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An ustructured, quadrilateral grid used for our application is shown below: first for the
world, then for the North Pacific. Minimum grid spacing is ~20km.
Forcing mechanisms for SEOM in our application include five
tidal components (M2, N2, S2, K1, O1),
and winds. Output is
presently barotropic with both tidal and subtidal frequencies.
Below are plots of tidal amplitude and relative phase for the M2
and K1 components.