Cassini projection

Cassini projection of the world

Cassini projection of the world modeled as a highly oblated ellipsoid with flattening 1:2 (= eccentricy ^√3⁄₂)

The Cassini projection is a map projection described by César-François Cassini de Thury in 1745.^[1] It is the transverse aspect of the equirectangular projection, in that the globe is first rotated so the central meridian becomes the "equator", and then the normal equirectangular projection is applied. Considering the earth as a sphere, the projection is composed of these operations:

$x = \arcsin(\cos(\varphi)\sin(\lambda))\,$

$y = \arctan\left(\frac{\tan(\varphi)}{\cos(\lambda)}\right)$

where λ is the longitude from the central meridian and φ is the latitude. When programming these equations, the inverse tangent function used is actually the atan2 function, with the first argument sin(φ) and the second cos(φ)cos(λ).

In practice, the projection has always been applied to models of the earth as an ellipsoid, which greatly complicates the mathematical development but is suitable for surveying. Nevertheless the use of the Cassini projection has largely been superseded by the Transverse Mercator projection, at least with central mapping agencies.

Distortions

Areas along the central meridian, and at right angles to it, are not distorted. Elsewhere, the distortion is largely in a north-south direction, and varies by the square of the distance from the central meridian. As such, the greater the longitudinal extent of the area, the worse the distortion becomes.

Due to this, the Cassini projection works best on long, narrow areas, and worst on wide areas.

See also

• Cassini Grid

References

1. Flattening the Earth: Two Thousand Years of Map Projections, John P. Snyder, 1993, pp. 74–76, ISBN 0-226-76747-7.

External links

• Media related to Cassini projection at Wikimedia Commons
• Table of examples and properties of all common projections, from radicalcartography.net
• Ordnance Survey GeoFacts on the Cassini Projection