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- W2897687514 abstract "Background rotation causes different flow structures and heat transfer efficiencies in Rayleigh–Bénard convection. Three main regimes are known: rotation unaffected, rotation affected and rotation dominated. It has been shown that the transition between rotation-unaffected and rotation-affected regimes is driven by the boundary layers. However, the physics behind the transition between rotation-affected and rotation-dominated regimes are still unresolved. In this study, we employ the experimentally obtained Lagrangian velocity and acceleration statistics of neutrally buoyant immersed particles to study the rotation-affected and rotation-dominated regimes and the transition between them. We have found that the transition to the rotation-dominated regime coincides with three phenomena; suppressed vertical motions, strong penetration of vortical plumes deep into the bulk and reduced interaction of vortical plumes with their surroundings. The first two phenomena are used as confirmations for the available hypotheses on the transition to the rotation-dominated regime while the last phenomenon is a new argument to describe the regime transition. These findings allow us to better understand the rotation-dominated regime and the transition to this regime." @default.
- W2897687514 created "2018-10-26" @default.
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- W2897687514 creator A5020707783 @default.
- W2897687514 creator A5028713841 @default.
- W2897687514 creator A5072818023 @default.
- W2897687514 date "2018-10-22" @default.
- W2897687514 modified "2023-10-05" @default.
- W2897687514 title "Velocity and acceleration statistics in rapidly rotating Rayleigh–Bénard convection" @default.
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- W2897687514 doi "https://doi.org/10.1017/jfm.2018.751" @default.
- W2897687514 hasPubMedCentralId "https://www.ncbi.nlm.nih.gov/pmc/articles/6218005" @default.
- W2897687514 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/30410188" @default.
- W2897687514 hasPublicationYear "2018" @default.
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