Oct 2026· Journal of Geodesy· Vol 100· 0 citations· 68 references
Abstract
GRACE/GRACE-FO missions recover gravity field from orbits observed by GPS and variations in inter-satellite distances obtained by the inter-satellite ranging systems. Compared to GRACE, GRACE-FO is also equipped with a laser ranging interferometer (LRI), a more precise inter-satellite ranging technology and the preferred choice for future gravity missions. While the majority of studies predominantly focus on stochastic errors, this research highlights the critical role of non-stochastic biases, specifically the range scale factor for the K-Band ranging (KBR) and LRI data, and baseline biases in GPS observations, i.e., offsets over the ~200 km separation. The effects of range scale factor and baseline biases on the gravity field spherical harmonic coefficients (SHCs) are evaluated through simplified bias models (SBM). We demonstrate that baseline biases exert an influence on the SHCs in a manner analogous to that of the range scale factor. At low SH degrees (2–8), range scale factor and baseline biases impact SHCs approximately proportional to the static gravity field coefficients. The SBM agrees well with error-free simulations, but deviations appear at higher degrees (8–60) when background model errors are included and scale biases are below 1 ppm. Additionally, the effectiveness of the SBM is validated using real GRACE-FO data. A strong correspondence was observed between the scale factor corrections and the C20 relative errors, which provides a practical basis for error budgeting in future missions. These findings indicate the significant impact of scale factors and baseline biases on gravity missions, which can be effectively evaluated using the SBM presented here.
The overall error in gravity field products derived from satellite-to-satellite tracking gravity missions like the Gravity Recovery and Climate Experiment Follow-On (GRACE-FO) is driven by a combination of temporal aliasing error, and measurement system error consisting of both stochastic and deterministic sources. Whi...
D. Wiese, A. Ludwig, Chirag Patel et al.· GRACE/GRACE-FO Science Team...· 0 citations
The GRACE/GRACE-FO mission has been monitoring monthly variations of the Earth’s gravity field for more than two decades. One source of error in the gravity field estimation process is the uncertainty of the satellites’ attitude. The errors of the attitude determination propagate to the inter-satellite range observatio...
Gabriel Valles-Valverde, Felix Öhlinger, T. Mayer-Gürr· GRACE/GRACE-FO Science Team...· 0 citations
Observations of mass changes in the cryosphere are critical to understanding the impact of climate change and constraining global projections of sea-level rise. Observations from satellite gravimetry missions, satellite altimetry, and Surface Mass Balance (SMB) models provide differing estimates of mass change at diffe...
E. Wilson, K. Ghobadi-Far, R. S. Nerem· GRACE/GRACE-FO Science Team...· 0 citations
Global static gravity models produced as spherical harmonic (SH) coefficients have a wide range of applications in geodesy, geophysics, oceanography, and satellite dynamics. It has been established that more information can be extracted from the observations using regional modeling compared to global spherical harmonic...
GFZ aims to distribute a reprocessed and improved RL07 Level-2 gravity field time series in the last quarter of 2026. Most of these improvements have been developed within the Research Unit “New Refined Observations of Climate Change from Spaceborne Gravity Missions” (NEROGRAV) funded by the German Research Foundation...
M. Hauk, C. Dahle, M. Murböck et al.· GRACE/GRACE-FO Science Team...· 0 citations
GRACE and GRACE Follow-On (GRACE-FO) provide the primary satellite gravimetry observations of terrestrial water storage (TWS) variations from 2002 onwards. However, continuously improving global hydrological models often span substantially longer periods, while their validation in the pre-GRACE era remains challenging...
F. Gałdyn, L. Jensen, R. Zajdel et al.· GRACE/GRACE-FO Science Team...· 0 citations
We use cookies to run the site and, with your consent, for analytics and to show ads.
See our Cookie Policy.