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Improved Atmospheric Stable Boundary Layer Formulations for Navy Seasonal Forecasting

Abstract : Most weather forecast models prescribes too much turbulent mixing in 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 synoptic-scale weather system has so far made impossible a satisfactory solution.