Tobler hyperelliptical projection

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Short description: Pseudocylindrical equal-area map projection
Tobler hyperelliptical projection of the world; α = 0, γ = 1.18314, k = 2.5
The Tobler hyperelliptical projection with Tissot's indicatrix of deformation; α = 0, k = 3

The Tobler hyperelliptical projection is a family of equal-area pseudocylindrical projections that may be used for world maps. Waldo R. Tobler introduced the construction in 1973 as the hyperelliptical projection, now usually known as the Tobler hyperelliptical projection.[1]

Overview

As with any pseudocylindrical projection, in the projection's normal aspect,[2] the parallels of latitude are parallel, straight lines. Their spacing is calculated to provide the equal-area property. The projection blends the cylindrical equal-area projection, which has straight, vertical meridians, with meridians that follow a particular kind of curve known as superellipses[3] or Lamé curves or sometimes as hyperellipses. A hyperellipse is described by xk+yk=γk, where γ and k are free parameters. Tobler's hyperelliptical projection is given as: x=λ[α+(1−α)(γk−yk)1/kγ]αy=sin⁡φ+α−1γ∫0y(γk−zk)1/kdz where λ is the longitude, φ is the latitude, and α is the relative weight given to the cylindrical equal-area projection. For a purely cylindrical equal-area, α=1; for a projection with pure hyperellipses for meridians, α=0; and for weighted combinations, 0<α<1.

When α=0 and k=1 the projection degenerates to the Collignon projection; when α=0, k=2, and γ=4/π the projection becomes the Mollweide projection.[4] Tobler favored the parameterization shown with the top illustration; that is, α=0, k=2.5, and γ≈1.183136.

See also

References

  1. ↑ Snyder, John P. (1993). Flattening the Earth: 2000 Years of Map Projections. Chicago: University of Chicago Press. p. 220. 
  2. ↑ Mapthematics directory of map projections
  3. ↑ "Superellipse" in MathWorld encyclopedia
  4. ↑ Tobler, Waldo (1973). "The hyperelliptical and other new pseudocylindrical equal area map projections". Journal of Geophysical Research 78 (11): 1753–1759. doi:10.1029/JB078i011p01753. Bibcode: 1973JGR....78.1753T.