Vorticity
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Continuum mechanics  

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In continuum mechanics, the vorticity is a pseudovector field that describes the local spinning motion of a continuum near some point (the tendency of something to rotate^{[1]}), as would be seen by an observer located at that point and traveling along with the flow.
Conceptually, vorticity could be determined by marking parts of a continuum in a small neighborhood of the point in question, and watching their relative displacements as they move along the flow. The vorticity vector would be twice the mean angular velocity vector of those particles relative to their center of mass, oriented according to the righthand rule. This quantity must not be confused with the angular velocity of the particles relative to some other point.
More precisely, the vorticity is a pseudovector field ω→, defined as the curl (rotational) of the flow velocity u→ vector. The definition can be expressed by the vector analysis formula:
where ∇ is the del operator. The vorticity of a twodimensional flow is always perpendicular to the plane of the flow, and therefore can be considered a scalar field.
The vorticity is related to the flow's circulation (line integral of the velocity) along a closed path by the (classical) Stokes' theorem.^{[2]} Namely, for any infinitesimal surface element C with normal direction n→ and area dA, the circulation dΓ along the perimeter of C is the dot product ω→ ∙ (dA n→) where ω→ is the vorticity at the center of C.^{[2]}
Many phenomena, such as the blowing out of a candle by a puff of air, are more readily explained in terms of vorticity, rather than the basic concepts of pressure and velocity. This applies, in particular, to the formation and motion of vortex rings.
The name vorticity was created by Horace Lamb in 1916^{[3]}.
Contents
Examples[edit]
In a mass of continuum that is rotating like a rigid body, the vorticity is twice the angular velocity vector of that rotation. This is the case, for example, in the central core of a Rankine vortex.
The vorticity may be nonzero even when all particles are flowing along straight and parallel pathlines, if there is shear (that is, if the flow speed varies across streamlines). For example, in the laminar flow within a pipe with constant cross section, all particles travel parallel to the axis of the pipe; but faster near that axis, and practically stationary next to the walls. The vorticity will be zero on the axis, and maximum near the walls, where the shear is largest.
Conversely, a flow may have zero vorticity even though its particles travel along curved trajectories. An example is the ideal irrotational vortex, where most particles rotate about some straight axis, with speed inversely proportional to their distances to that axis. A small parcel of continuum that does not straddle the axis will be rotated in one sense but sheared in the opposite sense, in such a way that their mean angular velocity about their center of mass is zero.
Example flows: Rigidbodylike vortex
v ∝ rParallel flow with shear Irrotational vortex
v ∝ 1/rwhere v is the velocity of the flow, r is the distance to the center of the vortex and ∝ indicates proportionality.
Absolute velocities around the highlighted point:Relative velocities (magnified) around the highlighted point Vorticity ≠ 0 Vorticity ≠ 0 Vorticity = 0
Another way to visualize vorticity is to imagine that, instantaneously, a tiny part of the continuum becomes solid and the rest of the flow disappears. If that tiny new solid particle is rotating, rather than just moving with the flow, then there is vorticity in the flow. In the figure below, the left subfigure demonstrates no vorticity, and the right subfigure demonstrates existence of vorticity.
Mathematical definition[edit]
Mathematically, the vorticity of a threedimensional flow is a pseudovector field, usually denoted by ω→, defined as the curl or rotational of the velocity field v→ describing the continuum motion. In Cartesian coordinates:
In words, the vorticity tells how the velocity vector changes when one moves by an infinitesimal distance in a direction perpendicular to it.
In a twodimensional flow where the velocity is independent of the z coordinate and has no z component, the vorticity vector is always parallel to the z axis, and therefore can be expressed as a scalar field multiplied by a constant unit vector z→:
Vorticity to Velocity[edit]
The inverse curl of a threedimensional vector field can be obtained with the BiotSavart law up to an integration constant, h→:
The vector field in the integrand has the shape of a rotation of center x, axis ω→ and falloff 1/px^3. Thus the resulting velocity can be understood as the field induced at p by a continuum of paddle wheels defined by vorticity. Because the integrand has a zero divergence, the BiotSavart integral produces an incompressible vector field. The integration constant, h→, is an irrotational field defined by the boundary conditions and the differential properties of v→. If v→ is known to be incompressible, then h→ must be the gradient of a harmonic field and is a solution to Laplace’s equation. Because of the singularity of the integrand when p=x, this integral usually cannot be computed with a Riemann sum and requires finding a set of simple shapes on which it has a closed form. One application for this formula is to recover the velocity field of a vorticity field that has evolved in time.
