An operational model based on an inverse method is developed for the s
tudy of tidal flow in coastal areas. Models based on inverse methods c
an accommodate large quantities of measured data within the model doma
in and do not require initial or boundary data in the state variables.
These are benefits that overcome the weaknesses in conventional direc
t models which can be ill-posed because of inadequate boundary data wh
ich cannot make use of extensive survey data. The method described in
the paper uses a direct minimisation technique, and the governing equa
tions are included as a weak constraint on the solution. This allows t
he relative influences of data and equations on the final solution to
be defined. The model is validated using idealised topographies in ter
ms of data assimilation, flow diversion by topography and tidal floodi
ng and drying over a shoal. (C) 1998 Elsevier Science B.V. All rights
reserved.