World Library  
Flag as Inappropriate
Email this Article


Article Id: WHEBN0000145381
Reproduction Date:

Title: Ellipsoid  
Author: World Heritage Encyclopedia
Language: English
Subject: Latitude, Map projection, Ellipse, Flattening, Ellipsoid method
Collection: Geometric Shapes, Quadrics, Surfaces
Publisher: World Heritage Encyclopedia


Tri-axial ellipsoid with distinct semi-axis lengths c>b>a
Tri-axial ellipsoid with distinct semi-axes a, b and c
Ellipsoids of revolution (spheroid) with a pair of equal semi-axes (a) and a distinct third semi-axis (c) which is an axis of symmetry. The ellipsoid is prolate (top) or oblate (bottom) as c is greater than or less than a.
Circular sections of an ellipsoid

An ellipsoid is a closed quadric surface that is a three-dimensional analogue of an ellipse. The standard equation of an ellipsoid centered at the origin of a Cartesian coordinate system and aligned with the axes is

{x^2 \over a^2}+{y^2 \over b^2}+{z^2 \over c^2}=1,

The points (a,0,0), (0,b,0) and (0,0,c) lie on the surface and the line segments from the origin to these points are called the semi-principal axes of length a, b, c. They correspond to the semi-major axis and semi-minor axis of the appropriate ellipses.

There are four distinct cases of which one is degenerate:

  • a>b>ctri-axial or (rarely) scalene ellipsoid;
  • a=b>coblate ellipsoid of revolution (oblate spheroid);
  • a=bprolate ellipsoid of revolution (prolate spheroid);
  • a=b=c — the degenerate case of a sphere;

Mathematical literature often uses 'ellipsoid' in place of 'tri-axial ellipsoid'. Scientific literature (particularly geodesy) often uses 'ellipsoid' in place of 'ellipsoid of revolution' and only applies the adjective 'tri-axial' when treating the general case. Older literature uses 'spheroid' in place of 'ellipsoid of revolution'.

Any planar cross section passing through the center of an ellipsoid forms an ellipse on its surface: this degenerates to a circle for sections normal to the symmetry axis of an ellipsoid of revolution (or all sections when the ellipsoid degenerates to a sphere.)


  • Generalised equations 1
  • Parameterization 2
  • Volume and surface area 3
    • Volume 3.1
    • Surface area 3.2
      • Approximate formula 3.2.1
  • Dynamical properties 4
  • Fluid properties 5
  • Equations in specific coordinate systems 6
    • Cartesian 6.1
    • Spherical 6.2
    • Cylindrical 6.3
  • See also 7
  • References 8
  • External links 9

Generalised equations

More generally, an arbitrarily oriented ellipsoid, centered at v, is defined by the solutions x to the equation

(\mathbf{x-v})^\mathrm{T}\! A\, (\mathbf{x-v}) = 1,

where A is a positive definite matrix and x, v are vectors.

The eigenvectors of A define the principal axes of the ellipsoid and the eigenvalues of A are the reciprocals of the squares of the semi-axes: a^{-2}, b^{-2} and c^{-2}.[1] An invertible linear transformation applied to a sphere produces an ellipsoid, which can be brought into the above standard form by a suitable rotation, a consequence of the polar decomposition (also, see spectral theorem). If the linear transformation is represented by a symmetric 3-by-3 matrix, then the eigenvectors of the matrix are orthogonal (due to the spectral theorem) and represent the directions of the axes of the ellipsoid: the lengths of the semiaxes are given by the eigenvalues. The singular value decomposition and polar decomposition are matrix decompositions closely related to these geometric observations.


The surface of the ellipsoid may be parameterized in several ways. One possible choice which singles out the 'z'-axis is:

\begin{align} x&=a\,\cos u\cos v,\\ y&=b\,\cos u\sin v,\\ z&=c\,\sin u;\end{align}\,\!
-{\pi}/{2}\leq u\leq+{\pi}/{2}, \qquad -\pi\leq v\leq+\pi.\!\,\!

