Katana VentraIP

Figure of the Earth

In geodesy, the figure of the Earth is the size and shape used to model planet Earth. The kind of figure depends on application, including the precision needed for the model. A spherical Earth is a well-known historical approximation that is satisfactory for geography, astronomy and many other purposes. Several models with greater accuracy (including ellipsoid) have been developed so that coordinate systems can serve the precise needs of navigation, surveying, cadastre, land use, and various other concerns.

For the historical development of the concept, see Spherical Earth and Flat Earth.

Equatorial radius (called semimajor axis), and polar radius (called semiminor axis);

and ;

eccentricity

and .

flattening

Clairaut's theorem

EGM96

Gravity formula

Gravity of Earth

Horizon §§ ​ and Curvature

Distance

Meridian arc

Theoretical gravity

Geodesy, Oxford 1952 and 1980.

Guy Bomford

Guy Bomford, Determination of the European geoid by means of . Rpt of Comm. 14, IUGG 10th Gen. Ass., Rome 1954.

vertical deflections

and Gottfried Gerstbach, Die horizontale Isostasie / Das isostatische Geoid 31. Ordnung. Geowissenschaftliche Mitteilungen Band 5, TU Wien 1975.

Karl Ledersteger

and Bernhard Hofmann, Physical Geodesy. Springer, Wien & New York 2005.

Helmut Moritz

Geodesy for the Layman, , St. Louis, 1983.

Defense Mapping Agency

Reference Ellipsoids (PCI Geomatics)

Reference Ellipsoids (ScanEx)

Archived 22 January 2009 at the Wayback Machine

Changes in Earth shape due to climate changes

Jos Leys "The shape of Planet Earth"