Earth spheroid in the context of "Oblate spheroid"

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⭐ Core Definition: Earth spheroid

An Earth ellipsoid or Earth spheroid is a mathematical figure approximating the Earth's shape and size, used as a reference frame for computations in geodesy, astronomy, and the geosciences. Various different reference ellipsoids have been used as approximations.

It is an oblate spheroid (an ellipsoid of revolution) whose minor axis (polar diameter), connecting the geographical poles, is approximately aligned with the Earth's axis of rotation. The ellipsoid is also defined by the major axis (equatorial axis); the difference between the two axes is slightly more than 21 km or 0.335%.

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Earth spheroid 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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Earth spheroid 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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