eastward over
Mojave Desert mountains. This phenomenon observed from ground level is extremely rare; most cloud-related Kármán vortex street activity is viewed from space. A vortex street forms only at a certain range of flow velocities, specified by a range of
Reynolds numbers (
Re), typically above a limiting
Re value of about 90. The (
global) Reynolds number for a flow is a measure of the ratio of
inertial to
viscous forces in the flow of a fluid around a body or in a channel, and may be defined as a
nondimensional parameter of the global speed of the whole fluid flow: \begin{align} \mathrm{Re}_L&=\frac{UL}{\nu_0}\\ \nu_0 &=\frac{\mu_0}{\rho_0}\\ \mathrm{Re}_L&=\frac{UL\rho_0}{\mu_0}\\ \end{align} where: • = the free stream
flow speed (i.e. the flow speed far from the fluid boundaries, ∞, like the body speed relative to the fluid at rest, or an inviscid flow speed, computed through the Bernoulli equation), which is the original global flow parameter, i.e. the target to be non-dimensionalised. • = a characteristic length parameter of the body or channel • 0 = the free stream
kinematic viscosity parameter of the fluid, which in turn is the ratio between: • 0 = the reference fluid density. • 0 = the free stream fluid
dynamic viscosity For common flows (which can usually be considered as incompressible or isothermal), the kinematic viscosity is everywhere uniform over all the flow field and constant in time, so there is no choice on the viscosity parameter, which becomes naturally the kinematic viscosity of the fluid being considered at the temperature being considered. On the other hand, the reference length is always an arbitrary parameter, so particular attention should be put when comparing flows around different obstacles or in channels of different shapes: the global Reynolds numbers should be referred to the same reference length. This is actually the reason for which the most precise sources for airfoil and channel flow data specify the reference length at the Reynolds number. The reference length can vary depending on the analysis to be performed: for a body with circle sections such as circular cylinders or spheres, one usually chooses the diameter; for an airfoil, a generic non-circular cylinder or a
bluff body or a revolution body like a fuselage or a submarine, it is usually the profile
chord or the profile thickness, or some other given widths that are in fact stable design inputs; for flow channels usually the
hydraulic diameter about which the fluid is flowing. For an aerodynamic profile, the reference length depends on the analysis. In fact, the profile chord is usually chosen as the reference length also for aerodynamic coefficient for wing sections and thin profiles in which the primary target is to maximize the lift coefficient or the lift/drag ratio (i.e. as usual in thin airfoil theory, one would employ the
chord Reynolds as the flow speed parameter for comparing different profiles). On the other hand, for fairings and struts the given parameter is usually the dimension of internal structure to be streamlined (let us think for simplicity it is a beam with circular section), and the main target is to minimize the drag coefficient or the drag/lift ratio. The main design parameter which becomes naturally also a reference length is therefore the profile thickness (the profile dimension or area perpendicular to the flow direction), rather than the profile chord. The range of
Re values varies with the size and shape of the body from which the
eddies are
shed, as well as with the
kinematic viscosity of the fluid. For the wake of a circular cylinder, for which the reference length is conventionally the diameter
d of the circular cylinder, the lower limit of this range is
Re ≈ 47. Eddies are shed continuously from each side of the circle boundary, forming rows of vortices in its wake. The alternation leads to the core of a vortex in one row being opposite the point midway between two vortex cores in the other row, giving rise to the distinctive pattern shown in the picture. Ultimately, the
energy of the vortices is consumed by viscosity as they move further down stream, and the regular pattern disappears. Above the
Re value of 188.5, the flow becomes three-dimensional, with periodic variation along the cylinder. Above
Re on the order of 105 at the
drag crisis, vortex shedding becomes irregular and turbulence sets in. When a single vortex is shed, an
asymmetrical flow pattern forms around the body and changes the
pressure distribution. This means that the alternate shedding of vortices can create
periodic lateral (sideways) forces on the body in question, causing it to vibrate. If the vortex shedding
frequency is similar to the
natural frequency of a body or structure, it causes
resonance. It is this forced vibration that, at the correct frequency, causes suspended
telephone or
power lines to "sing" and the
antenna on a car to vibrate more strongly at certain speeds. ==In meteorology==