Azimuthal equidistant projection
A map projection preserving correct distances and azimuths from a central point.
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The azimuthal equidistant projection is an azimuthal map projection distinguished by two key properties: all points on the map are shown at proportionally correct distances from a chosen center point, and all points are depicted at the correct azimuth, or direction, from that center point. This makes it the exponential map on a sphere. A common application is the polar projection, where all meridians appear as straight lines radiating from the pole, and distances from the pole are accurately represented. The flag of the United Nations features a well-known example of this polar azimuthal equidistant projection.
History
While the projection may have been used by ancient Egyptians for star maps in holy texts, the earliest surviving written description comes from an 11th-century work by the scholar al-Biruni. The oldest known terrestrial map using this projection is a pair of hemispheres created by Glareanus around 1510. However, Spanish and Portuguese cartographers employed it even earlier, as polar azimuthal hemispheres conveniently visualized the boundary established by the Treaty of Tordesillas in 1494. The projection appears in many Renaissance maps; Gerardus Mercator used it for an inset of the north polar region on his famous 1569 world map, and a world map by ‛Ali b.
Ahmad al-Sharafi of Sfax from 1571 is another early example. In France and Russia, it is known as the "Postel projection" after Guillaume Postel, who used it for a map in 1581. Many modern star chart planispheres also utilize the polar azimuthal equidistant projection. In the 21st century, the projection has been adopted by Flat Earthers as a map of a flat Earth, citing its use on the UN flag and its depiction of Antarctica as a ring around the map's edge.
Mathematical definition
Mathematically, a central point on the globe is chosen; all distances and azimuths from this point to any other point are correct. This center projects to the center of a circular map.
Points along a given azimuth project along a straight line from the center, and the distance from the center to any projected point equals the great-circle arc length on the globe. A limitation is that the maximum displayable distance is half the Earth's circumference, roughly 20,000 km. Distortions are minimal for distances under 10,000 km, moderate from 10,000 to 15,000 km, and severe beyond 15,000 km.
Lore & Background
While it may have been used by ancient Egyptians for star maps in some holy books, the earliest text describing the azimuthal equidistant projection is an 11th-century work by al-Biruni. The earliest extant terrestrial map in this projection is a pair of hemispheres by Glareanus of about 1510. The projection was nevertheless used earlier by Spanish and Portuguese mapmakers, as polar azimuthal hemispheres made it easy to visualize the boundary agreed at the Treaty of Tordesillas of 1494.
The projection appears in many Renaissance maps, and Gerardus Mercator used it for an inset of the north polar regions in sheet 13 and legend 6 of his well-known 1569 map. Another early example of this system is the world map by ‛Ali b. Ahmad al-Sharafi of Sfax in 1571.
In France and Russia this projection is named "Postel projection" after Guillaume Postel, who used it for a map in 1581. Many modern star chart planispheres use the polar azimuthal equidistant projection. The polar azimuthal equidistant projection has also been adopted by 21st century Flat Earthers as a map of the Flat Earth, particularly due to its use in the UN flag and its depiction of Antarctica as a ring around the edge of the Earth.
Reader's Guide
A point on the globe is chosen as "the center" in the sense that mapped distances and azimuth directions from that point to any other point will be correct. That point will project to the center of a circular projection. All points along a given azimuth will project along a straight line from the center, and the angle that the line subtends from the vertical is the azimuth angle. The distance from the center point to another projected point is the arc length along a great circle between them on the globe.
When the center point is the north pole, the equations simplify. With the circumference of the Earth being approximately 40,000 km, the maximum distance that can be displayed on an azimuthal equidistant projection map is half the circumference, or about 20,000 km. For distances less than 10,000 km distortions are minimal. For distances 10,000 - 15,000 km the distortions are moderate.
Distortions become severe when the distances are greater than 15,000 km. If the azimuthal equidistant projection map is centered about a point whose antipodal point lies on land and the map is extended to the maximum distance of 20,000 km the antipode point smears into a large circle. Azimuthal equidistant projection maps can be useful in terrestrial point to point communication, allowing the operator to determine the azimuth direction for a directional antenna. They can also be useful to show ranges of ballistic missiles.
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Sources
Compiled from Wikipedia and the sources listed below. Text from Wikipedia is available under CC BY-SA 4.0; this entry is adapted from it.
- Wikipedia: Azimuthal equidistant projection (CC BY-SA 4.0).
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