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Double-diffusive convection with two stabilizing gradients: strange consequences of magnetic buoyancy - MaRDI portal

Double-diffusive convection with two stabilizing gradients: strange consequences of magnetic buoyancy

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Publication:4881508

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DOI10.1017/S0022112095003946zbMath0859.76026MaRDI QIDQ4881508

Nigel Weiss, David W. Hughes

Publication date: 9 April 1997

Published in: Journal of Fluid Mechanics (Search for Journal in Brave)

zbMATH Keywords

bifurcation thermosolutal convection horizontal fluid layer magnetic boundary layers truncation of Fourier representation thermally unstable stratification

Mathematics Subject Classification ID

Absolute and convective instability and stability in hydrodynamic stability (76E15) Stability and instability of magnetohydrodynamic and electrohydrodynamic flows (76E25) Hydrodynamic and hydromagnetic problems in astronomy and astrophysics (85A30)

Related Items (2)

Bifurcation analysis for thermal convection in a rotating porous layer ⋮ Implication of cross-diffusion on the stability of double diffusive convection in an imposed magnetic field

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