Articles | Volume 19, issue 15
https://doi.org/10.5194/gmd-19-7369-2026
https://doi.org/10.5194/gmd-19-7369-2026
Development and technical paper
 | 
10 Aug 2026
Development and technical paper |  | 10 Aug 2026

Implementation of a three-dimensional planetary boundary layer parameterization in a coupled modeling system and evaluation of “gray zone” simulations of a wind-wave event off the US California Coast using observations

Eric A. Hendricks, Timothy W. Juliano, Branko Kosović, Sue Ellen Haupt, Brian J. Gaudet, and Geng Xia

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Cited articles

Burk, S. D. and Thompson, W. T.: The summertime low-level jet and marine boundary layer structure along the California coast, Mon. Weather Rev., 124, 668–686, https://doi.org/10.1175/1520-0493(1996)124<0668:TSLLJA>2.0.CO;2, 1996. a
Charnock, H.: Wind stress on a water surface, Q. J. Roy. Meteorol. Soc., 81, 639–640, 1955. a
Deskos, G., Lee, J. C. Y., Draxl, C., and Sprague, M. A.: Review of wind–wave coupling models for large-eddy simulation of the marine atmospheric boundary layer, J. Atmos. Sci., 78, 3025–3045, https://doi.org/10.1175/JAS-D-21-0003.1, 2021. a
DOI-USGS: COAWST, GitHub [code], https://github.com/jcwarner-usgs/COAWST.git (last access: 31 July 2026), 2026. a
Drennan, W. M., Graber, H. C., Hauser, D., and Quentin, C.: On the wave age dependence of wind stress over pure wind seas, J. Geophys. Res.-Oceans, 108, https://doi.org/10.1029/2000JC000715, 2003. a
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Short summary
A three-dimensional planetary boundary layer (PBL) parameterization, suited for mesoscale model grid spacings of 100–1000 m with improved treatment of unresolved horizontal mixing, is added to a coupled atmosphere/wave modeling system and the first coupled simulations are executed using the parameterization. Simulations of a significant wind-wave event demonstrate that the new parameterization has similar behaviors as one-dimensional PBL parameterizations and compares well with observations.
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