Evolution[edit]
The evolution of the vorticity field in time is described by the vorticity equation, which can be derived from the Navier–Stokes equations.
In many real flows where the viscosity can be neglected (more precisely, in flows with high Reynolds number), the vorticity field can be modeled well by a collection of discrete vortices, the vorticity being negligible everywhere except in small regions of space surrounding the axes of the vortices. This is clearly true in the case of twodimensional potential flow (i.e. twodimensional zero viscosity flow), in which case the flowfield can be modeled as a complexvalued field on the complex plane.
Vorticity is a useful tool to understand how the ideal potential flow solutions can be perturbed to model real flows. In general, the presence of viscosity causes a diffusion of vorticity away from the vortex cores into the general flow field. This flow is accounted for by the diffusion term in the vorticity transport equation. Thus, in cases of very viscous flows (e.g. Couette Flow), the vorticity will be diffused throughout the flow field and it is probably simpler to look at the velocity field than at the vorticity.
Vortex lines and vortex tubes[edit]
A vortex line or vorticity line is a line which is everywhere tangent to the local vorticity vector. Vortex lines are defined by the relation^{[4]}
where ω→ = (ω_{x}, ω_{y}, ω_{z}) is the vorticity vector in Cartesian coordinates.
A vortex tube is the surface in the continuum formed by all vortex lines passing through a given (reducible) closed curve in the continuum. The 'strength' of a vortex tube (also called vortex flux)^{[5]} is the integral of the vorticity across a crosssection of the tube, and is the same everywhere along the tube (because vorticity has zero divergence). It is a consequence of Helmholtz's theorems (or equivalently, of Kelvin's circulation theorem) that in an inviscid fluid the 'strength' of the vortex tube is also constant with time. Viscous effects introduce frictional losses and time dependence.
In a threedimensional flow, vorticity (as measured by the volume integral of the square of its magnitude) can be intensified when a vortex line is extended — a phenomenon known as vortex stretching.^{[6]} This phenomenon occurs in the formation of a bathtub vortex in outflowing water, and the buildup of a tornado by rising air currents.
Helicity is vorticity in motion along a third axis in a corkscrew fashion.
Vorticity meters[edit]
Rotatingvane vorticity meter[edit]
A rotatingvane vorticity meter was invented by Russian hydraulic engineer A. Ya. Milovich (1874–1958). In 1913 he proposed a cork with four blades attached as a device qualitatively showing the magnitude of the vertical projection of the vorticity and demonstrated a motionpicture photography of float's motion on the water surface in a model of river bend.^{[7]}
Rotatingvane vorticity meters are commonly shown in educational films on continuum mechanics (famous examples include the NCFMF's "Vorticity"^{[8]} and "Fundamental Principles of Flow" by Iowa Institute of Hydraulic Research^{[9]}).
Nonrotating vorticity meters[edit]
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Specific sciences[edit]
Aeronautics[edit]
In aerodynamics, the lift distribution over a finite wing may be approximated by assuming that each segment of the wing has a semiinfinite trailing vortex behind it. It is then possible to solve for the strength of the vortices using the criterion that there be no flow induced through the surface of the wing. This procedure is called the vortex panel method of computational fluid dynamics. The strengths of the vortices are then summed to find the total approximate circulation about the wing. According to the Kutta–Joukowski theorem, lift is the product of circulation, airspeed, and air density.
Atmospheric sciences[edit]
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 twodimensional flow parallel to the ground, so that the relative vorticity vector is generally scalar rotation quantity perpendicular to the ground. Vorticity is positive when  looking down onto the earth's surface  the wind turns counterclockwise. In the northern hemisphere, positive vorticity is called cyclonic rotation, and negative vorticity is anticyclonic rotation; the nomenclature is reversed in the Southern Hemisphere.
The absolute vorticity is computed from the air velocity relative to an inertial frame, and therefore includes a term due to the Earth's rotation, the Coriolis parameter.
The potential vorticity is absolute vorticity divided by the vertical spacing between levels of constant (potential) temperature (or entropy). The absolute vorticity of an air mass will change if the air mass is stretched (or compressed) in the vertical direction, but the potential vorticity is conserved in an adiabatic flow. As adiabatic flow predominates in the atmosphere, the potential vorticity is useful as an approximate tracer of air masses in the atmosphere over the timescale of a few days, particularly when viewed on levels of constant entropy.
