4.7 Article

EOT20: a global ocean tide model from multi-mission satellite altimetry

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EARTH SYSTEM SCIENCE DATA
卷 13, 期 8, 页码 3869-3884

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COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/essd-13-3869-2021

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EOT20 is the latest empirical ocean tide model derived using residual tidal analysis of satellite altimetry, showing significant improvements compared to the previous global model EOT11a, particularly in the coastal and shelf regions. The model provides amplitudes and phases of 17 tidal constituents on a global grid based on analysis of multiple satellite missions and includes recent data and missions, updated tidal models, improved coastal representation, and validation with tide gauges and ocean bottom pressure data.
EOT20 is the latest in a series of empirical ocean tide (EOT) models derived using residual tidal analysis of multi-mission satellite altimetry at DGFI-TUM. The amplitudes and phases of 17 tidal constituents are provided on a global 0.125 degrees grid based on empirical analysis of seven satellite altimetry missions and four extended missions. The EOT20 model shows significant improvements compared to the previous iteration of the global model (EOT11a) throughout the ocean, particularly in the coastal and shelf regions, due to the inclusion of more recent satellite altimetry data as well as more missions, the use of the updated FES2014 tidal model as a reference to estimated residual signals, the inclusion of the ALES retracker and improved coastal representation. In the validation of EOT20 using tide gauges and ocean bottom pressure data, these improvements in the model compared to EOT11a are highlighted with the root sum square (RSS) of the eight major tidal constituents improving by similar to 1.4 cm for the entire global ocean with the major improvement in RSS (similar to 2.2 cm) occurring in the coastal region. Concerning the other global ocean tidal models, EOT20 shows an improvement of similar to 0.2 cm in RSS compared to the closest model (FES2014) in the global ocean. Variance reduction analysis was conducted comparing the results of EOT20 with FES2014 and EOT11a using the Jason-2, Jason-3 and SARAL satellite altimetry missions. From this analysis, EOT20 showed a variance reduction for all three satellite altimetry missions with the biggest improvement in variance occurring in the coastal region. These significant improvements, particularly in the coastal region, provide encouragement for the use of the EOT20 model as a tidal correction for satellite altimetry in sea-level research. All ocean and load tide data from the model can be freely accessed at https://doi.org/10.17882/79489 (Hart-Davis et al., 2021). The tide gauges from the TICON dataset used in the validation of the tide model, are available at https://doi.org/10.1594/PANGAEA.896587 (Piccioni et al., 2018a).

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