On the rigid-lid approximation for two shallow layers of immiscible fluids with small density contrast
Résumé
The rigid-lid approximation is a commonly used simplification in the study of density-stratified fluids in oceanography. One assumes that the displacements of the surface are negligible compared with internal displacements. We offer a rigorous justification of this approximation in the case of two shallow layers of immiscible fluid with constant and quasi-equal mass densities. More precisely, we control the difference between the solutions of the Cauchy problem predicted by the shallow-water (Saint-Venant) system in the rigid-lid and free-surface configuration. We also describe explicitly the first-order behavior of the deformation of the surface in the latter situation.
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