Articles | Volume 19, issue 4
https://doi.org/10.5194/os-19-1123-2023
https://doi.org/10.5194/os-19-1123-2023
Research article
 | 
20 Jul 2023
Research article |  | 20 Jul 2023

Impact of sea level changes on future wave conditions along the coasts of western Europe

Alisée A. Chaigneau, Stéphane Law-Chune, Angélique Melet, Aurore Voldoire, Guillaume Reffray, and Lotfi Aouf

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Cited articles

Aarnes, O. J., Reistad, M., Breivik, Ø., Bitner-Gregersen, E., Ingolf Eide, L., Gramstad, O., Magnusson, A. K., Natvig, B., and Vanem, E.: Projected changes in significant wave height toward the end of the 21st century: Northeast Atlantic: PROJECTED CHANGES IN WAVE HEIGHT, J. Geophys. Res.-Oceans, 122, 3394–3403, https://doi.org/10.1002/2016JC012521, 2017. 
Alari, V.: Multi-Scale Wind Wave Modeling in the Baltic Sea, PhD thesis, 2013. 
Almar, R., Ranasinghe, R., Bergsma, E. W. J., Diaz, H., Melet, A., Papa, F., Vousdoukas, M., Athanasiou, P., Dada, O., Almeida, L. P., and Kestenare, E.: A global analysis of extreme coastal water levels with implications for potential coastal overtopping, Nat. Commun., 12, 3775, https://doi.org/10.1038/s41467-021-24008-9, 2021. 
Aouf, L. and Lefèvre, J.-M.: On the Impact of the Assimilation of SARAL/AltiKa Wave Data in the Operational Wave Model MFWAM, Mar. Geod., 38, 381–395, https://doi.org/10.1080/01490419.2014.1001050, 2015. 
Ardhuin, F., Rogers, E., Babanin, A. V., Filipot, J.-F., Magne, R., Roland, A., Westhuysen, A. van der, Queffeulou, P., Lefevre, J.-M., Aouf, L., and Collard, F.: Semiempirical Dissipation Source Functions for Ocean Waves. Part I: Definition, Calibration, and Validation, J. Phys. Oceanogr., 40, 1917–1941, https://doi.org/10.1175/2010JPO4324.1, 2010. 
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Short summary
Wind waves and swells are major drivers of coastal environment changes and can drive coastal marine hazards such as coastal flooding. In this paper, by using numerical modeling along the European Atlantic coastline, we assess how present and future wave characteristics are impacted by sea level changes. For example, at the end of the century under the SSP5-8.5 climate change scenario, extreme significant wave heights are higher by up to +40 % due to the effect of tides and mean sea level rise.