Abstract
An analytical, experimental and numerical study of boundary gravity currents propagating through a two-layer stratified ambient of finite vertical extent is presented. Gravity currents are supposed to originate from a lock-release apparatus; the (heavy) gravity current fluid is assumed to span the entire channel depth, H, at the initial instant. Our theoretical discussion considers slumping, supercritical gravity currents, i.e. those that generate an interfacial disturbance whose speed of propagation matches the front speed, and follows from the classical analysis of Benjamin (J Fluid Mech 31:209–248, 1968). In contrast to previous investigations, we argue that the interfacial disturbance must be parameterized so that its amplitude can be straightforwardly determined from the ambient layer depths. Our parameterization is based on sensible physical arguments; its accuracy is confirmed by comparison against experimental and numerical data. More generally, measured front speeds show positive agreement with analogue model predictions, which remain strictly single-valued. From experimental and numerical observations of supercritical gravity currents, it is noted that this front speed is essentially independent of the interfacial thickness, δ, even in the limiting case where δ = H so that the environment is comprised of a uniformly stratified ambient with no readily discernible upper or lower ambient layer. Conversely, when the gravity current is subcritical, there is a mild increase of front speed with δ. Our experiments also consider the horizontal distance, X, at which the front begins to decelerate. The variation of X with the interface thickness and the depths and densities of the ambient layers is discussed. For subcritical gravity currents, X may be as small as three lock lengths whereas with supercritical gravity currents, the gravity current may travel long distances at constant speed, particularly as the lower layer depth diminishes.
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References
Baines PG (1995) Topographic effects in stratified flows. Cambridge University Press, Cambridge
Benjamin TB (1968) Gravity currents and related phenomena. J Fluid Mech 31: 209–248
Bolster D, Hang A, Linden PF (2008) The front speed of intrusions into a continuously stratified medium. J Fluid Mech 594: 369–377
Cantero MI, Lee JR, Balachandar S, Garcia MH (2007) On the front velocity of gravity currents. J Fluid Mech 586: 1–39
Cheong H-B, Kuenen JJP, Linden PF (2006) The front speed of intrusive gravity currents. J Fluid Mech 552: 1–11
Faust KM, Plate EJ (1984) Experimental investigation of intrusive gravity currents entering stably stratified fluids. J Hydraul Res 22(5): 315–325
Flynn MR, Linden PF (2006) Intrusive gravity currents. J Fluid Mech 568: 193–202
Flynn MR, Boubarne T, Linden PF (2008) The dynamics of steady, partial-depth intrusive gravity currents. Atmos Ocean 46: 421–432
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
Holyer JY, Huppert HE (1980) Gravity currents entering a two-layer fluid. J Fluid Mech 100: 739–767
Keulegan GH (1957) An experimental study of the motion of saline water from locks into fresh water channels. Technical Report 5168, Nat. Bur. Stand. Report
Klemp JB, Rotunno R, Skamarock WC (1997) On the propagation of internal bores. J Fluid Mech 331: 81–106
Lim K, Ivey GN, Nokes R (2008) The generation of internal waves by tidal flow over continental shelf/slope topography. Environ Fluid Mech 8: 511–526
Linden PF, Lane-Serff GF, Smeed DA (1990) Emptying filling boxes: the fluid mechanics of natural ventilation. J Fluid Mech 212: 309–335
Liu QA, Linden PF (2006) The fluid dynamics of an underfloor air distribution system. J Fluid Mech 554: 323–341
Lowe RJ, Linden PF, Rottman JW (2005) The non-Boussinesq lock exchange problem. Part 1: Theory and experiments. J Fluid Mech 537: 101–124
Maxworthy T, Leilich J, Simpson J, Meiburg EH (2002) The propagation of a gravity current in a linearly stratified fluid. J Fluid Mech 453: 371–394
Nokes RI, Davidson MJ, Stepien CA, Veale WB, Oliver RL (2008) The front condition for intrusive gravity currents. J Hydraul Res 46: 788–801
Oster G (1965) Density gradients. Sci Am 213: 70–76
Pope SB (2000) Turbulent flows. Cambridge University Press, Cambridge
Rottman JW, Simpson JE (1983) Gravity currents produced by instantaneous releases of a heavy fluid in a rectangular channel. J Fluid Mech 135: 95–110
Rottman JW, Simpson JE (1989) The formation of internal bores in the atmosphere: a laboratory model. Q J R Meteorol Soc 115: 941–963
Shin JO, Dalziel SB, Linden PF (2004) Gravity currents produced by lock exchange. J Fluid Mech 521: 1–34
Simpson JE (1997) Gravity currents, 2nd edn. Cambridge University Press, Cambridge
Sutherland BR, Nault JT (2007) Intrusive gravity currents propagating along thin and thick interfaces. J Fluid Mech 586: 109–118
Sutherland BR, Kyba PJ, Flynn MR (2004) Intrusive gravity currents in two-layer fluids. J Fluid Mech 514: 327–353
Taylor JR (2008) Numerical simulations of the stratified oceanic bottom boundary layer. Ph.D. thesis, University of California, San Diego
Ungarish M (2008) Energy balances and front speed conditions of two-layer models for gravity currents produced by lock release. Acta Mech 579. doi:10.1007/s00707-008-0073-z
Ungarish M (2009) An introduction to gravity currents and intrusions. CRC Press, Boca Raton
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An erratum to this article can be found at http://dx.doi.org/10.1007/s10652-011-9208-1
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Tan, A.W., Nobes, D.S., Fleck, B.A. et al. Gravity currents in two-layer stratified media. Environ Fluid Mech 11, 203–223 (2011). https://doi.org/10.1007/s10652-010-9174-z
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DOI: https://doi.org/10.1007/s10652-010-9174-z