Construct · 3 fields · 3 citations
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In rigid-body mechanics the inertia ellipsoid (Poinsot's ellipsoid) is the quadric surface whose radius in any direction encodes the body's moment of inertia about an axis in that direction; its principal axes are the body's principal axes of inertia. Poinsot's construction then pictures torque-free rotation as this ellipsoid rolling without slipping on a fixed plane. Goldstein, Poole, and Safko's Classical mechanics develops both the ellipsoid and the construction. The referent is a quadric that represents how a body's rotational inertia is distributed in space.[1]
In multivariate statistics a confidence (or concentration) ellipsoid is the ellipsoidal region in parameter space that, at a chosen confidence level, is expected to contain the true mean vector. Its centre is the sample mean, while its orientation and the lengths of its axes come from the covariance matrix, so strongly correlated variables yield a tilted, elongated ellipsoid. Johnson and Wichern's Applied multivariate statistical analysis derives it from the sampling distribution. The referent is a multidimensional uncertainty region, unrelated to a spinning body's inertia beyond the shared quadric shape.[2]
In geodesy the reference ellipsoid is the smooth mathematical surface of revolution (such as GRS80 or WGS84) chosen to approximate the Earth's figure and to serve as the surface on which latitude, longitude, and ellipsoidal height are defined. Geodetic coordinates are given relative to it, while the undulating geoid is measured as a separation from it. Torge and Müller's Geodesy specifies the common reference ellipsoids and their parameters. The referent is the defined ellipsoid of revolution used as a geodetic datum, a deliberate idealisation rather than a measured physical shape.[3]
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