Direct and Large Eddy Simulation of Turbulence 1986
DOI: 10.1007/978-3-663-00197-3_13
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Simulation of the Turbulent Rayleigh-Benard Problem Using a Spectral/Finite Difference Technique

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Cited by 4 publications
(4 citation statements)
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“…In situations with a heated lower surface and Fig. 10(a) shows that S v switches its sign across the central region which is consistent with [69], [70], [66] and [27]. Cold descending plumes that collide with the bottom boundary layer (triggering instabilities that result in eruptions of hot accelerating plumes there) are faster than the newly-formed hot plumes leading to a negative S v near the bottom plate, and vice versa.…”
Section: Skewness and Distribution Functionsupporting
confidence: 66%
“…In situations with a heated lower surface and Fig. 10(a) shows that S v switches its sign across the central region which is consistent with [69], [70], [66] and [27]. Cold descending plumes that collide with the bottom boundary layer (triggering instabilities that result in eruptions of hot accelerating plumes there) are faster than the newly-formed hot plumes leading to a negative S v near the bottom plate, and vice versa.…”
Section: Skewness and Distribution Functionsupporting
confidence: 66%
“….5. More recently,Eidson, Hussaini and Zang (1986) have used a similar algorithm in a high resolution direct simulation of a turbulent Rayleigh-Benard flow. More recently,Eidson, Hussaini and Zang (1986) have used a similar algorithm in a high resolution direct simulation of a turbulent Rayleigh-Benard flow.…”
mentioning
confidence: 99%
“…In standard calculations such as Benard convection [33,34] or channel flow [35,37] the are products of sinusoids and possibly Chebychev polynomials. A realistic count of the number functions, N, in a realistic simulation gives a nominal number of 0(105).…”
mentioning
confidence: 99%