A simulation study on risks to wind turbine arrays from thunderstorm downbursts in different atmospheric stability conditions

Journal Article (2021)
Author(s)

Nan You Lu (National Taiwan University)

Lance Manuel (The University of Texas at Austin)

Patrick Hawbecker (University Corporation for Atmospheric Research)

Sukanta Basu (TU Delft - Atmospheric Remote Sensing)

DOI related publication
https://doi.org/10.3390/en14175407 Final published version
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Publication Year
2021
Language
English
Issue number
17
Volume number
14
Article number
5407
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Abstract

Thunderstorm downbursts have been reported to cause damage or failure to wind turbine arrays. We extend a large-eddy simulation model used in previous work to generate downburst-related inflow fields with a view toward defining correlated wind fields that all turbines in an array would experience together during a downburst. We are also interested in establishing what role contrasting atmospheric stability conditions can play on the structural demands on the turbines. This interest is because the evening transition period, when thunderstorms are most common, is also when there is generally acknowledged time-varying stability in the atmospheric boundary layer. Our results reveal that the structure of a downburst’s ring vortices and dissipation of its outflow play important roles in the separate inflow fields for turbines located at different parts of the array; these effects vary with stability. Interacting with the ambient winds, the outflow of a downburst is found to have greater impacts in an “average” sense on structural loads for turbines farther from the touchdown center in the stable cases. Worst-case analyses show that the largest extreme loads, although somewhat dependent on the specific structural load variable considered, depend on the location of the turbine and on the prevailing atmospheric stability. The results of our calculations show the highest simulated foreaft tower bending moment to be 85.4 MN-m, which occurs at a unit sited in the array farther from touchdown center of the downburst initiated in a stable boundary layer.