The objectives of planetary geodesy are to determine the gravity, topography and rotation of the planets. These measurements are put to two basic uses. In a somewhat pragmatic vein, the geodetic parameters are useful for navigational purposes: the motion of a spacecraft in orbit around a planet, relative to features of interest on the planetary surface, depends on the gravity, topography, and rotation of the planet. On the other hand, these same geodetic parameters provide the only remotely accessible information on the internal mass distribution in the planet.
The methods used to obtain geodetic information on the planets are quite diverse. The earliest estimates of planetary masses came from observing the orbital motions of natural satellites. For a small satellite, the size of the orbit (semimajor axis a) and the mean orbital angular velocity (mean motion n) are related to the mass of the primary body M via GM = a 3 n 2, where Gis the gravitational coupling constant. Through the...
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Earth; Earth rotation; Gravity fields of the terrestrial planets; Jupiter; Mars; Mars: gravity; Mercury; Moon: gravity; Neptune; Planet; Planetary rotation; Pluto; Saturn; Uranus; Venus; Venus: gravity
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Bills, B.G. (1997). Planetary geodesy . In: Encyclopedia of Planetary Science. Encyclopedia of Earth Science. Springer, Dordrecht. https://doi.org/10.1007/1-4020-4520-4_313
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