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IVèmes Journées, Dinard
A two-dimensional depth-averaged model for tide propagation and fine sediment transport is used to simulate the turbidity maximum in the Seine estuary. Hydrodynamic results are compared with field data in order to validate the model. Whatever the initial conditions are, the formation and the behaviour of the turbidity maximum during spring tides is correctly reproduced according ta field data. During neap tides,. deposition pattems roughly correlated with the low velocities are in gooddoi:10.5150/jngcgc.1996.030-b fatcat:jesmiuafdjfm7giflphnabfggy