The coupling between surface ozone (O₃) and vegetation significantly influences the regional to global climate. O₃ uptake by plant stomata inhibits the photosynthetic rate and stomatal conductance, impacting evapotranspiration through land surface ecosystems. Using a climate‒vegetation‒chemistry coupled model (the NASA GISS ModelE2 coupled with the Yale Interactive terrestrial Biosphere, or ModelE2-YIBs), we assess the global climatic responses to O₃‒vegetationinteractions during the boreal summer of the present day (2005–2014). High O₃ pollution reduces stomatal conductance, resulting in warmer and drier conditions worldwide. The most significant responses are found in the eastern U.S. and eastern China, where the surface air temperature increases by +0.33±0.87 °C and +0.56±0.38 °C, respectively. These temperature increases are accompanied by decreased latent heat and increased sensible heat in both regions. The O₃‒vegetation interaction also affects atmospheric pollutants. The surface maximum daily 8-hour average O₃ concentrations increase by +1.46±3.02 ppbv in eastern China and +1.15±1.77 ppbv in the eastern U.S. due to the O₃-induced inhibition of stomatal uptake. With reduced atmospheric stability following a warmer climate, increased cloud cover but decreased relative humidity jointly reduce aerosol optical depth by -0.06±0.01 (-14.67±12.15%) over eastern China. This study suggests that vegetation feedback should be considered for a more accurate assessment of climatic perturbations caused by tropospheric O₃.
 

臭氧-植被相互作用,气孔导度,地表气温,大气污染物,陆气相互作用；