The influence of Parker spiral on the reflection-driven turbulence
Khurram Abbas, Jonathan Squire
TL;DR
The paper addresses how Parker spiral geometry modifies reflection-driven turbulence (RDT) and heating in the solar wind by extending Dmitruk et al.'s RDT phenomenology to a Parker-spiral mean field and testing it with 3D expanding-box MHD simulations. It introduces an expanding-box framework, uses Elsässer variables, and analyzes how the Parker spiral reshapes perpendicular outer scales ${\ell_{\perp,\mathrm{T}}}$ and ${\ell_{\perp,\mathrm{N}}}$, thereby keeping the nonlinearity-to-expansion ratio ${\chi_{\rm exp}}$ above unity longer and sustaining energy dissipation. The results show that while the fundamental RDT dynamics persist in PS geometry, the azimuthal field causes 3D eddy deformation that curtails indefinite pancake formation, leading to ongoing heating and strongly imbalanced turbulence out to larger heliocentric distances; spectra, switchbacks, and compressibility diagnostics provide concrete observational predictions. These findings offer a path to reconcile solar-wind heating with in-situ observations and furnish testable signatures for upcoming spacecraft data.
Abstract
The solar wind is observed to undergo substantial heating as it expands through the heliosphere, with measured temperature profiles exceeding those expected from adiabatic cooling. A plausible source of this heating is reflection-driven turbulence (RDT), in which gradients in the background Alfvén speed partially reflect outward-propagating Alfvén waves, seeding counter-propagating fluctuations that interact and dissipate via turbulence. Previous RDT models assume a radial background magnetic field, but at larger radii the interplanetary field is known to be twisted into the Parker Spiral (PS). Here, we generalize RDT phenomenology to include a PS, using three-dimensional expanding-box magnetohydrodynamic (MHD) simulations to test the ideas and compare the resulting turbulence to the radial-background-field case. We argue that the underlying RDT dynamics remain broadly similar with a PS, but the controlling scales change: as the azimuthal field grows it "cuts across" perpendicularly stretched, pancake-like eddies, producing outer scales perpendicular to the magnetic field that are much smaller than in the radial-background case. Consequently, the outer-scale nonlinear turnover time increases more slowly with heliocentric distance in PS geometry, weakening the tendency (seen in radial-background models) for the cascade to 'freeze' into quasi-static, magnetically dominated structures. This allows the system to dissipate a larger fraction of the fluctuation energy as heat, also implying that the turbulence remains strongly imbalanced (with high normalized cross-helicity) out to larger heliocentric distances. We complement our heating results with a detailed characterization of the turbulence (e.g., spectra, switchbacks, and compressive fractions) providing a set of concrete predictions for comparison with spacecraft observations.
