Publications related to the GRACE Missions (no abstracts)

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Extraction of Time–Varying Signals in GNSS and Geophysical Interpretation: Methods, Advances, and Challenges

Li, Xiangjun, Wu, Shuguang, Li, Houpu, Liu, Bing, Bian, Shaofeng, and He, Yuefan, 2026. Extraction of Time–Varying Signals in GNSS and Geophysical Interpretation: Methods, Advances, and Challenges. Sensors, 26(17):5557, doi:10.3390/s26175557.

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@ARTICLE{2026Senso..26.5557L,
       author = {{Li}, Xiangjun and {Wu}, Shuguang and {Li}, Houpu and {Liu}, Bing and {Bian}, Shaofeng and {He}, Yuefan},
        title = "{Extraction of Time-Varying Signals in GNSS and Geophysical Interpretation: Methods, Advances, and Challenges}",
      journal = {Sensors},
     keywords = {GNSS coordinate time series, time-varying signal extraction, environmental loading deformation, geophysical interpretation, multi-source data fusion},
         year = 2026,
        month = sep,
       volume = {26},
       number = {17},
          eid = {5557},
        pages = {5557},
     abstract = "{What are the main findings? Maximum Likelihood Estimation (MLE) has
        become the standard for GNSS linear trend extraction because it
        jointly estimates trend parameters and stochastic noise
        covariance; by doing so, it corrects the up to 5--10-fold
        underestimation of velocity uncertainty that occurs when
        temporally correlated (colored) noise is present but a white-
        noise covariance is assumed. In large-sample benchmark tests on
        the CMONOC network reported by Wu et al., Variational Mode
        Decomposition (VMD) yields positive residual RMS improvement at
        97.9\% of stations (mean 69.8\%), outperforming SSA (90.5\% of
        stations); these results originate from the authors' prior work
        and await independent replication on other networks before
        generalization (See relevant sections in the manuscript for
        metric-related caveats). Li et al. reported interannual
        fluctuations of the annual period between 363 and 367 days at
        ten CMONOC stations; if such period drift proves widespread, it
        challenges signal separation methods built on fixed-frequency
        assumptions. Maximum Likelihood Estimation (MLE) has become the
        standard for GNSS linear trend extraction because it jointly
        estimates trend parameters and stochastic noise covariance; by
        doing so, it corrects the up to 5--10-fold underestimation of
        velocity uncertainty that occurs when temporally correlated
        (colored) noise is present but a white-noise covariance is
        assumed. In large-sample benchmark tests on the CMONOC network
        reported by Wu et al., Variational Mode Decomposition (VMD)
        yields positive residual RMS improvement at 97.9\% of stations
        (mean 69.8\%), outperforming SSA (90.5\% of stations); these
        results originate from the authors' prior work and await
        independent replication on other networks before generalization
        (See relevant sections in the manuscript for metric-related
        caveats). Li et al. reported interannual fluctuations of the
        annual period between 363 and 367 days at ten CMONOC stations;
        if such period drift proves widespread, it challenges signal
        separation methods built on fixed-frequency assumptions. What
        are the implications of the main findings? If the reported
        period drift of seasonal signals is confirmed on wider networks,
        future GNSS signal processing should move beyond fixed-frequency
        assumptions; time-varying frequency models (e.g.,
        UKF\_Amp\_Period) offer a viable path forward. Multi-source
        fusion (GNSS + InSAR + GRACE) is essential for separating
        coupled geophysical signals that cannot be resolved by any
        single technique. Self-supervised foundation models (e.g., GNSS-
        FM, currently an unreviewed preprint) point to a possible
        paradigm shift in GNSS time series analysis, but their
        geographic fairness and physical interpretability remain
        unvalidated. If the reported period drift of seasonal signals is
        confirmed on wider networks, future GNSS signal processing
        should move beyond fixed-frequency assumptions; time-varying
        frequency models (e.g., UKF\_Amp\_Period) offer a viable path
        forward. Multi-source fusion (GNSS + InSAR + GRACE) is essential
        for separating coupled geophysical signals that cannot be
        resolved by any single technique. Self-supervised foundation
        models (e.g., GNSS-FM, currently an unreviewed preprint) point
        to a possible paradigm shift in GNSS time series analysis, but
        their geographic fairness and physical interpretability remain
        unvalidated. Precise signal extraction and geophysical
        interpretation of Global Navigation Satellite System (GNSS)
        coordinate time series constitute the core foundation for
        establishing the International Terrestrial Reference Frame
        (ITRF) and inverting surface mass redistribution. This paper
        reviews major advances in this field across four dimensions:
        model framework, signal characteristics, extraction methods, and
        geophysical mechanisms. Key findings include: (1) Maximum
        Likelihood Estimation (MLE) has become the recognized standard
        for linear trend extraction: by jointly estimating deformation
        parameters and the noise covariance, it corrects the up to 5--
        10-fold underestimation of velocity uncertainty that arises in
        conventional least-squares analyses when colored noise is
        present but a white-noise covariance is assumed; (2) in CMONOC
        benchmark tests reported by Wu et al., Variational Mode
        Decomposition (VMD) achieves an average 69.8\% residual RMS
        reduction at 97.9\% of stations---results that are promising but
        not yet independently replicated on other networks---while the
        self-supervised model GNSS-FM (currently an unreviewed preprint)
        represents an emerging intelligent analysis paradigm; (3) the
        combined effect of atmospheric, non-tidal ocean and hydrological
        loading explains about 42\% of the residual power of the annual
        vertical signal globally after pole tide correction and reduces
        the weighted mean vertical annual amplitude from 4.19 mm to 3.19
        mm, while for horizontal components the fraction explained by
        current loading models is much smaller (amplitude ratio,
        explained variance and RMS/WRMS reduction are distinct metrics
        and are not directly interchangeable). This paper further
        highlights that the annual period was reported to fluctuate
        between 363 and 367 days at the ten CMONOC stations analyzed by
        Li et al.---a time variability that, if general, challenges
        fixed-frequency signal separation methods, although apparent
        period changes may also arise from amplitude/phase modulation,
        spectral leakage, finite-record effects, colored noise or data
        gaps---and it identifies thermoelastic deformation (TED) as a
        long-neglected but potentially quantifiable component, based on
        a recently released preprint dataset that has not yet undergone
        peer review. Finally, key research prospects are outlined,
        including physics-informed fusion methods, self-supervised
        foundation models, and a unified multi-source inversion
        framework.}",
          doi = {10.3390/s26175557},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2026Senso..26.5557L},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

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