Derivation of an intermediate viscous Serre-Green-Naghdi equation
Denys Dutykh (LAMA), Herv\'e Le Meur (LAMFA)

TL;DR
This paper discusses the ongoing derivation of a viscous Serre-Green-Naghdi model by combining inviscid Euler equations for the upper flow and Navier-Stokes equations for the boundary layer, within a specific flow regime.
Contribution
It presents a new approach to derive a viscous Serre-Green-Naghdi system considering a boundary layer modeled by a Prandtl-like equation.
Findings
Flow domain split into inviscid and viscous regions
Boundary layer reduces to a Prandtl-like equation
Further approximations needed for a practical model
Abstract
In this note we present the current status of the derivation of a viscous Serre-Green-Naghdi system. For this goal, the flow domain is separated into two regions. The upper region is governed by inviscid Euler equations, while the bottom region (the so-called boundary layer) is described by Navier-Stokes equations. We consider a particular regime linking the Reynolds number and the shallowness parameter. The computations presented in this note are performed in the fully nonlinear regime. The boundary layer flow reduces to a Prantdl-like equation. Further approximations seem to be needed to obtain a tractable model.
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Taxonomy
TopicsCoastal and Marine Dynamics · Fluid Dynamics and Turbulent Flows · Ocean Waves and Remote Sensing
