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Other Interesting Projections

Countless projections were devised in centuries of map-making. Many designs cannot be readily classified in the main groups (azimuthal, cylindrical, pseudocylindrical, conic or pseudoconic), even though their design is similar or derived.
A large number of projections whose graticule lines are circles or derived conic curves with different radii and centers are called polyconic (not to be confused with the particular group of polyconic projections). This is a broad and artificial category comprising otherwise unrelated projections.

Projections by Van der Grinten

Van der Grinten I map Van der Grinten III map
Van der Grinten's first projection (I) Modified van der Grinten's projection (III)
An American, Alphons J. van der Grinten published in 1904 and 1905 two projections, the first one devised as early as 1898.  Both were designed for the equatorial aspect, with straight Equator and central meridian; all other parallels and meridians were circular arcs, with nonconcentric meridians regularly spaced along the Equator.

Bludau proposed two modifications to the first version; the four designs soon came to be collectively (and confusingly) called "van der Grinten" projections:

  1. the first original projection, bounded by a circle
  2. Bludau's modification of I, with parallels crossing meridians at right angles
  3. Bludau's modification of I, with straight, horizontal parallels
  4. the second original projection, bounded by two identical circles with centers spaced 1.2 radii apart
Van der Grinten's proposals are examples of conventional designs, derived not from a perspective process but from an arbitrary geometric construction on the map plane. They are neither equal-area nor conformal (despite a superficial resemblance to projections by Lagrange, Eisenlohr and August), but intended to "look right", in the sense of conveying the notion of a round Earth without departing too much from Mercator's familiar shapes.
Van der Grinten IV map
Van der Grinten's second projection (IV)

The best known of all four, van der Grinten's I, also known simply as the Grinten projection, was widely used, especially after its choice for reference world maps by the National Geographic Society from 1922 to 1988. Of the others, only the III variant saw limited use.
Although the poles can be included in the map, areal distortion is large at high latitudes, thus most van der Grinten maps are clipped near parallels 80°N and 80°S.

Globular Projections by Maurer

Maurer's full-globular map
Maurer's "full-globular" map
The ancient group of globular projections includes circular arcs for both meridians and parallels, and maps ordinarily limited to a single hemisphere.
H. Maurer presented in 1922 three conventional projections resembling globular features.  The "full-globular" projection has meridians spaced like in van der Grinten's IV projection; parallels are equally spaced along the boundary meridians, and both the central meridian and the Equator have constant scale.  Each boundary meridian spans half the limiting circle, thus the whole world is set resembling a double-edged ax.
His two other globular proposals are called "all-globular" and "apparent-globular".

Orthoapsidal Projections

Beginning in 1943, the notable cartography teacher and author Erwin Raisz created a series of orthoapsidal projections mapping the sphere onto intermediary surfaces.  However, instead of "unrolled" like in cylindrical or conic maps, each surface is then projected orthographically onto the final plane.

Armadillo map in conventional form
Orthoapsidal ("Armadillo") map on part of a toroidal surface; tilt angle 20°, central meridian 10°E. Raisz's original map extended the eastern and western edges, with parallels spanning about 410° in order to avoid splitting Alaska and Siberia.

In the best-known orthoapsidal projection, called Armadillo (since it vaguely resembles the curling armored mammal), the sphere is mapped onto 1/4 of a degenerate torus with radii 1 and 1, which resembles a doughnut with a zero-sized hole. Parallels and meridians are equidistant circular arcs on the torus, but nonequidistant elliptical arcs in the final map.

Development of the Armadillo projection: the sphere is mapped to the region resembling half of a car tire, and that region to the blue projection plane

In the conventional form of the Armadillo map, Raisz preferred 10°E as the central meridian; the torus is then tilted 20 degrees and orthographically flattened onto the projection plane. Southern regions like Patagonia, New Zealand and Antarctica are hidden from view, and sometimes presented separately.

Orthoapsidal map on ellipsoid
Orthoapsidal map on a half-ellipsoid, eccentricity 1.75, tilt angle 20°; central meridian 10°E

Raisz also developed a map on one half of an oblate ellipsoid of rotation; the intermediate process is roughly a three-dimensional analogue of that applied by Aitoff to the azimuthal equidistant projection.

Another surface employed by Raisz was one half of a tilted hyperboloid of rotation of two sheets; in this case, a North polar map was interrupted in four identical lobes, resembling Maurer's S231 projection and, different from other orthoapsidal designs, showing the whole world. As drawn by Richard Edes Harrison, this projection was prominently featured in the cover of Scientific American 233(5); it is interrupted (at 60°E, 150°E, 120°W and 30°W) south of, apparently, 10°N. Harrison, known for his innovative and detailed maps, is quoted as characterizing it as "the most elegant of all world maps".

Orthoapsidal maps are neither conformal nor equal-area; parallels and meridians do not necessarily hold properties (like equidistance) of the intermediary surface.

Projections by Arden-Close

Arden-Close map of Eastern
  Hemisphere Arden-Close map extended to whole world
Arden-Close map of Eastern hemisphere, central meridian 70°E Variant Arden-Close map of whole world
Charles F. Arden-Close designed some map projections by averaging; his best-known (1943) is a simple arithmetical mean of one hemisphere of an equatorial equal-area cylindrical map with its transverse aspect, the Equator in one map coinciding with the central meridian in the other. Shaped like a square with circular corners, the result is neither conformal nor equal-area.
Doubling coordinate values, the method can be easily extended in order to show the whole world.

Work in Progress



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