Abstract

The Global Navigational Satellite System (GNSS) technique is naturally sensitive to the geocenter motion, similar to all satellite techniques. However, the GNSS-based estimates of the geocenter used to contain more orbital artifacts than the geophysical signals, especially for the Z component of the geocenter coordinates. This contribution conveys a discussion on the impact of solar radiation pressure (SRP) modeling on the geocenter motion estimates. To that end, we process 3 years of GPS, GLONASS, and Galileo observations (2017–2019), collected by a globally distributed network of the ground stations. All possible individual system-specific solutions, as well as combinations of the available constellations, are tested in search of characteristic patterns in geocenter coordinates. We show that the addition of a priori information about the SRP-based forces acting on the satellites using a box-wing model mitigates a great majority of the spurious signals in the spectra of the geocenter coordinates. The amplitude of the 3 cpy (about 121 days) signal for GLONASS has been reduced by a factor of 8.5. Moreover, the amplitude of the spurious 7 cpy (about 52 days) signal has been reduced by a factor of 5.8 and 3.1 for Galileo and GPS, respectively. Conversely, the box-wing solutions indicate increased amplitudes of the annual variations in the geocenter signal. The latter reaches the level of 10–11 mm compared to 4.4 and 6.0 mm from the satellite laser ranging observations of LAGEOS satellites and the corresponding GNSS series applying extended empirical CODE orbit model (ECOM2), respectively. Despite the possible improvement in the GLONASS-based Z component of the geocenter coordinates, we show that some significant power can still be found at periods other than annual. The GPS- and Galileo-based estimates are less affected; thus, a combination of GPS and Galileo leads to the best geocenter estimates.

Highlights

  • The geocenter motion is conventionally interpreted as the movement of the center of mass of the earth system, including the solid earth, atmosphere, and oceans, with respect to the origin of the reference frame (Wu et al 2012; Altamimi et al 2016)

  • No significant correlations are found for the equatorial geocenter coordinates (GCC) components; we limit the analysis to the GCC-Z only

  • 2 days have been selected for each constellation to reflect the epoch of the low and high GCC-Z

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Summary

Introduction

The geocenter motion is conventionally interpreted as the movement of the center of mass of the earth system, including the solid earth, atmosphere, and oceans, with respect to the origin of the reference frame (Wu et al 2012; Altamimi et al 2016). This movement is expressed by a three-dimensional vector known as geocenter coordinates (GCC). GNSS can determine the equatorial GCC components with good consistency to the other geodetic

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