The power of a validation strategy (that is, its ability to discrimina
te between good and bad model hypotheses) depends on what kind of data
are available and how the data are used to challenge the hypothesis.
Several validation strategies are examined from the perspective of pow
er and practical applicability. It is argued that validation using mul
tiresponse data in a catchment experiencing a shift in hydrologic regi
me due to disturbance or extreme climatic inputs is a considerably mor
e powerful strategy than traditional split-sample testing using stream
flow data alone in undisturbed catchments. A case study testing two mo
del hypotheses is presented using paired catchments for which multiple
-response data in the form of streamflow, stream chloride, and groundw
ater levels were available. The first catchment, Salmon, was maintaine
d as an established forest, while the second, Wights, was cIear-felled
and converted to pasture about 3 years after monitoring started. The
hypotheses consider the same lumped hydrosalinity model with the first
(H1) excluding a groundwater discharge zone and the second (H2) inclu
ding it. It was found that even with three concurrent responses from t
he undisturbed Salmon catchment, H1 could not be rejected, leaving an
important part of the model conceptualization unidentified. Moreover,
a streamflow split-sample test for the disturbed Wights catchment fail
ed to conclusively reject H1; parameters could be found which accurate
ly tracked the streamflow changes following forest clearing yet produc
ed erroneous simulations of responses such as stream chloride and grou
ndwater storage. It was only when H1 was subjected to the scrutiny of
three catchment responses from the disturbed Wights catchment that it
could be rejected. This highlights the importance of challenging model
hypotheses under the most demanding of tests, which, in this study, c
oincided with multiple-response validation in a disturbed catchment.