Phase Transition From Turbulence To Zonal Flows In The Hasegawa-Wakatani System
Pierre L. Guillon, \"Ozg\"ur D. G\"urcan

TL;DR
This paper investigates the transition from turbulence to zonal flows in the Hasegawa-Wakatani system, revealing a sharp, hysteretic phase transition influenced by the adiabaticity parameter and proposing a minimal model that captures this behavior.
Contribution
It identifies the critical adiabaticity parameter value for the turbulence transition and demonstrates that a minimal mode-based model can replicate the phase transition.
Findings
Sharp transition at C≈0.1 from 2D turbulence to zonal flows
Hysteresis observed around the transition point
Minimal 2x2 mode model reproduces the phase transition
Abstract
The transition between two-dimensional hydrodynamic turbulence and quasi-one-dimensional zonostrophic turbulence is examined in the modified Hasegawa-Wakatani system, which is considered as a minimal model of -plane-like drift-wave turbulence with an intrinsic instability. Extensive parameter scans were performed across a wide range of values for the adiabaticity parameter describing the strength of coupling between the two equations. A sharp transition from 2D isotropic turbulence to a quasi-1D system, dominated by zonal flows, is observed using the fraction of the kinetic energy of the zonal modes as the order parameter, at . It is shown that this transition exhibits a hysteresis loop around the transition point, where the adiabaticity parameter plays the role of the control parameter of its non-linear self-organisation. It was also observed that the radial…
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
Taxonomy
TopicsOceanographic and Atmospheric Processes · earthquake and tectonic studies
