2007
DOI: 10.1063/1.2742728
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Tornado-like flows

Abstract: Simple exact solutions for horizontal flows, with a stagnant funnel consisting of a lighter fluid and narrowing toward the ground, exhibit the main features of real tornadoes. The two-fluid model is quite robust, as it can be adapted to any vorticity distribution, any vertical stratification, and the effects of compressibility.

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Cited by 43 publications
(5 citation statements)
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“…The 2-magnet configuration clearly enhances the temperature fluctuations along the centreline. This is a consequence of the cold fluid stream that is carried by the strong swirling tornado-like motion (similar to that analysed in Yih [47]) that creates a vertically elongated thermal plume. It is noted that the 3-magnet configuration significantly reduces the level of temperature fluctuations along the centreline.…”
Section: Flow Turbulence and Heat Transfermentioning
confidence: 74%
“…The 2-magnet configuration clearly enhances the temperature fluctuations along the centreline. This is a consequence of the cold fluid stream that is carried by the strong swirling tornado-like motion (similar to that analysed in Yih [47]) that creates a vertically elongated thermal plume. It is noted that the 3-magnet configuration significantly reduces the level of temperature fluctuations along the centreline.…”
Section: Flow Turbulence and Heat Transfermentioning
confidence: 74%
“…The simplest model of a tornado is a vortex flow with a vertical axis of symmetry and a fixed core (or funnel) [26]. Figure 1 shows a diagram of the vortex under consideration.…”
Section: Simple Analytical Modelsmentioning
confidence: 99%
“…where Y(x, y) = ∂x ∂r ∂y ∂z − ∂x ∂z ∂y ∂ r is the Jacobian. Transformations of the original system of equations to the system of Equations ( 24)- (26) were made using known relations: ω φ = ∂U r /∂z − ∂U z /∂r, Γ = rU φ , U r = r −1 ∂Ψ/∂z, and U z = −r −1 ∂Ψ/∂r. Equations ( 24)-( 26) make up a system of three equations with three variables: the stream function Ψ, circulation Γ, and the azimuthal component of the vorticity ω φ .…”
Section: Early Numerical Studiesmentioning
confidence: 99%
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