Improving Wind Energy Forecasting through Numerical Weather Prediction Model Development

Author:

Olson Joseph B.1,Kenyon Jaymes S.1,Djalalova Irina1,Bianco Laura1,Turner David D.2,Pichugina Yelena1,Choukulkar Aditya1,Toy Michael D.1,Brown John M.2,Angevine Wayne M.1,Akish Elena3,Bao Jian-Wen2,Jimenez Pedro4,Kosovic Branko4,Lundquist Katherine A.5,Draxl Caroline6,Lundquist Julie K.7,McCaa Jim8,McCaffrey Katherine1,Lantz Kathy1,Long Chuck1,Wilczak Jim2,Banta Robert2,Marquis Melinda2,Redfern Stephanie7,Berg Larry K.9,Shaw Will9,Cline Joel10

Affiliation:

1. Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, and National Oceanic and Atmospheric Administration/Earth System Research Laboratory, Boulder, Colorado

2. National Oceanic and Atmospheric Administration/Earth System Research Laboratory, Boulder, Colorado

3. Science and Technology Corporation, Boulder, Colorado

4. National Center for Atmospheric Research, Boulder, Colorado

5. Lawrence Livermore National Laboratory, Livermore, California

6. National Renewable Energy Laboratory, Golden, Colorado

7. Department of Atmospheric and Oceanic Sciences, University of Colorado Boulder, Boulder, and National Renewable Energy Laboratory, Golden, Colorado

8. Vaisala, Inc., Seattle, Washington

9. Pacific Northwest National Laboratory, Richland, Washington

10. National Oceanic and Atmospheric Administration/National Weather Service, Washington, D.C.

Abstract

AbstractThe primary goal of the Second Wind Forecast Improvement Project (WFIP2) is to advance the state-of-the-art of wind energy forecasting in complex terrain. To achieve this goal, a comprehensive 18-month field measurement campaign was conducted in the region of the Columbia River basin. The observations were used to diagnose and quantify systematic forecast errors in the operational High-Resolution Rapid Refresh (HRRR) model during weather events of particular concern to wind energy forecasting. Examples of such events are cold pools, gap flows, thermal troughs/marine pushes, mountain waves, and topographic wakes. WFIP2 model development has focused on the boundary layer and surface-layer schemes, cloud–radiation interaction, the representation of drag associated with subgrid-scale topography, and the representation of wind farms in the HRRR. Additionally, refinements to numerical methods have helped to improve some of the common forecast error modes, especially the high wind speed biases associated with early erosion of mountain–valley cold pools. This study describes the model development and testing undertaken during WFIP2 and demonstrates forecast improvements. Specifically, WFIP2 found that mean absolute errors in rotor-layer wind speed forecasts could be reduced by 5%–20% in winter by improving the turbulent mixing lengths, horizontal diffusion, and gravity wave drag. The model improvements made in WFIP2 are also shown to be applicable to regions outside of complex terrain. Ongoing and future challenges in model development will also be discussed.

Publisher

American Meteorological Society

Subject

Atmospheric Science

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