The barotropic vorticity equation is the simplest way for forecasting the movement of Rossby waves (that is, the troughs and ridges of 500 hPa geopotential height) over a limited amount of time (a few days). In the 1950s, the first successful programs for numerical weather forecasting utilized that equation.
In modern numerical weather forecasting models and general circulation models (GCMs), vorticity may be one of the predicted variables, in which case the corresponding timedependent equation is a prognostic equation.
Helicity of the air motion is important in forecasting supercells and the potential for tornadic activity.
See also[edit]
 Barotropic vorticity equation
 D'Alembert's paradox
 Enstrophy
 Velocity potential
 Vortex
 Vortex tube
 Vortex stretching
 Vortical
 Horseshoe vortex
 Wingtip vortices
Fluid dynamics[edit]
Atmospheric sciences[edit]
References[edit]
 ^ Lecture Notes from University of Washington Archived October 16, 2015, at the Wayback Machine
 ^ ^{a} ^{b} Clancy, L.J., Aerodynamics, Section 7.11
 ^ Truesdell, C. (1954). The kinematics of vorticity (Vol. 954). Bloomington: Indiana University Press.
 ^ Kundu P and Cohen I. Fluid Mechanics.
 ^ Introduction to Astrophysical Gas Dynamics Archived June 14, 2011, at the Wayback Machine
 ^ Batchelor, section 5.2
 ^ Joukovsky N.E. (1914). "On the motion of water at a turn of a river". Matematicheskii Sbornik. 28.. Reprinted in: Collected works. 4. Moscow; Leningrad. 1937. pp. 193–216, 231–233 (abstract in English). "Professor Milovich's float", as Joukovsky refers this vorticity meter to, is schematically shown in figure on page 196 of Collected works.
 ^ National Committee for Fluid Mechanics Films Archived October 21, 2016, at the Wayback Machine
 ^ Films by Hunter Rouse — IIHR — Hydroscience & Engineering Archived April 21, 2016, at the Wayback Machine
Bibliography[edit]
 Clancy, L.J. (1975), Aerodynamics, Pitman Publishing Limited, London ISBN 0273011200
 "Weather Glossary"' The Weather Channel Interactive, Inc.. 2004.
 "Vorticity". Integrated Publishing.
Further reading[edit]
 Batchelor, G. K. (2000) [1967], An Introduction to Fluid Dynamics, Cambridge University Press, ISBN 0521663962
 Ohkitani, K., "Elementary Account Of Vorticity And Related Equations". Cambridge University Press. January 30, 2005. ISBN 0521819849
 Chorin, Alexandre J., "Vorticity and Turbulence". Applied Mathematical Sciences, Vol 103, SpringerVerlag. March 1, 1994. ISBN 0387941975
 Majda, Andrew J., Andrea L. Bertozzi, "Vorticity and Incompressible Flow". Cambridge University Press; 2002. ISBN 0521639484
 Tritton, D. J., "Physical Fluid Dynamics". Van Nostrand Reinhold, New York. 1977. ISBN 0198544936
 Arfken, G., "Mathematical Methods for Physicists", 3rd ed. Academic Press, Orlando, Florida. 1985. ISBN 0120598205
External links[edit]
Wikimedia Commons has media related to Vorticity. 
 Weisstein, Eric W., "Vorticity". Scienceworld.wolfram.com.
 Doswell III, Charles A., "A Primer on Vorticity for Application in Supercells and Tornadoes". Cooperative Institute for Mesoscale Meteorological Studies, Norman, Oklahoma.
 Cramer, M. S., "Navier–Stokes Equations  Vorticity Transport Theorems: Introduction". Foundations of Fluid Mechanics.
 Parker, Douglas, "ENVI 2210  Atmosphere and Ocean Dynamics, 9: Vorticity". School of the Environment, University of Leeds. September 2001.
 Graham, James R., "Astronomy 202: Astrophysical Gas Dynamics". Astronomy Department, UC Berkeley.
 "Spherepack 3.1". (includes a collection of FORTRAN vorticity program)
 "Mesoscale Compressible Community (MC2)^{[permanent dead link]} RealTime Model Predictions". (Potential vorticity analysis)