In this paper we apply the generalized Taylor Galerkin finite element model
to simulate bore wave propagation in a domain of two dimensions. For stabi
lity and accuracy reasons, we generalize the model through the introduction
of four free parameters. One set of parameters is rigorously determined to
obtain the high-order finite element solution. The other set of free param
eters is determined from the underlying discrete maximum principle to obtai
n the monotonic solutions. The resulting two models are used in combination
through the flux correct transport technique of Zalesak, thereby construct
ing a finite element model which has the ability to capture hydraulic disco
ntinuities. In addition, this paper highlights the implementation of two Kr
ylov subspace iterative solvers, namely, the bi-conjugate gradient stabiliz
ed (Bi-CGSTAB) and the generalized minimum residual (GMRES) methods. For th
e sake of comparison, the multifrontal direct solver is also considered. Th
e performance characteristics of the investigated solvers are assessed usin
g results of a standard test widely used as a benchmark in hydraulic modeli
ng. Based on numerical results, it is shown that the present finite element
method can render the technique suitable for solving shallow water equatio
ns with sharply varying solution pro les. Also, the GMRES solver is shown t
o have a much better convergence rate than the Bi-CGSTAB solver, thereby sa
ving much computing time compared to the multifrontal solver.