1. Introduction
A vortex is not a spiral drawn in a fluid. It is a flow field in organized rotation around an axis. The trajectories of fluid particles can be circular, helical or spiral depending on conditions, but the vortex itself is a three-dimensional dynamic structure.
2. The Navier-Stokes Equations
Vortices are solutions of the Navier-Stokes equations, which describe the motion of viscous fluids. Vorticity ω = ∇ × v measures the local rotation of the fluid. A vortex corresponds to a region of concentrated vorticity.
Kelvin's theorem states that in a perfect fluid, the circulation around a material contour is conserved. This explains the persistence of vortices: once formed, they tend to maintain their structure.
3. Types of Vortex
The Rankine vortex combines a solid-rotation core (velocity proportional to radius) and an outer potential-flow region (velocity inversely proportional to radius). It is the most widely used model for tornadoes and bathtub vortices.
- Free vortex (potential): v = Γ/(2πr), irrotational outside core
- Forced vortex (solid): v = ωr, rotation like a rigid body
- Rankine vortex: combination of both
- Burgers vortex: with axial stretching, tornado model
4. Cyclones and the Coriolis Force
Tropical cyclones are large-scale atmospheric vortices. Their rotation — counterclockwise in the northern hemisphere, clockwise in the southern — is imposed by the Coriolis force, which results from Earth's rotation. It is not the bathtub that spins in a given direction depending on the hemisphere: at that scale, Coriolis is negligible.
5. Conservation of Angular Momentum
When a fluid converges toward an axis, its angular momentum is conserved: L = mvr = constant. If r decreases, v increases. This is why a skater who pulls in her arms spins faster, and why wind accelerates at the core of a cyclone. This acceleration is the dynamic signature of the converging spiral.
6. Conclusion
A vortex is a structured solution of the equations of fluid mechanics, not a simple visual spiral. Its apparent shape depends on the type of vortex, viscosity, scale and boundary conditions. Conservation of angular momentum is its central organizing principle.
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