Articles | Volume 16
Adv. Sci. Res., 16, 11–29, 2019
Adv. Sci. Res., 16, 11–29, 2019
22 Mar 2019
22 Mar 2019

Teleconnections and Extreme Ocean States in the Northeast Atlantic Ocean

Emily Gleeson et al.

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Cited articles

Ardhuin, F., Rogers, E., Babanin, A. V., Filipot, J.-F., Magne, R., Roland, A., van der Westhuysen, A., 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,, 2010. a
Atan, R., Goggins, J., and Nash, S.: A Detailed Assessment of the Wave Energy Resource at the Atlantic Marine Energy Test Site, Energies, 9, 967,, 2016. a, b
Barnston, A. and Livezey, E.: Classification, seasonality and persistence of low-frequency atmospheric circulation patterns, Mon. Weather Rev., 115, 1083–1126, 1987. a, b
Bertin, X., Prouteau, E., and Letetrel, C.: A significant increase in waveheight in the North Atlantic Ocean over the 29th century, Global Planet. Change, 106, 77–83, 2013. a
Bueh, C. and Nakamura, H.: Scandinavian pattern and its climatic impact, Q. J. Roy. Meteor. Soc., 133, 2117–2131,, 2007. a
Short summary
The Northeast Atlantic possesses an energetic and variable wind and wave climate which has a large potential for renewable energy extraction. The role of surface winds in the generation of ocean waves means that global atmospheric circulation patterns and wave climate characteristics are inherently connected. In this study we investigated the influence of large scale atmospheric oscillations on waves in the Northeast Atlantic using a high resolution wave projection dataset.