Abstract

One-dimensional models of exchange flows driven by horizontal density gradients are well known for performing poorly in situations with weak turbulent mixing. The main issue with these models is that the horizontal density gradient is usually imposed as a constant, leading to non-physically high stratification known as runaway stratification. Here, we propose two new parametrizations of the horizontal density gradient leading to one-dimensional models able to tackle strongly stratified exchange flows at high and low Schmidt number values. The models are extensively tested against results from laminar two-dimensional simulations and are shown to outperform the models using the classical constant parametrization for the horizontal density gradients. Four different flow regimes are found by exploring the parameter space defined by the gravitational Reynolds number Reg, the Schmidt number Sc, and the aspect ratio of the channel Γ. For small values of RegΓ, when diffusion dominates, all models perform well. However, as RegΓ increases, two clearly distinct regimes emerge depending on the Sc value, with an equally clear distinction of the performance of the one-dimensional models.

Highlights

  • Gravity-driven exchange flows due to horizontal density differences occur in many natural environmental situations, for example, at the junction between two water bodies with different densities, such as the ocean and a river

  • The results show that the new parametrization of the density gradient leads to a significant improvement in the ability of 1D models to reproduce the density profiles obtained from numerical simulations of a 2D reference model

  • We introduce two new parametrizations for the horizontal density gradient driving environmental exchange flows that can be incorporated in one-dimensional water column models

Read more

Summary

Introduction

Gravity-driven exchange flows due to horizontal density differences occur in many natural environmental situations, for example, at the junction between two water bodies with different densities, such as the ocean and a river. Strong (vertical) stratification limits vertical mixing in the water column, and these exchange flows are known for driving disproportionately large horizontal transport of different substances such as pollutants, sediment, and microorganisms (Geyer and MacCready 2014). These properties make the understanding of exchange flows of the utmost importance in coastal oceanography. In 1D or 3D-HP models, the horizontal density differences are often parametrized using an imposed, constant horizontal density gradient This choice allows to reformulate the governing equations (i.e., those for momentum and transport of salinity or density) in such a way that the mean velocity variable and the mean density variable are independent of the horizontal coordinate (an example of a reformulation is given in Appendix A). The performance of the models is discussed as a function of their suitability to be incorporated in water column models and their suitability as homogeneous forcing in 3D-HP models

Numerical setup
Salinity distribution in the channel: flow regime identification
Proposals for one-dimensional models
Mathematical formulation
Limiting cases
Numerical results: model comparison
Extension to flows with a no-stress top boundary condition
Findings
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call