Preprints
https://doi.org/10.5194/essd-2021-97
https://doi.org/10.5194/essd-2021-97

  26 Mar 2021

26 Mar 2021

Review status: a revised version of this preprint was accepted for the journal ESSD and is expected to appear here in due course.

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

Michael Geoffrey Hart-Davis1, Gaia Piccioni1,2, Denise Dettmering1, Christian Schwatke1, Marcello Passaro1, and Florian Seitz1 Michael Geoffrey Hart-Davis et al.
  • 1Deutsches Geodätisches Forschungsinstitut der Technischen Universität München (DGFI-TUM), Arcisstrasse 21, 80333 München, Germany
  • 2Now at: Enel Global Trading S.p.A. Address: V.le Regina Margherita 125, 00198 Rome, Italy

Abstract. 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 seventeen tidal constituents are provided on a global 0.125-degree 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-square sum (RSS) of the eight major tidal constituents improving by ~3 cm for the entire global ocean with the major improvement in RSS (~3.5 cm) occurring in the coastal region. Concerning the other global ocean tidal models, EOT20 shows an improvement of ~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, provides 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).

Michael Geoffrey Hart-Davis et al.

Status: closed

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  • CC1: 'Comment on essd-2021-97', Haidong Pan, 13 Apr 2021