Articles | Volume 9, issue 8
https://doi.org/10.5194/wes-9-1727-2024
https://doi.org/10.5194/wes-9-1727-2024
Research article
 | 
19 Aug 2024
Research article |  | 19 Aug 2024

Underestimation of strong wind speeds offshore in ERA5: evidence, discussion and correction

Rémi Gandoin and Jorge Garza

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Cited articles

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, 101848–10167, https://doi.org/10.1016/j.ocemod.2021.101848, 2021. 
Araújo da Silva, M. P., Rocadenbosch, F., Farré-Guarné, J., Salcedo-Bosch, A., González-Marco, D., and Peña, A.: Assessing Obukhov Length and Friction Velocity from Floating Lidar Observations: A Data Screening and Sensitivity Computation Approach, Remote Sens., 14, 1394, https://doi.org/10.3390/rs14061394, 2022. 
Ayet, A. and Chapron, B.: The dynamical coupling of wind-waves and atmospheric turbulence: a review of theoretical and phenomenological models, Bound.-Lay. Meteorol., 183, 1–33, https://doi.org/10.1007/s10546-021-00666-6, 2022. 
Bentamy, A., Grodsky, S. A., Cambon, G., Tandeo, P., Capet, X., Roy, C., Herbette, S., and Grouazel, A.: Twenty-Seven Years of Scatterometer Surface Wind Analysis over Eastern Boundary Upwelling Systems, Remote Sens., 13, 940, https://doi.org/10.3390/rs13050940, 2021. 
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ERA5 has become the workhorse of most wind resource assessment applications, as it compares better with in situ measurements than other reanalyses. However, for design purposes, ERA5 suffers from a drawback: it underestimates strong wind speeds offshore (approx. from 10 m s−1). This is not widely discussed in the scientific literature. We address this bias and proposes a simple, robust correction. This article supports the growing need for use-case-specific validations of reanalysis datasets.
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