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Sensitivity of Turbine-Height Wind Speeds to Parameters in the Planetary Boundary-Layer Parametrization Used in the Weather Research and Forecasting Model: Extension to Wintertime Conditions

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Abstract

We extend the model sensitivity analysis of Yang et al. (Boundary-Layer Meteorol 162: 117–142, 2017) to include results for February 2011, in addition to May of the same year. We investigate the sensitivity of simulated hub-height wind speeds to the selection of 12 parameters applied in the Mellor–Yamada–Nakanishi–Niino planetary boundary-layer parametrization in the Weather Research and Forecasting model, including parameters used to represent the dissipation of turbulence kinetic energy (TKE), Prandtl number (Pr), and turbulence length scales. Differences in the sensitivity of the ensemble of simulated wind speed to the various parameters can largely be explained by changes in the static stability. The largest monthly differences are found during the day, while the sensitivity to many of the parameters during the night is similar regardless of the month. This finding is consistent with an increased frequency of daytime stable conditions in February compared to May. The spatial variability of the sensitivity to TKE dissipation and Pr can also be attributed to variability in the static stability across the domain at any point in time.

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References

  • Berg LK, Pekour M, Nelson D (2012) Description of the Columbia Basin wind energy study (CBWES). PNNL-22036. Pacific Northwest National Laboratory

  • Mesinger F, DiMego G, Kalnay E, Mitchell K, Shafran PC, Ebisuzaki W, Jović D, Woollen J, Rogers E, Berbery EH, Ek MB, Fan Y, Grumbine R, Higgins W, Li H, Lin Y, Manikin G, Parrish D, Shi W (2006) North American regional reanalysis. Bull Am Meteorol Soc 87(3):343–360

    Article  Google Scholar 

  • Nakanishi M (2001) Improvement of the Mellor-Yamada turbulence closure model based on large-eddy simulation data. Boundary-Layer Meteorol 99(3):349–378

    Article  Google Scholar 

  • Nakanishi M, Niino H (2004) An improved Mellor-Yamada level-3 model with condensation physics: its design and verification. Boundary-Layer Meteorol 112(1):1–31

    Article  Google Scholar 

  • Nakanishi M, Niino H (2009) Development of an improved turbulence closure model for the atmospheric boundary layer. J Meteorol Soc Jpn 87(5):895–912

    Article  Google Scholar 

  • Skamarock WC, Klemp JB, Dudhia J, Gill DO, Barker DM, Duda MG, Huang X-Y, Wang W, Powers JG (2008) A description of the advanced research WRF version 3. NCAR/TN-475 + STR. NCAR

  • Yang Q, Berg LK, Pekour M, Fast JD, Newsom RK, Stoelinga M, Finley C (2013) Evaluation of WRF-predicted near-hub-height winds and ramp events over a Pacific Northwest site with complex terrain. J Appl Meteorol Climatol 52:1753–1763

    Article  Google Scholar 

  • Yang B, Qian Y, Berg LK, Ma P-L, Wharton S, Bulaevskaya V, Yan H, Hou Z, Shaw WJ (2017) Sensitivity of turbine-height wind speeds to parameters in planetary boundary-layer and surface-layer schemes in the Weather Research and Forecasting model. Boundary-Layer Meteorol 162(1):117–142

    Article  Google Scholar 

Download references

Acknowledgements

This work has been supported by the U.S. Department of Energy’s Wind Power Program. The Pacific Northwest National Laboratory (PNNL) is operated for the US Department of Energy by Battelle Memorial Institute under contract DE-AC07-76RL01830. The PNNL Institutional Computing (PIC) provided computational resources. The NARR datasets were freely obtained from the CISL Research Data Archive at http://rda.ucar.edu/datasets/ds608.0/. WRF model output data used in this study are stored at PNNL and are available upon request from the corresponding author. Data from CBWES are available from the U.S. Department of Energy Atmospheric Radiation Measurement (ARM) data archive. Dr. Ben Kravitz (PNNL) is thanked for his comments on an earlier version of the manuscript.

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Correspondence to Larry K. Berg.

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Berg, L.K., Liu, Y., Yang, B. et al. Sensitivity of Turbine-Height Wind Speeds to Parameters in the Planetary Boundary-Layer Parametrization Used in the Weather Research and Forecasting Model: Extension to Wintertime Conditions. Boundary-Layer Meteorol 170, 507–518 (2019). https://doi.org/10.1007/s10546-018-0406-y

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  • DOI: https://doi.org/10.1007/s10546-018-0406-y

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