## An atmospheric boundary layer model forced by the operational ECMWF - model |

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12 hours 3-dimensional model 50 meters albedo approximate ATMOSPHERIC BOUNDARY LAYER average mixing ratio average potential temperature BL average potential BL height boundary layer height boundary layer model Bowen ratio bulk Richardson number cloud physics computed constant cooling Deardorff 1972 dewpoint temperature diurnal range ECMWF ECMWF-model Equation of difference Equation of energy evaporation forecasts geostrophic wind ground heat conduction height h Horizontal advections July and August lapse rate large scale model latent heat flux low clouds MAE BL-model meter level meter temperature mixing ratio qm night positive bias precipitation predictions present model put equal radiative relative humidity roughness parameter second term sensible heat flux simulations snow soil humidity solar radiation specific heat capacity stable BL surface temperature temperature and mixing tial temperature tion top of BL turbulent unstable BL unstable boundary layer upper level upper model level vertical BL average vertical velocity wind speed Z A Experiment