4.7 Article

Impact of physical parameterizations on wind simulation with WRF V3.9.1.1 under stable conditions at planetary boundary layer gray-zone resolution: a case study over the coastal regions of North China

Journal

GEOSCIENTIFIC MODEL DEVELOPMENT
Volume 15, Issue 21, Pages 8111-8134

Publisher

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/gmd-15-8111-2022

Keywords

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Funding

  1. National Natural Science Foundation of China [42088101, 42075168]
  2. Technology Innovation Guidance Program of Hebei Province [21475401D]
  3. National Key Research and Development Program of China [2020YFF0304401]

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This study investigates the impact of different physical parameterizations on the simulation of wind fields under stable weather conditions. The results show that the planetary boundary layer (PBL) schemes have the greatest influence on wind speed simulation, followed by shortwave-longwave radiation (SW-LW) schemes and microphysics (MP) schemes. The MYJ scheme exhibits the best temporal correlation with observed wind speed among all PBL schemes. The performance of the WRF model is found to be better for coastal stations compared to inland stations.
Reliable simulation of wind fields under stable weather conditions is vital for preventing air pollution. In this study, we investigate how different physical parameterizations impact simulated near-surface wind at 10m height over the coastal regions of North China using the Weather Research and Forecasting (WRF) model with a horizontal grid spacing of 0.5 km. We performed 640 simulations using combinations of 10 planetary boundary layer (PBL), 16 microphysics (MP), and four shortwave-longwave radiation (SW-LW) schemes. Model performance is evaluated using measurements from 105 weather station observations. The results show that the WRF model can reproduce the temporal variation of wind speed in a reasonable way. The simulated wind speed is most sensitive to the PBL schemes, followed by SW-LW schemes and MP schemes. Among all PBL schemes, the MYJ scheme shows the best temporal correlation with the observed wind speed, while the Yonsei University (YSU) scheme has the lowest model bias. DudhiaRRTM and MYDM7 show the best model performances out of all SW-LW and MP schemes, respectively, and the interactions among schemes also have large influences on wind simulation. Further investigation indicates that model sensitivity is also impacted by ocean proximity and elevation. For example, for coastal stations, MYNN shows the best correlation with observations among all PBL schemes, while God- dard shows the smallest bias of SW-LW schemes; these results are different from those of inland stations. In general, according to the bias metrics, WRF simulates wind speed less accurately for inland stations compared to coastal stations, and the model performance tends to degrade with increasing elevation. The WRF model shows worse performance in simulating wind direction under stable conditions over the study area, with lower correlation scores compared to wind speed. Our results indicate the role parameterizations play in wind simulation under stable weather conditions and provide a valuable reference for further research in the study area and nearby regions.

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