A two dimensional explicit finite element hydrodynamic model was developed
to study near shore flow circulation near the month of the Niagara River di
scharge into Lake Ontario and to investigate the influence of grid spatial
resolution on the model results. An extensive set of numerical experiments
was carried our, using more than 40 different numerical grid meshes. Lagran
gian tracer paths were calculated to illustrate the flow trajectories under
different hydrodynamic forcing conditions and goon comparison with field d
ata reported in the literature is shown. Spatial step sizes of slightly les
s than 100 m were found to be sufficient for modeling near-shore flow struc
ture, while much larger steps (several km) were used farther off-shore. Thi
s model allows a better understanding of the effects of various forcing con
ditions (primarily wind) on the flow and mixing characteristics of the Niag
ara River discharge and formation of the coastal boundary current along the
southern shoreline of Lake Ontario.