activity
20212026
collaborators

7 papers

math.AP2026

The shallow--water limit of linear water waves over a discontinuous bottom

Martin Oen Paulsen

We rigorously justify the zero--dispersion limit of linear water waves over a sharp bottom step, recovering the shallow-water equations as a transmission problem, and describe the…

math.AP2025

The F. John model and Cummins' equations for freely floating objects

David Lannes, Martin Oen Paulsen

In this paper, we address the well-posedness theory of F. John's problem for freely floating objects in a two-dimensional framework. This problem is a linear description of the int…

math.AP2023

Justification of the Benjamin-Ono equation as an internal water waves model

Martin Oen Paulsen

In this paper, we give the first rigorous justification of the Benjamin-Ono equation as an internal water wave model on the physical time scale. Let be the small para…

math.AP2023

Rigorous derivation of weakly dispersive shallow water models with large amplitude topography variations

Louis Emerald, Martin Oen Paulsen

We derive rigorously from the water waves equations new irrotational shallow water models for the propagation of surface waves in the case of uneven topography in horizontal dimens…

math.AP2023

Long time well-posedness and full justification of a Whitham-Green-Naghdi system

Louis Emerald, Martin Oen Paulsen

We establish the full justification of a "Whitham-Green-Naghdi" system modeling the propagation of surface gravity waves with bathymetry in the shallow water regime. It is an asymp…

math.AP2022

Long time well-posedness of Whitham-Boussinesq systems

Martin Oen Paulsen

Consideration is given to three different full dispersion Boussinesq systems arising as asymptotic models in the bi-directional propagation of weakly nonlinear surface waves in sha…

physics.flu-dyn2021

A Nonlinear Formulation of Radiation Stress and Applications to Cnoidal Shoaling

Martin O. Paulsen, Henrik Kalisch

In this article we provide formulations of energy flux and radiation stress consistent with the scaling regime of the Korteweg-de Vries (KdV) equation. These quantities can be used…