The parameters may be interpreted as spherical coordinates. For constant u, that is on the ellipse which is the intercept with a constant z plane, v then plays the role of the eccentric anomaly for that ellipse. For constant v on a plane through the Oz axis the parameter u plays the same role for the ellipse of intersection. Two other similar parameterizations are possible, each with their own interpretations. Only on an ellipse of revolution can a unique definition of reduced latitude be made.

Volume and surface area


The volume of the internal part of the ellipsoid is

V= \frac{4}{3}\pi abc ,\!

Note that this equation reduces to that of the volume of a sphere when all three elliptic radii are equal, and to that of an oblate or prolate spheroid when two of them are equal.

The volume of an ellipsoid is two thirds the volume of a circumscribed elliptic cylinder.

The volumes of the maximum inscribed and minimum circumscribed boxes are respectively:

V_\max =\frac{8}{3\sqrt 3} abc, \qquad V_\min = 8abc.

The volume of an ellipse of dimension higher than 3 can be calculated using the dimensional constant given for the volume of a hypersphere. One can also define ellipsoids in higher dimensions, as the images of spheres under invertible linear transformations. The spectral theorem can again be used to obtain a standard equation akin to the one given above.

Surface area

The surface area of a general (tri-axial) ellipsoid is[2][3]

S=2\pi c^2+ \frac{2\pi ab}{\sin\phi} \left(E(\phi,k)\, \sin^2\phi + F(\phi,k)\, \cos^2\phi \right),
\cos\phi = \frac{c}{a}, \qquad k^2 =\frac{a^2(b^2-c^2)}{b^2(a^2-c^2)}, \qquad a\ge b \ge c,

and where F(φ,k) and E(φ,k) are incomplete elliptic integrals of the first and second kind respectively.[1]

The surface area of an ellipsoid of revolution (or spheroid) may be expressed in terms of elementary functions:

S_{\rm oblate} = 2\pi a^2\left(1+\frac{1-e^2}{e}\tanh^{-1}e\right) \quad\mbox{where}\quad e^2=1-\frac{c^2}{a^2}\quad(c
S_{\rm prolate} = 2\pi a^2\left(1+\frac{c}{ae}\sin^{-1}e\right) \quad\qquad\mbox{where}\;\quad e^2=1-\frac{a^2}{c^2}\quad(c>a),

which, as follows from basic trigonometric identities, are equivalent expressions (i.e. the formula for S_{\rm oblate} can be used to calculate the surface area of a prolate ellipsoid and vice versa). In both cases e may again be identified as the eccentricity of the ellipse formed by the cross section through the symmetry axis. (See ellipse). Derivations of these results may be found in standard sources, for example Mathworld.[4]

Approximate formula

S\approx 4\pi\!\left(\frac{ a^p b^p+a^p c^p+b^p c^p }{3}\right)^{1/p}.\,\!

Here p ≈ 1.6075 yields a relative error of at most 1.061%;[5] a value of p = 8/5 = 1.6 is optimal for nearly spherical ellipsoids, with a relative error of at most 1.178%.

In the "flat" limit of c much smaller than a, b, the area is approximately 2πab.

Dynamical properties

The mass of an ellipsoid of uniform density ρ is:

m = \rho V = \rho \frac{4}{3} \pi abc\,\!

The moments of inertia of an ellipsoid of uniform density are:

I_{\mathrm{xx}} = \frac{1}{5} m( b^2+c^2),\qquad I_{\mathrm{yy}} = \frac{1}{5} m(c^2+a^2),\qquad I_{\mathrm{zz}} = \frac{1}{5} m(a^2+b^2),
I_{\mathrm{xy}}= I_{\mathrm{yz}} = I_{\mathrm{zx}} =0.\,\!

For a=b=c these moments of inertia reduce to those for a sphere of uniform density.

