The physiological response of terrestrial vegetation when directly exp
osed to an increase in atmospheric carbon dioxide (CO2) concentration
could result in warming over the continents in addition to that due to
the conventional CO2 ''greenhouse effect.'' Results from a coupled bi
osphere-atmosphere model (SiB2-GCM) indicate that, for doubled CO2 con
ditions, evapotranspiration will drop and air temperature will increas
e over the tropical continents, amplifying the changes resulting from
atmospheric radiative effects. The range of responses in surface air t
emperature and terrestrial carbon uptake due to increased CO2 are proj
ected to be inversely related in the tropics year-round and inversely
related during the growing season elsewhere.