Coupling Mesoscale Budget Components to Large-Eddy Simulations for Wind-Energy Applications

Journal Article (2021)
Author(s)

Caroline Draxl (National Renewable Energy Laboratory)

D.J.N. Allaerts (National Renewable Energy Laboratory, TU Delft - Wind Energy)

Eliot Quon (National Renewable Energy Laboratory)

Matt Churchfield (National Renewable Energy Laboratory)

Research Group
Wind Energy
Copyright
© 2021 Caroline Draxl, D.J.N. Allaerts, Eliot Quon, Matt Churchfield
DOI related publication
https://doi.org/10.1007/s10546-020-00584-z
More Info
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Publication Year
2021
Language
English
Copyright
© 2021 Caroline Draxl, D.J.N. Allaerts, Eliot Quon, Matt Churchfield
Research Group
Wind Energy
Bibliographical Note
Green Open Access added to TU Delft Institutional Repository ‘You share, we take care!’ – Taverne project https://www.openaccess.nl/en/you-share-we-take-care Otherwise as indicated in the copyright section: the publisher is the copyright holder of this work and the author uses the Dutch legislation to make this work public. @en
Issue number
1
Volume number
179
Pages (from-to)
73-98
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Abstract

To simulate the airflow through a wind farm across a wide range of atmospheric conditions, microscale models (e.g., large-eddy simulation, LES, models) have to be coupled with mesoscale models, because microscale models lack the atmospheric physical processes to represent time-varying local forcing. Here we couple mesoscale model outputs to a LES solver by applying mesoscale momentum- and temperature-budget components from the Weather Research and Forecasting model to the governing equations of the Simulator fOr Wind Farm Applications model. We test whether averaging the budget components affects the LES results with regard to quantities of interest to wind energy. Our study focuses on flat terrain during a quiescent diurnal cycle. The simulation results are compared with observations from a 200-m tall meteorological tower and a wind-profiling radar, by analyzing time series, profiles, rotor-averaged quantities, and spectra. While results show that averaging reduces the spatio-temporal variability of the mesoscale momentum-budget components, when coupled with the LES model, the mesoscale bias (in comparison with observations of wind speed and direction, and potential temperature) is not reduced. In contrast, the LES technique can correct for shear and veer. In both cases, however, averaging the budget components shows no significant impact on the mean flow quantities in the microscale and is not necessary when coupling mesocale budget components to the LES model.

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