A review of a calibration method developed earlier (Ibrahim and Liong,
1992) is presented. The method generates optimal values for single ev
ents. It entails randomizing the calibration parameters over bounds su
ch that a system response under consideration is bounded. Within the b
ounds, which are narrow and generated automatically, explicit response
surface representation of the response is obtained using experimental
design techniques and regression analysis. The optimal values are obt
ained by searching on the response surface for a point at which the pr
edicted response is equal to the measured response and the value of th
e joint probability density function at that point in a transformed sp
ace is the highest. The method is demonstrated on a catchment in Singa
pore. The issue of global optimal values is addressed by applying the
method on wider bounds. The results indicate that the optimal values a
rising from the narrow set of bounds are, indeed, global. Improvements
which are designed to achieve comparably accurate estimates but with
less expense are introduced. A linear response surface model is used.
Two approximations of the model are studied. The first is to fit the m
odel using data points generated from simple Monte Carlo simulation; t
he second is to approximate the model by a Taylor series expansion. Ve
ry good results are obtained from both approximations. Two methods of
obtaining a single estimate from the individual event's estimates of t
he parameters are presented. The simulated and measured hydrographs of
four verification storms using these estimates compare quite well.