Bifurcation-theoretic origin of RPO11
Determine the bifurcation-theoretic origin of the relative periodic orbit RPO11 in vertical convection, specifying the invariant solution or bifurcation mechanism that generates RPO11.
References
We stopped the continuation at $(Ra, T) = (6680, 212)$ for the lower branch and at $(Ra, T) = (6680, 230.6)$ for the upper branch; its origin remains unknown.
— Natural convection in a vertical channel. Part 3. Bifurcations of many (additional) unstable equilibria and periodic orbits
(2504.05524 - Zheng et al., 7 Apr 2025) in Section 4.8.2 (RPO11: saddle-node bifurcations)