3.9 Article

WRF-simulated low-level jets over Iowa: characterization and sensitivity studies

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WIND ENERGY SCIENCE
卷 6, 期 4, 页码 1015-1030

出版社

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/wes-6-1015-2021

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  1. US Department of Energy, Office of Science [DE-SC0016438, DE-SC0016605, DE-AC02-05CH11231]
  2. National Science Foundation, Directorate for Education and Human Resources [DGE-1650441]
  3. National Science Foundation, Directorate for Computer and Information Science and Engineering [ACI-1541215, TG-ATM170024]

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Output from 6 months of high-resolution simulations with the Weather Research and Forecasting (WRF) model were analyzed to characterize local low-level jets (LLJs) over Iowa for winter and spring. The results indicate that LLJs are most frequently associated with nocturnal stable stratification and low turbulent kinetic energy, which makes them more common during the winter months. Sensitivity analyses showed that LLJ characteristics are highly variable with different definitions, but implementing polynomial interpolation reduced sensitivity of LLJ characteristics to down-sampling.
Output from 6 months of high-resolution simulations with the Weather Research and Forecasting (WRF) model are analyzed to characterize local low-level jets (LLJs) over Iowa for winter and spring in the contemporary climate. Low-level jets affect rotor plane aerodynamic loading, turbine structural loading and turbine performance, and thus accurate characterization and identification are pertinent. Analyses using a detection algorithm wherein the wind speed above and below the jet maximum must be below 80% of the jet wind speed within a vertical window of approximately 20-530ma.g.l. (above ground level) indicate the presence of an LLJ in at least one of the 14 700 4km x 4km grid cells over Iowa on 98% of nights. Nocturnal LLJs are most frequently associated with stable stratification and low turbulent kinetic energy (TKE) and hence are more frequent during the winter months. The spatiotemporal mean LLJ maximum (jet core) wind speed is 9.55ms(-1), and the mean height is 182 m. Locations of high LLJ frequency and duration across the state are seasonally varying, with a mean duration of 3.5 h. The highest frequency occurs in the topographically complex northwest of the state in winter and in the flatter northeast of the state in spring. Sensitivity of LLJ characteristics to the (i) LLJ definition and (ii) vertical resolution at which the WRF output is sampled is examined. LLJ definitions commonly used in the literature are considered in the first sensitivity analysis. These sensitivity analyses indicate that LLJ characteristics are highly variable with definition. Use of different definitions identifies both different frequencies of LLJs and different LLJ events. Further, when the model output is down-sampled to lower vertical resolution, the mean jet core wind speed height decreases, but spatial distributions of regions of high frequency and duration are conserved. Implementation of a polynomial interpolation to extrapolate down-sampled output to full-resolution results in reduced sensitivity of LLJ characteristics to down-sampling.

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