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Azimuthal equidistant projection

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An azimuthal equidistant projection is a specific type of azimuthal map projection. It is a mathematical method used to flatten a sphere onto a plane. This projection is unique because it preserves two specific qualities from a single center point. First, all points on the map show the correct proportional distance from that center. Second, all points show the correct azimuth, which is the direction from the center. Because it preserves these two things, it is often called the exponential map on a sphere.

To understand how this works, you must first choose a center point on the globe. This point is defined by its latitude (φ) and longitude (λ). On the flat map, this point becomes the center of a circular projection. Every other point on the globe is then mapped based on its relationship to this center. All points along a specific azimuth will appear as a straight line coming from the center. The distance from the center to any other point is the arc length along a great circle. In a polar projection, the North or South Pole serves as the center. In this setup, all meridians, or lines of longitude, appear as straight lines.

Azimuthal equidistant projection with Tissot's indicatrix
Azimuthal equidistant projection with Tissot's indicatrix

The mathematical relationship between the globe and the map is quite precise. The distance from the center, known as ρ, is calculated using the arc length. The angle θ represents the azimuth angle from the vertical. When the North Pole is the center, the equations become much simpler. The latitude of the center becomes zero, and the longitude is treated as arbitrary. This allows mathematicians to use Cartesian coordinates to plot the points on a flat surface. These formulas ensure that the distance and direction remain accurate from the chosen origin.

History shows that humans have explored these concepts for centuries. While ancient Egyptians might have used similar ideas for star maps, the first written description is from the 11th century. It was recorded by the scholar al-Biruni. Later, Spanish and Portuguese mapmakers used polar azimuthal hemispheres to visualize ocean boundaries. This was helpful for the Treaty of Tordesillas in 1494. During the Renaissance, many famous cartographers used this system. Gerardus Mercator included it in his 1569 map to show the North Polar regions. In France and Russia, the system is often called the Postel projection. This honors Guillaume Postel, who used it for a map in 1581.

Azimuthal equidistant projection with Tissot's indicatrix
Azimuthal equidistant projection with Tissot's indicatrix

Every map projection has limits regarding distortion. On an azimuthal equidistant map, distortion depends on the distance from the center. If the distance is less than 10,000 kilometers, the distortions are minimal. When distances reach 10,000 to 20,000 kilometers, the distortions become moderate. However, distortions become severe when distances exceed 20,000 kilometers. Since the Earth's circumference is approximately 40,000 kilometers, the maximum possible distance is half that amount. If a map is centered on a point where the opposite side, or antipode, is on land, the map may look very strange. For example, a map centered on Taipei can cause South America to appear heavily distorted.

Azimuthal equidistant projection with Tissot's indicatrix
Azimuthal equidistant projection with Tissot's indicatrix

This projection has many practical applications in our modern world. It is very useful for terrestrial point-to-point communication. A radio operator can use the map to find the correct direction for an antenna. By finding the target location on the map, the operator determines the necessary azimuth angle. They can then use an electric rotator to point the antenna accurately. The map is most effective when it is centered near the operator's actual location. Additionally, these maps are used to show the range of ballistic missiles. By using concentric circles, a map can show how far a missile can travel from a starting point.

Azimuthal equidistant projection with Tissot's indicatrix
Azimuthal equidistant projection with Tissot's indicatrix

Beyond communication and military use, the projection appears in unexpected places. The flag of the United Nations uses a polar azimuthal equidistant projection. This design shows the world from a top-down view of the poles. Many modern star charts, known as planispheres, also use this polar version to map the sky. Interestingly, the projection has also been adopted by 21st-century Flat Earthers. They use it to represent a Flat Earth, where Antarctica appears as a ring around the edge. This shows how a single mathematical tool can be interpreted in very different ways.

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