Fine grids with small spacing in; boundary-fitted coordinates are normally
used to treat the computation of fluid dynamics for estuarine areas and tid
al flats. However, the adoption of Cartesian components of velocity vectors
in this kind of non-orthogonal coordinates will definitely result in a dif
ficulty in solving implicitly the transformed momentum equations, and also
complicate the wet-dry point judgement used for flood areas. To solve this
problem, equations in terms of generalized contravariant velocity vectors i
n curvilinear coordinates are derived in the present study, by virtue of wh
ich, an Alternative-Direction-Implicit numerical scheme in non-orthogonal g
rids would then be easily obtained, and wet-dry point judgement would as we
ll be largely simplified. A comparison is made between the explicit scheme
and implicit scheme, showing that the present model is accurate and numeric
ally stable for computations of fluid dynamics for estuarine areas and tida
l flats.