2}}

In all cases, ϕ {\displaystyle \phi \,} is the latitude, λ {\displaystyle \lambda \,} is the longitude, and λ 0 {\displaystyle \lambda _{0}\,} is the central meridian of the projection.

Notes

  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

References

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


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