Measurements from WFIP2 profiling instruments in the Columbia River Basin indicate a propensity of the HRRR model to prematurely erode cold, stably stratified low-level air, often contributing to significant errors in turbine-height wind speed forecasts. To help mitigate this problem, the MYNN scheme in the HRRRWFIP2 contains experimental modifications designed to improve the representation of local mixing within the planetary boundary layer and free atmosphere. These modifications include (1) a revision of the MYNN buoyancy length scale, (2) elimination of the influence of the surface-layer length scale at heights away from the ground, and (3) a reformulation of the MYNN master-length-scale blending approach. Drawing from wind-ramp events sampled during the WFIP2 field campaign, we examine case studies that demonstrate improved wind-forecast skill stemming from these MYNN scheme modifications in stably stratified flow. Results from reforecasts in the 3-km HRRRWFIP2 and its concurrent 750-m nest will be presented, along with long-term verification statistics.
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