Artist's conception of Haumea, a Jacobi-ellipsoid dwarf planet, with its two moons

Ellipsoids and cuboids rotate stably along their major or minor axes, but not along their median axis. This can be seen experimentally by throwing an eraser with some spin. In addition, moment of inertia considerations mean that rotation along the major axis is more easily perturbed than rotation along the minor axis.[6]

One practical effect of this is that scalene astronomical bodies such as Haumea generally rotate along their minor axes (as does Earth, which is merely oblate); in addition, because of tidal locking, moons in synchronous orbit such as Mimas orbit with their major axis aligned radially to their planet.

A relaxed ellipsoid, that is, one in hydrostatic equilibrium, has an oblateness a − c directly proportional to its mean density and mean radius. Ellipsoids with a differentiated interior—that is, a denser core than mantle—have a lower oblateness than a homogeneous body. Over all, the ratio (b–c)/(a−c) is approximately 0.25, though this drops for rapidly rotating bodies.[7]

The terminology typically used for bodies physically rotating on their minor axis -- not necessarily ellipsoids of revolution, in their mathematical construction -- and whose shape is determined by their gravitational field is Maclaurin spheroid (oblate spheroid) and Jacobi ellipsoid (scalene ellipsoid). At faster rotations, piriform or oviform shapes can be expected, but these are not stable.

Fluid properties

The ellipsoid is the most general shape for which it has been possible to calculate the

External links

  1. ^
  2. ^ F. W. J. Olver, D. W. Lozier, R. F. Boisvert, and C. W. Clark, editors, 2010, NIST Handbook of Mathematical Functions (Cambridge University Press), available on line at (see next reference).
  3. ^ NIST (National Institute of Standards and Technology) at
  4. ^ Prolate Spheroid at Mathworld
  5. ^ Final answers by Gerard P. Michon (2004-05-13). See Thomsen's formulas and Cantrell's comments.
  6. ^ Goldstein, H G (1980). Classical Mechanics, (2nd edition) Chapter 5.
  7. ^
  8. ^ Dusenbery, David B. (2009).Living at Micro Scale, Harvard University Press, Cambridge, Mass. ISBN 978-0-674-03116-6.


See also

{r^2 \cos^2\! \theta \over a^2}+{r^2 \sin^2\! \theta \over b^2}+{z^2 \over c^2}=1,


{r^2 \cos^2\! \theta\, \sin^2 \!\phi \over a^2}+{r^2 \sin^2 \!\theta\, \sin^2 \!\phi \over b^2}+{r^2 \cos^2\! \phi \over c^2}=1,


{x^2 \over a^2}+{y^2 \over b^2}+{z^2 \over c^2}=1,


Equations in specific coordinate systems


This article was sourced from Creative Commons Attribution-ShareAlike License; additional terms may apply. World Heritage Encyclopedia content is assembled from numerous content providers, Open Access Publishing, and in compliance with The Fair Access to Science and Technology Research Act (FASTR), Wikimedia Foundation, Inc., Public Library of Science, The Encyclopedia of Life, Open Book Publishers (OBP), PubMed, U.S. National Library of Medicine, National Center for Biotechnology Information, U.S. National Library of Medicine, National Institutes of Health (NIH), U.S. Department of Health & Human Services, and, which sources content from all federal, state, local, tribal, and territorial government publication portals (.gov, .mil, .edu). Funding for and content contributors is made possible from the U.S. Congress, E-Government Act of 2002.
Crowd sourced content that is contributed to World Heritage Encyclopedia is peer reviewed and edited by our editorial staff to ensure quality scholarly research articles.
By using this site, you agree to the Terms of Use and Privacy Policy. World Heritage Encyclopedia™ is a registered trademark of the World Public Library Association, a non-profit organization.

Copyright © World Library Foundation. All rights reserved. eBooks from Hawaii eBook Library are sponsored by the World Library Foundation,
a 501c(4) Member's Support Non-Profit Organization, and is NOT affiliated with any governmental agency or department.