Articles | Volume 13, issue 8
Earth Syst. Sci. Data, 13, 3869–3884, 2021
Earth Syst. Sci. Data, 13, 3869–3884, 2021
Data description paper
10 Aug 2021
Data description paper | 10 Aug 2021

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

Michael G. Hart-Davis et al.

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Cited articles

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Bosch, W., Dettmering, D., and Schwatke, C.: Multi-mission cross-calibration of satellite altimeters: Constructing a long-term data record for global and regional sea level change studies, Remote Sens.-Basel, 6, 2255–2281, 2014. a, b
Brockley, D. J., Baker, S., Féménias, P., Martinez, B., Massmann, F.-H., Otten, M., Paul, F., Picard, B., Prandi, P., Roca, M., Rudenko, S., Scharroo, R., and Visser, P.: REAPER: Reprocessing 12 years of ERS-1 and ERS-2 altimeters and microwave radiometer data, IEEE T. Geosci. Remote, 55, 5506–5514, 2017. a, b
Cancet, M., Andersen, O., Abulaitijiang, A., Cotton, D., and Benveniste, J.: Improvement of the Arctic Ocean Bathymetry and Regional Tide Atlas: First Result on Evaluating Existing Arctic Ocean Bathymetric Models, in: Fiducial Reference Measurements for Altimetry, edited by: Mertikas, S. and Pail, R., Springer, Cham, Switzerland, pp. 55–63, 2019. a
Short summary
Ocean tides are an extremely important process for a variety of oceanographic applications, particularly in understanding coastal sea-level rise. Tidal signals influence satellite altimetry estimations of the sea surface, which has resulted in the development of ocean tide models to account for such signals. The EOT20 ocean tide model has been developed at DGFI-TUM using residual analysis of satellite altimetry, with the focus on improving the estimation of ocean tides in the coastal region.