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Kraichnan ultimate regime: a standalone construct

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Kraichnanultimate regime1 CONSTRUCTKraichnan ultimateKRAICHNAN · FLUID MECHANICS

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Fluid mechanics

the predicted state of thermal convection at very high Rayleigh number in which boundary layers become turbulent and heat transport rises faster than in classical scaling.

In fluid mechanics, Kraichnan ultimate regime refers to the predicted state of thermal convection at very high Rayleigh number in which boundary layers become turbulent and heat transport rises faster than in classical scaling. This meaning comes from Kraichnan (1962) in The Physics of Fluids.[1]

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Nearby constructs

boundary4 fields · 4 citationsjingle · one word, four constructsconvection3 fields · 3 citationsinvariant · one construct, three systemsheat2 fields · 2 citationsjingle · one word, two constructs

References

  1. Kraichnan, R. H. (1962). Turbulent Thermal Convection at Arbitrary Prandtl Number. The Physics of Fluids, 5(11), 1374-1389. https://doi.org/10.1063/1.1706533

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