Publications related to the GRACE Missions (no abstracts)

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Seasonal Cycle in Sea Level Across the Coastal Zone

Ponte, Rui M. and Schindelegger, Michael, 2024. Seasonal Cycle in Sea Level Across the Coastal Zone. Earth and Space Science, 11(12):2024EA003978, doi:10.1029/2024EA003978.

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BibTeX

@ARTICLE{2024ESS...1103978P,
       author = {{Ponte}, Rui M. and {Schindelegger}, Michael},
        title = "{Seasonal Cycle in Sea Level Across the Coastal Zone}",
      journal = {Earth and Space Science},
     keywords = {sea level, seasonal cycle, tide gauge, satellite altimetry, GRACE, sea level budget},
         year = 2024,
        month = dec,
       volume = {11},
       number = {12},
        pages = {2024EA003978},
     abstract = "{Data from tide gauges and satellite altimeters are used to provide an
        up-to-date assessment of the mean seasonal cycle in sea level
        ({\ensuremath{\zeta}} ) over most of the global coastal ocean.
        The tide gauge records, where available, depict a
        {\ensuremath{\zeta}} seasonal cycle with complex spatial
        structure along and across continental boundaries, and an annual
        oscillation dominating over semiannual variability, except in a
        few regions (e.g., the northwestern Gulf of Mexico). Comparisons
        between tide gauge and altimeter data reveal substantial root-
        mean-square differences and only slight improvements in
        agreement when using along-track data optimized for coastal
        applications. Quantification of the uncertainty in the altimeter
        products, inferred from comparing gridded and along-track
        estimates, indicate that differences to tide gauges partly
        reflect short-scale features of the seasonal cycle in proximity
        to the coasts. We additionally probe the {\ensuremath{\zeta}}
        seasonal budget using satellite gravimetry-based manometric
        estimates and steric terms calculated from the World Ocean Atlas
        2023. Focusing on global median values, the sum of the estimated
        steric and manometric harmonics can explain {\ensuremath{\sim}}
        65\% (respectively 40\%) of the annual (semiannual) variance in
        the coastal {\ensuremath{\zeta}} observations. We identify
        several regions, for example, the Australian seaboard, where the
        seasonal {\ensuremath{\zeta}} budget is not closed and
        illustrate that such analysis is mainly limited by the coarse
        spatial resolution of present satellite-derived mass change
        products. For most regions with a sufficiently tight budget
        closure, we find that although the importance of the manometric
        term generally increases with decreasing water depth, steric
        contributions are non-negligible near coastlines, especially at
        the annual frequency.}",
          doi = {10.1029/2024EA003978},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2024E&SS...1103978P},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

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