Peirce quincuncial projection

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Peirce quincuncial projection of the world. The red equator is a square whose corners are the only four points on the map at which the projection fails to be conformal. Peirce quincuncial projection SW 20W.JPG
Peirce quincuncial projection of the world. The red equator is a square whose corners are the only four points on the map at which the projection fails to be conformal.
The Peirce quincuncial projection with Tissot's indicatrix of deformation. Peirce Quincuncial with Tissot's Indicatrices of Distortion.svg
The Peirce quincuncial projection with Tissot's indicatrix of deformation.

The Peirce quincuncial projection [1] is a conformal map projection developed by Charles Sanders Peirce in 1879. The projection has the distinctive property that it can be tiled ad infinitum on the plane, with edge-crossings being completely smooth except for four singular points per tile. The projection has seen use in digital photography for portraying 360° views. The description quincuncial refers to the arrangement of four quadrants of the globe around the center hemisphere in an overall square pattern. Typically the projection is oriented such that the north pole lies at the center.

Contents

History

The maturation of complex analysis led to general techniques for conformal mapping, where points of a flat surface are handled as numbers on the complex plane. While working at the U.S. Coast and Geodetic Survey, the American philosopher Charles Sanders Peirce published his projection in 1879 (Peirce 1879), [2] having been inspired by H. A. Schwarz's 1869 conformal transformation of a circle onto a polygon of n sides (known as the Schwarz–Christoffel mapping). In the normal aspect, Peirce's projection presents the Northern Hemisphere in a square; the Southern Hemisphere is split into four isosceles triangles symmetrically surrounding the first one, akin to star-like projections. In effect, the whole map is a square, inspiring Peirce to call his projection quincuncial, after the arrangement of five items in a quincunx.

After Peirce presented his projection, two other cartographers developed similar projections of the hemisphere (or the whole sphere, after a suitable rearrangement) on a square: Guyou in 1887 and Adams in 1925. [3] The three projections are transversal versions of each other (see related projections below).

Formal description

The Peirce quincuncial projection is "formed by transforming the stereographic projection with a pole at infinity, by means of an elliptic function". [4] The Peirce quincuncial is really a projection of the hemisphere, but its tessellation properties (see below) permit its use for the entire sphere. The projection maps the interior of a circle onto the interior of a square by means of the Schwarz–Christoffel mapping, as follows: [5]

where sd is the ratio of two Jacobi elliptic functions: sn/dn; w is the mapped point on the plane as a complex number (w = x + iy); and r is the stereographic projection with a scale of 1/2 at the center. An elliptic integral of the first kind can be used to solve for w. The comma notation used for sd(u,k) means that 1/2 is the modulus for the elliptic function ratio, as opposed to the parameter [which would be written sd(u|m)] or the amplitude [which would be written sd(u\α)]. The mapping has a scale factor of 1/2 at the center, like the generating stereographic projection.

Properties

According to Peirce, his projection has the following properties (Peirce, 1879):

Tiled Peirce quincuncial maps

Tessellated version of the Peirce quincuncial map Peirce quincuncial projection SW 20W tiles.JPG
Tessellated version of the Peirce quincuncial map

The projection tessellates the plane; i.e., repeated copies can completely cover (tile) an arbitrary area, each copy's features exactly matching those of its neighbors. (See the example to the right). Furthermore, the four triangles of the second hemisphere of Peirce quincuncial projection can be rearranged as another square that is placed next to the square that corresponds to the first hemisphere, resulting in a rectangle with aspect ratio of 2:1; this arrangement is equivalent to the transverse aspect of the Guyou hemisphere-in-a-square projection. [6]

Known uses

Using the Peirce quincuncial projection to present a spherical panorama. PeircePanorama2007.jpg
Using the Peirce quincuncial projection to present a spherical panorama.

Like many other projections based upon complex numbers, the Peirce quincuncial has been rarely used for geographic purposes. One of the few recorded cases is in 1946, when it was used by the U.S. Coast and Geodetic Survey world map of air routes. [6] It has been used recently to present spherical panoramas for practical as well as aesthetic purposes, where it can present the entire sphere with most areas being recognizable. [7]

In transverse aspect, one hemisphere becomes the Adams hemisphere-in-a-square projection (the pole is placed at the corner of the square). Its four singularities are at the North Pole, the South Pole, on the equator at 25°W, and on the equator at 155°E, in the Arctic, Atlantic, and Pacific oceans, and in Antarctica. [8] That great circle divides the traditional Western and Eastern hemispheres.

In oblique aspect (45 degrees) of one hemisphere becomes the Guyou hemisphere-in-a-square projection (the pole is placed in the middle of the edge of the square). Its four singularities are at 45 degrees north and south latitude on the great circle composed of the 20°W meridian and the 160°E meridians, in the Atlantic and Pacific oceans. [8] That great circle divides the traditional western and eastern hemispheres.

See also

Related Research Articles

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Gnomonic projection map projection

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Universal polar stereographic coordinate system coordinate system

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Guyou hemisphere-in-a-square projection

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.

Adams hemisphere-in-a-square projection

The Adams hemisphere-in-a-square is a conformal map projection for a hemisphere. It is a transverse version of the Peirce quincuncial projection, and is named after American cartographer Oscar Sherman Adams, who published it in 1925. When it is used to represent the entire sphere it is known as the Adams doubly periodic projection. Like many conformal projections, conformality fails at certain points, in this case at the four corners.

In cartography, a conformal map projection is one in which every angle between two curves that cross each other on Earth is preserved in the image of the projection, i.e. the projection is a conformal map in the mathematical sense. For example, if two roads cross each other at a 39° angle, then their images on a map with a conformal projection cross at a 39° angle.

Riemann sphere model of the extended complex plane plus a point at infinity

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Stereographic projection in cartography

The stereographic projection, also known as the planisphere projection or the azimuthal conformal projection, is a conformal map projection whose use dates back to antiquity. Like the orthographic projection and gnomonic projection, the stereographic projection is an azimuthal projection, and when on a sphere, also a perspective projection.

References

  1. A Quincuncial Projection of the Sphere by Charles Sanders Peirce. 1890.
    I. Frischauf. Bemerkungen zu C. S. Peirce Quincuncial Projection. (Tr., Comments on C. S. Peirce Quincuncial Projection.)
    A Treatise on Projections by Thomas Craig. U.S. Government Printing Office, 1882. p 132
    Science, Volume 11. Moses King, 1900. p 186
  2. (Lee, 1976) gives 1877 as the year in which the projection was conceived, citing "US Coast Survey Report for the Year Ending with June 1877", 191192.
  3. Lee, L. P. (1976). "Conformal Projections Based on Jacobian Elliptic Functions". Cartographica. 13: 67–101. doi:10.3138/X687-1574-4325-WM62.CS1 maint: ref=harv (link)
  4. Peirce, C.S. (1879). "A quincuncial projection of the sphere". American Journal of Mathematics. 2 (4): 394–396. doi:10.2307/2369491. JSTOR   2369491.
  5. Lee, L.P. (1976). Conformal Projections Based on Elliptic Functions. Cartographica. pp. 67–69.
  6. 1 2 Snyder, John P. (1989). An Album of Map Projections, Professional Paper 1453 (PDF). US Geological Survey. pp. 190, 236.
  7. German, Daniel; d'Angelo, Pablo; Gross, Michael; Postle, Bruno (June 2007). "New Methods to Project Panoramas for Practical and Aesthetic Purposes". Proceedings of Computational Aesthetics 2007. Banff: Eurographics. pp. 15–22.
  8. 1 2 Carlos A. Furuti. Map Projections:Conformal Projections.

Further reading