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Earth gravity field model
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The introduction to this paper is provided in Section 1, while the computational program is described in detail in Section 2. The study results and evaluations are presented and discussed in Sections 3 and 4, respectively.
9p
vimulcahy
02-10-2023
5
2
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The main aims of physical geodesy are to study the shape of the Earth, its gravity field and the geoid which is an equipotential surface closest to the mean sea level. Precise geoid determination has been an important research topic in geodesy and geophysics in the past two decades. Scientists and government agencies all around the world have made great efforts on the development of highaccuracy geoid models.
182p
runthenight07
01-03-2023
7
2
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The main aims of physical geodesy are to study the shape of the Earth, its gravity field and the geoid which is an equipotential surface closest to the mean sea level. Precise geoid determination has been an important research topic in geodesy and geophysics in the past two decades. Scientists and government agencies all around the world have made great efforts on the development of high-accuracy geoid models.
182p
runthenight04
02-02-2023
7
3
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Gravity data inversion or interpretation requires the removal of the gravitational effects of the a priori known geologic and/or morphologic features within the Earth’s system to model and reveal the remaining signals of the unknown anomalous subsurface density distributions. The Bouguer gravity anomalies reduced by the normal gravitational field of the Earth and the gravitational attraction of the topographic masses above the sea level are frequently used in geophysics for this purpose.
12p
tanmocphong
29-01-2022
7
0
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