摘要:Increasing concentrations of atmospheric carbon dioxide (CO2)
influence climate by suppressing canopy transpiration in addition to its well-known greenhouse
gas effect. The decrease in plant transpiration is due to changes in plant physiology (reduced
opening of plant stomata). Here, we quantify such changes in water flux for various levels of
CO2 concentrations using the National Center for Atmospheric Research's (NCAR)
Community Land Model. We find that photosynthesis saturates after 800 ppmv
(parts per million, by volume) in this model. However, unlike photosynthesis,
canopy transpiration continues to decline at about 5.1% per 100 ppmv increase in
CO2 levels. We also find that the associated reduction in latent heat flux is primarily
compensated by increased sensible heat flux. The continued decline in canopy
transpiration and subsequent increase in sensible heat flux at elevated
CO2 levels implies that incremental warming associated with the physiological effect of
CO2 will not abate
at higher CO2 concentrations, indicating important consequences for the global water and carbon cycles from anthropogenic
CO2 emissions.