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  2. Vorticity - Wikipedia

    en.wikipedia.org/wiki/Vorticity

    The relative vorticity is the vorticity relative to the Earth induced by the air velocity field. This air velocity field is often modeled as a two-dimensional flow parallel to the ground, so that the relative vorticity vector is generally scalar rotation quantity perpendicular to the ground.

  3. Vorticity equation - Wikipedia

    en.wikipedia.org/wiki/Vorticity_equation

    The vorticity equation of fluid dynamics describes the evolution of the vorticity ω of a particle of a fluid as it moves with its flow; that is, the local rotation of the fluid (in terms of vector calculus this is the curl of the flow velocity). The governing equation is:

  4. Vortex - Wikipedia

    en.wikipedia.org/wiki/Vortex

    Conceptually, the vorticity could be observed by placing a tiny rough ball at the point in question, free to move with the fluid, and observing how it rotates about its center. The direction of the vorticity vector is defined to be the direction of the axis of rotation of this imaginary ball (according to the right-hand rule ) while its length ...

  5. Circulation (physics) - Wikipedia

    en.wikipedia.org/wiki/Circulation_(physics)

    Circulation can be related to curl of a vector field V and, more specifically, to vorticity if the field is a fluid velocity field, =.. By Stokes' theorem, the flux of curl or vorticity vectors through a surface S is equal to the circulation around its perimeter, [4] = = =

  6. Helmholtz's theorems - Wikipedia

    en.wikipedia.org/wiki/Helmholtz's_theorems

    Fluid elements initially free of vorticity remain free of vorticity. Helmholtz's theorems have application in understanding: Generation of lift on an airfoil; Starting vortex; Horseshoe vortex; Wingtip vortices. Helmholtz's theorems are now generally proven with reference to Kelvin's circulation theorem.

  7. Potential vorticity - Wikipedia

    en.wikipedia.org/wiki/Potential_vorticity

    where is the relative vorticity, is the layer depth, and is the Coriolis parameter. The conserved quantity, in parenthesis in equation (3), was later named the shallow water potential vorticity. For an atmosphere with multiple layers, with each layer having constant potential temperature, the above equation takes the form

  8. Turbulence - Wikipedia

    en.wikipedia.org/wiki/Turbulence

    Turbulent flows have non-zero vorticity and are characterized by a strong three-dimensional vortex generation mechanism known as vortex stretching. In fluid dynamics, they are essentially vortices subjected to stretching associated with a corresponding increase of the component of vorticity in the stretching direction—due to the conservation ...

  9. Rankine vortex - Wikipedia

    en.wikipedia.org/wiki/Rankine_vortex

    Animation of a Rankine vortex. Free-floating test particles reveal the velocity and vorticity pattern. The Rankine vortex is a simple mathematical model of a vortex in a viscous fluid. It is named after its discoverer, William John Macquorn Rankine.