The 3D PBL parameterization is based on the turbulence model of Mellor and Yamada. Our implementation in the Weather Research and Forecasting model uses an algebraical model (Level 2) to diagnose the turbulent fluxes. The divergence of these fluxes provides the tendencies related to 3D turbulent mixing of the resolved variables.
An idealized numerical experiment has been designed to quantify the benefits of the 3D representation. The case prescribes a surface heat flux heterogeneity in the North to South direction and initial meridional winds. Under this set up, the solution should be homogeneous in the North to South direction. Three simulations are performed. The first one uses a standard 1D PBL parameterization in conjunction with horizontal diffusion. The second experiment uses our 3D PBL parameterization. The two experiments use a grid spacing of 200 m. To complement the previous simulations, the third experiment consists of an ensemble of large-eddy simulations using 40 m grid cell size. It will be shown that accounting for the horizontal turbulent fluxes in the 3D PBL parameterization is necessary to ensure the homogeneous North-to-South solution. These results suggest that is possible to remove current inconsistencies in the treatment of vertical and horizontal mixing with a 3D PBL parameterization.