Improved atmospheric stable boundary layer formulations for Navy Seasonal Forecasting

Many large-scale weather forecast models prescribes too much turbulent mixing stably stratified conditions, which causes problems with the depth of nocturnal or high-latitude winter boundary layers, lack of inertially driven low-level wind maxima and inversion-capped low clouds. The link between the turbulent momentum flux and the associated Ekman pumping and therefore the lifetime of synopticscale weather system has so far made impossible a satisfactory solution.