4.7 Article

Evaluation of the Consistency of Three GRACE Gap-Filling Data

期刊

REMOTE SENSING
卷 14, 期 16, 页码 -

出版社

MDPI
DOI: 10.3390/rs14163916

关键词

satellite gravity; time variable gravity; time-series analysis; spatial analysis; sea level change; gap-filling; triple collocation

资金

  1. Hebei Key Laboratory of Earthquake Dynamics Open Fund [FZ202214]
  2. University of Chinese Academy of Sciences Research Start-up Grant [110400M003]
  3. Self-Funded Project of Scientific Research and Development Plan of Langfang Science and Technology Bureau [2020013045, 2021011030]
  4. Central University Basic Research Fund of China [2020013045, ZY20215159]
  5. Key Project of Science and Technology Research for Universities of Hebei Province [ZD2020407]
  6. Hebei Key Laboratory of Earthquake Disaster Prevention and Risk Assessment [FZ213109]
  7. Beijing Key Laboratory of Urban Spatial Information Engineering [20220102]

向作者/读者索取更多资源

This study systematically analyzes and compares three spherical harmonic coefficient gap-filling products and provides a reference for users to select a suitable product. Additionally, a new scheme based on the triple collocation method is proposed to fuse these datasets into a more robust solution.
The Gravity Recovery and Climate Experiment (GRACE) gravity mission has become a leading platform for monitoring temporal changes in the Earth's global gravity field. However, the usability of GRACE data is severely limited by 11 months of missing data between the GRACE and GRACE Follow-on (GRACE-FO) missions. To date, several approaches have been proposed to fill this data gap in the form of spherical harmonic coefficients (an expression of the Earth's gravity field, SHCs). However, systematic analysis to reveal the characteristics and consistency of the datasets produced by these latest gap-filling techniques is yet to be carried out. Here, three SHC gap-filling products are systematically analyzed and compared: (1) Combining high-low satellite-to-satellite tracking with satellite laser ranging (SLR) observations (QuantumFrontiers, QF), (2) SLR-based recovery incorporating the GRACE empirical orthogonal function decomposition model proposed by the Institute of Geodesy and Geoinformation at the University of Bonn (hereafter, denoted as IGG), and (3) applying the singular spectrum analysis approach (SSA). The results show that (1) the SHCs of the QF, IGG, and SSA data are consistent up to degree 12; (2) the IGG and SSA data give similar results over the 11 gap months, but the IGG shows a faster increase in the mean ocean water mass and the SSA appears to better capture the interannual variation in the terrestrial water storage; and (3) the noise level increases significantly in the high-degree terms (l > 16) of the QF data, so these data are only applicable for large-scale mass migration research. These results provide a reference for users to select a gap-filling product. Finally, we propose a new scheme based on the triple collocation method to derive a weight matrix to fuse these three datasets into a more robust solution.

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