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Poseidon Ocean Model | |
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Analysis of Poseidon run in reduced gravity mode (Report by Barry Klinger pdf here)

Tropical Instability Waves as seen in Pacific SST from the last year of run ECOADS. Contour interval is 1 C.

Equatorial potential temperature for E-COADS (black), assimilation run (blue), and difference (red for positive, cyan for negative), for 4 months. E-COADS data is average of pairs of end-of-month climatology, while assimilation run is monthly average [of daily measures?]. Temperature contours are 12, 16, 20, 24, 28 C; difference contours are [.25, .5, 1, 2, 4] C
This run was begun on Dec, 1969. It has a full barotropic component, and uses the Poseidon quasi-isopycnal quadratic spline remapping, 8th order Shapiro filter on velocity and mass, as well as a Biharmonic viscosity with Smagorinsky coefficients (but 0 background biharmonic viscosity). Run results for 1976 are featured, while we wait for the upgrade to halem's OS.
Barotropic component, realistic topography.



This run is a spin-up with climatological boundary conditions

This is the same run as shown for the ACC instantaneous surface currents.
| ©2003 Paul Schopf, School of Computational Sciences George Mason University | Home Code Support |