Hostname: page-component-6766d58669-h8lrw Total loading time: 0 Render date: 2026-05-15T02:07:04.361Z Has data issue: false hasContentIssue false
  • English
  • Français

Inside the head and tail of a turbulent gravity current

Published online by Cambridge University Press:  01 February 2016

Graham O. Hughes
Graham O. Hughes*
Affiliation:
Research School of Earth Sciences, The Australian National University, Canberra ACT 2601, Australia
Rights & Permissions [Opens in a new window]

Abstract

Gravity currents are an important buoyancy-driven flow in environmental, geophysical and industrial settings. Turbulence and mixing is commonplace in these flows, but is typically overlooked in theoretical models and predictions. Sher & Woods (J. Fluid Mech., vol. 784, 2015, pp. 130–162) have quantified the velocity and density structure in turbulent gravity currents by combining high-quality experimental data with new theory. Their insights are set to stimulate significant advances in the area.

JFM classification

Geophysical and Geological Flows: Gravity currents Geophysical and Geological Flows: Stratified flows Turbulent Flows: Stratified turbulence

Information

Type
Focus on Fluids
Information
Journal of Fluid Mechanics , Volume 790 , 10 March 2016 , pp. 1 - 4
Check for updates
Copyright
© 2016 Cambridge University Press 

1. Introduction

Sea breezes, katabatic winds, thunderstorm outflows, avalanches, industrial gas spillages, estuarine salt intrusions, dam bursts, dust storms, pyroclastic flows and dense-slope plumes in the oceans are all examples of gravity currents. These flows form when buoyancy forces cause fluid of one density to encroach along a boundary into an ambient environment of different density (figure 1). The boundary can be inclined, but is often assumed to be horizontal. The typical structure of a gravity current consists of a bulbous ‘head’ and propagating front, where a strong density gradient between the two fluids is maintained, and a ‘tail’ extending back towards the initial source (figure 1 b). Intense turbulence is often apparent in the vicinity of the head, and mass and tracers are transported laterally over a significant distance.

Figure 1.

(a) Dust storm in Afghanistan (photograph: Cpl Daniel Wiepen; 45158327.jpg from defenceimages.mod.uk, Open Government License nationalarchives.gov.uk/doc/open-government-licence/; Crown Copyright 2014), (b) schematic diagram of flow structure in a vertical plane through a turbulent gravity current (delineated nominally by the dashed line; after figures 1(a) and 8 of Sher & Woods (Reference Sher and Woods2015)). Density and velocity structure is indicated by shading and bold arrows, respectively.

Early studies established the broad characteristics of gravity currents. Benjamin (Reference Benjamin1968) considered the momentum balance for an immiscible inviscid and steady current in a channel, predicting the front propagation speed and that energy must be dissipated in most cases. Studies since then focusing on the front speed have highlighted different dynamical regimes (summarized below for currents in which viscous drag at the boundary is unimportant). Following initial release of the current, the front speed is constant but at least 15 % less than Benjamin’s prediction (Huppert & Simpson Reference Huppert and Simpson1980; Shin, Dalziel & Linden Reference Shin, Dalziel and Linden2004), the suggested reason being the mismatch between the resulting velocity structure and that assumed in the theory. If a limited volume of source fluid is available to the current, the constant-speed regime (also known as the ‘slumping’ phase) persists until exhaustion of the source is communicated to the head (see Rottman & Simpson Reference Rottman and Simpson1983 for details). A second regime follows in which the current is well described by an approximately self-similar dynamical balance between buoyancy and inertia forces, and the front speed $u_{n}$ decays with time $t$ ( $u_{n}\sim t^{-1/3}$ , Huppert & Simpson (Reference Huppert and Simpson1980)).

