Dimits transition in three-dimensional ion-temperature-gradient turbulence
Plamen G. Ivanov, Alexander A. Schekochihin, William Dorland

TL;DR
This paper extends the understanding of the Dimits transition from 2D to 3D ion-temperature-gradient turbulence, revealing stable zonal flow structures and the role of parasitic modes in energy transfer.
Contribution
It introduces a 3D fluid model for ion-temperature-gradient turbulence that demonstrates a stable Dimits regime with zonal staircases, unlike the unstable 2D case.
Findings
A stable finite-amplitude saturated state is found in 3D.
Parasitic modes enhance thermal diffusion and energy transfer.
Zonal staircase states are robust in 3D with sufficient parallel extension.
Abstract
We extend our previous work on the 2D Dimits transition in ion-scale turbulence (Ivanov et al. 2020) to include variations along the magnetic field. We consider a three-field fluid model for the perturbations of electrostatic potential, ion temperature, and ion parallel flow in a constant-magnetic-curvature geometry without magnetic shear. It is derived in the cold-ion, long-wavelength asymptotic limit of the gyrokinetic theory. Just as in the 2D model, a low-transport (Dimits) regime exists and is found to be dominated by a quasi-static staircase-like arrangement of strong zonal flows and zonal temperature. This zonal staircase is formed and maintained by a negative turbulent viscosity for the zonal flows. Unlike the 2D model, the 3D one does not suffer from an unphysical blow up beyond the Dimits threshold where the staircase becomes nonlinearly unstable. Instead, a well-defined…
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Taxonomy
TopicsMagnetic confinement fusion research · Solar and Space Plasma Dynamics · Ionosphere and magnetosphere dynamics
