Atmospheric general circulation models used for climate simulation and
weather forecasting require the fluxes of radiation, heat, water vapo
r, and momentum across the land-atmosphere interlace to be specified.
These fluxes are calculated by submodels called land surface parameter
izations. Over the last 20 years, these parameterizations have evolved
from sim pie, unrealistic schemes into credible representations of th
e global soil-vegetation-atmosphere transfer system as advances in pla
nt physiological and hydrological research, advances in satellite data
interpretation, and the results of large-scale field experiments have
been exploited. Some modem schemes incorporate biogeochemical and eco
logical knowledge and, when coupled with advanced climate and ocean mo
dels, will be capable of modeling the biological and physical response
s of the Earth system to global change, for example, increasing atmosp
heric carbon dioxide.