An ellipsoid is a closed, convex surface in three dimensions that generalizes the circle and the ellipse. In its standard centered form it can be written as x²/a² + y²/b² + z²/c² = 1, where a, b and c are the semi-axes along three mutually perpendicular principal directions. When a = b = c the shape is a sphere; when two axes are equal it is a spheroid (a stretched or flattened sphere) often compared to a rugby ball. The planar analogue of an ellipsoid is the ellipse.

Mathematical description and properties

Algebraically, an ellipsoid is a level set of a positive definite quadratic form: {x in R^3 : x^T A x = 1} for a symmetric positive definite matrix A. Equivalently it is the image of the unit sphere under an invertible linear map, which explains many of its geometric properties. Ellipsoids are strictly convex, centrally symmetric, and every planar cross-section is an ellipse (or a circle in special cases).

Types and special cases

  • Sphere: a = b = c.
  • Spheroid: a = b ≠ c. If c < a it is oblate (flattened at the poles); if c > a it is prolate (stretched) — see oblate spheroid.
  • Triaxial ellipsoid: a, b, c all distinct.

Volume is simple: V = (4/3)πabc. Surface area has no elementary closed form in the general triaxial case and is expressed using elliptic integrals, though formulas simplify for spheres and spheroids.

History and geodetic importance

Ellipsoids have long been used to model planetary shapes. The Earth is approximately an oblate spheroid — slightly wider at the equator than pole-to-pole — and geodesists use an idealized reference ellipsoid to perform map projections and coordinate computations because it simplifies mathematics compared with the irregular geoid. Classical scientific work on planetary flattening dates back to Newton and later refinements in surveying and astronomy.

Applications and notable facts

  • Geodesy and cartography: reference surfaces and map projections for the Earth and other bodies.
  • Linear algebra and statistics: covariance matrices define confidence ellipsoids used in multivariate analysis and principal component analysis.
  • Mechanics and optics: inertia ellipsoids describe mass distribution; mirror and refractive designs use confocal ellipsoids for focus properties.
  • Computer graphics and collision detection: ellipsoids serve as simple bounding volumes and are easily transformed by affine maps.

Because any ellipsoid is an affine transform of a sphere, many problems reduce to a spherical case by applying the inverse transform. Intersections of ellipsoids with planes produce ellipses, and the study of focal, confocal, and conjugate properties of ellipsoids connects geometry with differential equations and classical mechanics.