Oblate ellipsoid in the context of "Geodesics on an ellipsoid"

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⭐ Core Definition: Oblate ellipsoid

A spheroid, also known as an ellipsoid of revolution or rotational ellipsoid, 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. A spheroid has circular symmetry.

If the ellipse is rotated about its major axis, the result is a prolate spheroid, elongated like a rugby ball. The American football is similar but has a pointier end than a spheroid could. If the ellipse is rotated about its minor axis, the result is an oblate spheroid, flattened like a lentil or a plain M&M. If the generating ellipse is a circle, the result is a sphere.

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👉 Oblate ellipsoid in the context of Geodesics on an ellipsoid

The study of geodesics on an ellipsoid arose in connection with geodesy specifically with the solution of triangulation networks. The figure of the Earth is well approximated by an oblate ellipsoid, a slightly flattened sphere. A geodesic is the shortest path between two points on a curved surface, analogous to a straight line on a plane surface. The solution of a triangulation network on an ellipsoid is therefore a set of exercises in spheroidal trigonometry (Euler 1755).

If the Earth is treated as a sphere, the geodesics are great circles (all of which are closed) and the problems reduce to ones in spherical trigonometry. However, Newton (1687) showed that the effect of the rotation of the Earth results in its resembling a slightly oblate ellipsoid: in this case, the equator and the meridians are the only simple closed geodesics. Furthermore, the shortest path between two points on the equator does not necessarily run along the equator. Finally, if the ellipsoid is further perturbed to become a triaxial ellipsoid (with three distinct semi-axes), only three geodesics are closed.

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Oblate ellipsoid in the context of Earth radius

Earth radius (denoted as R🜨 or RE) is the distance from the center of Earth to a point on or near its surface. Approximating the figure of Earth by an Earth spheroid (an oblate ellipsoid), the radius ranges from a maximum (equatorial radius, denoted a) of about 6,378 km (3,963 mi) to a minimum (polar radius, denoted b) of nearly 6,357 km (3,950 mi).

A globally-average value is usually considered to be 6,371 kilometres (3,959 mi) with a 0.3% variability (±10 km) for the following reasons.The International Union of Geodesy and Geophysics (IUGG) provides three reference values: the mean radius (R1) of three radii measured at two equator points and a pole; the authalic radius, which is the radius of a sphere with the same surface area (R2); and the volumetric radius, which is the radius of a sphere having the same volume as the ellipsoid (R3). All three values are about 6,371 kilometres (3,959 mi).

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Oblate ellipsoid in the context of Universal Transverse Mercator

The Universal Transverse Mercator (UTM) is a projected coordinate system based on the transverse Mercator map projection of the Earth spheroid. As a map projection, it transforms geographic coordinates of locations on Earth's surface to assign plane coordinates to them. It is a horizontal position representation, which means it ignores altitude and treats the earth surface as an oblate ellipsoid. The system divides Earth into 60 zones and projects each to the plane as a basis for its coordinates. Specifying a location means specifying the zone and the x, y coordinate in that plane.

UTM parameter specifications vary by nation or region or mapping system. However, most zones in UTM span 6 degrees of longitude, and each has a designated central meridian. In each zone, the scale factor at the central meridian is specified to be 0.9996 of true scale (for most UTM systems in use). Therefore maps, atlases, and topographic grid systems built from an appropriate collection of UTM zones cover a region with planar maps with well-controlled, minimal distortion. For this reason, UTM coordinates are used in many nations and regions for topographic mapping, as well as more generally for pinpointing locations.

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