Applications of a moving surface drag model: From Stokes waves to offshore wind farms

@misc{ayala2026applications,
  title = {{Applications of a moving surface drag model: From Stokes waves to offshore wind farms}},
  author = {Manuel Ayala and Zein Sadek and Raul. B Cal and Dennice. F Gayme and Charles Meneveau},
  howpublished = {arXiv},
  year = {2026},
  month = sep,
  doi = {10.48550/arxiv.2609.22448},
  eprint = {2609.22448},
  archivePrefix = {arXiv},
  url = {https://arxiv.org/abs/2609.22448},
  note = {CC BY 4.0},
}

TY  - UNPB
TI  - Applications of a moving surface drag model: From Stokes waves to offshore wind farms
AU  - Manuel Ayala
AU  - Zein Sadek
AU  - Raul. B Cal
AU  - Dennice. F Gayme
AU  - Charles Meneveau
PY  - 2026
DA  - 2026/09/18
PB  - arXiv
DO  - 10.48550/arxiv.2609.22448
UR  - https://arxiv.org/abs/2609.22448
AB  - Offshore wind farms operate within the marine atmospheric boundary layer, where ocean waves can modify air-sea momentum transfer, turbine inflow, and wake recovery. Wave-resolved simulations can capture phase-dependent wind--wave interactions, but their computational cost and implementation complexity limit their use in large atmospheric and wind-farm domains. This study describes applications and tests of the recently proposed moving surface drag (MOSD) model, a flat-bottom wall-stress formulation for horizontally resolved moving waves, to a sequence of increasingly complex wind--wave and offshore wind-energy applications. The model is first evaluated for turbulent flow over Stokes-like waves using laboratory measurements, where it reproduces mean velocity profiles and captures the qualitative structure of wave-induced motions, although their amplitude is underpredicted. MOSD is then applied to broadband wave spectra fields and offshore wind-farm boundary layers, showing good agreement with mean velocity profiles from wave-resolved simulations across different wave ages, grid resolutions, and turbine spacings. Finally, exploratory offshore wind-farm simulations using MOSD under conventionally neutral conditions demonstrate its application at wind-farm scale. Large-scale waves leave detectable signatures in near-surface velocity spectra, but these signatures decay with height and do not produce clear peaks in temporal spectra of aggregate turbine power. Overall, the results demonstrate that the MOSD model provides a tractable framework for incorporating resolved wave effects in wind-wave and offshore wind-farm simulations.
ER  -