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A spheroid is a quadric surface obtained by rotating an ellipse about one of its principal axes; in other words, an ellipsoid with two equal semi-diameters. If the ellipse is rotated about its major axis, the result is a prolate (elongated) spheroid, like a 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 its rotation, the Earth's shape is more like an oblate spheroid than a sphere. In cartography, in fact, the Earth is often assumed to be a standard oblate spheroid. In the current World Geodetic System model, the radius is approximately 6,378.137 km at the equator and 6,356.752 km at the poles (a difference of over 21 km).
EquationA spheroid centered at the origin and rotated about the z axis is defined by the implicit equation where a is the horizontal, transverse radius at the equator, and b is the vertical, conjugate radius.[1] Surface areaA prolate spheroid has surface area where An oblate spheroid has surface area
VolumeThe volume of a spheroid (of any kind) is CurvatureIf a spheroid is parameterized as where and its mean curvature is Both of these curvatures are always positive, so that every point on a spheroid is elliptic. See alsoReferencesExternal linksQuestions for article: spheroid mean curvature gaussian curvature, spheroid mean curvature gaussian curvature |
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