A comparative study of coastal circulation by means of two depth-avera
ged numerical models, a finite difference and a finite element model,
is undertaken. From the application of the models to Amvrakikos Gulf,
a nearly enclosed coastal water body of particular ecological interest
in Western Greece, me following conclusions are drawn. (i) Circulatio
n patterns calculated for the same eddy viscosity coefficient with bot
h models are essentially identical. (ii) Increasing the value of eddy
viscosity coefficient results in a significant reduction of the magnit
ude of the flow velocities with no major changes on the general flow p
attern. (iii) Preliminary calculations with the finite difference mode
l show that the incorporation of the k-epsilon turbulence model has mi
nor effects on the results, but it improves the rate of convergence. (
iv) Calculations with both models using alternative conditions in the
open sea boundary show only minor differences in the proximity of the
boundary.