4.4 Article

Periodic orbits exhibit oblique stripe patterns in plane Couette flow

Journal

PHYSICAL REVIEW FLUIDS
Volume 6, Issue 11, Pages -

Publisher

AMER PHYSICAL SOC
DOI: 10.1103/PhysRevFluids.6.114401

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Transitional plane Couette flow can exhibit regular turbulent-laminar stripe patterns with large-scale pattern wavelength and an oblique orientation relative to the laminar flow direction due to spatiotemporally chaotic dynamics. An analysis of the Navier-Stokes equations shows unstable equilibrium solutions capturing the spatial structure of the oblique stripe patterns. Unstable periodic orbits embedded in the symmetry subspace of plane Couette flow may mediate the transition between turbulent flows with oblique patterns and laminar flow.
Spatiotemporally chaotic dynamics of transitional plane Couette flow may give rise to regular turbulent-laminar stripe patterns with a large-scale pattern wavelength and an oblique orientation relative to the laminar flow direction. A recent dynamical systems analysis of the oblique stripe pattern demonstrated that the Navier-Stokes equations have unstable equilibrium solutions that capture the three-dimensional spatial structure of the oblique stripe patterns. While equilibrium solutions are embedded in the turbulence supporting set and capture spatial features of the flow, a description of the dynamics requires evolving time-periodic solutions. These periodic orbits are unstable, expected to lie dense in the invariant set supporting turbulence, are shadowed by the chaotic trajectory and may allow for a quantitative description of turbulent statistics via periodic orbit expansions. Here we identify unstable periodic orbits that not only show oblique large-scale amplitude modulation in space but also have a characteristic time evolution. The periodic orbits represent standing waves that slowly propagate across wavy velocity streaks in the flow on viscous diffusion timescales. The unstable periodic orbits are embedded in the edge of chaos in a symmetry subspace of plane Couette flow and thereby may mediate transition to and from turbulent flows with oblique patterns.

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