A simple, generalized saturated zone formulation is presented in this
paper to relax the assumption of an exponential function originally ma
de in TOPMODEL. This saturated zone model is based on the concept of a
'discharge : relative storage' (Q Delta S) function which is derived
empirically, using recession curve analysis, and may be of arbitrary f
orm. The generalized formulation is applied to the Seternbekken MINIFE
LT catchment in Norway, where detailed distributed water table data ha
ve been measured. These water table data are used to suggest an empiri
cal, power law modification of the topographic a/tan beta index. Resul
ts for the simulation through time of discharges and water table depth
s at a few locations show that the generalized saturated zone formulat
ion is as efficient a simulator of the observed data as a conventional
TOPMODEL, but requires one parameter less to be calibrated. The simul
ation of detailed water table distributions is only approximate in bot
h cases. The modified power law index shows only a small improvement b
ut provides a basis for a discussion of possible sources of error in t
he TOPMODEL assumptions for this site. (C) 1997 by John Wiley & Sons,
Ltd.