An ellipsoid is a surface that can be obtained from a sphere by deforming it by means of directional scalings, or more generally, of an affine transformation.
An ellipsoid is a quadric surface; that is, a surface that may be defined as the zero set of a polynomial of degree two in three variables. Among quadric surfaces, an ellipsoid is characterized by either of the two following properties. Every planar cross section is either an ellipse, or is empty, or is reduced to a single point (this explains the name, meaning "ellipse-like"). It is Bounded set, which means that it may be enclosed in a sufficiently large sphere.
An ellipsoid has three pairwise perpendicular axes of symmetry which intersect at a Central symmetry, called the center of the ellipsoid. The that are delimited on the axes of symmetry by the ellipsoid are called the principal axes, or simply axes of the ellipsoid. If the three axes have different lengths, the figure is a triaxial ellipsoid (rarely scalene ellipsoid), and the axes are uniquely defined.
If two of the axes have the same length, then the ellipsoid is an ellipsoid of revolution, also called a spheroid. In this case, the ellipsoid is invariant under a rotation around the third axis, and there are thus infinitely many ways of choosing the two perpendicular axes of the same length. In the case of two axes being the same length:
If the three axes have the same length, the ellipsoid is a sphere.
The points , and lie on the surface. The line segments from the origin to these points are called the principal semi-axes of the ellipsoid, because are half the length of the principal axes. They correspond to the semi-major axis and semi-minor axis of an ellipse.
In spherical coordinate system for which , the general ellipsoid is defined as:
where is the polar angle and is the azimuthal angle.
When , the ellipsoid is a sphere.
When , the ellipsoid is a spheroid or ellipsoid of revolution. In particular, if , it is an oblate spheroid; if , it is a prolate spheroid.
x &= a\sin\theta\cos\varphi,\\
y &= b\sin\theta\sin\varphi,\\
z &= c\cos\theta,
\end{align}\,\!
where
0 \le \theta \le \pi,\qquad
0 \le \varphi < 2\pi.
These parameters may be interpreted as spherical coordinates, where is the polar angle and is the azimuth angle of the point of the ellipsoid..
Measuring from the equator rather than a pole,
x &= a\cos\theta\cos\lambda,\\
y &= b\cos\theta\sin\lambda,\\
z &= c\sin\theta,
\end{align}\,\!
where
-\tfrac{\pi}2 \le \theta \le \tfrac{\pi}2,\qquad
0 \le \lambda < 2\pi,
is the [[reduced latitude]], parametric latitude, or eccentric anomaly and is azimuth or longitude.
Measuring angles directly to the surface of the ellipsoid, not to the circumscribed sphere,
x \\ y \\ z
\end{bmatrix} =
R \begin{bmatrix}
\cos\gamma\cos\lambda\\
\cos\gamma\sin\lambda\\
\sin\gamma
\end{bmatrix}
\,\!
where
R ={} &\frac{abc}{\sqrt{c^2 \left(b^2\cos^2\lambda + a^2\sin^2\lambda\right) \cos^2\gamma
+ a^2 b^2\sin^2\gamma}}, \\[3pt]
&-\tfrac{\pi}2 \le \gamma \le \tfrac{\pi}2,\qquad
0 \le \lambda < 2\pi.
\end{align}
would be geocentric latitude on the Earth, and is longitude. These are true spherical coordinates with the origin at the center of the ellipsoid.
In geodesy, the geodetic latitude is most commonly used, as the angle between the vertical and the equatorial plane, defined for a biaxial ellipsoid. For a more general triaxial ellipsoid, see ellipsoidal latitude.
The volume of an ellipsoid is the volume of a circumscribed elliptic cylinder, and the volume of the circumscribed box. The volumes of the inscribed and circumscribed boxes are respectively:
V_\text{inscribed} = \frac{8}{3\sqrt{3}} abc,\qquad
V_\text{circumscribed} = 8abc.
where
\cos(\varphi) = \frac{c}{a},\qquad
k^2 = \frac{a^2\left(b^2 - c^2\right)}{b^2\left(a^2 - c^2\right)},\qquad
a \ge b \ge c,
and where and are incomplete elliptic integrals of the first and second kind respectively.
