Kelvin-Helmholtz instability is one of basic cases of flow instability. It is responsible for a wide range of phenomena in the natural environment (e.g. ocean waves, atmospheric flows) and in industrial installations (e.g. slug formation, water hammer).
The Kelvin-Helmholtz instability develops at the interface between two fluids that are moving at different velocities. Small interface deformations influence the local pressure distribution, which may amplify the initial deformations. Shear forces between both fluid flows distort the initially linear waves into a much more complex interface topology (more @ ).
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11 months ago 00:00:08 1
Mesoscale Auroral Curls in Iceland
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Buoyancy stabilised Kelvin-Helmholtz instability (lattice Boltzmann and finite volume)
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Vortex formation in free jet caused by Kelvin-Helmholtz instability
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Kelvin Helmholtz
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2019-05 - Modeling turbulence (2D)
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Kelvin–Helmholtz flow instability simulation with adaptive mesh refinement
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Kelvin Helmholtz instability (fresh water above dyed brine)
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Transition to turbulence in pipe flow (Reynolds experiment)
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Collapse of dyed antibubble in a soap solution
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Ink drops on glycerol layer
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Double diffusive convection (hot dyed water over cold water)
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Mixing layer in a rectangular channel
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Marangoni flows of oleic acid-ethanol drop (with ink) into water
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Vortex tube formation using magnetic stirrer
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Benard-Marangoni instability
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Wave phenomena in a ripple tank
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Tea leaf paradox (Secondary flows)
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Vortex dipoles in a vibrating soap film
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CUDA Fluid dynamics: Kelvin-Helmholtz Instability
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Simflowny - Kelvin Helmholtz instability high resolution
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Space Developing Shear Layer with Weak Inflow Turbulence
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2D Numerical simulation of Kelvin-Helmholtz instability