Online model calibration for a simplified LES model in pursuit of real-time closed-loop wind farm control

Journal Article (2018)
Author(s)

B.M. Doekemeijer (TU Delft - Team Jan-Willem van Wingerden)

Sjoerd Boersma (TU Delft - Team Jan-Willem van Wingerden)

Lucy Y. Pao (University of Colorado)

Torben Knudsen (Aalborg University)

Jan Willem Van Wingerden (TU Delft - Team Jan-Willem van Wingerden)

Research Group
Team Jan-Willem van Wingerden
Copyright
© 2018 B.M. Doekemeijer, S. Boersma, Lucy Y. Pao, Torben Knudsen, J.W. van Wingerden
DOI related publication
https://doi.org/10.5194/wes-3-749-2018
More Info
expand_more
Publication Year
2018
Language
English
Copyright
© 2018 B.M. Doekemeijer, S. Boersma, Lucy Y. Pao, Torben Knudsen, J.W. van Wingerden
Related content
Research Group
Team Jan-Willem van Wingerden
Issue number
2
Volume number
3
Pages (from-to)
749-765
Reuse Rights

Other than for strictly personal use, it is not permitted to download, forward or distribute the text or part of it, without the consent of the author(s) and/or copyright holder(s), unless the work is under an open content license such as Creative Commons.

Abstract

Wind farm control often relies on computationally inexpensive surrogate models to predict the dynamics inside a farm. However, the reliability of these models over the spectrum of wind farm operation remains questionable due to the many uncertainties in the atmospheric conditions and tough-to-model dynamics at a range of spatial and temporal scales relevant for control. A closed-loop control framework is proposed in which a simplified model is calibrated and used for optimization in real time. This paper presents a joint state-parameter estimation solution with an ensemble Kalman filter at its core, which calibrates the surrogate model to the actual atmospheric conditions. The estimator is tested in high-fidelity simulations of a nine-turbine wind farm. Exclusively using measurements of each turbine's generated power, the adaptability to modeling errors and mismatches in atmospheric conditions is shown. Convergence is reached within 400 s of operation, after which the estimation error in flow fields is negligible. At a low computational cost of 1.2 s on an 8-core CPU, this algorithm shows comparable accuracy to the state of the art from the literature while being approximately 2 orders of magnitude faster.