The uncertainties in soil hydraulic functions and soil hydraulic parameters
affect the performance of land-surface schemes used in climate and weather
prediction models. The soil hydraulic model of Clapp and Hornberger is mos
t widely used in land-surface modelling, while other models favoured by soi
l physicists are hardly used for the purpose. In this study, we give a summ
ary of four soil hydraulic models and examine the impact of these models on
the performance of a land-surface scheme. It is found that inconsistency i
n soil hydraulic functions and parameters leads to different outcomes in la
nd-surface modelling. We introduce a technique to match the soil hydraulic
parameters for different models, so that the disagreement in the descriptio
n of soil hydraulic properties among different models is reduced, while int
rinsic differences in the soil hydraulic functions remain. The numerical te
sts also show that the land-surface model has a degree of tolerance to the
uncertainties in soil hydraulic models, at least in the case of off-line si
mulations. The van Genuchten model performs well, but is numerically expens
ive. The Brooks-Corey and Clapp-Homberger models are sufficiently accurate
with numerical efficiency, and are therefore more suitable for land-surface
schemes used in atmospheric models.