Many efforts have been made to develop numerical models of biospheric
processes in recent years. Generally speaking, three classes of global
terrestrial biosphere models have emerged: (1) soil-vegetation-atmosp
here transfer (SVAT) models, (2) terrestrial biogeochemistry models (T
BMs), and (3) potential vegetation models (PVMs). In this manuscript,
I summarize the main characteristics of these models and discuss the n
eed for a more fully integrated biosphere model, which would combine a
spects of (1), (2) and (3) in a single modelling framework.