||It has been suggested that Oblate spheroid and Prolate spheroid be merged into this article. (Discuss) Proposed since June 2014.|
|oblate spheroid||prolate spheroid|
If the ellipse is rotated about its major axis, the result is a prolate (elongated) spheroid, like an American football or rugby ball. If the ellipse is rotated about its minor axis, the result is an oblate (flattened) spheroid, like a lentil. If the generating ellipse is a circle, the result is a sphere.
Because of the combined effects of gravitation and rotation, the Earth's shape is roughly that of a sphere slightly flattened in the direction of its axis. For that reason, in cartography the Earth is often approximated by an oblate spheroid instead of a sphere. The current World Geodetic System model uses a spheroid whose radius is 6,378.137 km at the equator and 6,356.752 km at the poles.
The word spheroid originally meant an approximately spherical body, admitting irregularities even beyond the bi- or tri-axial ellipsoidal shape, and that is how it is used in some older papers on geodesy (for example, referring to truncated spherical harmonic expansions of the Earth). In case there is risk of confusion, it is beneficial to state for clarity the one definition intended.
The equation of a tri-axial ellipsoid centred at the origin with semi-axes a,b, c aligned along the coordinate axes is
The equation of a spheroid with Oz as the symmetry axis is given by setting a=b:
The semi-axis a is the equatorial radius of the spheroid, and c is the distance from centre to pole along the symmetry axis. There are two possible cases:
- c < a : oblate spheroid
- c > a : prolate spheroid
The case of a=c reduces to a sphere.
An oblate spheroid with c < a has surface area
The oblate spheroid is generated by rotation about the Oz axis of an ellipse with semi-major axis a and semi-minor axis c, therefore e may be identified as the eccentricity. (See ellipse). A derivation of this result may be found at.
A prolate spheroid with c > a has surface area
The prolate spheroid is generated by rotation about the Oz axis of an ellipse with semi-major axis c and semi-minor axis a, therefore e may again be identified as the eccentricity. (See ellipse). A derivation of this result may be found at.
These formulas are identical in the sense that the formula for can be used to calculate the surface area of a prolate spheroid and vice versa. However, e then becomes imaginary and can no longer directly be identified with the eccentricity. Both of these results may be cast into many other forms using standard mathematical identities and relations between parameters of the ellipse.
The volume inside a spheroid (of any kind) is . If A=2a is the equatorial diameter, and C=2c is the polar diameter, the volume is .
If a spheroid is parameterized as
and its mean curvature is
Both of these curvatures are always positive, so that every point on a spheroid is elliptic.