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Contribution analysis of the addition of laser ranging interferometry on GRACE-FO gravity field estimation under different accelerometer calibration schemes

Chen, Qiujie, Shen, Zhanglin, Nie, Yufeng, Shen, Yunzhong, and Zhang, Xingfu, 2025. Contribution analysis of the addition of laser ranging interferometry on GRACE-FO gravity field estimation under different accelerometer calibration schemes. Advances in Space Research, 75(2):1913–1930, doi:10.1016/j.asr.2024.10.038.

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@ARTICLE{2025AdSpR..75.1913C,
       author = {{Chen}, Qiujie and {Shen}, Zhanglin and {Nie}, Yufeng and {Shen}, Yunzhong and {Zhang}, Xingfu},
        title = "{Contribution analysis of the addition of laser ranging interferometry on GRACE-FO gravity field estimation under different accelerometer calibration schemes}",
      journal = {Advances in Space Research},
     keywords = {Satellite gravimetry, GRACE-FO, LRI, KBR},
         year = 2025,
        month = jan,
       volume = {75},
       number = {2},
        pages = {1913-1930},
     abstract = "{To investigate the influence of K-Band microwave ranging (KBR) and Laser
        Ranging Interferometer (LRI) inter-satellite range-rates from
        the GRACE-FO mission on the recovery of gravity fields, this
        paper explores two distinct methods for accelerometer scale
        estimation, namely diagonal matrix parameterization and full
        matrix parameterization. Integrating both KBR and LRI data from
        GRACE-FO into gravity field recovery, we have derived six new
        time series of monthly gravity field solutions based on two
        different accelerometer calibration approaches, entitled
        KBRLRI\_Com (incorporating both KBR and LRI data), KBR\_Only
        (using pure KBR data), LRI\_Only (solely utilizing LRI data)
        truncate to degree and order 60 over the period from January
        2019 to June 2022. Analyses of KBRLRI\_Com, KBR\_Only, and
        LRI\_Only reveal the following findings: (1) LRI demonstrates
        significant advantages over KBR in both diagonal and full scale
        matrix scenarios, across the time and frequency domains, which
        shows lower root mean square (RMS) values of the post-fit
        residuals in the time domain and substantially lower noise at
        higher frequencies; (2) the comparison between KBRLRI\_Com,
        KBR\_Only, and LRI\_Only in terms of geoid degree error suggests
        that KBRLRI\_Com agrees well with KBR\_Only and LRI\_Only at the
        low degrees (below degree 30), while effectively reducing the
        high-frequency noise, especially when the diagonal scale
        matrices are employed; the benefit of KBRLRI\_Com solution is
        mainly attributed to the enhanced quantity of ranging
        observations. (3) by analyzing the signal and noise over the
        globe, ocean, Australian continent, and Amazon and Ganges river
        basins, we find that KBRLRI\_Com is highly consistent with
        KBR\_Only and LRI\_Only in terms of spatial signals, while
        KBRLRI\_Com exhibits less spatial noise; when employing diagonal
        and full matrices, the noise of gravity field solutions derived
        by incorporating LRI data is mitigated by 8.8 \% and 3.9 \% over
        the global ocean compared to KBR\_Only, as well as 7.6 \% and
        3.2 \% in the Australian continent; especially in the diagonal
        matrix case, the incorporation of LRI measurements for
        calculating monthly gravity fields results in a more pronounced
        decrease of spatial noise. (4) in the oceanic region, KBR\_Only
        and LRI\_Only have average RMS values of 11.3 cm and 11.6 cm in
        diagonal matrices, respectively, and 10.2 cm and 11.6 cm in the
        full matrix, indicating a generally comparable level of accuracy
        between the two models.}",
          doi = {10.1016/j.asr.2024.10.038},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2025AdSpR..75.1913C},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

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