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Spherical Coordinates

A coordinate system based on a sphere, typically using latitude and longitude to specify locations on the Earth.

Spherical Coordinates

Define Spherical Coordinates

Three values—a radius and two angles—are used to represent points in three-dimensional space using spherical coordinates. Particularly helpful for places on or close to a sphere, such as Earth, is this system.


The definition of a point in the spherical coordinate system is as follows:


  • Radius (r) is the distance between the point and the origin, or the sphere's centre.

  • The polar angle, also known as the zenith angle, is the angle formed by the point and the positive vertical axis (θ).

  • Measured from a reference direction (often the x-axis), the azimuthal angle (φ) is the angle of rotation around the vertical axis.

Related Keywords

The spherical coordinate system represents a point in 3D space using its distance from the origin (r), the angle from the z-axis (\theta), and the angle in the xy-plane (\phi).

Spherical coordinates use radius, polar angle, and azimuthal angle to extend polar coordinates, which define a point by its distance from the origin and an angle, to three dimensions.

Cartesian to spherical conversion changes (x, y, z) into (r, \theta, \phi), where r = \sqrt{x^2 + y^2 + z^2}, \theta = \arccos(z/r), and \phi = \arctan2(y, x). It’s useful for problems with radial symmetry.

In astronomy, GPS, navigation, and map-making, spherical geometry is used to study figures on a sphere, model planets, and determine the shortest routes.

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