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examples/projections/misc
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Eckert IV
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=========
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+ The Eckert IV projection, presented by the German cartographer Max
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+ Eckert-Greiffendorff in 1906, is a pseudo-cylindrical equal-area projection. Central
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+ meridian and all parallels are straight lines; other meridians are equally spaced
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+ elliptical arcs. The scale is true along latitude 40°30’.
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+
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``Kf[central meridian]/width``: Give the optional central meridian (default is the
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center of the region) and the map width.
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"""
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Eckert VI
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=========
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+ The Eckert VI projections, presented by the German cartographer
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+ Max Eckert-Greiffendorff in 1906, is a pseudo-cylindrical equal-area projection.
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+ Central meridian and all parallels are straight lines; other meridians are equally
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+ spaced sinusoids. The scale is true along latitude 49°16’.
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+
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``Ks[central meridian]/width``: Give the optional central meridian (default is the
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center of the region) and the map width.
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"""
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Hammer
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======
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+ The equal-area Hammer projection, first presented by the German mathematician
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+ Ernst von Hammer in 1892, is also known as Hammer-Aitoff (the Aitoff projection looks
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+ similar, but is not equal-area). The border is an ellipse, equator and central
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+ meridian are straight lines, while other parallels and meridians are complex curves.
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+
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``H[central meridian]/width``: Give the optional central meridian (default is the center
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of the region) and the map width.
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"""
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Mollweide
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=========
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+ This pseudo-cylindrical, equal-area projection was developed by the German
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+ mathematician and astronomer Karl Brandan Mollweide in 1805. Parallels are unequally
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+ spaced straight lines with the meridians being equally spaced elliptical arcs. The
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+ scale is only true along latitudes 40°44’ north and south. The projection is used
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+ mainly for global maps showing data distributions. It is occasionally referenced under
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+ the name homalographic projection.
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+
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``W[central meridian]/width``: Give the optional central meridian (default is the center
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of the region) and the map width.
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"""
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Robinson
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========
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+ The Robinson projection, presented by the American geographer and cartographer
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+ Arthur H. Robinson in 1963, is a modified cylindrical projection that is neither
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+ conformal nor equal-area. Central meridian and all parallels are straight lines; other
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+ meridians are curved. It uses lookup tables rather than analytic expressions to make
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+ the world map “look” right 22. The scale is true along latitudes 38. The projection was
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+ originally developed for use by Rand McNally and is currently used by the
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+ National Geographic Society.
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+
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``N[central meridian]/width``: Give the optional central meridian (default is the center
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of the region) and the map width.
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"""
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Sinusoidal
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==========
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+ The sinusoidal projection is one of the oldest known projections, is equal-area, and
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+ has been used since the mid-16th century. It has also been called the
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+ “Equal-area Mercator” projection. The central meridian is a straight line; all other
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+ meridians are sinusoidal curves. Parallels are all equally spaced straight lines, with
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+ scale being true along all parallels (and central meridian).
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+
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``I[central meridian]/width``: Give the optional central meridian (default is the center
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of the region) and the map width.
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"""
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Van der Grinten
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===============
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+ The Van der Grinten projection, presented by Alphons J. van der Grinten in 1904, is
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+ neither equal-area nor conformal. Central meridian and Equator are straight lines;
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+ other meridians are arcs of circles. The scale is true along the Equator only. Its
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+ main use is to show the entire world enclosed in a circle.
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+
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``V[central meridian]/width``: Give the optional central meridian (default is the center
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of the region) and the map width.
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"""
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Winkel Tripel
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=============
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+ In 1921, the German mathematician Oswald Winkel a projection that was to strike a
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+ compromise between the properties of three elements (area, angle and distance). The
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+ German word “tripel” refers to this junction of where each of these elements are least
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+ distorted when plotting global maps. The projection was popularized when Bartholomew
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+ and Son started to use it in its world-renowned “The Times Atlas of the World” in the
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+ mid-20th century. In 1998, the National Geographic Society made the Winkel Tripel as
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+ its map projection of choice for global maps.
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+
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+ Naturally, this projection is neither conformal, nor equal-area. Central meridian and
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+ equator are straight lines; other parallels and meridians are curved. The projection is
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+ obtained by averaging the coordinates of the Equidistant Cylindrical and Aitoff
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+ (not Hammer-Aitoff) projections. The poles map into straight lines 0.4 times the
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+ length of equator.
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+
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``R[central meridian]/width``: Give the optional central meridian (default is the center
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of the region) and the map width.
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"""
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