The Bottomley map projection is a pseudoconical equal area map projection defined as:
where
and àis the latitude, û is the longitude from the central meridian, and ÃÂ<sub>1</sub> is the given parallel of the projection which determines its shape, all in radians.
The inverse projection is then given by:
where
Parallels (i.e. lines of latitude) are concentric elliptical arcs of constant eccentricity equal to cos ÃÂ<sub>1</sub>, centred on the North Pole. On the central meridian, shapes are not distorted, but elsewhere they are. Different projections can be produced by altering the eccentricity of the arcs, making it vary between the sinusoidal projection and the Werner projection. For larger values of ÃÂ<sub>1</sub>, it produces a heart shape.
It was introduced by Henry Bottomley as an alternative to the Bonne projection to reduce the extent of extreme distortion at the edges and give a more satisfying overall shape.