Turbulence in the vicinity of the gravity current head arises from instabilities owing to shear between the current and ambient flow and of the vorticity field generated by passage of the front over a no-slip boundary (leading to ‘lobe and cleft’ structures; Härtel, Meiburg & Necker (Reference Härtel, Meiburg and Necker2000)). Turbulent eddies exchange mass and momentum between the current and ambient fluid, and lead to mixing of the density field if the fluids are miscible. The turbulence results in additional drag on the current and dissipation of energy, but the dynamical importance of these effects is unclear (e.g. Shin et al. (Reference Shin, Dalziel and Linden2004) found that the propagation speed and the effective current depth are well predicted by an energy-conserving theory). Although many previous measurements have highlighted rich density and velocity structure in a turbulent gravity current (e.g. Hacker, Linden & Dalziel Reference Hacker, Linden and Dalziel1996; Hallworth et al. Reference Hallworth, Phillips, Huppert and Sparks1996; Kneller, Bennett & McCaffrey Reference Kneller, Bennett and McCaffrey1999; Shin et al. Reference Shin, Dalziel and Linden2004; Marino, Thomas & Linden Reference Marino, Thomas and Linden2005), most previous theoretical models have assumed a highly idealized form based on lateral and/or depth averaging of the structure. While these idealizations can capture some dynamics associated with mixing (because the total buoyancy anomaly in the flow is conserved; Huppert Reference Huppert2006), the internal structure of the current and its role in the overall flow remains an outstanding question.

2. Overview

Sher & Woods (Reference Sher and Woods2015) have advanced our understanding of gravity current dynamics with detailed measurements and theoretical modelling of the flow structure. They have considered the sudden release of dense fluid to form a turbulent current that propagates into a miscible ambient fluid over a large horizontal distance (up to 25 times the length of the initial source volume). Laboratory data suggest a fresh interpretation of the circulation in the current, the key observations being (see figure 1 b):

  1. (i) fluid that has the largest density contrast with the ambient is always found towards the base of the current head;

  2. (ii) the fluid identified in (i) circulates towards the front from behind, i.e. its flow speed exceeds the front speed $u_{n}$ ;

  3. (iii) strong turbulent mixing arises where the ambient fluid is displaced past the head and maintains shear instabilities on the current;

  4. (iv) some mixed fluid in the ‘wake’ region is displaced backwards (both relative to the front and, to a lesser extent, in a stationary frame of reference);

  5. (v) the density contrast in the head decays gradually as mixed fluid in (iv) is deposited into the stratified tail region and begins to be recirculated back to the head (as in (ii));

  6. (vi) the current head height $h$ (about 38 % of the total flow depth, based on a threshold concentration) and the proportion of displaced ambient fluid that is mixed into the current (60–80 %) are both insensitive to the flow parameters.

The emerging picture is of a current evolving towards a self-similar flow structure that is attenuated gradually by turbulent mixing. Unmixed source fluid is present in the head during the slumping phase, despite intense mixing there (see discussion by Hacker et al. (Reference Hacker, Linden and Dalziel1996), Hallworth et al. (Reference Hallworth, Phillips, Huppert and Sparks1996), Fragoso, Patterson & Wettlaufer (Reference Fragoso, Patterson and Wettlaufer2013)). Sher & Woods (Reference Sher and Woods2015) have highlighted how the mixing and the recirculation (in (v)) accounts for creation of a strongly stratified tail region and a density contrast in the current that decreases with distance behind the head (see also Marino et al. (Reference Marino, Thomas and Linden2005)). The ongoing recirculation of the least-dilute fluid in the current ((i) and (ii)) maintains a relatively sharp density gradient at the front. One interesting feedback is that this density gradient will act to stabilize the current head against shear instability, thus reducing both the level of turbulence that would otherwise be present and the attenuation rate of the overall flow structure. Sher & Woods (Reference Sher and Woods2015) have found that the front is characterized by an approximately constant Froude number $Fr=u_{n}/(g^{\prime }h)^{1/2}\approx 0.9$ (where $g^{\prime }$ is a depth-averaged reduced gravity), consistent with recent previous work (Shin et al. Reference Shin, Dalziel and Linden2004; Marino et al. Reference Marino, Thomas and Linden2005). Interestingly, they have observed circulation speeds in (ii) that are approximately 35 % faster than the front speed in the slumping phase, and much closer to those expected if energy was conserved in the flow (Benjamin Reference Benjamin1968; see discussion in Härtel et al. Reference Härtel, Meiburg and Necker2000; Shin et al. Reference Shin, Dalziel and Linden2004). This differential is indicative of the Reynolds stresses (owing to the turbulent eddies and entrainment) and inertial drag exerted at the head of the current, where the predominant dissipation of energy occurs.

Sher & Woods (Reference Sher and Woods2015) have developed a new theoretical description of the velocity and density field in a gravity current by assuming that the dynamical influence of turbulent entrainment and mixing is concentrated at the head. Their predictions are a good match to the experimental data, and show that the structure and flow in the self-similar regime are well described by an approximate balance between buoyancy and inertia forces. Their work both helps provide a unified interpretation of previous literature and highlights the dynamics necessary to improve gravity current models for many applications.

