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Contribution of GPS horizontal displacements for inferring terrestrial water storage variations in the northwestern United States

Wei, Na and Feng, Jianhe, 2026. Contribution of GPS horizontal displacements for inferring terrestrial water storage variations in the northwestern United States. Journal of Geodesy, 100(6):40, doi:10.1007/s00190-026-02069-2.

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@ARTICLE{2026JGeod.100...40W,
       author = {{Wei}, Na and {Feng}, Jianhe},
        title = "{Contribution of GPS horizontal displacements for inferring terrestrial water storage variations in the northwestern United States}",
      journal = {Journal of Geodesy},
     keywords = {Terrestrial water storage, GPS, Seasonal water variation, Regularization method, Three-dimensional displacements, Engineering, Geomatic Engineering},
         year = 2026,
        month = jun,
       volume = {100},
       number = {6},
          eid = {40},
        pages = {40},
     abstract = "{Using GPS displacements to infer terrestrial water storage (TWS)
        provides an important perspective for water resource monitoring.
        However, GPS horizontal displacements with higher precision are
        often overlooked in most previous studies. This study
        incorporates three-dimensional (3D) GPS displacements to improve
        the daily TWS estimates in the Pacific Northwest of the United
        States from 2006 to 2021. In the 3D inversion, the conventional
        Tikhonov regularization, commonly employed for the vertical-only
        inversion, tends to produce overly smooth TWS spatial patterns.
        To address this issue, we propose an updated regularization
        method. The performance of 3D GPS inversion in capturing the
        seasonal TWS variability was evaluated through comparisons with
        hydrological models, the Gravity Recovery and Climate Experiment
        (GRACE), and in situ water measurements. We further quantify the
        contribution of GPS horizontal displacements by comparing 3D and
        vertical-only inversion results. Compared with the vertical-only
        results, the mean annual amplitude of 3D GPS-inferred TWS
        decreases by 17\%, from 161 to 134 mm, bringing it closer to
        hydrological model estimates (130 mm). Synthetic experiments
        further indicate that vertical-only inversion tends to yield
        amplified seasonal TWS amplitudes in this region. In addition,
        the 3D GPS-inferred TWS exhibits substantially improved
        agreement with in situ observations, with higher correlations at
        94\% of snow measurement sites and 76\% of gage height stations.
        Therefore, these improvements highlight the critical role of GPS
        horizontal displacements in achieving more accurate TWS
        estimates.}",
          doi = {10.1007/s00190-026-02069-2},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2026JGeod.100...40W},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

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