Preprints
https://doi.org/10.5194/wes-2023-71
https://doi.org/10.5194/wes-2023-71
07 Jul 2023
 | 07 Jul 2023
Status: a revised version of this preprint is currently under review for the journal WES.

Tropical cyclone low-level wind speed, shear, and veer: sensitivity to the boundary layer parameterization in WRF

Sara Müller, Xiaoli Guo Larsén, and David Verelst

Abstract. Mesoscale modeling can be used to analyze key parameters for wind turbine load assessment in a large variety of tropical cyclones. However, the modeled wind structure of tropical cyclones is known to be sensitive to the boundary layer scheme. We analyze modeled wind speed, shear, and wind veer across a wind turbine rotor plane in the eyewall and rainband region. We further assess the sensitivity of wind speed, shear, and veer to the boundary layer parameterization. Three model realizations of typhoon Megi over the open ocean using three frequently used boundary layer schemes in the Weather Research and Forecasting model are analyzed. All three typhoon simulations reasonably reproduce the cyclone track and structure. The boundary layer parametrization causes up to 21 % differences in median hub height wind speed between the simulations. The simulated wind speed variability is further dependent on the boundary layer scheme. The modeled wind shear is smaller or equal to the current IEC standard regardless of the boundary layer scheme for the eyewall and rainband region. While the surface inflow angle is sensitive to the boundary layer simulation, wind veer in the lowest 400 m of the atmospheric boundary layer is less affected by the boundary layer parametrization. Simulated wind veer reaches values up to 1.8 × 10⁻² ° m ⁻¹ (1.1 × 10 ⁻² ° m ⁻¹) in the eyewall region (rainband region) and is relatively small compared to moderate wind speed regimes. On average, simulated wind speed shear and wind veer are highest in the eyewall region. Yet strong spatial organization of wind shear and veer along the rainbands may increase wind turbine loads, due to rapid coherent wind profile changes at the turbine location.

Sara Müller, Xiaoli Guo Larsén, and David Verelst

Status: final response (author comments only)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on wes-2023-71', Anonymous Referee #1, 22 Jul 2023
    • AC1: 'Reply on RC1 and RC2', Sara Müller, 24 Nov 2023
  • RC2: 'Comment on wes-2023-71', Anonymous Referee #2, 20 Oct 2023
    • AC1: 'Reply on RC1 and RC2', Sara Müller, 24 Nov 2023
Sara Müller, Xiaoli Guo Larsén, and David Verelst
Sara Müller, Xiaoli Guo Larsén, and David Verelst

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Short summary
Tropical cyclone winds are challenging for wind turbines. We analyze a tropical cyclone before landfall in a mesoscale model. The simulated wind speeds and the storm structure are sensitive to the boundary parametrization. However, independent of the boundary layer parametrization the change in wind speed and wind direction with height are small relative to wind turbine design standards. Spatial organization of the wind field along the rainbands may cause rapid changes at a turbine location.
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