Free-surface Euler equations with density variations, and shallow-water limit
Th\'eo Fradin

TL;DR
This paper extends the analysis of free-surface Euler equations to include density variations and vorticity, providing well-posedness results and justifying the shallow-water limit with a focus on long-time behavior.
Contribution
It introduces a framework for the well-posedness of Euler equations with density variations and establishes the convergence to shallow-water equations, including long-time existence results.
Findings
Established well-posedness in Sobolev spaces for the extended system.
Proved convergence from free-surface Euler to shallow-water equations.
Demonstrated existence of solutions on a logarithmic time-scale.
Abstract
In this paper we study the well-posedness in Sobolev spaces of the incompressible Euler equations in an infinite strip delimited from below by a non-flat bottom and from above by a free-surface. We allow the presence of vorticity and density variations, and in these regards the present system is an extension of the well-studied water waves equations. When the bottom is flat and with no density variations (but when the flow is not necessarily irrotational), our study provides an alternative proof of the already known large-time well-posedness results for the water waves equations. Our main contribution is that we allow for the presence of density variations, while also keeping track of the dependency in the shallow water parameter. This allows us to justify the convergence from the free-surface Euler equations towards the non-linear shallow water equations in this setting. Using an…
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
Taxonomy
TopicsAquatic and Environmental Studies · Coastal and Marine Dynamics · Ocean Waves and Remote Sensing
