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Geodetic evidence of water mass loss from global navigation satellite system measured land uplift in Türkiye

Ansari, Kutubuddin and Kayıkçı, Emine Tanır, 2026. Geodetic evidence of water mass loss from global navigation satellite system measured land uplift in Türkiye. Journal of Hydrology, 677:135787, doi:10.1016/j.jhydrol.2026.135787.

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BibTeX

@ARTICLE{2026JHyd..67735787A,
       author = {{Ansari}, Kutubuddin and {Kay{\i}k{\c{c}}{\i}}, Emine Tan{\i}r},
        title = "{Geodetic evidence of water mass loss from global navigation satellite system measured land uplift in T{\"u}rkiye}",
      journal = {Journal of Hydrology},
     keywords = {Terrestrial water storage, GRACE, GLDAS, GLWS, Singular Spectrum Analysis, Vertical land motion},
         year = 2026,
        month = sep,
       volume = {677},
          eid = {135787},
        pages = {135787},
     abstract = "{This study quantifies terrestrial water storage (TWS) variations in
        T{\"u}rkiye (2009--2024) using vertical land motion derived from
        a dense Global Navigation Satellite System (GNSS) network.
        Singular Spectrum Analysis (SSA) was applied to separate long-
        term deformation from seasonal oscillations in GNSS height time
        series, and elastic loading inversion was performed to convert
        vertical displacement into monthly equivalent water height (EWH)
        estimates. The resulting monthly GNSS-based TWS estimates were
        validated with Global Land Water Storage (GLWS), Global Land
        Data Assimilation (GLDAS)-Noah and Gravity Recovery and Climate
        Experiment (GRACE) products. Results reveal pronounced TWS
        depletion-induced uplift across Southeastern T{\"u}rkiye and
        Central Anatolia, reflecting groundwater stress in agricultural
        basins, while coastal and northern regions show positive water
        anomalies controlled by precipitation and snowmelt recharge.
        Seasonal amplitudes peak over the Black Sea and western regions,
        with phase shifts showing earlier TWS maxima in eastern snow-fed
        basins. Although GNSS-derived amplitudes are lower due to the
        sparse network and inversion smoothing, strong seasonal
        coherence with GRACE, GLDAS, and GLWS confirms the robustness of
        the approach. Overall, this work provides the first GNSS-based
        hydro-geodetic assessment of TWS over T{\"u}rkiye and
        demonstrates GNSS as a complementary tool for drought monitoring
        and climate-driven water-storage evaluation.}",
          doi = {10.1016/j.jhydrol.2026.135787},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2026JHyd..67735787A},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

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