Guyou hemisphere-in-a-square projection

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Guyou doubly periodic projection of the world.

The Guyou hemisphere-in-a-square projection is a conformal map projection for the hemisphere. It is an oblique aspect of the Peirce quincuncial projection.


The projection was developed by Émile Guyou of France in 1887.[1]

Formal description[edit]

The projection can be computed as an oblique aspect of the Peirce quincuncial projection by rotating the axis 45 degrees. It can also be computed by rotating the coordinates −45 degrees before computing the stereographic projection; this projection is then remapped into a square whose coordinates are then rotated 45 degrees.[2]

The projection is conformal except for the four corners of each hemisphere’s square. Like other conformal polygonal projections, the Guyou is a Schwarz-Christoffel mapping.


Its properties are very similar to those of the Peirce quincuncial:

  • Each hemisphere is represented as a square, the sphere as a rectangle of aspect ratio 2:1.
  • The part where the exaggeration of scale amounts to double that at the centre of each square is only 9% of the area of the sphere, against 13% for the Mercator and 50% for the stereographic[3]
  • The curvature of lines representing great circles is, in every case, very slight, over the greater part of their length.[3]
  • It is conformal everywhere except at the corners of the square that corresponds to each hemisphere, where two meridians change direction abruptly twice each; the Equator is represented by a horizontal line.
  • It can be tessellated in all directions.

Related projections[edit]

See also[edit]


  1. ^ Snyder, John P. (1993). Flattening the Earth. University of Chicago. ISBN 0-226-76746-9. 
  2. ^ L.P. Lee (1976). "Conformal Projections based on Elliptic Functions". Cartographica 13 (Monograph 16, supplement No. 1 to Canadian Cartographer). 
  3. ^ a b C.S. Peirce (December 1879). "A Quincuncial Projection of the Sphere". American Journal of Mathematics (The Johns Hopkins University Press) 2 (4): 394–396. doi:10.2307/2369491. JSTOR 2369491.