Effects of non-uniform temperature gradient and Coriolis force on Bénard-Marangoni's instability
DOI10.1007/BF01176361zbMath0591.76064MaRDI QIDQ1075161
N. Rudraiah, V. Ramachandramurthy
Publication date: 1986
Published in: Acta Mechanica (Search for Journal in Brave)
Coriolis forceeigenvalueslinear stability analysisGalerkin techniqueonset of convectionabsence of rotationcombined surface-tension and buoyancy forcediscontinuous change in cell sizefree adiabatic upper boundaryhorizontal layer of Boussinesq fluidlimiting case of uniform temperature gradientmechanism for suppressing or augmenting convectionnon- uniform temperature gradientrigid isothermal lower boundarysingle-term Galerkin expansion
Absolute and convective instability and stability in hydrodynamic stability (76E15) General theory of rotating fluids (76U05) Diffusion and convection (76Rxx)
Related Items (2)
Cites Work
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- Marangoni convection in a rotating fluid layer with non-uniform temperature gradient
- Effects of non-uniform temperature gradients on Benard-Marangoni's instability
- The method of weighted residuals and variational principles. With application in fluid mechanics, heat and mass transfer
- On convection cells induced by surface tension
- The onset of transient convective instability
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