This paper describes a study in which, for the first time, advanced systems
-engineering parameter-estimation techniques were applied to data from seve
ral field studies to estimate the preferred set of parameters for some of t
he most com mon biomes represented in an advanced Soil-Vegetation-Atmospher
e Transfer (SVAT) scheme (BATS2, a recent version of the Biosphere-Atmosphe
re Transfer Scheme): the effect on modelled climate was also investigated.
Observational data from field sites in Brazil, Canada, Arizona and Kansas/O
klahoma in the USA, and the Netherlands were chosen as representative of tr
opical rain forest, coniferous forest. semi-arid vegetation, agricultural c
rops, and grassland biomes, respectively. Together, these five biomes make
up 50% of the land area represented in BATS. Multi-criteria calibration alg
orithms do not produce a unique set of model parameters and, when different
combinations of the available objective functions at each sire are conside
red. the number of solutions increases substantially. The need for a single
parameter-set for each site (biome) is an important practical issue that w
as necessarily addressed in this study. A procedure was defined in which op
timized parameter-sets were successively discarded by successively applying
a cut-off threshold to single observable objective functions following a p
reference hierarchy. In this study, only the vegetation-related parameters
are calibrated for each of the five biomes and implemented into BATS?; howe
ver, in a separate experiment, the effect of including soil parameters in t
he optimization was investigated. When the calibrated parameters are adopte
d and used in BATS2, there are significant changes between the climates cal
culated in an eight-year run with version 3 of the Community Climate Model
and in an equivalent right-year run in which the original default parameter
s were used. The overall conclusion of this exploratory study is that advan
ced parameter-estimation techniques and appropriate field data can be used
successfully to improve representation of surface exchanges and the modelle
d climate given by a GCM, by defining appropriate values for vegetation-rel
ated parameters in an advanced SVAT scheme.