The surface area of this general ellipsoid can also be expressed in terms of , one of the Carlson symmetric forms of elliptic integrals:
Simplifying the above formula using properties of , this can also be expressed in terms of the volume of the ellipsoid :
Unlike the expression with and , the equations in terms of do not depend on the choice of an order on , , and .
The surface area of an ellipsoid of revolution (or spheroid) may be expressed in terms of elementary functions:
S_\text{oblate} = 2\pi a^2\left(1 + \frac{c^2}{ea^2} \operatorname{artanh}e\right),
\qquad\text{where }e^2 = 1 - \frac{c^2}{a^2}\text{ and }(c < a),
or
S_\text{oblate} = 2\pi a^2\left(1 + \frac{1 - e^2}{e} \operatorname{artanh}e\right)
or
and
S_\text{prolate} = 2\pi a^2\left(1 + \frac{c}{ae} \arcsin e\right)
\qquad\text{where } e^2 = 1 - \frac{a^2}{c^2}\text{ and } (c > a),
which, as follows from basic trigonometric identities, are equivalent expressions (i.e. the formula for can be used to calculate the surface area of a prolate ellipsoid and vice versa). In both cases 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.
Here yields a relative error of at most 1.061%; Final answers by Gerard P. Michon (2004-05-13). See Thomsen's formulas and Cantrell's comments. a value of is optimal for nearly spherical ellipsoids, with a relative error of at most 1.178%.
In the "flat" limit of much smaller than and , the area is approximately , equivalent to .
Wanted: Three vectors (center) and , (conjugate vectors), such that the ellipse can be represented by the parametric equation
Solution: The scaling transforms the ellipsoid onto the unit sphere and the given plane onto the plane with equation
Where (i.e. the plane is horizontal), let
Where , let
In any case, the vectors are orthogonal, parallel to the intersection plane and have length (radius of the circle). Hence the intersection circle can be described by the parametric equation
The reverse scaling (see above) transforms the unit sphere back to the ellipsoid and the vectors are mapped onto vectors , which were wanted for the parametric representation of the intersection ellipse.
How to find the vertices and semi-axes of the ellipse is described in ellipse.
Example: The diagrams show an ellipsoid with the semi-axes which is cut by the plane .
A pins-and-string construction of an ellipsoid of revolution is given by the pins-and-string construction of the rotated ellipse.
The construction of points of a triaxial ellipsoid is more complicated. First ideas are due to the Scottish physicist J. C. Maxwell (1868). W. Böhm: Die FadenKonstruktion der Flächen zweiter Ordnung, Mathemat. Nachrichten 13, 1955, S. 151 Main investigations and the extension to quadrics was done by the German mathematician O. Staude in 1882, 1886 and 1898.Staude, O.: Ueber Fadenconstructionen des Ellipsoides. Math. Ann. 20, 147–184 (1882) Staude, O.: Ueber neue Focaleigenschaften der Flächen 2. Grades. Math. Ann. 27, 253–271 (1886). Staude, O.: Die algebraischen Grundlagen der Focaleigenschaften der Flächen 2. Ordnung Math. Ann. 50, 398 - 428 (1898). A description of the pins-and-string construction of ellipsoids and hyperboloids is contained in the book Geometry and the Imagination by David Hilbert & Cohn-Vossen.D. Hilbert & S Cohn-Vossen: Geometry and the imagination, Chelsea New York, 1952, , p. 20
&\frac{x^2}{r_x^2} + \frac{y^2}{r_y^2} + \frac{z^2}{r_z^2} = 1 \\
&r_x = \tfrac{1}{2}(l - a + c), \quad
r_y = {\textstyle \sqrt{r^2_x - c^2}}, \quad
r_z = {\textstyle \sqrt{r^2_x - a^2}}.
\end{align}
The lower part of the diagram shows that and are the foci of the ellipse in the -plane, too. Hence, it is confocal to the given ellipse and the length of the string is . Solving for yields ; furthermore .
From the upper diagram we see that and are the foci of the ellipse section of the ellipsoid in the -plane and that .
