Recent efforts to project vegetation responses to climatic warming have emp
hasized the tight linkages between climate and vegetation distribution. Her
e we provide several examples indicating that the direct effects of climati
c warming on boreal vegetation can be qualitatively different than the indi
rect effects mediated by climatic responses of herbivores. These herbivore-
mediated vegetation responses to climatic warming will likely vary regional
ly. In southern Fennoscandia, we project that the climatically induced chan
ges in animal populations should enhance the density of spruce at the expen
se of pine and broadleafed trees. In northern Fennoscandia we project reduc
ed herbivory on broadleafed trees and increased herbivory on pine, leading
to an increase in broadleafed trees and spruce and a reduction in pine. Cli
matic warming in interior Alaska may reduce herbivory on broadleafed trees
and increase herbivory on evergreen spruce, thus reinforcing the impact of
increased fire frequency.