vorticity's Usage Examples:

In continuum mechanics, vorticity is a pseudovector field that describes the local spinning motion of a continuum near some point (the tendency of something.

The distribution of velocity, vorticity (the curl of the flow velocity), as well as the concept of circulation.

hypotheses are the pancake model, the hierarchy model, and the primordial vorticity theory.

In fluid mechanics, potential vorticity (PV) is a quantity which is proportional to the dot product of vorticity and stratification.

the Coriolis force and conservation of potential vorticity which leads to changes of relative vorticity.

origin(s) of the vertical vorticity is (are), such as the tilting of horizontal vorticity into the vertical or vertical vorticity in the ambient environment.

the mechanism by which vorticity is generated.

In general, the evolution of vorticity can be broken into contributions.

in the jet stream (as shown in diagram) reflect cyclonic filaments of vorticity.

} The vorticity, ω {\displaystyle \omega } , of a flow can be defined in terms of its.

The vorticity equation of fluid dynamics describes evolution of the vorticity ω of a particle of a fluid as it moves with its flow, that is, the local.

potential vorticity, that transport is balanced by a narrow, intense poleward current, which flows along the western coast, allowing the vorticity introduced.

and vorticity are the circulation per unit area, taken around a local infinitesimal loop.

In potential flow of a fluid with a region of vorticity, all.

The barotropic vorticity equation assumes the atmosphere is nearly barotropic, which means that the direction and speed of the geostrophic wind are independent.

curvature vorticity and positive shear vorticity, respectively.

Ahead of a shortwave there is large-scale lift due to divergence from positive vorticity advection.

{\displaystyle \sigma _{ab}=\theta _{ab}-{\frac {1}{3}}\,\theta \,h_{ab}} and the vorticity tensor ω a b = h m a h n b X [ m ; n ] {\displaystyle \omega _{ab}={h^{m}}_{a}\.

observation from Stokes' solution for the oscillating Stokes flow is that vorticity oscillations are confined to a thin boundary layer and damp exponentially.

required to maintain this match between the absolute vorticity of a water column and the planetary vorticity, while the right represents the applied force of.

tornadoes occurring with a parent cloud in its growth stage and with its vorticity originating in the boundary layer.

_{ab}={h^{m}}_{a}\,{h^{n}}_{b}X_{[m;n]}} are known as the expansion tensor and vorticity tensor respectively.

interaction, specifically between the Stokes drift velocity and the mean-flow vorticity.