Rayleigh number

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In fluid mechanics, the Rayleigh number for a fluid is a dimensionless number associated with the heat transfer within the fluid. When the Rayleigh number is below the critical value for that fluid, heat transfer is primary in the form of conduction; when it exceeds the critical value, heat transfer is primarily in the form of convection.

The Rayleigh number is named after Lord Rayleigh and is defined as the product of the Grashof number, which describes the relationship between buoyancy and viscosity within a fluid, and the Prandtl number, which describes the relationship between momentum diffusivity and thermal diffusivity.

For free convection near a vertical wall, this number is

$\mathit{Ra}_{x,c} = \mathit{Gr}_{x,c}\mathit{Pr} = \frac{g \beta} {\nu \alpha} (T_s - T_\infin) x^3$

where

Ra = Rayleigh number
Gr = Grashof number
Pr = Prandtl number
g = Gravity
x = Characteristic length
T_s = Surface temperature
T_∞ = Quiescent temperature (fluid temperature far from the surface of the object)
ν = Kinematic viscosity
α = Thermal diffusivity
β = Thermal expansion coefficient

For most engineering purposes, the Rayleigh number is large, somewhere around 10⁶ and 10⁸.

In geophysics the Rayleigh number is of fundamental importance: it indicates the presence and strength of convection within a fluid body such as the Earth's mantle, which is a solid but which behaves as a fluid over geological time scales. The low value for the Earth's mantle indicates that convection occurs throughout the mantle as a whole, and not just within mantle layers.