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A concurrent simulation of circulation and tides with MPIOM/TP6M L40, forced by surface fluxes derived from NCEP/NCAR reanalysis and by luni-solar tidal potential.
The concurrent simulation of ocean circulations and ocean tides is carried out with the Max-Planck Institute Ocean Model (MPIOM/TP6M L40 mpiom-1.6.3.) forced by the full luni-solar tidal potential as an