The Werner projection is a pseudoconic equal-area map projection sometimes called the Stab-Werner or Stabius-Werner projection. Like other heart-shaped projections,[specify] it is also categorized as cordiform. Stab-Werner refers to two originators: Johannes Werner (1466–1528), a parish priest in Nuremberg, refined and promoted this projection that had been developed earlier by Johannes Stabius (Stab) of Vienna around 1500.
The projection is a limiting form of the Bonne projection, having its standard parallel at one of the poles (90°N/S).[1][2] Distances along each parallel and along the central meridian are correct, as are all distances from the north pole.
^Snyder, John P (1993), Flattening the Earth: Two Thousand Years of Map Projections, pp. 60–2, ISBN 0-226-76747-7.
^———————— (1987), "Map Projections—A Working Manual", Professional Paper, United States Geological Survey, pp. 138–0.
The Wernerprojection is a pseudoconic equal-area map projection sometimes called the Stab-Werner or Stabius-Wernerprojection. Like other heart-shaped...
Pole). The Bonne projection can be seen as an intermediate projection in the unwinding of a Wernerprojection into a Sinusoidal projection; an alternative...
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Different projections can be produced by altering the eccentricity of the arcs, making it vary between the sinusoidal projection and the Wernerprojection. For...
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(cordiform) projection map later developed further by Johannes Werner. It is called the Werner map projection, but also the Stabius-Werner or the Stab-Werner projection...
sinusoidal projection and the Bonne projection. The Wernerprojection places its standard parallel at the North Pole; a sinusoidal projection places its...
Bonne projection for continental maps. The Wernerprojection is only used today for instructional purposes and as a novelty. In this work, Werner also...
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those lines. Similar projections which wrap the east and west parts of the sinusoidal projection around the North Pole are the Werner and the intermediate...
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