• Sorted by Date • Sorted by Last Name of First Author •
Gao, Geng, Zheng, Wei, Sun, Yongjin, Du, Jiankang, Zhao, Yongqi, and Zhao, Minxing, 2026. GRACE–FO gravity field recovery from integer ambiguity resolved kinematic orbits and decorrelated stochastic model. Advances in Space Research, 77(3):3844–3857, doi:10.1016/j.asr.2025.10.095.
• from the NASA Astrophysics Data System • by the DOI System •
@ARTICLE{2026AdSpR..77.3844G,
author = {{Gao}, Geng and {Zheng}, Wei and {Sun}, Yongjin and {Du}, Jiankang and {Zhao}, Yongqi and {Zhao}, Minxing},
title = "{GRACE-FO gravity field recovery from integer ambiguity resolved kinematic orbits and decorrelated stochastic model}",
journal = {Advances in Space Research},
keywords = {GRACE-FO, Gravity field recovery, Integer ambiguity resolution, Kinematic orbit, Stochastic model},
year = 2026,
month = feb,
volume = {77},
number = {3},
pages = {3844-3857},
abstract = "{The Gravity Recovery And Climate Experiment (GRACE) series missions have
revolutionized our understanding of Earth gravity field by
combining Global Positioning System (GPS) tracking and inter-
satellite K-band ranging (KBR) to monitor global mass transport
with unprecedented resolution and continuity. Within the
Celestial Mechanics Approach (CMA), GPS-based kinematic
orbits{\textemdash}together with their stochastic
characteristics{\textemdash}are treated as pseudo-observations
to simultaneously reconstruct satellite orbits and recover Earth
gravity field. Nevertheless, ambiguity-float kinematic orbits
and epoch-wise covariance models, which are simplified versions
of the fully populated covariance matrices derived from GPS
observation noise propagation, remain widely used, thereby
limiting further improvements in the accuracy of CMA solutions.
This study investigates the impact of applying integer ambiguity
resolution (IAR) to enhance kinematic orbit precision and reduce
temporal correlations in the stochastic model. These refinements
enable the use of simplified epoch-wise covariance matrices
without compromising solution consistency. Using GRACE Follow-On
(GFO) data from November 2019, we evaluate the effects of IAR-
based orbits and decorrelated covariance structures within a
least squares framework incorporating variance component
estimation (VCE). Monthly gravity fields are estimated up to
degree and order 60 using GPS-only observations, and up to 96
when K-band range-rate (KRR) data are incorporated. The
reconstructed IAR-based orbits exhibit three-dimensional root
mean square (3D RMS) errors close to 1 cm, a significant
improvement over float solutions ({\ensuremath{\sim}}2.5 cm). In
GPS-only solutions, gravity fields based on IAR and float orbits
remain consistent up to degree and order 45, diverging beyond
this{\textemdash}despite the nominal resolution limit of
{\ensuremath{\sim}}1300 km. In joint GPS and KRR solutions,
discrepancies appear beyond degree and order 25 between IAR- and
float-based models, as well as with the GFO Science Data System
(SDS) RL06.1 products{\textemdash}manifested as more pronounced
northâsouth striping artifacts in global mass distributions. To
address this issue, we apply a fixed-weight strategy to
kinematic ambiguity-fixed orbits and KRR observations, which
substantially improves the consistency of the resulting gravity
field with SDS models and outperforms both float and IAR
solutions derived under VCE. This suggests that the superior
precision of IAR-based orbits leads to relatively higher
weighting of the kinematic positions, which in turn reduces the
effective contribution of KBR observations to gravity field
recovery and biases the estimates toward the polar-orbit-
dominated sensitivity of the GFO constellation. These results
highlight the importance of an adequate stochastic description
of kinematic positions, which depends not only on observation
quality but also on the underlying modeling, including ambiguity
resolution and background force models.}",
doi = {10.1016/j.asr.2025.10.095},
adsurl = {https://ui.adsabs.harvard.edu/abs/2026AdSpR..77.3844G},
adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
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