2006
DOI: 10.1017/s0956792506006693
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An intrusion layer in stationary incompressible fluids: Part 1: Periodic waves

Abstract: Waves on a neutrally buoyant intrusion layer moving into otherwise stationary fluid are studied. There are two interfacial free surfaces, above and below the moving layer, and a train of waves is present. A small amplitude linearized theory shows that there are two different flow types, in which the two interfaces are either in phase or else move oppositely. The former flow type occurs at high phase speed and the latter is a low-speed solution. Nonlinear solutions are computed for large amplitude waves, using … Show more

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Cited by 8 publications
(21 citation statements)
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References 24 publications
(31 reference statements)
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“…There it was assumed that all three fluid layers had the same density. This linearized solution was generalized in Paper 1 [8] to allow all three fluid layers to have different densities, and it was confirmed there also that two different propagation modes are possible. There is a high-speed type in which both interfaces move in phase, and a low-speed branch for which the two interfaces move oppositely.…”
Section: Introductionmentioning
confidence: 67%
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“…There it was assumed that all three fluid layers had the same density. This linearized solution was generalized in Paper 1 [8] to allow all three fluid layers to have different densities, and it was confirmed there also that two different propagation modes are possible. There is a high-speed type in which both interfaces move in phase, and a low-speed branch for which the two interfaces move oppositely.…”
Section: Introductionmentioning
confidence: 67%
“…Similar kinds of flows may be produced pyroclastically due to volcanic eruptions, as discussed by Nield & Woods [12]. Three-layer atmospheric intrusion flows can also occur above rivers, and the 'Bridgewater Gerry' in Hobart in Tasmania is a striking example of this effect; see Figure 13 in Paper 1 [8], for example.…”
Section: Introductionmentioning
confidence: 78%
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