“…This study is devoted to an effect of destabilization of axisymmetric natural convection flows by a weak superimposed nonuniform rotation. In classical models, such as a rotating infinite layer (see, e.g., Chandrasekhar, 1961;Koschmieder,1993;Fernando & Smith IV, 2001;Kloosterziel & Carnevale, 2003;Lewis, 2010) or rotating cylinders and annuli (see, e.g., Lucas et al, 1983;Goldstein at al., 1993, Lopez & Marquez, 2009Rubio et al, 2010), increasing rotation usually leads to stabilization of the flow, i.e., to the growth of the critical Rayleigh number or other critical parameters describing magnitude of the buoyancy force. We do not review here numerous studies of the two above mentioned models, but address the reader to references in the cited papers.…”