Throughout Australia, there are strong regional differences in hydrological
response to landscape and climate; however, in general terms, in Australia
n catchments the flows are typically peakier, base flows are of lower propo
rtion, runoff coefficients are smaller, and dry periods are longer and more
variable, than in European and North American catchments. In this context,
this paper assesses the model types available to improve understanding and
prediction of catchment flows and transport. Included in this is the conce
pt of information and its influence on appropriate model complexity, as wel
l as a characterization of the principal factors inhibiting model performan
ce. The ability to predict the effects on flows and water quality of anythi
ng but major changes in climate and land use is limited. Improvement of und
erstanding and prediction relies on the following: more rigorous testing of
models to assess their ability to separate climate and land use effects on
hydrological response; the use acid improved interpretation of spatial dat
a; more and better monitoring of hydrological response at a range of scales
; complementary use of conceptual and distributed models; and integration o
f modelling with other information such as that from geochemical studies in
cluding tracer analysis.