In this study, it is shown that the complexity of Soil Vegetation Atmospher
e Transfer (SVAT) models leads to an equifinality of functional behaviour-m
any parameterizations from many areas of the parameter space lead to very s
imilar responses. individual parameters derived by calibration (i.e. model
inversion) against limited measurements are, therefore, highly uncertain. D
ue to the non-linear internal behaviour of SVAT models, aggregation of unce
rtainly known parameter fields to parameterize landscape scale variability
in surface fluxes will yield highly uncertain predictions. A disaggregation
approach suggested by Beven (1995) requires that the land surface be repre
sented by a linear sum of a number of representative parameterizations or f
unctional types. This study explores the nature of the parameter space in t
erms of a simple definition of functional behaviour. Parameter interactions
producing similar predicted behaviours are investigated through applicatio
n of Principal Component Analyses. These reveal the lack of a dominant glob
al interaction indicating the presence of highly-complex parameter interact
ions throughout the feasible parameter space.