A two-dimensional model of shear-flow transition

Abstract

We explore a two-dimensional dynamical system modeling transition in shear flows to try to understand the nature of an 'edge' state. The latter is an invariant set in phase space separating the basin of attraction B of the laminar state into two parts distinguished from one another by the nature of relaminarizing orbits. The model is parametrized by R, a stand-in for Reynolds number. The origin is a stable equilibrium point for all values of R and represents the laminar flow. The system possesses four critical parameter values at which qualitative changes take place, Rsn, Rh, Rbh and R∞. The origin is globally stable if R < Rsn but for R > Rsn has two further equilibrium points, Xlb and Xub . Of these Xlb is unstable for all values of R > Rsn whereas Xub is stable for R < Rbh and therefore possesses its own basin of attraction D. At R = Rh a homoclinic bifurcation takes place with the simultaneous formation of a homoclinic loop and an edge state. For Rh < R < Rbh the edge state, which is the stable manifold of Xlb, forms part of ∂ B, the boundary of the basin of attraction of the origin. The other part of ∂ B is a periodic orbit P bounding D. P and D shrink with increasing R. At R = Rbh there is a 'backwards Hopf' bifurcation at which Xub loses its stability and P and D disappear. For Rbh < R < R∞ the edge is 'pure' in the sense that it is the only phase space structure that lies outside the basin of attraction of the origin. As R increases the point Xlb recedes to progressively greater distances, with a singularity at R = R∞ where it becomes infinite. For R > R∞ Xlb has reappeared, the edge state has disappeared, and the geometrical structure favors permanent transition from the laminar state, increasingly so for increasing values of R.

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