3. Future

The observation of many gravity currents as highly turbulent suggests that they are complicated flows. Many existing theoretical models yield bulk predictions for currents with neglect of the effects associated with turbulence, including dissipation, mixing and the creation of velocity and density structure. Therefore, the new insights of Sher & Woods (Reference Sher and Woods2015) will have significant benefits for applications that rely on accurate prediction of the passage of tracers, such as hazard management.

An important outstanding question concerns the behaviour of a gravity current in a deep ambient fluid. Benjamin (Reference Benjamin1968) showed that energy must be dissipated in this situation and, although an aim of several studies has been measuring the energetics associated with mixing (e.g. Shin et al. Reference Shin, Dalziel and Linden2004; Fragoso et al. Reference Fragoso, Patterson and Wettlaufer2013), the energy budget for a current in a deep ambient fluid remains to be comprehensively understood. Furthermore, previous studies (e.g. Huppert & Simpson Reference Huppert and Simpson1980; Shin et al. Reference Shin, Dalziel and Linden2004; Marino et al. Reference Marino, Thomas and Linden2005) have typically characterized the current in terms of the Froude number $Fr=u_{n}/(g^{\prime }h)^{1/2}$ at the front, but this condition does not close the problem because both the front speed $u_{n}$ and the current height $h$ are unknown (Huppert Reference Huppert2006). Understanding the velocity and density structure in the current and ambient fluid (see also Marino et al. Reference Marino, Thomas and Linden2005) could offer an interesting avenue for progress on this problem.

References

Benjamin, T. B. 1968 Gravity currents and related phenomena. J. Fluid Mech. 31, 209–248.Google Scholar
Fragoso, A. T., Patterson, M. D. & Wettlaufer, J. S. 2013 Mixing in gravity currents. J. Fluid Mech. 734, R2.CrossRefGoogle Scholar
Hacker, J., Linden, P. F. & Dalziel, S. B. 1996 Mixing in lock-release gravity currents. Dyn. Atmos. Oceans 24, 183–195.Google Scholar
Hallworth, M. A., Phillips, J., Huppert, H. E. & Sparks, R. S. J. 1996 Entrainment into two-dimensional and axisymmetric turbulent gravity currents. J. Fluid Mech. 308, 289–312.Google Scholar
Härtel, C., Meiburg, E. & Necker, F. 2000 Analysis and direct numerical simulation of the flow at a gravity-current head. Part 1. Flow topology and front speed for slip and no-slip boundaries. J. Fluid Mech. 418, 189–212.CrossRefGoogle Scholar
Huppert, H. E. 2006 Gravity currents: a personal perspective. J. Fluid Mech. 554, 299–322.Google Scholar
Huppert, H. E. & Simpson, J. E. 1980 The slumping of gravity currents. J. Fluid Mech. 99, 785–799.Google Scholar
Kneller, B., Bennett, S. J. & McCaffrey, W. D. 1999 Velocity structure, turbulence and fluid stresses in experimental gravity currents. J. Geophys. Res. 104, 5281–5291.Google Scholar
Marino, B. M., Thomas, L. P. & Linden, P. F. 2005 The front condition for gravity currents. J. Fluid Mech. 536, 49–78.Google Scholar
Rottman, J. W. & Simpson, J. E. 1983 Gravity currents produced by instantaneous releases of a heavy fluid in a rectangular channel. J. Fluid Mech. 135, 95–110.Google Scholar
Sher, D. & Woods, A. W. 2015 Gravity currents: entrainment, stratification and self-similarity. J. Fluid Mech. 784, 130–162.CrossRefGoogle Scholar
Shin, J. O., Dalziel, S. B. & Linden, P. F. 2004 Gravity currents produced by lock exchange. J. Fluid Mech. 521, 1–34.Google Scholar
Figure 0

Figure 1. (a) Dust storm in Afghanistan (photograph: Cpl Daniel Wiepen; 45158327.jpg from defenceimages.mod.uk, Open Government License nationalarchives.gov.uk/doc/open-government-licence/; Crown Copyright 2014), (b) schematic diagram of flow structure in a vertical plane through a turbulent gravity current (delineated nominally by the dashed line; after figures 1(a) and 8 of Sher & Woods (2015)). Density and velocity structure is indicated by shading and bold arrows, respectively.