Anthropogenic greenhouse gases are expected to induce changes in globa
l climate that can alter ecosystems in ways that, in turn, may further
affect climate. Such climate-ecosystem interactions can generate eith
er positive or negative feedbacks to the climate system, thereby eithe
r enhancing or diminishing the magnitude of global climate change. Imp
ortant terrestrial feedback mechanisms include CO2 fertilization (nega
tive feedbacks), carbon storage in vegetation and soils (positive and
negative feedbacks), vegetation albedo (positive feedbacks), and peatl
and methane emissions (positive and negative feedbacks). While the pro
cesses involved are complex, not readily quantifiable, and demonstrate
both positive and negative feedback potential, we conclude that the c
ombined effect of the feedback mechanisms reviewed here will likely am
plify climate change relative to current projections that have not yet
adequately incorporated these mechanisms.