Azimuthal equidistant projection

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 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. == Mathematical definition ==

applied to the azimuthal equidistant projection: The orange spots on the map are all circular on the sphere. The more the circular spots appear stretched, the more the distortion created by the projection. 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, with referring to latitude and referring to longitude. 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. By this description, then, the point on the plane specified by will be projected to Cartesian coordinates: x = \rho \sin \theta, \qquad y = -\rho \cos \theta The relationship between the coordinates of the point on the globe, and its latitude and longitude coordinates is given by the equations: \begin{align} \cos \frac{\rho}{R} &= \sin \varphi_0 \sin \varphi + \cos \varphi_0 \cos \varphi \cos \left(\lambda - \lambda_0\right) \\ \tan \theta &= \frac{\cos \varphi \sin \left(\lambda - \lambda_0\right)}{\cos \varphi_0 \sin \varphi - \sin \varphi_0 \cos \varphi \cos \left(\lambda - \lambda_0\right)} \end{align} When the center point is the north pole, equals \pi/2 and is arbitrary, so it is most convenient to assign it the value of 0. This assignment significantly simplifies the equations for and to: \rho = R \left( \frac{\pi}{2} - \varphi \right), \qquad \theta = \lambda~~ == Limitation ==

With the circumference of the Earth being approximately , the maximum distance that can be displayed on an azimuthal equidistant projection map is half the circumference, or about . For distances less than distortions are minimal. For distances the distortions are moderate. Distortions become severe when the distances are greater than . 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 the antipode point smears into a large circle. This is shown in the example of two maps centered about Los Angeles, and Taipei. The antipode for Los Angeles is in the south Indian Ocean hence there is not much significant distortion of land masses for the Los Angeles centered map except for East Africa and Madagascar. On the other hand, Taipei's antipode is near the Argentina–Paraguay border, causing the Taipei centered map to severely distort South America. == Applications ==

Azimuthal equidistant projection maps can be useful in terrestrial point to point communication. This type of projection allows the operator to easily determine in which direction to point their directional antenna. The operator simply finds on the map the location of the target transmitter or receiver (i.e. the other antenna being communicated with) and uses the map to determine the azimuth angle needed to point the operator's antenna. The operator would use an electric rotator to point the antenna. The map can also be used in one way communication. For example if the operator is looking to receive signals from a distant radio station, this type of projection could help identify the direction of the distant radio station. In order for the map to be useful, the map should be centered as close as possible about the location of the operator's antenna. Azimuthal equidistant projection maps can also be useful to show ranges of ballistic missiles, as demonstrated by the map below. The map is centered on North Korea, along with concentric circle overlays showing the different ranges of the country's missiles. ==See also==