Rayleigh–Bénard convection is a fundamental fluid dynamics phenomenon that significantly
influences heat transfer in various natural and industrial processes, such as geophysical …

The influence of anisotropic thermal diffusive coefficient on the stability of a horizontal fluid
planar layer rotating about its vertical axis and permeated by the horizontal homogeneous …

The anisotropy in the Earth's outer core strongly influences some convection processes very
important in Core Dynamics. For instance, some instabilities in rotating magnetoconvection …