Abstract: The structure of the boundary layer for the process of the strong weather after the passage of a cold front is discussed, using the data of the acoustic radar,the temperature and the wind speed obtained from the 80 meters meteorological tower, and the radiosonde sounding and the analyses of the weather maps. It is shown that the formation of the strong wind is closely correlated to the subsidence of the upper cold air, as swell as the process of the boundary layer. The analytical results indicate that the weather process of the strong wind is formed probably by the interaction of the momentum flux with the haat flux due to the subsidence of the cold air in the boundary layer.