Small-Scale Properties of Turbulent Rayleigh-Bénard Convection
By Detlef Lohse, K. Xia. 2010
858 citations recorded by the source corpus.
Subfields: Computational Mechanics, Environmental Engineering, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/f210a48ef05eaac7a483005f190be28bc9a58cb2
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Computational Mechanics
- Detlef Lohse
- S. Grossmann
- Richard J.A.M. Stevens
- Roberto Verzicco
- A. Alexakis
- F. Rincon
- Luca Biferale
- Michel Rieutord
In Environmental Engineering
- Detlef Lohse
- Richard J.A.M. Stevens
- S. Grossmann
- F. Rincon
- Roberto Verzicco
- Luca Biferale
- Michel Rieutord
- A. Alexakis
In Global and Planetary Change
- Detlef Lohse
- S. Grossmann
- Richard J.A.M. Stevens
- Roberto Verzicco
- A. Alexakis
- F. Rincon
- Luca Biferale
- Michel Rieutord
Citations in the corpus
- Cascades and transitions in turbulent flows (2018, background): “A channel flow is only one of the many instances where turbulence is fed by multi-scale injections, other paradigmatic examples are given by natural convection [303], turbulence with power-law [595, 596] or fractal forcing [597] and atmospheric flows with simultane-”
- High-Reynolds number Taylor-Couette turbulence. (2016, background): “…both experimentally with various setups and numerically with several codes (see e.g. the reviews by Siggia 1994; Ahlers, Grossmann & Lohse 2009; Lohse & Xia 2010), for TC flow there was much less activity, the most visible exception being the Austin-Maryland experiment by Lathrop, Fineberg &…”
- Radial boundary layer structure and Nusselt number in Rayleigh–Bénard convection (2009, background): “Turbulent Rayleigh–Bénard convection (RBC), continues to be a topic of intense research (Ahlers, Grossmann & Lohse 2009; Lohse & Xia 2010).”
- The Sun’s Supergranulation (2010, background): “…strongly suggest that the basic phenomenology of Rayleigh–Bénard turbulence at vertical and horizontal scales smaller than the vertical extent of the domain considered should be similar to that of Navier–Stokes turbulence in the inertial-range (Rincon 2006; Lohse and Xia 2010; Kumar et al. 2014).”