Model turbulent floods with the Smagorinski large eddy closure

TL;DR

This paper introduces a turbulence modeling approach for floods, tides, and tsunamis using the Smagorinski large eddy closure, enabling better prediction of fluid dynamics during extreme inundations.

Contribution

It develops a new coupled model for fluid depth and turbulent velocity based on boundary conditions and slow manifold theory, improving turbulence representation in flood simulations.

Findings

Model captures internal turbulent shear in floods.

Allows for large variations in fluid depth during inundations.

Provides a foundation for predicting erosion and transport in turbulent flows.

Abstract

Floods, tides and tsunamis are turbulent, yet conventional models are based upon depth averaging inviscid irrotational flow equations. We propose to change the base of such modelling to the Smagorinksi large eddy closure for turbulence in order to appropriately match the underlying fluid dynamics. Our approach allows for large changes in fluid depth to cater for extreme inundations. The key to the analysis underlying the approach is to choose surface and bed boundary conditions that accommodate a constant turbulent shear as a nearly neutral mode. Analysis supported by slow manifold theory then constructs a model for the coupled dynamics of the fluid depth and the mean turbulent lateral velocity. The model resolves the internal turbulent shear in the flow and thus may be used in further work to rationally predict erosion and transport in turbulent floods.