GRACE and GRACE-FO Related Publications (no abstracts)

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Detection and attribution of intra-annual mass component of sea-level variations along the Norwegian coast

Mangini, Fabio, Bonaduce, Antonio, Chafik, Léon, Raj, Roshin, and Bertino, Laurent, 2023. Detection and attribution of intra-annual mass component of sea-level variations along the Norwegian coast. Scientific Reports, 13:15334, doi:10.1038/s41598-023-40853-8.

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@ARTICLE{2023NatSR..1315334M,
       author = {{Mangini}, Fabio and {Bonaduce}, Antonio and {Chafik}, L{\'e}on and {Raj}, Roshin and {Bertino}, Laurent},
        title = "{Detection and attribution of intra-annual mass component of sea-level variations along the Norwegian coast}",
      journal = {Scientific Reports},
         year = 2023,
        month = sep,
       volume = {13},
          eid = {15334},
        pages = {15334},
     abstract = "{Reliable sea-level observations in coastal regions are needed to assess
        the impact of sea level on coastal communities and ecosystems.
        This paper evaluates the ability of in-situ and remote sensing
        instruments to monitor and help explain the mass component of
        sea level along the coast of Norway. The general agreement
        between three different GRACE/GRACE-FO mascon solutions and a
        combination of satellite altimetry and hydrography gives us
        confidence to explore the mass component of sea level in coastal
        areas on intra-annual timescales. At first, the estimates reveal
        a large spatial-scale coherence of the sea-level mass component
        on the shelf, which agrees with Ekman theory. Then, they suggest
        a link between the mass component of sea level and the along-
        slope wind stress integrated along the eastern boundary of the
        North Atlantic, which agrees with the theory of poleward
        propagating coastal trapped waves. These results highlight the
        potential of the sea-level mass component from GRACE and GRACE-
        FO, satellite altimetry and the hydrographic stations over the
        Norwegian shelf. Moreover, they indicate that GRACE and GRACE-FO
        can be used to monitor and understand the intra-annual
        variability of the mass component of sea level in the coastal
        ocean, especially where in-situ measurements are sparse or
        absent.}",
          doi = {10.1038/s41598-023-40853-8},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2023NatSR..1315334M},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

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