Publications related to the GRACE Missions (no abstracts)

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Regional sea level trend budget over 2004–2022

Bouih, Marie, Barnoud, Anne, Yang, Chunxue, Storto, Andrea, Blazquez, Alejandro, Llovel, William, Fraudeau, Robin, and Cazenave, Anny, 2025. Regional sea level trend budget over 2004–2022. Ocean Science, 21(4):1425–1440, doi:10.5194/os-21-1425-2025.

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@ARTICLE{2025OcSci..21.1425B,
       author = {{Bouih}, Marie and {Barnoud}, Anne and {Yang}, Chunxue and {Storto}, Andrea and {Blazquez}, Alejandro and {Llovel}, William and {Fraudeau}, Robin and {Cazenave}, Anny},
        title = "{Regional sea level trend budget over 2004{\textendash}2022}",
      journal = {Ocean Science},
         year = 2025,
        month = jul,
       volume = {21},
       number = {4},
        pages = {1425-1440},
     abstract = "{Closure of the regional sea level trend budget is investigated over the
        2004{\textendash}2022 time span by comparing trend patterns from
        the satellite altimetry-based sea level with the sum of
        contributions, i.e. the thermosteric, halosteric, manometric and
        GRD (gravitational, rotational, and deformational fingerprints
        due to past and ongoing land ice melt) components. The
        thermosteric and halosteric components are based on Argo data
        (down to 2000 m). For the manometric component, two approaches
        are considered: one using GRACE/GRACE Follow-On satellite
        gravimetry data and the other using ocean reanalyses-based
        sterodynamic sea level data corrected for local steric effects.
        For the latter, six different ocean reanalyses are considered,
        including two reanalyses that do not assimilate satellite
        altimetry data. The results show significantly high residuals in
        the North Atlantic for both approaches. In a few other regions,
        small-scale residuals of smaller amplitude are observed and
        attributed to the finer resolution of altimetry data compared to
        the coarser resolution of data sets used for the components. The
        observed strong residual signal in the North Atlantic points to
        Argo-based salinity errors in this region. However, it is not
        excluded that other factors also contribute to the reported non-
        closure of the budget in this area.}",
          doi = {10.5194/os-21-1425-2025},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2025OcSci..21.1425B},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

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