\overline r_y^2 = r_y^2 - \lambda, \quad
\overline r_z^2 = r_z^2 - \lambda
then from the equations of
r_x^2 - r_z^2 = a^2, \quad
r_y^2 - r_z^2 = a^2 - c^2 = b^2
one finds, that the corresponding focal conics used for the pins-and-string construction have the same semi-axes as ellipsoid . Therefore (analogously to the foci of an ellipse) one considers the focal conics of a triaxial ellipsoid as the (infinite many) foci and calls them the focal curves of the ellipsoid.O. Hesse: Analytische Geometrie des Raumes, Teubner, Leipzig 1861, p. 287
The converse statement is true, too: if one chooses a second string of length and defines
One can also define a hyperellipsoid as the image of a sphere under an invertible affine transformation. The spectral theorem can again be used to obtain a standard equation of the form
The volume of an -dimensional hyperellipsoid can be obtained by replacing by the product of the semi-axes in the formula for the volume of a hypersphere:
The of are the principal axes of the ellipsoid, and the of are the reciprocals of the squares of the semi-axes (in three dimensions these are , and ). pp. 17–18. In particular:
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 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 semi-axes are computed from the eigenvalues. The singular value decomposition and polar decomposition are matrix decompositions closely related to these geometric observations.
For every positive definite matrix , there exists a unique positive definite matrix denoted , such that this notation is motivated by the fact that this matrix can be seen as the "positive square root" of The ellipsoid defined by can also be presented as
where S( 0,1) is the unit sphere around the origin.
An affine transformation can be represented by a translation with a vector and a regular 3 × 3 matrix :
where are the column vectors of matrix .
A parametric representation of an ellipsoid in general position can be obtained by the parametric representation of a unit sphere (see above) and an affine transformation:
If the vectors form an orthogonal system, the six points with vectors are the vertices of the ellipsoid and are the semi-principal axes.
A surface normal vector at point is
For any ellipsoid there exists an Implicit surface . If for simplicity the center of the ellipsoid is the origin, , the following equation describes the ellipsoid above: Computerunterstützte Darstellende und Konstruktive Geometrie. Uni Darmstadt (PDF; 3,4 MB), S. 88.
The moments of inertia of an ellipsoid of uniform density are
I_\mathrm{xx} &= \tfrac{1}{5}m\left(b^2 + c^2\right), &
I_\mathrm{yy} &= \tfrac{1}{5}m\left(c^2 + a^2\right), &
I_\mathrm{zz} &= \tfrac{1}{5}m\left(a^2 + b^2\right), \\[3pt]
I_\mathrm{xy} &= I_\mathrm{yz} = I_\mathrm{zx} = 0.
\end{align}
For these moments of inertia reduce to those for a sphere of uniform density.
Ellipsoids and 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.Goldstein, H G (1980). Classical Mechanics, (2nd edition) Chapter 5.
One practical effect of this is that scalene astronomical bodies such as generally rotate along their minor axes (as does Earth, which is merely oblate spheroid); in addition, because of tidal locking, moons in synchronous orbit such as Mimas orbit with their major axis aligned radially to their planet.
A spinning body of homogeneous self-gravitating fluid will assume the form of either a Maclaurin spheroid (oblate spheroid) or Jacobi ellipsoid (scalene ellipsoid) when in hydrostatic equilibrium, and for moderate rates of rotation. At faster rotations, non-ellipsoidal piriform or oviform shapes can be expected, but these are not stable.
where is a scale factor, is an -dimensional random vector with median vector (which is also the mean vector if the latter exists), is a positive definite matrix which is proportional to the covariance matrix if the latter exists, and is a function mapping from the non-negative reals to the non-negative reals giving a finite area under the curve.Frahm, G., Junker, M., & Szimayer, A. (2003). Elliptical copulas: applicability and limitations. Statistics & Probability Letters, 63(3), 275–286. The multivariate normal distribution is the special case in which for quadratic form .
Thus the density function is a scalar-to-scalar transformation of a quadric expression. Moreover, the equation for any contour line states that the quadric expression equals some constant specific to that value of the density, and the iso-density surface is an ellipsoid.
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