Articles | Volume 18, issue 6
https://doi.org/10.5194/os-18-1665-2022
https://doi.org/10.5194/os-18-1665-2022
Research article
 | 
22 Nov 2022
Research article |  | 22 Nov 2022

Accuracy of numerical wave model results: application to the Atlantic coasts of Europe

Matias Alday, Fabrice Ardhuin, Guillaume Dodet, and Mickael Accensi

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Cited articles

Accensi, M., Alday, M., Maisondieu, C., Raillard, N., Darbynian, D., Old, C., Sellar, B., Thilleul, O., Perignon, Y., Payne, G., O'Boyle, L., Fernandez, L., Dias, F., Chumbinho, R., and Guitton, G.: ResourceCODE framework: A high-resolution wave parameter dataset for the European Shelf and analysis toolbox, https://archimer.ifremer.fr/doc/00736/84812/ (last access: 12 March 2022), 2021. a, b
Alday, M., Accensi, M., Ardhuin, F., and Dodet, G.: A global wave parameter database for geophysical applications. Part 3: Improved forcing and spectral resolution, Ocean Model., 166, 101848, https://doi.org/10.1016/j.ocemod.2021.101848, 2021. a, b, c, d, e, f, g, h
Alves, J.-H. G. M., Wittmann, P., Sestak, M., Schauer, J., Stripling, S., Bernier, N. B., McLean, J., Chao, Y., Chawla, A., Tolman, H., Nelson, G., and Klotz, S.: The NCEP-FNMOC Combined Wave Ensemble Product: Expanding Benefits of Interagency Probabilistic Forecasts to the Oceanic Environment, B. Am. Meterol. Soc., 94, 1893–1905, https://doi.org/10.1175/BAMS-D-12-00032.1, 2013. a
Ardhuin, F. and Roland, A.: Coastal wave reflection, directional spreading, and seismo-acoustic noise sources, J. Geophys. Res., 117, C00J20, https://doi.org/10.1029/2011JC007832, 2012. a
Ardhuin, F., O'Reilly, W. C., Herbers, T. H. C., and Jessen, P. F.: Swell transformation across the continental shelf. Part I: Attenuation and directional broadening, J. Phys. Oceanogr., 33, 1921–1939, https://doi.org/10.1175/1520-0485(2003)033<1921:STATCS>2.0.CO;2, 2003. a, b, c
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Short summary
Obtaining accurate results from wave models in coastal regions is typically more difficult. This is due to the complex interactions between waves and the local environment characteristics like complex shorelines, sea bottom topography, the presence of strong currents, and other processes that include wave growth and decay. In the present study we analyze which elements can be adjusted and/or included in order to reduce errors in the modeled output.