Articles | Volume 15, issue 5
Ocean Sci., 15, 1287–1305, 2019
https://doi.org/10.5194/os-15-1287-2019

Special issue: Developments in the science and history of tides (OS/ACP/HGSS/NPG/SE...

Ocean Sci., 15, 1287–1305, 2019
https://doi.org/10.5194/os-15-1287-2019

Research article 02 Oct 2019

Research article | 02 Oct 2019

Predictability of non-phase-locked baroclinic tides in the Caribbean Sea

Edward D. Zaron

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Ocean Sci., 17, 147–180, https://doi.org/10.5194/os-17-147-2021,https://doi.org/10.5194/os-17-147-2021, 2021
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Cited articles

Alfonso-Sosa, E.: First MODIS Images Catalog of Aves Ridge Solitons in the Caribbean Sea (2008-2013), working notes published on the author's web site, 33 pages, available at: https://www.academia.edu/5500852/First_MODIS_Images_Catalog_of_Aves_Ridge_Solitons_in_the_Caribbean_Sea_2008-2013, (last access: 27 September 2019), 2013. a
Alfonso-Sosa, E.: Seiches Costeros de Puerto Rico, Ocean Physics Education, Puerto Rico, 2015. a
Ansong, J. K., Arbic, B. K., Alford, M. H., Buijsman, M. C., Shriver, J. F., Zhao, Z., Richman, J. G., Simmons, H. L., Timko, P. G., Wallcraft, A. J., and Zamudio, L.: Semidiurnal internal tide energy fluxes and their variability in a global ocean model and moored observations, J. Geophys. Res., 122, 1882–1900, 2017. a
Aslam, T., Hall, R. A., and Dye, S. T.: Internal tides in a dendritic submarine canyon, Prog. Oceanogr., 169, 20–32, 2018. a
Barron, C. N., Kara, A. B., Rhodes, R. C., Rowley, C., and Smedstad, L. F.: Validation Test Report of the 1/8 Global Navy Coastal Ocean Model Nowcast/Forecast System, Tech. Rep. NRL/MR/7320–07-9019, Naval Research Laboratory, Stennis Space Center, MS, 2007. a
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Short summary
Ocean forecasting systems predict ocean water level, but the accuracy of predictions varies as a function of the forecast lead time and the dynamics causing water level variability. This study investigates the accuracy of predictions of tidal water levels in the AMSEAS forecast system, with emphasis on the small (roughly 5 cm) fluctuations associated with the baroclinic tide.