The 1 : √2 mode interaction and heteroclinic networks in Boussinesq convection
Podvigina, O; Ashwin, P
Date: 1 January 2007
Journal
Physica D
Publisher
Elsevier
Publisher DOI
Abstract
Methods of equivariant bifurcation theory are applied to Boussinesq convection in a plane layer
with stress-free horizontal boundaries and an imposed square lattice periodicity in the horizontal
directions. We consider the problem near the onset of instability of the uniform conducting state
where spatial roll patterns with two ...
Methods of equivariant bifurcation theory are applied to Boussinesq convection in a plane layer
with stress-free horizontal boundaries and an imposed square lattice periodicity in the horizontal
directions. We consider the problem near the onset of instability of the uniform conducting state
where spatial roll patterns with two different wavelengths in the ratio 1 : √2 become simultaneously
unstable at a mode interaction. Centre manifold reduction yields a normal form on C4 with very
rich dynamical behavior. For a fixed Prandtl number P the mode interaction occurs at an isolated
point in the parameter plane (R,L) (where R is the Rayleigh number and L the length of the
horizontal periodicities) and acts as an organizing center for many nearby bifurcations. The normal
form predicts appearance of many steady states and travelling waves, which are classified by their
symmetries. It also predicts the appearance of robust heteroclinic networks involving steady states
with several different symmetries, and robust attractors of generalized heteroclinic type that include
connections from equilibria to subcycles. This is the first example of a heteroclinic network in a
fluid dynamical system that has ‘depth’ greater than one. The normal form dynamics is in good
correspondence (both quantitatively and qualitatively) with direct numerical simulations of the full
convection equations.
Mathematics and Statistics
Faculty of Environment, Science and Economy
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