Kelvin–Helmholtz instability

E648721

Kelvin–Helmholtz instability is a fluid dynamical phenomenon in which velocity shear between layers of fluid (or plasma) with different densities leads to characteristic wave-like billows and turbulent mixing at their interface.

All labels observed (1)

Label Occurrences
Kelvin–Helmholtz instability canonical 3

How this entity was disambiguated

Statements (51)

Predicate Object
instanceOf fluid dynamical instability ⓘ
hydrodynamic instability ⓘ
plasma instability ⓘ
characterizedBy growth of perturbations at a shear layer ⓘ
rolling up of the shear layer into vortices ⓘ
describedBy Navier–Stokes equations ⓘ
linear stability analysis ⓘ
magnetohydrodynamics ⓘ
field astrophysics ⓘ
atmospheric science ⓘ
fluid dynamics ⓘ
oceanography ⓘ
plasma physics ⓘ
hasCause density contrast between fluid layers ⓘ
velocity shear between fluid layers ⓘ
hasConsequence enhanced mixing of chemical species ⓘ
enhanced mixing of heat ⓘ
enhanced mixing of momentum ⓘ
transition to turbulence ⓘ
hasParameter Alfvén Mach number in magnetized flows ⓘ
Mach number ⓘ
Reynolds number ⓘ
Richardson number ⓘ
hasType compressible Kelvin–Helmholtz instability ⓘ
incompressible Kelvin–Helmholtz instability ⓘ
magnetized Kelvin–Helmholtz instability ⓘ
stratified Kelvin–Helmholtz instability ⓘ
mathematicallyModeledBy dispersion relation for shear layers ⓘ
namedAfter Hermann von Helmholtz ⓘ
William Thomson, 1st Baron Kelvin ⓘ
linked to: Lord Kelvin
observedIn accretion disks ⓘ
astrophysical jets ⓘ
cloud formations in the Earth’s atmosphere ⓘ
ocean surface waves ⓘ
planetary atmospheres ⓘ
shear layers in rivers and estuaries ⓘ
solar wind–magnetosphere boundary ⓘ
tokamak edge plasmas ⓘ
occursAt interface between two fluids ⓘ
interface between two plasmas ⓘ
relatedTo Rayleigh–Taylor instability ⓘ
shear flow turbulence ⓘ
requires finite density contrast or compressibility effects ⓘ
sufficient velocity difference across the interface ⓘ
resultsIn turbulent mixing ⓘ
vortex formation ⓘ
wave-like billows ⓘ
stabilizedBy magnetic tension ⓘ
strong density stratification ⓘ
surface tension ⓘ
viscosity ⓘ

How these facts were elicited

Referenced by (3)

Full triples — surface form annotated when it differs from this entity's canonical label.

Stratified Flows → includesConcept → Kelvin–Helmholtz instability ⓘ
Rayleigh–Taylor instability → relatedTo → Kelvin–Helmholtz instability ⓘ
Holmboe instability → contrastedWith → Kelvin–Helmholtz instability ⓘ