Boundary Layer (BL) parameterization plays a crucial role in numerical weather models by integrating the effects of small-scale turbulent motions on larger-scale prognostic variables at grid resolution. It accounts for turbulent transport of temperature, moisture, and momentum, which are essential for improving model accuracy. The ultimate goal of BL parameterization is to correct the model output to better reflect real atmospheric conditions. Evaluating aspects of the BL, such as the 2-meter temperature, helps enhance forecasts and improve model performance.