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The Unsteady Taylor--Vortex Dynamo is Fast

Liam O'Connor, Daniel Lecoanet, Geoffrey M. Vasil, Kyle C. Augustson, Florentin Daniel, Evan H. Anders, Keaton J. Burns, Jeffrey S. Oishi, Benjamin P. Brown

Abstract

Astrophysical and geophysical fluids commonly generate organized magnetic fields, despite having enormous magnetic Reynolds numbers $\rm{Rm}$ and abundant small-scale turbulence. Flow-induced dynamo action produces these fields, with the ``kinematic dynamo problem'' devoted to determining the rate at which a flow exponentially amplifies weak magnetic fields. However, previous studies on high-Rm kinematic dynamos have generated flows via imposed volumetric forcing or oscillatory boundary conditions. In this letter, we investigate a system with three important attributes: realistic flow conditions, fast dynamo action (operational for $\rm{Rm}\to\infty$), and a subharmonic spatio-temporal structure. We show that unsteady Taylor--vortex flow, a regime observed in laboratory experiments, gives rise to fast dynamos with time and length scales twice those of the flow at high $\rm{Rm}$. By numerically integrating a Floquet system driven by periodic oscillations of Taylor vortices, we solve the kinematic dynamo problem up to $\rm{Rm} = 3.2 \cdot 10^6$, calculating the dynamo's growth rate as a function of Rm and streamwise wavenumber. We find the onset of instability and compute Finite-Time Lyapunov Exponents, which identify the regions of Lagrangian chaos required for fast dynamo action. To our knowledge, unsteady Taylor--vortex flow produces the most physically motivated fast dynamo to date.

The Unsteady Taylor--Vortex Dynamo is Fast

Abstract

Astrophysical and geophysical fluids commonly generate organized magnetic fields, despite having enormous magnetic Reynolds numbers and abundant small-scale turbulence. Flow-induced dynamo action produces these fields, with the ``kinematic dynamo problem'' devoted to determining the rate at which a flow exponentially amplifies weak magnetic fields. However, previous studies on high-Rm kinematic dynamos have generated flows via imposed volumetric forcing or oscillatory boundary conditions. In this letter, we investigate a system with three important attributes: realistic flow conditions, fast dynamo action (operational for ), and a subharmonic spatio-temporal structure. We show that unsteady Taylor--vortex flow, a regime observed in laboratory experiments, gives rise to fast dynamos with time and length scales twice those of the flow at high . By numerically integrating a Floquet system driven by periodic oscillations of Taylor vortices, we solve the kinematic dynamo problem up to , calculating the dynamo's growth rate as a function of Rm and streamwise wavenumber. We find the onset of instability and compute Finite-Time Lyapunov Exponents, which identify the regions of Lagrangian chaos required for fast dynamo action. To our knowledge, unsteady Taylor--vortex flow produces the most physically motivated fast dynamo to date.
Paper Structure (1 equation, 5 figures)

This paper contains 1 equation, 5 figures.

Figures (5)

  • Figure 1: Snapshots of the dynamo cycle are shown at the beginning ($t=0$, panes A, B, and C) and after one quarter of a period ($t=T/4$, panes D, E, and F). At both times, we plot the streamwise velocity (panes A and D) and streamwise magnetic field at $\rm{Rm} = 1.5\cdot 10^3$ (panes B and E) and $\rm{Rm} = 1.5\cdot 10^5$ (panes C and F). Both dynamos were generated at streamwise wavenumber $k_y = 0.18$. We observe Taylor vortices in the streamwise velocity field, given by two pairs of counter-rotating cells which transport momentum between thin boundary layers. As the plumes of these cells oscillate in $z$, the magnetic field is amplified in ring-like structures in alternating regions between plumes, such that the rings co-rotate. At $t=0$, we observe two rings rotating clockwise. At $t=T/4$, there is a transition toward counterclockwise rotating rings which form in regions where the magnetic field was initially weak. The $\rm{Rm}=1.5\cdot 10^3$ dynamo (panes B and E) has a more diffuse structure than $\rm{Rm}=1.5\cdot 10^5$ (panes C and F). Both dynamos are dominated by the $k_z = 1$ mode, whereas the velocity field is primarily $k_z = 2$.
  • Figure 2: Growth rates vs. streamwise wavenumber ($k_y$) for various $\rm{Rm}$. The onset of instability occurs at $\rm{Rm}=36.9$ and $k_y=0.29$ while the dominant $k_y=1.0$ mode becomes marginally stable when $\rm{Rm}=861$. As $\rm{Rm}$ increases, the maximizing $k_y$ decreases for individual extrema while higher $k_y$ modes become dominant.
  • Figure 3: The magnetic growth rate is plotted as a function of Rm for streamwise wavenumbers $k_y=0.18, \, 0.29, \, 1.0$. For $k_y=1.0$, we observe cusp points where the growth rate's derivative with respect to $\rm{Rm}$ appears discontinuous. Evidence for a fast dynamo is observed at high $\rm{Rm}$, where the growth rate exhibits no appreciable dependence on $\rm{Rm}$. Triangle markers denote cases where the Floquet modes' period is equal to the flow's oscillation period $T$. Circular points denote Floquet modes with period $2T$ and the cases marked by stars have even longer periods or exhibit quasiperiodicity.
  • Figure 4: We plot the FTLE as a function of position for $t=0$ and $t=T/4$. These results were obtained using particle tracking initialized with the flow states shown in Figure \ref{['big']}. Positive FTLEs with sensitive spatial dependence indicate large regions of Lagrangian chaos enveloping the Taylor vortices.
  • Figure 5: $k_{\rm{eff}}^2 / \rm{Rm}$ as a function of $\rm{Rm}$ for $k_y = 0.18, \, 0.29,$ and $1.0$. This quantity becomes constant for large $\rm{Rm}$, implying $k_{\rm{eff}} \sim \rm{Rm}^{1/2}$. Marker and color conventions match those described in the caption of Figure \ref{['gamma_rm']}.