• Sorted by Date • Sorted by Last Name of First Author •
Xu, Pengfei, Jiang, Tao, Zhang, Chuanyin, Qu, Guoqing, Zhang, Hanwei, and Li, Wanqiu, 2025. Temporal variations of the geoid and dynamic maintenance of height reference frame using surface mass loading and GRACE/GRACE-FO data. Geophysical Journal International, 242(2):ggaf215, doi:10.1093/gji/ggaf215.
• from the NASA Astrophysics Data System • by the DOI System •
@ARTICLE{2025GeoJI.242..215X,
author = {{Xu}, Pengfei and {Jiang}, Tao and {Zhang}, Chuanyin and {Qu}, Guoqing and {Zhang}, Hanwei and {Li}, Wanqiu},
title = "{Temporal variations of the geoid and dynamic maintenance of height reference frame using surface mass loading and GRACE/GRACE-FO data}",
journal = {Geophysical Journal International},
year = 2025,
month = aug,
volume = {242},
number = {2},
eid = {ggaf215},
pages = {ggaf215},
abstract = "{High-precision geoid models have traditionally been static, neglecting
temporal variations. However, achieving geoid accuracy within
1-2 cm and maintaining dynamic height reference frames
necessitates consideration of geoid spatiotemporal variations.
Gravity Recovery and Climate Experiment/GRACE Follow-On
(GRACE/GRACE-FO) and surface mass loading models provide means
to estimate geoid changes, but their accuracy and reliability
require further validation. This study proposes a method for
dynamically maintaining regional height reference frames by
integrating Global Navigation Satellite System (GNSS) reference
stations as core nodes and incorporating time-varying geoid
data. This method dynamically corrects station heights by
computing normal height variations using GNSS observations and
geoid changes. Experiments conducted in Beijing and Shandong
derived geoid changes using GRACE/GRACE-FO and surface mass
loading, validated against long-term GNSS observations and
leveling surveys. Results show a strong correlation (R
{\ensuremath{\approx}} 0.9; NSE > 0.4) between geoid changes
derived from GRACE and surface mass loading, although amplitude
discrepancies of up to 4 mm existed. In 41 experimental cases,
accuracy improvement was observed in over 90 per cent of
instances following geoid change corrections. In Beijing, 18 out
of 26 results achieved accuracy improvements exceeding 20 per
cent, five of which surpassed 90 per cent. In Shandong, 11 out
of 15 results improved by over 10 per cent, including five
exceeding 40 per cent. These findings confirm the feasibility
and effectiveness of using GRACE/GRACE-FO and surface mass
loading to estimate geoid changes. The proposed method
significantly improves the accuracy of dynamic height reference
frame maintenance, providing valuable insights for further
refinement of geoid models.}",
doi = {10.1093/gji/ggaf215},
adsurl = {https://ui.adsabs.harvard.edu/abs/2025GeoJI.242..215X},
adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
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