The impact of wave model source terms and coupling strategies to rapidly developing waves across the north-west European shelf during extreme events

Valiente, Nieves G.; Saulter, Andrew; Edwards, John M.; Lewis, Huw W.; Castillo Sanchez, Juan M. Castillo; Bruciaferri, Diego; Bunney, Christopher; Siddorn, John ORCID: https://orcid.org/0000-0003-3848-8868. 2021 The impact of wave model source terms and coupling strategies to rapidly developing waves across the north-west European shelf during extreme events. Journal of Marine Science and Engineering, 9 (4), 403. https://doi.org/10.3390/jmse9040403

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Abstract/Summary

Prediction of severe natural hazards requires accurate forecasting systems. Recently, there has been a tendency towards more integrated solutions, where different components of the Earth system are coupled to explicitly represent the physical feedbacks between them. This study focuses on rapidly developing waves under extratropical storms to understand the impact of different wave source term parameterisations in the WAVEWATCH III (WWIII) model (ST4 and ST6) and coupling strategies (surface roughness closure versus surface stress closure) on the accuracy of the Met Office regional atmosphere‑ocean‑wave coupled research system for the north‑west (NW) European shelf (UKC4). Results of a study focused on simulations during winter 2013/14 demonstrate that ST6 allows for a faster wave growth than the ST4 parameterisation but might degrade low to mid energy wave states. The difference between ST6 and ST4 in wave growth is larger for higher wind speeds and short fetches. The experiment with ST4 and roughness closure consistently under‑predicts the wave growth in those locations where fetch dependence is an important factor (i.e., seas at the East (E) of Ireland and the UK for storms coming from the NW‑WNW). The implementation in the wave model of ST6 physics with the stress closure coupling strategy appears to improve growth of young wind‑seas, reducing bias in those locations where the storms are underestimated. The slower wave growth when using surface roughness closure seems to be related to an underestimation of the momentum transfer computed by the wave model when coupling the wind speeds. For very young to young wind seas, this can be overcome when the surface stress is computed by the atmospheric model and directly passed to the ocean.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.3390/jmse9040403
ISSN:	2077-1312
Date made live:	12 Apr 2021 10:10 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/530029

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