Abstract: Based on observations by a dual-thodolite anemometer tracking balanced balloons and an American Gill UVW anemogtaph for complccatedeunderlying surface in Meizhou,eastern Guangdong,turbulent fluctuations of the Lagrangina and Eulerian systems are determined for the area.Following the Taylor formular in respecttto a few reference frames,horizontal and vertical turbulence intensity and atmospheric diffusion parameters σ_y and σ_x are then computed and compered with those obtained by the PG method ann BNL experiments. It is found that within heights less than 100m above the ground σ_y aegeσ_x are larger than values of PG and BNL with all conditions of stability and siratification.