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arxiv: 1812.03752 · v1 · pith:5TOQVR7Rnew · submitted 2018-12-10 · ⚛️ physics.flu-dyn · nlin.PS· physics.geo-ph· physics.plasm-ph

Folding of the frozen-in-fluid di-vorticity field in two-dimensional hydrodynamic turbulence

classification ⚛️ physics.flu-dyn nlin.PSphysics.geo-phphysics.plasm-ph
keywords di-vorticityfieldalphaexponentiallyfoldinghydrodynamicmaximumquasi-shocks
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The vorticity rotor field ${\bf B}=\mbox{rot}\,\mathbf{\omega}$ (di-vorticity) for freely decaying two-dimensional hydrodynamic turbulence due to a tendency to breaking is concentrated in the vicinity of the lines corresponding to the position of the vorticity quasi-shocks. The maximum value of the di-vorticity $B_{max}$ at the stage of quasi-shocks formation increases exponentially in time, while the thickness $\ell(t)$ of the maximum area in the transverse direction to the vector ${\bf B}$ decreases in time also exponentially. It is numerically shown that $B_{max} (t)$ depends on the thickness according to the power law: $B_{max}(t)\sim \ell^{-\alpha}(t)$, where the exponent $\alpha\approx 2/3$. This behavior indicates in favor of folding for the divergence-free vector field of the di-vorticity.

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