Self-consistent determination of the Earth’s GM, geocenter motion and figure axis orientation

• Published in: Journal of geodesy 2020-12, Vol.94 (12), Article 113
• Main Authors: Couhert, A., Bizouard, C., Mercier, F., Chanard, K., Greff, M., Exertier, P.
• Format: Article
• Language: English
• Subjects: Astrophysics; Earth and Environmental Science; Earth Sciences; Geophysics/Geodesy; Original Article; Physics
• ISSN: 0949-7714; 1432-1394
• DOI: 10.1007/s00190-020-01450-z

The very low-degree Earth’s gravity coefficients, associated with the largest-scale mass redistribution in the Earth’s fluid envelope (atmosphere, oceans and continental hydrology), are the most poorly known. In particular, the first three degree geopotential terms are important, as they relate to intrinsic Earth’s mass references: gravitational coefficient ( GM ) of the Earth (degree 0), geocenter motion (degree 1), Earth’s figure axis orientation (degree 2). This paper presents a self-consistent determination of these three properties of the Earth. The main objective is to deal with the remaining sources of altimetry satellite orbit uncertainties affecting the fundamental record of sea surface height measurements. The analysis identifies the modeling errors, which should be mitigated when estimating the geocenter coordinates from Satellite Laser Ranging (SLR) observations. The long-term behavior of the degree-0 and -2 spherical harmonics is also observed over the 34-year period 1984–2017 from the long-time history of satellite laser tracking to geodetic spherical satellites. From the analysis of the evolution of these two coefficients, constraints regarding the Earth’s rheology and uncertainties in the value of GM could be inferred. Overall, the influence of the orbit characteristics, SLR station ranging/position biases and satellite signature effects, measurement modeling errors (tropospheric corrections, non-tidal deformations) are also discussed.