The land surface process of the Qinghai-Xizang （Tibet） Plateau has an important impact on China's weather and climate.Mount Emei is in the southeast edge of the Qinghai-Xizang （Tibet） Plateau.It is necessary place for the eastward movement of the plateau system， and the place where the southwest vortex begins to develop.Based on the atmospheric boundary layer gradient tower data， radiation observation data and surface flux data of Emeishan station on the eastern edge of Qinghai-Xizang （Tibet） Plateau from December 2019 to November 2020， this paper uses the eddy correlation method to analyze the changes of surface flux and evapotranspiration near the surface layer in Emeishan area， and estimates the zero plane displacement， aerodynamic roughness， aerothermal roughness Kinetic and thermodynamic parameters such as momentum flux transport coefficient and sensible heat flux transport coefficient.The main conclusions are as follows： The temperature in the canopy is higher than that in the canopy during the day， but the opposite at night.The relative humidity in the canopy is higher than that on the canopy， and the diurnal variation of wind speed near the ground is more obvious in the upper layer than that in the lower layer.The seasonal variation characteristics of near ground temperature， relative humidity and wind speed are obvious.The vertical wind profile has significantly different correlation and inflection point phenomenon in the canopy and above the canopy.The growth rate of wind speed below the inflection point with height is significantly smaller than that above the inflection point.The annual average value of zero plane displacement d is 10.45 m； The annual mean values of aerodynamic roughness Z _0m and thermodynamic roughness roughness Z _0h are 1.65 m and 9.95 m respectively.The annual average values of momentum flux transport coefficient C_D and sensible heat flux transport coefficient C_H are 1.58×10^-2 and 3.79×10^-3 respectively.Aerodynamic roughness fluctuates greatly with season， while aerothermodynamic roughness is opposite.The occurrence times and amount of precipitation have obvious seasonal changes.There are more precipitation days and precipitation in July， and the daily change of precipitation is obvious， showing the typical characteristics of night rain in Western Sichuan Basin.The daily variation amplitude of sensible heat flux and latent heat flux is large.The latent heat flux is dominant in summer and sensible heat transport is dominant in winter.The evapotranspiration of each day mainly occurs from 08:00 （Beijing Time the same as after） to 17:00， and reaches the maximum from 11:00 to 14:00， and the seasonal difference is obvious.