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Bifurcation theory for vortices with application to boundary layer eruption

Published online by Cambridge University Press:  27 February 2019

Anne R. Nielsen
Affiliation:
Department of Applied Mathematics and Computer Science, Technical University of Denmark, 2800 Lyngby, Denmark
Matthias Heil
Affiliation:
School of Mathematics, University of Manchester, Oxford Road, Manchester M13 9PL, UK
Morten Andersen
Affiliation:
Department of Science and Environment, Roskilde University, 4000 Roskilde, Denmark
Morten Brøns*
Affiliation:
Department of Applied Mathematics and Computer Science, Technical University of Denmark, 2800 Lyngby, Denmark
*
†Email address for correspondence: mobr@dtu.dk

Abstract

We develop a bifurcation theory describing the conditions under which vortices are created or destroyed in a two-dimensional incompressible flow. We define vortices using the $Q$-criterion and analyse the vortex structure by considering the evolution of the zero contours of $Q$. The theory identifies topological changes of the vortex structure and classifies these as four possible types of bifurcations, two occurring away from boundaries, and two occurring near no-slip walls. Our theory provides a description of all possible codimension-one bifurcations where time is treated as the bifurcation parameter. To illustrate our results, we consider the early stages of boundary layer eruption at moderate Reynolds numbers in the range from $Re=750$ to $Re=2250$. By analysing numerical simulations of the phenomenon, we show how to describe the eruption process as sequences of the four possible bifurcations of codimension one. Our simulations show that there is a single codimension-two point within our parameter range. This codimension-two point arises at $Re=1817$ via the coalescence of two codimension-one bifurcations which are associated with the creation and subsequent destruction of one of the vortices that erupt from the boundary layer. We present a theoretical description of this process and explain how the occurrence of this phenomenon separates the parameter space into two regions with distinct evolution of the topology of the vortices.

Information

Type
JFM Papers
Copyright
© 2019 Cambridge University Press 
Figure 0

Figure 1.Illustration of how a small change in time away from $t^{\ast }$ affects the topological structure of the contour curve, $Q=0$, close to a non-critical point $(x^{\ast },y^{\ast })$. Since the topological structure is unchanged, $(x^{\ast },y^{\ast })$ is not a bifurcation point.

Figure 1

Figure 2.Illustration of the local changes in structure of the $Q=0$ contour curve during a punching bifurcation. The figure shows the forward version where $\text{sign}(\unicode[STIX]{x2202}_{t}Q_{0})\neq \text{sign}(\text{tr}(H_{0}^{Q}))$. At the bifurcation value $t=0$, $(0,0)$ is the only point where $Q=0$.

Figure 2

Figure 3.Illustration of the local changes in structure of the $Q=0$ contour curves during a pinching bifurcation. The solid lines illustrate the topology in a neighbourhood of the bifurcation point $(0,0)$. The dashed lines in panels (a–c) show an example of a possible global structure for the case where the bifurcation results in the splitting of a single vortex into two; panels (d–f) illustrate the case when two vortices merge.

Figure 3

Figure 4.Illustration of how a small change in time affects the topological structure of the contour curve, $\widetilde{Q}=0$, close to a non-critical boundary point $(0,0)$. Since the topological structure is unchanged, $(0,0)$ is not a bifurcation point.

Figure 4

Figure 5.Illustration of the local changes in structure under a wall-punching bifurcation. The figure illustrates the forward version where $\text{sign}(\unicode[STIX]{x2202}_{t}\widetilde{Q}_{0})\neq \text{sign}(\unicode[STIX]{x2202}_{y}\widetilde{Q}_{0})$. The solid lines are the visible zero contour curves of $Q$, while the dotted lines are outside the region containing the fluid.

Figure 5

Figure 6.Illustration of the local changes in structure under a wall-pinching bifurcation. The figure illustrates the forward version where $\text{sign}(\unicode[STIX]{x2202}_{t}\widetilde{Q}_{0})\neq \text{sign}(\unicode[STIX]{x2202}_{y}\widetilde{Q}_{0})$. The solid lines are the visible zero contour curves of $Q$, while the dotted line is outside the region containing the fluid.

Figure 6

Figure 7.Initial configuration of the boundary layer eruption problem. A Gaussian vortex is placed at a distance $d$ from the no-slip wall; and $c$ is the characteristic length for the Gaussian distribution.

Figure 7

Figure 8.Numerical results for $Re=2063$ at the following time steps: (a) $t=11$, (b) $t=48$, (c) $t=117$, (d) $t=197$, (e) $t=256$, (f) $t=293$, (g) $t=395$, (h) $t=464$ and (i) $t=597$. Each panel shows a zoom in on the region close to the initial vortex, where $x\in [-2,1.5]$. The vorticity contours with values from $-0.3$ to $0.3$ are coloured in blue and red. Regions with positive $Q$-value are encircled by white lines, which correspond to the zero contour curves of $Q$.

Figure 8

Figure 9.Bifurcation diagram of the eruption process. The red dots marked with a letter correspond to the plots shown in figure 8. The black squares, connected by solid lines, mark the bifurcation points observed in the simulations. The grey arrows indicate in which sequence the bifurcations are encountered in a flow with a given Reynolds number.