The linear stability of mixed convection in a vertical channel flow
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Publication:4354506
DOI10.1017/S0022112096008026zbMath0905.76029OpenAlexW2122091630MaRDI QIDQ4354506
Publication date: 9 February 1999
Published in: Journal of Fluid Mechanics (Search for Journal in Brave)
Full work available at URL: https://doi.org/10.1017/s0022112096008026
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Related Items (13)
Weakly nonlinear stability analysis of non-isothermal Poiseuille flow in a vertical channel ⋮ Finite amplitude analysis of non-isothermal parallel flow in a vertical channel filled with a highly permeable porous medium ⋮ Influence of inertia and drag terms on the stability of mixed convection in a vertical porous-medium channel ⋮ Solitary vortex solutions in a sheared and differentially heated vertical fluid layer with stable stratification ⋮ A direct numerical simulation of transition phenomena in a mixed convection channel flow. ⋮ Effect of internal heat source on stability analysis of a highly permeable vertical porous channel filled with nanofluid ⋮ Magnetohydrodynamic mixed convection flow in a vertical channel filled with porous media ⋮ Influence of Prandtl number on stability of mixed convective flow in a vertical channel filled with a porous medium ⋮ Numerical investigation of electrohydrodynamic instability in a vertical porous layer ⋮ Stability of mixed convection in an anisotropic vertical porous channel ⋮ Mixed convection with variable viscosity in a vertical annulus with uniform wall temperatures ⋮ Stability of natural convective motion induced by internal heat sources in a slot with a moving sidewall ⋮ Suppression of turbulence and travelling waves in a vertical heated pipe
Cites Work
- Is a fully-developed and non-isothermal flow possible in a vertical pipe?
- Finite-amplitude instability of mixed-convection in a heated vertical pipe
- A note on the relation between temporally-increasing and spatially-increasing disturbances in hydrodynamic stability
- Finite-amplitude instability of mixed convection
- Thermal instability in a horizontal fluid layer: effect of boundary conditions and non-linear temperature profile
- Accurate solution of the Orr–Sommerfeld stability equation
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