Classical and symmetrical horizontal convection: detaching plumes and oscillations
From MaRDI portal
Publication:5222599
DOI10.1017/jfm.2020.211zbMath1460.86019OpenAlexW3014637532MaRDI QIDQ5222599
No author found.
Publication date: 6 April 2020
Published in: Journal of Fluid Mechanics (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1017/jfm.2020.211
Hydrology, hydrography, oceanography (86A05) General theory of rotating fluids (76U05) Convective turbulence (76F35)
Related Items
Horizontal convective flow from a line heat source located at the liquid–gas interface in presence of surface film ⋮ Data‐driven identification of the spatiotemporal structure of turbulent flows by streaming dynamic mode decomposition ⋮ Regime transitions in thermally driven high-Rayleigh number vertical convection
Cites Work
- Unnamed Item
- Unnamed Item
- Horizontal convection: effect of aspect ratio on Rayleigh number scaling and stability
- Comparison of computational codes for direct numerical simulations of turbulent Rayleigh-Bénard convection
- Fluctuations in turbulent Rayleigh–Bénard convection: The role of plumes
- Scaling in thermal convection: a unifying theory
- Convection driven by differential heating at a horizontal boundary
- Horizontal convection is non-turbulent
- A theoretical model for horizontal convection at high Rayleigh number
- Very viscous horizontal convection
- Convection by a horizontal thermal gradient
- Mean flow structure in horizontal convection
- Transition and turbulence in horizontal convection: linear stability analysis
- Horizontal convection dynamics: insights from transient adjustment
- Horizontal Convection