Azimuthal Equidistant


The most significant characteristic is that both distance and direction are accurate from the central point. This projection can accommodate all aspects: equatorial, polar, and oblique.

Illustration of Azimuthal Equidistant projection

Projection method

Planar—the world is projected onto a flat surface from any point on the globe. Although all aspects are possible, the one used most commonly is the polar aspect, in which all meridians and parallels are divided equally to maintain the equidistant property. Oblique aspects centered on a city are also common.

Point of tangency

A single point, usually the North or the South Pole, is defined by degrees of latitude and longitude.

Linear graticules

Polar—straight meridians are divided equally by concentric circles of latitude.

Equatorial—the equator and the projection's central meridian are linear and meet at a 90 degree angle.

Oblique—the central meridian is straight, but there are no 90 degree intersections except along the central meridian.



Except at the center, all shapes are distorted. Distortion increases from the center.


Distortion increases outward from the center point.


True directions from the center outward.


Distances for all aspects are accurate from the center point outward. For the polar aspect, the distances along the meridians are accurate, but there is a pattern of increasing distortion along the circles of latitude, outward from the center.


Usually limited to 90° from the center, although it can project the entire globe. Polar-aspect projections are best for regions within a 30° radius because there is only minimal distortion.

Scale distortion of the projection

Degrees from center

Percentage of scale distortion along parallels











Scale distortion of the projection

Uses and applications

Routes of air and sea navigation—these maps will focus on an important location as their central point and use an appropriate aspect.

If this projection is used on the entire globe, the immediate hemisphere can be recognized and resembles the Lambert Azimuthal projection. The outer hemisphere greatly distorts shapes and areas. In the extreme, a polar-aspect projection centered on the North Pole will represent the South Pole as its largest outermost circle. The function of this extreme projection is that, regardless of the conformal and area distortion, an accurate presentation of distance and direction from the center point is maintained.

Learn more about the Lambert Azimuthal projection



  • False Easting
  • False Northing
  • Central Meridian
  • Latitude of Origin

Azimuthal Equidistant Auxiliary Sphere (Desktop version 9.3 and later)

  • False Easting
  • False Northing
  • Central Meridian
  • Latitude of Origin
  • Auxiliary Sphere Type

The Auxiliary Sphere Type parameter accepts 0 (use semimajor axis or radius of the geographic coordinate system), 1 (use semiminor axis or radius), 2 (calculate and use authalic radius), or 3 (use authalic radius and convert geodetic latitudes to authalic latitudes).


  • Radius of the sphere of reference:
  • Longitude of center of projection
  • Latitude of center of projection
  • False Easting (meters)
  • False Northing (meters)

Supported on spheres only.


A geographic coordinate systems pdf file which contains lists of supported gcs and vcs.


A projected coordinate systems pdf file which contains lists of supported pcs.


A geographic transformations pdf file which contains lists of supported geographic and vertical transformations.

Related Topics