Abstract
The influence of the horizontal component of the temperature gradient on nonlinear regimes of oscillatory convection developed under the joint action of buoyant and thermocapillary effects in a multilayer system is investigated. Two-dimensional convective regimes are studied by the finite difference method. Rigid heat-insulated lateral walls are considered. It is found that the region of nonlinear asymmetric oscillations is restricted by the Grashof number values, both from below and from above, by the steady states.
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