Under the influence of global warming，the surface temperature of lakes on the Qinghai-Xizang Plateau，along with the total duration and mean intensity of lake heatwaves，has exhibited significant increases. These trends amplify the susceptibility of lake surface temperatures to heating during thermal stratification periods，accelerating summer warming rates and potentially inducing surface hypoxia. Previous studies analyzing lake heatwave characteristics have predominantly focused on spatially averaged metrics across broad regions， leaving the specific heatwave dynamics of Qinghai Lake poorly characterized. To address this knowledge gap， this study integrates in-situ observations of Qinghai Lake's water temperature and surface temperature，meteorological data from Gangcha Station，MODIS land surface temperature products，the Third Pole high-resolution near-surface meteorological forcing dataset（TPMFD），and simulations from the one-dimensional Freshwater Lake Model（FLake）to investigate long-term changes in surface temperature and heatwave characteristics of Qinghai Lake from 1980 to 2022. Through correlation analysis and detrended decomposition methods，the driving mechanisms underlying these changes were systematically elucidated. The research shows that：（1）The air temperature，specific humidity and wind speed of TPMFD reanalysis data are highly correlated with those observed by Gangcha meteorological station，and the biases（BIAS）and root mean square errors（RMSE）are small. The correlation coefficients of the two data are 0. 96，0. 84 and 0. 74，respectively，and the BIAS is 0. 55 ℃，0. 00068 g·g-1 and -0. 31 m·s-1，respectively. The RMSE is 0. 59 ℃，0. 00069 g·g-1 and 0. 38 m·s-1，respectively. The change rate of the air temperature in TPMFD［0. 48 °C·（10a）-1］is close to that of the observed air temperature［0. 44 °C·（10a）-1］. The variation rate of the specific humidity in TPMFD［0. 0001 g·g-1·（10a） -1］is consistent with the observed variation rate. The variation rate of the wind speed in TPMFD［-0. 1 m·s-1· （10a）-1］is slightly smaller than that of the observation［-0. 25 m·s-1·（10a）-1］. Moreover，the change rates of the air temperature，specific humidity，and wind speed in both TPMFD and the Gangcha Meteorological Station have passed the significance test at the 95% confidence level. The simulated water temperature and lake surface temperature of Qinghai Lake have a very good correlation with the in-situ observed water temperature and lake surface temperature of Qinghai Lake，and the biases and root mean square errors are relatively small. The longterm sequential simulated lake surface temperature also has a good correlation with the MODIS surface temperature，and both the BIAS and RMSE are within a reasonable range. The correlation coefficients between the simulation results and the three kinds of observations are 0. 99，0. 96，and 0. 98 respectively，the BIAS are 0. 25 °C， -0. 1 °C，and 0. 87 °C respectively，and the RMSE are 0. 58 °C，2. 65 °C，and 2. 20 °C respectively.（2）From 1980 to 2022，both the characteristics of the lake surface temperature and lake heatwaves in Qinghai Lake showed a significant increasing trend（p<0. 05）. The frequency of lake heatwaves fluctuated between 0 and 6 times. The total number of days with lake heatwaves each year increased significantly. The total number of days in 2022 reached 150 days. The mean lake heatwave duration in most years exceeded 10 days per occurrence. The maximum lake heatwave duration in 2022 even reached 76 days，and the mean lake heatwave intensity increased significantly. The intensity levels of heatwaves in Qinghai Lake in 2016 and 2022 were in a "severe" state，which is two orders of magnitude stronger than the multi-year average intensity level（"moderate" level）.（3）Air temperature，specific humidity，downward long-wave radiation，downward short-wave radiation，and air pressure are positively correlated with the increase in the simulated lake surface temperature. Moreover，they are positively correlated with the increase in the total days of lake heatwaves. Furthermore，they are positively correlated with the enhancement of the mean intensity. However wind speed is negatively correlated with the increase in the simulated lake surface temperature and positively correlated with the increase in the total days of lake heatwaves and the enhancement of the mean intensity. The meteorological factors that positively contribute to the increase in lake surface temperature，from largest to smallest，are air temperature（23. 83%），specific humidity（20. 52%）， wind speed （16. 05%），downward long-wave radiation （14. 79%），and downward short-wave radiation （10. 68%）. The meteorological factors that positively contribute to the increase in the total days of lake heat‐ waves are air temperature（37. 54%），wind speed（35. 86%），specific humidity（30. 03%），downward longwave radiation（28. 27%），and downward short-wave radiation（27. 72%）. The meteorological factors that positively contribute to the enhancement of lake heatwave intensity are air temperature（13. 25%），wind speed （13. 07%），specific humidity（12. 35%），downward long-wave radiation（11. 05%），and downward shortwave radiation（10. 98%）. Air pressure has an inhibitory effect on the increase in lake surface temperature，the total days of lake heatwaves，and the mean intensity.