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Rayleigh-Bénard convections

Rayleigh-Bénard convections is the plural of Rayleigh-Bénard convection.

Meaning of Rayleigh-Bénard convection

Noun

Rayleigh-Bénard convection (countable and uncountable, plural Rayleigh-Bénard convections)

  1. A type of natural convection, occurring in a planar horizontal layer of fluid heated from below, in which the fluid develops a regular pattern of convection cells known as Bénard cells.

Questions about Rayleigh-Bénard convections

What is Rayleigh-Bénard convections the plural of?
Rayleigh-Bénard convections is the plural of Rayleigh-Bénard convection.

Words near Rayleigh-Bénard convections in the dictionary

  1. Rayleigh scatterings
  2. Rayleigh wave
  3. Rayleigh waves
  4. Rayleigh's resolution limit
  5. Rayleigh-Bénard convection
  6. Rayleigh-Bénard convections
  7. Rayleigh-Jeans law
  8. Rayleigh-Taylor instabilities
  9. Rayleigh-Taylor instability
  10. rayleighs
  11. rayles

Source and license

Adapted from Wiktionary: Rayleigh-Bénard convections (page history and authors); Rayleigh-Bénard convection (page history and authors). Text available under the Creative Commons Attribution-ShareAlike 4.0 license. Word.ws reformatted the entry and added links. Wiktionary data of 2026-09-02.

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