Environmental Fluid Mechanics

, Volume 15, Issue 5, pp 1035–1051 | Cite as

Axisymmetric gravity currents in two-layer density-stratified media

  • R. M. Sahuri
  • A. K. Kaminski
  • M. R. Flynn
  • M. Ungarish
Original Article

Abstract

Numerous studies have considered the flow of a rectilinear, high Reynolds number, Boussinesq gravity current through a two-layer stratified ambient, however, far less is known concerning the analogue axisymmetric problem. Whereas in both instances there is the possibility of a dynamic coupling between the gravity current front and the waves that are excited by its forward advance, axisymmetric gravity currents entail the added complexity of a radially-diverging flow. Because a steady-state formulation cannot then be developed, we instead present a one-layer shallow water model that describes the flow evolution for various initial conditions and ambient stratifications. We also report upon \(>\!\!30\) full- and partial-depth lock release laboratory experiments that span a densitometric range \(0 \le S < 0.8868\) where \(S=(\rho _1-\rho _2)/(\rho _c-\rho _2)\) in which \(\rho _c\), \(\rho _1\) and \(\rho _2\) denote, respectively, the densities of the gravity current and lower and upper ambient layers. Of principal interest is the initial front speed of the gravity current for which good agreement is observed between laboratory measurement and shallow water numerical simulation, despite the limiting assumptions of the latter. The horizontal distance over which the initial front speed is maintained may span several lock-lengths, however, this depends on whether or not the gravity current is substantially impacted by the interfacial wave(s). For example, when the lower ambient layer is moderate and \(S\) is large, the transfer of momentum from the gravity current front to the wave may lead to a deceleration so severe that gravity current fluid is swept in the \(-r\) direction. The connection between our analysis and problems of pollution dispersion is briefly outlined.

Keywords

Gravity currents Ambient stratification Interfacial waves  Shallow water theory 

Notes

Acknowledgments

Financial support was generously provided by NSERC through the Discovery, USRA and RTI Grant programs. The tank used in the experimental portion of this study was fabricated in the Dept. of Mech. Eng. Machine Shop at the Univ. of Alberta. The ESM videos were produced with the kind assistance of Mr. Esmatullah Naikyar.

Supplementary material

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Copyright information

© Springer Science+Business Media Dordrecht 2015

Authors and Affiliations

  • R. M. Sahuri
    • 1
    • 2
  • A. K. Kaminski
    • 3
  • M. R. Flynn
    • 4
  • M. Ungarish
    • 5
  1. 1.Deparment of Mechanical EngineeringUniversity of AlbertaEdmontonCanada
  2. 2.Spartech ManufacturingCalgaryCanada
  3. 3.Department of Applied Mathematics and Theoretical PhysicsUniversity of CambridgeCambridgeUK
  4. 4.Department of Mechanical Engineering and Institute for Geophysical ResearchU. AlbertaEdmontonCanada
  5. 5.Department of Computer ScienceTechnionHaifaIsrael

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