Articles | Volume 18, issue 14
https://doi.org/10.5194/gmd-18-4499-2025
https://doi.org/10.5194/gmd-18-4499-2025
Model evaluation paper
 | 
24 Jul 2025
Model evaluation paper |  | 24 Jul 2025

Low-level jets in the North and Baltic seas: mesoscale model sensitivity and climatology using WRF V4.2.1

Bjarke T. E. Olsen, Andrea N. Hahmann, Nicolas G. Alonso-de-Linaje, Mark Žagar, and Martin Dörenkämper

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Cited articles

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Baas, P., Bosveld, F. C., Baltink, H. K., and Holtslag, A. A.: A climatology of nocturnal low-level jets at Cabauw, J. Appl. Meteorol. Climatol., 48, 1627–1642, https://doi.org/10.1175/2009JAMC1965.1, 2009. a, b, c
Blackadar, A. K.: Boundary layer wind maxima and their significance for the growth of nocturnal inversions, B. Am. Meteorol. Soc., 38, 283–290, 1957. a, b, c
Bougeault, P. and Lacarrere, P.: Parameterization of Orography-Induced Turbulence in a Mesobeta–Scale Model, Mon. Weather Rev., 117, 1872– 1890, https://doi.org/10.1175/1520-0493(1989)117<1872:POOITI>2.0.CO;2, 1989. a, b
Capon, R. A.: Wind speed-up in the Dover Straits with the Met Office New Dynamics model, Meteorol. Appl., 10, 229–237, https://doi.org/10.1017/S1350482703003037, 2003. a, b, c
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Short summary
Low-level jets (LLJs) are strong winds in the lower atmosphere that are important for wind energy as turbines get taller. This study compares a weather model (WRF) with real data across five North and Baltic Sea sites. Adjusting the model improved accuracy over the widely used ERA5. In key offshore regions, LLJs occur 10–15 % of the time and significantly boost wind power, especially in spring and summer, contributing up to 30 % of total capacity in some areas.
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