The finite-element. semi-implicit, and semi-Lagrangian methods are combined
together to solve the shallow-water equations using unstructured triangula
r meshes. Triangular finite elements are attractive for ocean modeling beca
use of their flexibility for representing irregular boundaries and for loca
l mesh refinement. A kriging interpolator is used for the semi-Lagrangian a
dvection. leading to an accurate representation of the slow Rossby modes. T
he terms that govern fast gravitational oscillations are discretized using
the semi-implicit scheme, thereby circumventing a severe time step restrict
ion. A low-order velocity-surface-elevation finite-element basis-function p
air is used for the spatial discretization. Results of test problems to sim
ulate slowly propagating Rossby modes illustrate the promise of the propose
d approach for ocean modeling.