Laboratory experiments on Rayleigh-Bénard convection in a 2-layer system have been conducted. Remarkable nonlinear coupling is observed for Rayleigh numbers not far above the critical one. Two examples are described: the first one displays a steady resonance pattern with two rolls above each roll of the bottom layer, while in the second example, a pseudoperiodic time oscillation is observed, with a single time-dependent horizontal wavelength. In both cases, the coupling is predominantly “thermal”, implying that some kind of interface viscosity is present.
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Cardin et al. (1991) studied this question.
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