Advances in Science and Research
Advances in Science and Research
ASR
Articles | Volume 13
Articles | Volume 13
https://doi.org/10.5194/asr-13-107-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/asr-13-107-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Articles | Volume 13
08 Jul 2016
 | 08 Jul 2016

Influence of sea surface roughness length parameterization on Mistral and Tramontane simulations

Anika Obermann, Benedikt Edelmann, and Bodo Ahrens

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Latest update: 21 Nov 2024
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Short summary
Simulated surface winds in atmospheric models depend, among others, on the parameterization of the sea surface roughness. Three parameterizations (variation of Charnock parameter) were tested in the western Mediterranean area during Mistral events with the regional climate model COSMO-CLM. While the whole sea level pressure pattern did not change much, a larger Charnock parameter led to lower wind speeds and a rotation of the wind direction.
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