Abstract
Deviations of the shape of a cosmic body from spherical symmetry show up in its gravitational field; conversely, corrections to the monopole gravitational field GM/r provide important information about the interior. The main deviation is due to rotation and corresponds to a correction in the gravitational potential proportional to 1/r3 (the quadrupole term). Smaller disturbances in the mass distribution produce on the surface smaller corrections which decrease with a higher power of the distance from the centre. The gravitational field of a generic, non-spherical body is appropriately described by a powerful mathematical tool, the set of spherical harmonic functions. This chapter introduces this tool and applies it to the earth. The physics of gravity anomalies of small size is also discussed.
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Further Reading
A good and classical textbook on geodesy and theoretical gravimetry is W.A. Heiskanen and H. Moritz, Physical Geodesy, Freeman (1967).
On an easier level and with greater concern for applications, is G.D. Garland, The Earth’s Shape and Gravity, Pergamon Press (1965).
We also quote W.M. Kaula, Theory of Satellite Geodesy, Blaisdell, Waltham, Mass. (1966)
M. Caputo, The Gravity Field of the Earth, Academic Press (1967).
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© 1990 Kluwer Academic Publishers
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Bertotti, B., Farinella, P. (1990). The Gravitational Field of a Planet. In: Physics of the Earth and the Solar System. Geophysics and Astrophysics Monographs, vol 31. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-1916-7_2
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DOI: https://doi.org/10.1007/978-94-009-1916-7_2
Publisher Name: Springer, Dordrecht
Print ISBN: 978-94-010-7355-4
Online ISBN: 978-94-009-1916-7
eBook Packages: Springer Book Archive