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The 79 pages that link to Turbulence, each with the reason it gives.

• Hydrostatic equilibriumCompared with: Turbulent flows violate the at-rest assumption behind the hydrostatic description.

• HydrodynamicsCompared with: It emerges when liquid motion becomes unstable and strongly mixed.

• Laminar flowCompared with: Unlike laminar flow, turbulence continually transports momentum across the stream.

• Gravitational instabilityCompared with: Turbulent motions can support a cloud on large scales while promoting dense structures locally.

• MicrofluidicsCompared with: It contrasts with the smooth, usually laminar flows common in microchannels.

• Aerodynamic dragCompared with: Turbulence can raise skin friction yet delay separation and reduce pressure drag.

• Flow separationCompared with: Turbulent mixing can replenish near-wall momentum and delay separation.

• Blood flowCompared with: Unlike laminar flow, turbulence raises energy losses and can occur at high velocity or near narrowed vessels.

• Volumetric flow rateCompared with: Its fluctuating velocities make flow-rate measurement depend on averaging over time and area.

• Cold brew coffeeCompared with: Unlike stirred or flowing extraction, many cold-brew methods leave grounds largely undisturbed.

• Dynamic viscosityCompared with: Viscosity opposes velocity gradients, while turbulence greatly increases mixing and momentum transport.

• Open-channel flowCompared with: Channel flow can be turbulent; this is a separate regime distinction from having a free surface.

• HemodynamicsCompared with: It departs from the orderly-flow assumptions behind basic resistance equations.

• StreamliningCompared with: Turbulent boundary layers resist separation better but usually increase skin friction.

• Hagen–Poiseuille equationCompared with: The equation does not describe the extra momentum transport of turbulence.

• Flow velocityCompared with: Its velocity fluctuates across space and time, unlike orderly laminar motion.

• Coandă effectCompared with: Turbulence changes entrainment and attachment, so the effect depends on the jet's flow regime.

• Betz's lawCompared with: Real atmospheric flow departs from the steady, uniform assumptions behind the ideal limit.

• CurrentCompared with: Turbulent currents mix and fluctuate, unlike orderly laminar flow.

• Edge of chaosCompared with: Turbulence is a prominent chaotic regime, rather than a boundary between order and chaos.

• Feigenbaum constantsCompared with: Period-doubling scaling is a specific route to chaos, not a universal account of turbulent onset.

• Geophysical fluid dynamicsCompared with: Geophysical flows can be turbulent, but their rotation and stratification make that turbulence anisotropic.

• Laminar flow reactorCompared with: It contrasts with the orderly layers and limited transverse mixing of this reactor.

• Complex fluidsCompared with: Turbulence is flow complexity from inertia, unlike material complexity arising from internal structure.

• Low Reynolds number flowCompared with: It contrasts with the typically smooth, inertia-dominated behavior absent at very low Reynolds numbers.

• Vertical draftCompared with: A draft is a coherent vertical motion; turbulence can disrupt or contain one.

• Wind (meteorology)Compared with: It describes chaotic fluctuations that can occur within otherwise organized wind.